Guess What, California? Now You Need to Prepare for Erupting Volcanoes
Days, Weeks, Years? Scientists Say Hawaii Volcano Eruption Has No End In Sight
If You Think You Understand the Death of the Dinosaurs, You’re Wrong
Active Volcanoes Spotted on Venus
The Great 1815 Tambora Eruption: What if This Volcano Blew Today?
Scientists Discover Natural Glass Created by Volcanoes and Lightning
Dinosaur Extinction: New Research Favors Volcanism as Cause
Yosemite's Tuolumne Meadows: A Long-standing Geological Puzzle
Famous Sunset Paintings Reflect Key Air Pollution Events From the Past
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His work has also appeared on the \u003cem>The California Report\u003c/em> morning show and \u003cem>KQED News\u003c/em>. His production credits include \u003cem>The California Report, The California Report Magazine\u003c/em> and KQED's local news podcast \u003cem>The Bay\u003c/em>. Other credits include NPR's \u003cem>All Things Considered\u003c/em>, WNYC's \u003cem>Science Friday\u003c/em>, WBUR's \u003cem>Here & Now\u003c/em>, WIRED and SFGate. Peter graduated from Brown University and earned a master's degree in journalism from Stanford. He's covered everything from homelessness to wildfires, health, the environment, arts and Thanksgiving in San Quentin prison. In other lives, he played rock n roll music and studied neuroscience. You can email him at: parcuni@kqed.org","avatar":"https://secure.gravatar.com/avatar/d5032f6f27199d478af34ad2e1d98732?s=600&d=blank&r=g","twitter":"peterarcuni","facebook":null,"instagram":null,"linkedin":null,"sites":[{"site":"news","roles":["editor"]},{"site":"science","roles":["editor"]}],"headData":{"title":"Peter Arcuni | KQED","description":"Reporter","ogImgSrc":"https://secure.gravatar.com/avatar/d5032f6f27199d478af34ad2e1d98732?s=600&d=blank&r=g","twImgSrc":"https://secure.gravatar.com/avatar/d5032f6f27199d478af34ad2e1d98732?s=600&d=blank&r=g"},"isLoading":false,"link":"/author/parcuni"}},"breakingNewsReducer":{},"campaignFinanceReducer":{},"firebase":{"requesting":{},"requested":{},"timestamps":{},"data":{},"ordered":{},"auth":{"isLoaded":false,"isEmpty":true},"authError":null,"profile":{"isLoaded":false,"isEmpty":true},"listeners":{"byId":{},"allIds":[]},"isInitializing":false,"errors":[]},"navBarReducer":{"navBarId":"news","fullView":true,"showPlayer":false},"navMenuReducer":{"menus":[{"key":"menu1","items":[{"name":"News","link":"/","type":"title"},{"name":"Politics","link":"/politics"},{"name":"Science","link":"/science"},{"name":"Education","link":"/educationnews"},{"name":"Housing","link":"/housing"},{"name":"Immigration","link":"/immigration"},{"name":"Criminal Justice","link":"/criminaljustice"},{"name":"Silicon Valley","link":"/siliconvalley"},{"name":"Forum","link":"/forum"},{"name":"The California Report","link":"/californiareport"}]},{"key":"menu2","items":[{"name":"Arts & Culture","link":"/arts","type":"title"},{"name":"Critics’ Picks","link":"/thedolist"},{"name":"Cultural Commentary","link":"/artscommentary"},{"name":"Food & Drink","link":"/food"},{"name":"Bay Area Hip-Hop","link":"/bayareahiphop"},{"name":"Rebel Girls","link":"/rebelgirls"},{"name":"Arts Video","link":"/artsvideos"}]},{"key":"menu3","items":[{"name":"Podcasts","link":"/podcasts","type":"title"},{"name":"Bay Curious","link":"/podcasts/baycurious"},{"name":"Rightnowish","link":"/podcasts/rightnowish"},{"name":"The Bay","link":"/podcasts/thebay"},{"name":"On Our Watch","link":"/podcasts/onourwatch"},{"name":"Mindshift","link":"/podcasts/mindshift"},{"name":"Consider This","link":"/podcasts/considerthis"},{"name":"Political Breakdown","link":"/podcasts/politicalbreakdown"}]},{"key":"menu4","items":[{"name":"Live Radio","link":"/radio","type":"title"},{"name":"TV","link":"/tv","type":"title"},{"name":"Events","link":"/events","type":"title"},{"name":"For Educators","link":"/education","type":"title"},{"name":"Support KQED","link":"/support","type":"title"},{"name":"About","link":"/about","type":"title"},{"name":"Help Center","link":"https://kqed-helpcenter.kqed.org/s","type":"title"}]}]},"pagesReducer":{},"postsReducer":{"stream_live":{"type":"live","id":"stream_live","audioUrl":"https://streams.kqed.org/kqedradio","title":"Live Stream","excerpt":"Live Stream information currently unavailable.","link":"/radio","featImg":"","label":{"name":"KQED Live","link":"/"}},"stream_kqedNewscast":{"type":"posts","id":"stream_kqedNewscast","audioUrl":"https://www.kqed.org/.stream/anon/radio/RDnews/newscast.mp3?_=1","title":"KQED Newscast","featImg":"","label":{"name":"88.5 FM","link":"/"}},"science_1938782":{"type":"posts","id":"science_1938782","meta":{"index":"posts_1591205157","site":"science","id":"1938782","score":null,"sort":[1552078501000]},"guestAuthors":[],"slug":"guess-what-california-now-you-need-to-prepare-for-erupting-volcanoes","title":"Guess What, California? Now You Need to Prepare for Erupting Volcanoes","publishDate":1552078501,"format":"aside","headTitle":"Guess What, California? Now You Need to Prepare for Erupting Volcanoes | KQED","labelTerm":{},"content":"\u003cp>https://www.youtube.com/watch?v=nZD9K4q55jk\u003c/p>\n\u003cp>Earthquakes, wildfires, floods. If you live in California, you’re likely aware of these natural hazards and the dangers associated with them.\u003c/p>\n\u003cp>But according to a U.S. Geological Survey \u003ca href=\"https://pubs.er.usgs.gov/publication/sir20185159\" target=\"_blank\" rel=\"noopener\">report\u003c/a> released last week, California is also home to eight volcanic areas, posing threats categorized from moderate to very high. Seven of these areas are considered active, with molten rock bubbling underneath.\u003c/p>\n\u003cp>These volcanic hotpots span the length of California from Medicine Lake in the far northern region of the state down to Salton Buttes near the U.S.-Mexico border. Clear Lake volcanic field, in Lake County, is roughly 100 miles from both San Francisco and Sacramento.\u003c/p>\n\u003cp>Other active sites include Mount Shasta and Lassen Volcanic Center in Northern California, as well as Long Valley Volcanic Region near Mammoth Lakes, and Coso Volcanic Field, east of a string of unincorporated communities along Highway 395.\u003c/p>\n\u003cfigure id=\"attachment_1938836\" class=\"wp-caption alignnone\" style=\"max-width: 604px\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-1938836\" src=\"https://ww2.kqed.org/science/wp-content/uploads/sites/35/2019/03/img6940.png\" alt=\"\" width=\"604\" height=\"668\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2019/03/img6940.png 604w, https://cdn.kqed.org/wp-content/uploads/sites/35/2019/03/img6940-160x177.png 160w\" sizes=\"(max-width: 604px) 100vw, 604px\">\u003cfigcaption class=\"wp-caption-text\">Sites of California’s eight volcanic hotspots. \u003ccite>(USGS California Volcano Observatory)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>The \u003ca href=\"https://pubs.usgs.gov/sir/2018/5159/sir20185159.pdf\" target=\"_blank\" rel=\"noopener\">report\u003c/a>, titled “California’s Exposure to Volcanic Hazards,” was compiled by the USGS \u003ca href=\"https://volcanoes.usgs.gov/observatories/calvo/\" target=\"_blank\" rel=\"noopener\">California Volcano Observatory\u003c/a> in collaboration with the California Governor’s Office of Emergency Services and the California Geological Survey.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>Based on records of volcanic history, geologists calculate the chance of an eruption in California over the next 30 years at 16 percent. For comparison, scientists have pegged the 30-year probability of a major earthquake in the Bay Area along the San Andreas Fault at about 22 percent.\u003c/p>\n\u003cp>Jessica Ball, a geologist with the California Volcano Observatory and a co-author on the report, says many Californians aren’t aware of the possibilities of a volcanic eruption in the state. Volcanoes operate over longer timescales, she said.\u003c/p>\n\u003cp>“In California, earthquakes tend to take front and center. We have had more of them in the 20th century and 21st century than we have had volcanic activity. So it’s sort of out of people’s memories that we’ve got active volcanoes in the state.”\u003c/p>\n\u003cp>The last \u003ca href=\"https://www.kqed.org/science/30444/four-days-in-may-mount-lassen-erupted-100-years-ago\" target=\"_blank\" rel=\"noopener\">series of eruptions\u003c/a> in California occurred from 1914 to 1917 within the Lassen Volcanic Center, with an explosive eruption of Lassen Peak on May 22, 1915. Lava flows, hot ash, mudslides and avalanches resulting from the eruptions had major impacts on the surrounding region.\u003c/p>\n\u003cp>https://www.youtube.com/watch?v=KvmInz9TgMw\u003c/p>\n\u003cp>The purpose of the report, which was requested by the Office of Emergency Services, was to compile scientific knowledge about volcanoes in California and outline the major hazards that could result should one erupt.\u003c/p>\n\u003cp>“Each volcano has its own hazards,” Ball said. Medicine Lake, for example, could face lava flows. Whereas the Lassen region should be more concerned with lahars (mudslides) or high-speed “pyroclastic flows” of ash and lava powered by pressurized gas, which are a main cause of eruption-related fatalities.\u003c/p>\n\u003cfigure id=\"attachment_1938839\" class=\"wp-caption alignnone\" style=\"max-width: 800px\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-medium wp-image-1938839\" src=\"https://ww2.kqed.org/science/wp-content/uploads/sites/35/2019/03/img6941_900w_863h-800x767.png\" alt=\"\" width=\"800\" height=\"767\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2019/03/img6941_900w_863h-800x767.png 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2019/03/img6941_900w_863h-160x153.png 160w, https://cdn.kqed.org/wp-content/uploads/sites/35/2019/03/img6941_900w_863h-768x736.png 768w, https://cdn.kqed.org/wp-content/uploads/sites/35/2019/03/img6941_900w_863h-32x32.png 32w, https://cdn.kqed.org/wp-content/uploads/sites/35/2019/03/img6941_900w_863h.png 900w\" sizes=\"(max-width: 800px) 100vw, 800px\">\u003cfigcaption class=\"wp-caption-text\">The possible hazards of a volcanic eruption in California. \u003ccite>(USGS California Volcano Observatory)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>Ball says the focus of the work was to home in on “populations, resources and infrastructure that are potentially in harm’s way.”\u003c/p>\n\u003cp>The urban areas that stand to be most affected are around Mount Shasta, where over 100,000 people live, work or travel within the hazard zone daily. Redding, in particular, lies relatively close to all three of the active volcanoes in far-northern California.\u003c/p>\n\u003cp>Mount Shasta last erupted in 1786. An eruption of Shasta, according to Ball, could result in a range of hazards with varying severity.\u003c/p>\n\u003cp>Volcanic ash clouds, for example, might pose a threat to air quality, flight patterns, road conditions, and water supply. Depending on the location and nature of the eruption, lava or pyroclastic flows could warrant evacuations.\u003c/p>\n\u003cp>“What we’re hoping is that our partners — land managers and emergency managers and decision-makers in the state — will take the information that we provided and start making their own plans for how to help people deal with these hazards,” Ball said.\u003c/p>\n\u003cp>Public Information Officer Shawn Boyd of the Office of Emergency Services says the agency incorporates the threat of California’s volcanoes into their emergency response planning.\u003c/p>\n\u003cp>Reports from USGS and the California Volcano Observatory are used to inform the state’s Volcano Preparedness Plan, which is part of California’s greater \u003ca href=\"https://www.caloes.ca.gov/PlanningPreparednessSite/Documents/California_State_Emergency_Plan_2017.pdf\" target=\"_blank\" rel=\"noopener\">emergency plan\u003c/a>.\u003c/p>\n\u003cp>“We look at the volcanic hazards in California the same way we do at any other disaster,” Boyd said.\u003c/p>\n\u003cp>Cynthia Pridmore, a geologist with the California Geological Survey who also contributed to the new USGS report, says it’s key for local agencies to stay informed about volcanic activity the same way they do for earthquakes, tsunamis and other dangers. For the general public, she says, the report is a chance to get prepared.\u003c/p>\n\u003cp>“If you’re in one of these regions, it’s just another reason you need to have one of those to-go kits.”\u003c/p>\n\u003cp>Volcanic activity in California is monitored by the Volcano Observatory n Menlo Park. Up-to-date information on all seven of California’s active volcanoes is available on its \u003ca href=\"https://volcanoes.usgs.gov/observatories/calvo/\" target=\"_blank\" rel=\"noopener\">website\u003c/a>.\u003c/p>\n\u003cp>In the event of an eruption, observatory will \u003ca href=\"https://volcanoes.usgs.gov/index.html\">issue alerts\u003c/a> and report to Cal OES to initiate emergency protocols along with local counties.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>“We don’t want [people] to get scared,” Ball says. “We’re not talking doomsday scenarios. We just want them to know that these hazards could happen sometime in the future and that they might be called on to make decisions about their safety and their livelihood.”\u003c/p>\n\n","blocks":[],"excerpt":"California could see a significant volcanic eruption sometime in the next 30 years, according to a report by the U.S. Geological Survey.","status":"publish","parent":0,"modified":1704848811,"stats":{"hasAudio":false,"hasVideo":true,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":26,"wordCount":950},"headData":{"title":"Guess What, California? Now You Need to Prepare for Erupting Volcanoes | KQED","description":"California could see a significant volcanic eruption sometime in the next 30 years, according to a report by the U.S. Geological Survey.","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":"","schema":{"@context":"http://schema.org","@type":"Article","headline":"Guess What, California? Now You Need to Prepare for Erupting Volcanoes","datePublished":"2019-03-08T20:55:01.000Z","dateModified":"2024-01-10T01:06:51.000Z","image":"https://cdn.kqed.org/wp-content/uploads/2020/02/KQED-OG-Image@1x.png"}},"source":"Geology","sticky":false,"path":"/science/1938782/guess-what-california-now-you-need-to-prepare-for-erupting-volcanoes","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\u003cp>\u003cspan class='utils-parseShortcode-shortcodes-__youtubeShortcode__embedYoutube'>\n \u003cspan class='utils-parseShortcode-shortcodes-__youtubeShortcode__embedYoutubeInside'>\n \u003ciframe\n loading='lazy'\n class='utils-parseShortcode-shortcodes-__youtubeShortcode__youtubePlayer'\n type='text/html'\n src='//www.youtube.com/embed/nZD9K4q55jk'\n title='//www.youtube.com/embed/nZD9K4q55jk'\n allowfullscreen='true'\n style='border:0;'>\u003c/iframe>\n \u003c/span>\n \u003c/span>\u003c/p>\u003cp>\u003cp>Earthquakes, wildfires, floods. If you live in California, you’re likely aware of these natural hazards and the dangers associated with them.\u003c/p>\n\u003cp>But according to a U.S. Geological Survey \u003ca href=\"https://pubs.er.usgs.gov/publication/sir20185159\" target=\"_blank\" rel=\"noopener\">report\u003c/a> released last week, California is also home to eight volcanic areas, posing threats categorized from moderate to very high. Seven of these areas are considered active, with molten rock bubbling underneath.\u003c/p>\n\u003cp>These volcanic hotpots span the length of California from Medicine Lake in the far northern region of the state down to Salton Buttes near the U.S.-Mexico border. Clear Lake volcanic field, in Lake County, is roughly 100 miles from both San Francisco and Sacramento.\u003c/p>\n\u003cp>Other active sites include Mount Shasta and Lassen Volcanic Center in Northern California, as well as Long Valley Volcanic Region near Mammoth Lakes, and Coso Volcanic Field, east of a string of unincorporated communities along Highway 395.\u003c/p>\n\u003cfigure id=\"attachment_1938836\" class=\"wp-caption alignnone\" style=\"max-width: 604px\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-1938836\" src=\"https://ww2.kqed.org/science/wp-content/uploads/sites/35/2019/03/img6940.png\" alt=\"\" width=\"604\" height=\"668\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2019/03/img6940.png 604w, https://cdn.kqed.org/wp-content/uploads/sites/35/2019/03/img6940-160x177.png 160w\" sizes=\"(max-width: 604px) 100vw, 604px\">\u003cfigcaption class=\"wp-caption-text\">Sites of California’s eight volcanic hotspots. \u003ccite>(USGS California Volcano Observatory)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>The \u003ca href=\"https://pubs.usgs.gov/sir/2018/5159/sir20185159.pdf\" target=\"_blank\" rel=\"noopener\">report\u003c/a>, titled “California’s Exposure to Volcanic Hazards,” was compiled by the USGS \u003ca href=\"https://volcanoes.usgs.gov/observatories/calvo/\" target=\"_blank\" rel=\"noopener\">California Volcano Observatory\u003c/a> in collaboration with the California Governor’s Office of Emergency Services and the California Geological Survey.\u003c/p>\n\u003cp>\u003c/p>\u003c/div>","attributes":{"named":{},"numeric":[]}},{"type":"component","content":"","name":"ad","attributes":{"named":{"label":"fullwidth"},"numeric":["fullwidth"]}},{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>Based on records of volcanic history, geologists calculate the chance of an eruption in California over the next 30 years at 16 percent. For comparison, scientists have pegged the 30-year probability of a major earthquake in the Bay Area along the San Andreas Fault at about 22 percent.\u003c/p>\n\u003cp>Jessica Ball, a geologist with the California Volcano Observatory and a co-author on the report, says many Californians aren’t aware of the possibilities of a volcanic eruption in the state. Volcanoes operate over longer timescales, she said.\u003c/p>\n\u003cp>“In California, earthquakes tend to take front and center. We have had more of them in the 20th century and 21st century than we have had volcanic activity. So it’s sort of out of people’s memories that we’ve got active volcanoes in the state.”\u003c/p>\n\u003cp>The last \u003ca href=\"https://www.kqed.org/science/30444/four-days-in-may-mount-lassen-erupted-100-years-ago\" target=\"_blank\" rel=\"noopener\">series of eruptions\u003c/a> in California occurred from 1914 to 1917 within the Lassen Volcanic Center, with an explosive eruption of Lassen Peak on May 22, 1915. Lava flows, hot ash, mudslides and avalanches resulting from the eruptions had major impacts on the surrounding region.\u003c/p>\u003c/p>\u003cp>\u003cspan class='utils-parseShortcode-shortcodes-__youtubeShortcode__embedYoutube'>\n \u003cspan class='utils-parseShortcode-shortcodes-__youtubeShortcode__embedYoutubeInside'>\n \u003ciframe\n loading='lazy'\n class='utils-parseShortcode-shortcodes-__youtubeShortcode__youtubePlayer'\n type='text/html'\n src='//www.youtube.com/embed/KvmInz9TgMw'\n title='//www.youtube.com/embed/KvmInz9TgMw'\n allowfullscreen='true'\n style='border:0;'>\u003c/iframe>\n \u003c/span>\n \u003c/span>\u003c/p>\u003cp>\u003cp>The purpose of the report, which was requested by the Office of Emergency Services, was to compile scientific knowledge about volcanoes in California and outline the major hazards that could result should one erupt.\u003c/p>\n\u003cp>“Each volcano has its own hazards,” Ball said. Medicine Lake, for example, could face lava flows. Whereas the Lassen region should be more concerned with lahars (mudslides) or high-speed “pyroclastic flows” of ash and lava powered by pressurized gas, which are a main cause of eruption-related fatalities.\u003c/p>\n\u003cfigure id=\"attachment_1938839\" class=\"wp-caption alignnone\" style=\"max-width: 800px\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-medium wp-image-1938839\" src=\"https://ww2.kqed.org/science/wp-content/uploads/sites/35/2019/03/img6941_900w_863h-800x767.png\" alt=\"\" width=\"800\" height=\"767\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2019/03/img6941_900w_863h-800x767.png 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2019/03/img6941_900w_863h-160x153.png 160w, https://cdn.kqed.org/wp-content/uploads/sites/35/2019/03/img6941_900w_863h-768x736.png 768w, https://cdn.kqed.org/wp-content/uploads/sites/35/2019/03/img6941_900w_863h-32x32.png 32w, https://cdn.kqed.org/wp-content/uploads/sites/35/2019/03/img6941_900w_863h.png 900w\" sizes=\"(max-width: 800px) 100vw, 800px\">\u003cfigcaption class=\"wp-caption-text\">The possible hazards of a volcanic eruption in California. \u003ccite>(USGS California Volcano Observatory)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>Ball says the focus of the work was to home in on “populations, resources and infrastructure that are potentially in harm’s way.”\u003c/p>\n\u003cp>The urban areas that stand to be most affected are around Mount Shasta, where over 100,000 people live, work or travel within the hazard zone daily. Redding, in particular, lies relatively close to all three of the active volcanoes in far-northern California.\u003c/p>\n\u003cp>Mount Shasta last erupted in 1786. An eruption of Shasta, according to Ball, could result in a range of hazards with varying severity.\u003c/p>\n\u003cp>Volcanic ash clouds, for example, might pose a threat to air quality, flight patterns, road conditions, and water supply. Depending on the location and nature of the eruption, lava or pyroclastic flows could warrant evacuations.\u003c/p>\n\u003cp>“What we’re hoping is that our partners — land managers and emergency managers and decision-makers in the state — will take the information that we provided and start making their own plans for how to help people deal with these hazards,” Ball said.\u003c/p>\n\u003cp>Public Information Officer Shawn Boyd of the Office of Emergency Services says the agency incorporates the threat of California’s volcanoes into their emergency response planning.\u003c/p>\n\u003cp>Reports from USGS and the California Volcano Observatory are used to inform the state’s Volcano Preparedness Plan, which is part of California’s greater \u003ca href=\"https://www.caloes.ca.gov/PlanningPreparednessSite/Documents/California_State_Emergency_Plan_2017.pdf\" target=\"_blank\" rel=\"noopener\">emergency plan\u003c/a>.\u003c/p>\n\u003cp>“We look at the volcanic hazards in California the same way we do at any other disaster,” Boyd said.\u003c/p>\n\u003cp>Cynthia Pridmore, a geologist with the California Geological Survey who also contributed to the new USGS report, says it’s key for local agencies to stay informed about volcanic activity the same way they do for earthquakes, tsunamis and other dangers. For the general public, she says, the report is a chance to get prepared.\u003c/p>\n\u003cp>“If you’re in one of these regions, it’s just another reason you need to have one of those to-go kits.”\u003c/p>\n\u003cp>Volcanic activity in California is monitored by the Volcano Observatory n Menlo Park. Up-to-date information on all seven of California’s active volcanoes is available on its \u003ca href=\"https://volcanoes.usgs.gov/observatories/calvo/\" target=\"_blank\" rel=\"noopener\">website\u003c/a>.\u003c/p>\n\u003cp>In the event of an eruption, observatory will \u003ca href=\"https://volcanoes.usgs.gov/index.html\">issue alerts\u003c/a> and report to Cal OES to initiate emergency protocols along with local counties.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>“We don’t want [people] to get scared,” Ball says. “We’re not talking doomsday scenarios. We just want them to know that these hazards could happen sometime in the future and that they might be called on to make decisions about their safety and their livelihood.”\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/science/1938782/guess-what-california-now-you-need-to-prepare-for-erupting-volcanoes","authors":["11368"],"categories":["science_35","science_38","science_40"],"tags":["science_3840","science_3370","science_3834","science_838","science_1999","science_944"],"featImg":"science_1938945","label":"source_science_1938782"},"science_1923693":{"type":"posts","id":"science_1923693","meta":{"index":"posts_1591205157","site":"science","id":"1923693","score":null,"sort":[1525880338000]},"guestAuthors":[],"slug":"days-weeks-years-scientists-say-hawaii-volcano-eruption-has-no-end-in-sight","title":"Days, Weeks, Years? Scientists Say Hawaii Volcano Eruption Has No End In Sight","publishDate":1525880338,"format":"standard","headTitle":"Days, Weeks, Years? Scientists Say Hawaii Volcano Eruption Has No End In Sight | KQED","labelTerm":{"site":"science"},"content":"\u003cp>The eruption at Hawaii’s Kilauea volcano continues. The lava has \u003ca href=\"http://www.hawaiicounty.gov/active-alerts\">now destroyed at least\u003c/a> 35 structures and covered the equivalent of more than 75 football fields.\u003c/p>\n\u003cp>Scientists have been tracking this event since it started last week — but there are still big unanswered questions, the biggest of which is when it will end.\u003c/p>\n\u003cp>The Kilauea volcano on Hawaii’s Big Island has been erupting for more than 30 years. Lava levels in the Pu’u O’o crater and the volcano’s summit rose in recent weeks, says Wendy Stovall, a volcanologist \u003ca href=\"https://www.usgs.gov/staff-profiles/wendy-stovall?qt-staff_profile_science_products=3#qt-staff_profile_science_products\">with the U.S. Geological Survey\u003c/a>. They were “inflating like a balloon, because magma was getting backed up from below,” she says.\u003c/p>\n\u003cp>Then last week, the magma at Pu’u O’o plummeted. “The whole bottom of the crater floor dropped out and the magma completely drained away from that system,” says Stovall.\u003c/p>\n\u003cp>Scientists don’t know what started this latest event, but there are two possibilities, says Stovall: “Either there’s an increase in magma supply, or something blocked the system, something blocked the pathway out of the system.”\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>In other words, suddenly more molten rock shot up from deep inside the Earth, or there was a clog. Whatever the cause, the pressurized magma had to go somewhere. It turned away from the crater, heading underground, flowing into spaces between the rocks along what’s known as the volcano’s East Rift Zone.\u003c/p>\n\u003cp>That set off a series of earthquakes, including a 6.9 magnitude temblor that hit on Friday and could be felt across the island. Stovall said that by tracking the earthquakes and deformations in the ground, they could see the direction the magma was heading.\u003c/p>\n\u003cp>“Honestly it was pretty frightening to see where the magma was going,” says Stovall. That’s because it was headed toward a lush residential area — Leilani Estates, where more than 1,700 people were ordered to evacuate. Video \u003ca href=\"https://www.facebook.com/350778808336211/videos/1692083604205718/\">posted on social media by Demian Barrios\u003c/a> shows flaming lava gushing out, destroying a road.\u003c/p>\n\u003cp>Here’s why the lava rips apart the ground, says \u003ca href=\"https://denison.edu/people/erik-klemetti\">Denison University volcanologist Erik Klemetti\u003c/a>: “It’s like a leaky pipe or a burst pipe, where the magma is moving down the conduit system and it just reaches a point where the pressure builds enough that you start cracking the surface above.”\u003c/p>\n\u003cp>There are now at least 12 of these fissures in the ground as of Tuesday in and around Leilani Estates, according to \u003ca href=\"http://www.hawaiicounty.gov/active-alerts\">Hawaii’s civil defense\u003c/a>.\u003c/p>\n\u003cp>Scientists are tracking earthquakes and the composition of gas coming out of the cracks in the ground, which hints at whether the eruption will intensify. But what will happen longer-term is much more difficult to predict, says Bill Chadwick, a \u003ca href=\"https://www.pmel.noaa.gov/eoi/staff/chadwick.html\">volcanologist at NOAA\u003c/a>.\u003c/p>\n\u003cp>“We can’t really peer through the ground and see it exactly in all its details and intricacies,” Chadwick says. Scientists can’t predict when this eruption will end. “It could last days, weeks, years. All that’s possible. It’s hard to say, unfortunately.”\u003c/p>\n\u003cp>This makes it unique compared with other natural hazards like hurricanes or tornadoes, where there is a clear endpoint, Stovall says.\u003c/p>\n\u003cp>“Volcanoes will build up pressure, and then they’ll release that pressure in eruption, and then they’ll pause,” says Stovall. “And then they’ll build up pressure again and release the pressure in another eruption and then they’ll pause again.”\u003c/p>\n\u003cp>Stovall adds: “As long as there’s magma supplying the system we’re expecting more of the same to happen.”\u003c/p>\n\u003cp>The uncertainty makes it extremely difficult for the residents of Leilani Estates to know what their future holds, which worries Klemetti.\u003c/p>\n\u003cp>“When a house today might look like it’s perfectly safe, it might get taken out by a lava flow five years from now if the eruption keeps on going,” he says.\u003c/p>\n\u003cp>At the same time, it provides what Stovall calls a once-in-a-lifetime research opportunity for scientists. “The things that we will learn in the wake of this eruption will change the way we see volcanoes for the future.”\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>Scientists are trying to gather as much data as possible, and Stovall says that the information they obtain has the potential to change their understanding of how this volcano functions — which could help keep neighboring communities safe in the future.\u003c/p>\n\u003cdiv class=\"fullattribution\">Copyright 2018 NPR. To see more, visit http://www.npr.org/.\u003cimg decoding=\"async\" src=\"https://www.google-analytics.com/__utm.gif?utmac=UA-5828686-4&utmdt=Days%2C+Weeks%2C+Years%3F+Scientists+Say+Hawaii+Volcano+Eruption+Has+No+End+In+Sight&utme=8(APIKey)9(MDAxOTAwOTE4MDEyMTkxMDAzNjczZDljZA004)\">\u003c/div>\n\n","blocks":[],"excerpt":"Scientists are closely tracking the eruption at Hawaii's Kilauea volcano. But there's still a lot that they don't know about the eruption — most notably, when it's going to be over.","status":"publish","parent":0,"modified":1704927922,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":21,"wordCount":784},"headData":{"title":"Days, Weeks, Years? Scientists Say Hawaii Volcano Eruption Has No End In Sight | KQED","description":"Scientists are closely tracking the eruption at Hawaii's Kilauea volcano. But there's still a lot that they don't know about the eruption — most notably, when it's going to be over.","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":"","schema":{"@context":"http://schema.org","@type":"Article","headline":"Days, Weeks, Years? Scientists Say Hawaii Volcano Eruption Has No End In Sight","datePublished":"2018-05-09T15:38:58.000Z","dateModified":"2024-01-10T23:05:22.000Z","image":"https://cdn.kqed.org/wp-content/uploads/2020/02/KQED-OG-Image@1x.png"}},"sticky":false,"nprByline":"Merrit Kennedy\u003cbr />NPR","nprImageAgency":"U.S. Geological Survey via AP","nprStoryId":"609503580","nprApiLink":"http://api.npr.org/query?id=609503580&apiKey=MDAxOTAwOTE4MDEyMTkxMDAzNjczZDljZA004","nprHtmlLink":"https://www.npr.org/sections/thetwo-way/2018/05/08/609503580/days-weeks-years-scientists-say-hawaiis-erupting-volcano-has-no-end-in-sight?ft=nprml&f=609503580","nprRetrievedStory":"1","nprPubDate":"Wed, 09 May 2018 10:35:00 -0400","nprStoryDate":"Tue, 08 May 2018 18:04:00 -0400","nprLastModifiedDate":"Wed, 09 May 2018 10:07:11 -0400","nprAudio":"https://ondemand.npr.org/anon.npr-mp3/npr/me/2018/05/20180509_me_days_weeks_years_scientists_say_hawaiis_erupting_volcano_has_no_end_in_sight.mp3?orgId=1&topicId=1007&d=167&p=3&story=609503580&ft=nprml&f=609503580","nprAudioM3u":"http://api.npr.org/m3u/1609650317-824101.m3u?orgId=1&topicId=1007&d=167&p=3&story=609503580&ft=nprml&f=609503580","audioTrackLength":168,"path":"/science/1923693/days-weeks-years-scientists-say-hawaii-volcano-eruption-has-no-end-in-sight","audioUrl":"https://ondemand.npr.org/anon.npr-mp3/npr/me/2018/05/20180509_me_days_weeks_years_scientists_say_hawaiis_erupting_volcano_has_no_end_in_sight.mp3?orgId=1&topicId=1007&d=167&p=3&story=609503580&ft=nprml&f=609503580","parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cp>The eruption at Hawaii’s Kilauea volcano continues. The lava has \u003ca href=\"http://www.hawaiicounty.gov/active-alerts\">now destroyed at least\u003c/a> 35 structures and covered the equivalent of more than 75 football fields.\u003c/p>\n\u003cp>Scientists have been tracking this event since it started last week — but there are still big unanswered questions, the biggest of which is when it will end.\u003c/p>\n\u003cp>The Kilauea volcano on Hawaii’s Big Island has been erupting for more than 30 years. Lava levels in the Pu’u O’o crater and the volcano’s summit rose in recent weeks, says Wendy Stovall, a volcanologist \u003ca href=\"https://www.usgs.gov/staff-profiles/wendy-stovall?qt-staff_profile_science_products=3#qt-staff_profile_science_products\">with the U.S. Geological Survey\u003c/a>. They were “inflating like a balloon, because magma was getting backed up from below,” she says.\u003c/p>\n\u003cp>Then last week, the magma at Pu’u O’o plummeted. “The whole bottom of the crater floor dropped out and the magma completely drained away from that system,” says Stovall.\u003c/p>\n\u003cp>Scientists don’t know what started this latest event, but there are two possibilities, says Stovall: “Either there’s an increase in magma supply, or something blocked the system, something blocked the pathway out of the system.”\u003c/p>\n\u003cp>\u003c/p>\u003c/div>","attributes":{"named":{},"numeric":[]}},{"type":"component","content":"","name":"ad","attributes":{"named":{"label":"fullwidth"},"numeric":["fullwidth"]}},{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>In other words, suddenly more molten rock shot up from deep inside the Earth, or there was a clog. Whatever the cause, the pressurized magma had to go somewhere. It turned away from the crater, heading underground, flowing into spaces between the rocks along what’s known as the volcano’s East Rift Zone.\u003c/p>\n\u003cp>That set off a series of earthquakes, including a 6.9 magnitude temblor that hit on Friday and could be felt across the island. Stovall said that by tracking the earthquakes and deformations in the ground, they could see the direction the magma was heading.\u003c/p>\n\u003cp>“Honestly it was pretty frightening to see where the magma was going,” says Stovall. That’s because it was headed toward a lush residential area — Leilani Estates, where more than 1,700 people were ordered to evacuate. Video \u003ca href=\"https://www.facebook.com/350778808336211/videos/1692083604205718/\">posted on social media by Demian Barrios\u003c/a> shows flaming lava gushing out, destroying a road.\u003c/p>\n\u003cp>Here’s why the lava rips apart the ground, says \u003ca href=\"https://denison.edu/people/erik-klemetti\">Denison University volcanologist Erik Klemetti\u003c/a>: “It’s like a leaky pipe or a burst pipe, where the magma is moving down the conduit system and it just reaches a point where the pressure builds enough that you start cracking the surface above.”\u003c/p>\n\u003cp>There are now at least 12 of these fissures in the ground as of Tuesday in and around Leilani Estates, according to \u003ca href=\"http://www.hawaiicounty.gov/active-alerts\">Hawaii’s civil defense\u003c/a>.\u003c/p>\n\u003cp>Scientists are tracking earthquakes and the composition of gas coming out of the cracks in the ground, which hints at whether the eruption will intensify. But what will happen longer-term is much more difficult to predict, says Bill Chadwick, a \u003ca href=\"https://www.pmel.noaa.gov/eoi/staff/chadwick.html\">volcanologist at NOAA\u003c/a>.\u003c/p>\n\u003cp>“We can’t really peer through the ground and see it exactly in all its details and intricacies,” Chadwick says. Scientists can’t predict when this eruption will end. “It could last days, weeks, years. All that’s possible. It’s hard to say, unfortunately.”\u003c/p>\n\u003cp>This makes it unique compared with other natural hazards like hurricanes or tornadoes, where there is a clear endpoint, Stovall says.\u003c/p>\n\u003cp>“Volcanoes will build up pressure, and then they’ll release that pressure in eruption, and then they’ll pause,” says Stovall. “And then they’ll build up pressure again and release the pressure in another eruption and then they’ll pause again.”\u003c/p>\n\u003cp>Stovall adds: “As long as there’s magma supplying the system we’re expecting more of the same to happen.”\u003c/p>\n\u003cp>The uncertainty makes it extremely difficult for the residents of Leilani Estates to know what their future holds, which worries Klemetti.\u003c/p>\n\u003cp>“When a house today might look like it’s perfectly safe, it might get taken out by a lava flow five years from now if the eruption keeps on going,” he says.\u003c/p>\n\u003cp>At the same time, it provides what Stovall calls a once-in-a-lifetime research opportunity for scientists. “The things that we will learn in the wake of this eruption will change the way we see volcanoes for the future.”\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>Scientists are trying to gather as much data as possible, and Stovall says that the information they obtain has the potential to change their understanding of how this volcano functions — which could help keep neighboring communities safe in the future.\u003c/p>\n\u003cdiv class=\"fullattribution\">Copyright 2018 NPR. To see more, visit http://www.npr.org/.\u003cimg decoding=\"async\" src=\"https://www.google-analytics.com/__utm.gif?utmac=UA-5828686-4&utmdt=Days%2C+Weeks%2C+Years%3F+Scientists+Say+Hawaii+Volcano+Eruption+Has+No+End+In+Sight&utme=8(APIKey)9(MDAxOTAwOTE4MDEyMTkxMDAzNjczZDljZA004)\">\u003c/div>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/science/1923693/days-weeks-years-scientists-say-hawaii-volcano-eruption-has-no-end-in-sight","authors":["byline_science_1923693"],"categories":["science_38"],"tags":["science_944"],"label":"science"},"science_123833":{"type":"posts","id":"science_123833","meta":{"index":"posts_1591205157","site":"science","id":"123833","score":null,"sort":[1437397209000]},"guestAuthors":[],"slug":"if-you-think-you-understand-the-death-of-the-dinosaurs-youre-wrong","title":"If You Think You Understand the Death of the Dinosaurs, You’re Wrong","publishDate":1437397209,"format":"standard","headTitle":"If You Think You Understand the Death of the Dinosaurs, You’re Wrong | KQED","labelTerm":{"site":"science"},"content":"\u003cp>http://www.kqed.org/.stream/anon/radio/science/2015/07/20150720ScienceDinosaurrocks.mp3\u003c/p>\n\u003cp>A “Jurassic Park” sequel is once again dominating the box office this summer, underscoring the star power of dinosaurs. But, captivated as we are with bringing them back, scientists still argue over what caused their extinction 66 million years ago.\u003c/p>\n\u003cp>It’s not as settled as you might think.\u003c/p>\n\u003cp>I put the question to Charles Marshall, director of the University of California \u003ca href=\"http://www.ucmp.berkeley.edu/\">Museum of Paleontology\u003c/a> in Berkeley: “Do we know what killed the dinosaurs?”\u003c/p>\n\u003cp>“No.” He repeated it emphatically, “No.” (Pause) “I guess the answer is no.”\u003c/p>\n\u003caside class=\"pullquote alignleft\">‘There were dozens of hypotheses, and basically no one took any of them seriously.’\u003ccite>Charles Marshall,UC Museum of Paleontology Director\u003c/cite>\u003c/aside>\n\u003cp>We were sitting in Marshall’s fifth-floor office, not far from the skull of a triceratops relative and some fossilized feet the size of tree stumps. He told me as recently as the 1970s, there wasn’t even a good guess as to what killed the dinosaurs.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>“There were dozens of hypotheses, and basically no one took any of them seriously.”\u003c/p>\n\u003cp>That is, until Berkeley scientists — led by Luis Alvarez (a Nobel laureate in physics) and his geologist son Walter Alvarez — brought forward the idea that Earth was slammed by a meteorite or comet roughly the size of San Francisco.\u003c/p>\n\u003cp>The theory and its backers got a major boost a few years later with the discovery of a 110-mile-wide crater on present-day Mexico’s Yucatan Peninsula.\u003c/p>\n\u003cp>“With the finding of the smoking gun, then the fact that there was a large meteorite started to become broadly accepted,” Marshall said. “So it sort’ve started to evolve into meteorite versus volcanism as the two hypotheses.”\u003c/p>\n\u003cfigure id=\"attachment_124231\" class=\"wp-caption alignright\" style=\"max-width: 800px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/07/IMG_8518.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-medium wp-image-124231\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/07/IMG_8518-800x600.jpg\" alt=\"Charles Marshall looks at a cast of a bird related to puffins and the Great Auk, found in southern California’s Monterey Formation.\" width=\"800\" height=\"600\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/IMG_8518-800x600.jpg 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/IMG_8518-400x300.jpg 400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/IMG_8518-1440x1080.jpg 1440w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/IMG_8518-1400x1050.jpg 1400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/IMG_8518-1180x885.jpg 1180w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/IMG_8518-960x720.jpg 960w\" sizes=\"(max-width: 800px) 100vw, 800px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Charles Marshall looks at a cast of a bird related to puffins and the Great Auk, found in southern California’s Monterey Formation. \u003ccite>(Daniel Potter/KQED)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>Indeed, volcanoes have been hard to keep off the list of known suspects. Going back hundreds of millions of years, every other big extinction (barring the present day’s) is connected to volcanism.\u003c/p>\n\u003cp>Plus, around the same time as the meteorite impact and the disappearance of dinosaurs from the fossil record (along with many species, down to tiny ocean creatures), there was also a massive wave of volcanic activity in India – in a place known as the Deccan Traps.\u003c/p>\n\u003cp>So for years scientists have argued back and forth: Impact! Volcanoes! Impact! …\u003c/p>\n\u003cp>Until recently, when Berkeley geophysicist Mark Richards \u003ca href=\"http://gsabulletin.gsapubs.org/content/early/2015/04/30/B31167.1.abstract\">offered this idea\u003c/a>: “I realized that the size of the impact is likely large enough to have triggered volcanic systems around the planet.”\u003c/p>\n\u003cp>\u003cstrong>Bigger Than Big\u003c/strong>\u003c/p>\n\u003cp>Richards calculates that the energy of a rock the size of Mount Everest slamming down from space was enough to unleash a magnitude 11 quake. That is not a typo. When I told Richards I thought the scale only went to 10, he told me that’s actually not true.\u003c/p>\n\u003cp>In earthquake terms, higher than 10 is a nightmare. Such a quake would be hundreds of times worse than the “big one” that hit San Francisco in 1906. Richards says it would’ve rattled the globe – even the volcanoes on the other side of the world in India.\u003c/p>\n\u003cfigure id=\"attachment_124232\" class=\"wp-caption alignleft\" style=\"max-width: 414px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/07/IMG_8537-e1437167252247.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\" wp-image-124232\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/07/IMG_8537-e1437167252247-800x738.jpg\" alt=\"A relative to the present day Komodo dragon, the owner of this skull (left) sported flippers and could grow more than 20 feet long. To the right in Charles Marshall's lab sits an Allosaurus foot.\" width=\"414\" height=\"382\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/IMG_8537-e1437167252247-800x738.jpg 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/IMG_8537-e1437167252247-400x369.jpg 400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/IMG_8537-e1437167252247-1440x1329.jpg 1440w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/IMG_8537-e1437167252247-1400x1292.jpg 1400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/IMG_8537-e1437167252247-1180x1089.jpg 1180w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/IMG_8537-e1437167252247-960x886.jpg 960w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/IMG_8537-e1437167252247.jpg 2007w\" sizes=\"(max-width: 414px) 100vw, 414px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">A relative to the present day Komodo dragon, the owner of this skull (left) sported flippers and could grow more than 20 feet long. To the right in Charles Marshall’s lab sits an Allosaurus foot. \u003ccite>(Daniel Potter/KQED)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>“So the idea is that system may have been kicked into high gear by the impact.”\u003c/p>\n\u003cp>Richards is careful to say that if he’s right, and the two events are connected, we still don’t know precisely what killed the dinosaurs. Rather, the proposal points the way toward a new investigation, says Paul Renne, director of the \u003ca href=\"http://www.bgc.org/\">Berkeley Geochronology Center\u003c/a> and coauthor of Richards’ paper.\u003c/p>\n\u003cp>“We just have to abandon the idea that it’s one or the other,” Renne said.\u003c/p>\n\u003cp>Both the impact itself and a wave of volcanism would have the potential to unleash massive outpourings of noxious gases, resulting in wild swings in temperature.\u003c/p>\n\u003cp>One factor might’ve been a release of CO2, say from so much vaporized limestone, resulting, along with other greenhouse gases, in a long-term warming effect.\u003c/p>\n\u003cfigure id=\"attachment_124230\" class=\"wp-caption alignright\" style=\"max-width: 530px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/07/4DPotter1.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\" wp-image-124230\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/07/4DPotter1-800x600.jpg\" alt=\"India’s Deccan Traps, described by geologists as a “large igneous province,” were formed over thousands of years as layer upon layer of lava flowed out and cooled, right around the same time the dinosaurs died.\" width=\"530\" height=\"397\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/4DPotter1-800x600.jpg 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/4DPotter1-400x300.jpg 400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/4DPotter1-1440x1080.jpg 1440w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/4DPotter1-1400x1050.jpg 1400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/4DPotter1-1180x885.jpg 1180w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/4DPotter1-960x720.jpg 960w\" sizes=\"(max-width: 530px) 100vw, 530px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">India’s Deccan Traps, described by geologists as a “large igneous province,” were formed over hundreds of thousands of years as layer upon layer of lava flowed out and cooled, right around the same time the dinosaurs died. \u003ccite>(Paul Renne/BGC)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>Renne says there could’ve also been an abundance of sulfate aerosols, “which, if they get up into the atmosphere, can actually reflect enough sunlight it results in cooling.”\u003c/p>\n\u003cp>In fact, one could argue for a double event – sudden cooling first, followed by a long, hot period from the greenhouse effect. Whether the dinosaurs died in a single bad weekend, or the lifetime of an animal as the food web collapsed, or several millenia, remains unclear.\u003c/p>\n\u003cp>“The potential effects of either an impact or massive volcanism in many respects can be the same. The symptoms would be indistinguishable,” Renne says.\u003c/p>\n\u003cp>\u003cstrong>Increasing Precision\u003c/strong>\u003c/p>\n\u003cp>To better understand the impact and its possible connection to the eruptions in India, the next step will be establishing a narrower range of dates. For Renne, this entails using a basement room full of mass spectrometers to test rocks from the Deccan Traps. Canvas sacks full of such rocks are heaped in the hallway outside his office.\u003c/p>\n\u003cp>“I’m a rock aficionado, and I have lots of beautiful rocks and big crystals. These are some of the ugliest rocks you’ll ever see,” Renne said, producing a sample that to my untrained eye might as well have been gravel from a nearby quarry.\u003c/p>\n\u003cfigure id=\"attachment_124234\" class=\"wp-caption alignleft\" style=\"max-width: 355px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/07/Skeletons.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\" wp-image-124234\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/07/Skeletons-800x1067.jpg\" alt=\"A fossilized Pteranodon swoops above Tyrannosaurus rex at the University of California Museum of Paleontology in Berkeley.\" width=\"355\" height=\"474\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/Skeletons-800x1067.jpg 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/Skeletons-400x533.jpg 400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/Skeletons-1440x1920.jpg 1440w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/Skeletons-1400x1867.jpg 1400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/Skeletons-1180x1573.jpg 1180w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/Skeletons-960x1280.jpg 960w\" sizes=\"(max-width: 355px) 100vw, 355px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">A fossilized Pteranodon swoops above Tyrannosaurus rex at the University of California Museum of Paleontology in Berkeley. \u003ccite>(Daniel Potter/KQED)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>Dating these rocks is a slow process, involving shipping a few dozen milligrams out of state to be irradiated and then sent back for testing. It can take months.\u003c/p>\n\u003cp>Nearby is a wood-paneled room that houses a magnetometer — another tool for dating prehistoric rocks. This is Courtney Sprain’s speciality; she’s a Ph.D. student who also coauthored Richards’ paper.\u003c/p>\n\u003cp>Sprain spends part of each summer in Montana gathering samples from coal beds, and told me by the end of each day she tends to resemble a chimneysweep.\u003c/p>\n\u003cp>When the Earth’s magnetic core shifts (we’re not sure why this happens), it leaves a record in the rocks. Sprain teases out these clues to refine the timescale.\u003c/p>\n\u003cp>“We’re getting precision of 20-thousand years,” she says, “whereas before it was 500-thousand, a million.”\u003c/p>\n\u003cp>Really, what would be ideal, if unrealistic, is precision down to what day of the week the impact occurred. But getting it under 10,000 years would be helpful.\u003c/p>\n\u003cp>Geologist Eldridge Moores, a distinguished professor emeritus at U.C. Davis, known for his role in the John McPhee book “Assembling California,” says it’s like a detective trying to figure out someone’s exact time of death.\u003c/p>\n\u003cp>“You have to know that – it’s essential information before you can answer the next question, which is why. The same is true with the dinosaurs.”\u003c/p>\n\u003cp>Moores was sitting with me at his house in Davis, a copy of Mark Richards’ paper on the dining room table before him, when I asked him the question: Do we know what killed the dinosaurs?\u003c/p>\n\u003cp>[ad floatright]\u003c/p>\n\u003cp>He told me no — but he thinks we’re getting closer.\u003c/p>\n\n","blocks":[],"excerpt":"A meteorite killed the dinosaurs. Or was it volcanism? U.C. Berkeley scientists say the two were connected.","status":"publish","parent":0,"modified":1704931542,"stats":{"hasAudio":true,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":39,"wordCount":1342},"headData":{"title":"If You Think You Understand the Death of the Dinosaurs, You’re Wrong | KQED","description":"A meteorite killed the dinosaurs. Or was it volcanism? U.C. Berkeley scientists say the two were connected.","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":"","schema":{"@context":"http://schema.org","@type":"Article","headline":"If You Think You Understand the Death of the Dinosaurs, You’re Wrong","datePublished":"2015-07-20T13:00:09.000Z","dateModified":"2024-01-11T00:05:42.000Z","image":"https://cdn.kqed.org/wp-content/uploads/2020/02/KQED-OG-Image@1x.png"}},"sticky":false,"path":"/science/123833/if-you-think-you-understand-the-death-of-the-dinosaurs-youre-wrong","audioUrl":"http://www.kqed.org/.stream/anon/radio/science/2015/07/20150720ScienceDinosaurrocks.mp3","audioDuration":null,"audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\u003c/div>","attributes":{"named":{},"numeric":[]}},{"type":"component","content":"","name":"audioLink","attributes":{"named":{"src":"http://www.kqed.org/.stream/anon/radio/science/2015/07/20150720ScienceDinosaurrocks.mp3"},"numeric":[]}},{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cp>A “Jurassic Park” sequel is once again dominating the box office this summer, underscoring the star power of dinosaurs. But, captivated as we are with bringing them back, scientists still argue over what caused their extinction 66 million years ago.\u003c/p>\n\u003cp>It’s not as settled as you might think.\u003c/p>\n\u003cp>I put the question to Charles Marshall, director of the University of California \u003ca href=\"http://www.ucmp.berkeley.edu/\">Museum of Paleontology\u003c/a> in Berkeley: “Do we know what killed the dinosaurs?”\u003c/p>\n\u003cp>“No.” He repeated it emphatically, “No.” (Pause) “I guess the answer is no.”\u003c/p>\n\u003caside class=\"pullquote alignleft\">‘There were dozens of hypotheses, and basically no one took any of them seriously.’\u003ccite>Charles Marshall,UC Museum of Paleontology Director\u003c/cite>\u003c/aside>\n\u003cp>We were sitting in Marshall’s fifth-floor office, not far from the skull of a triceratops relative and some fossilized feet the size of tree stumps. He told me as recently as the 1970s, there wasn’t even a good guess as to what killed the dinosaurs.\u003c/p>\n\u003cp>\u003c/p>\u003c/div>","attributes":{"named":{},"numeric":[]}},{"type":"component","content":"","name":"ad","attributes":{"named":{"label":"fullwidth"},"numeric":["fullwidth"]}},{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>“There were dozens of hypotheses, and basically no one took any of them seriously.”\u003c/p>\n\u003cp>That is, until Berkeley scientists — led by Luis Alvarez (a Nobel laureate in physics) and his geologist son Walter Alvarez — brought forward the idea that Earth was slammed by a meteorite or comet roughly the size of San Francisco.\u003c/p>\n\u003cp>The theory and its backers got a major boost a few years later with the discovery of a 110-mile-wide crater on present-day Mexico’s Yucatan Peninsula.\u003c/p>\n\u003cp>“With the finding of the smoking gun, then the fact that there was a large meteorite started to become broadly accepted,” Marshall said. “So it sort’ve started to evolve into meteorite versus volcanism as the two hypotheses.”\u003c/p>\n\u003cfigure id=\"attachment_124231\" class=\"wp-caption alignright\" style=\"max-width: 800px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/07/IMG_8518.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-medium wp-image-124231\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/07/IMG_8518-800x600.jpg\" alt=\"Charles Marshall looks at a cast of a bird related to puffins and the Great Auk, found in southern California’s Monterey Formation.\" width=\"800\" height=\"600\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/IMG_8518-800x600.jpg 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/IMG_8518-400x300.jpg 400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/IMG_8518-1440x1080.jpg 1440w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/IMG_8518-1400x1050.jpg 1400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/IMG_8518-1180x885.jpg 1180w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/IMG_8518-960x720.jpg 960w\" sizes=\"(max-width: 800px) 100vw, 800px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Charles Marshall looks at a cast of a bird related to puffins and the Great Auk, found in southern California’s Monterey Formation. \u003ccite>(Daniel Potter/KQED)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>Indeed, volcanoes have been hard to keep off the list of known suspects. Going back hundreds of millions of years, every other big extinction (barring the present day’s) is connected to volcanism.\u003c/p>\n\u003cp>Plus, around the same time as the meteorite impact and the disappearance of dinosaurs from the fossil record (along with many species, down to tiny ocean creatures), there was also a massive wave of volcanic activity in India – in a place known as the Deccan Traps.\u003c/p>\n\u003cp>So for years scientists have argued back and forth: Impact! Volcanoes! Impact! …\u003c/p>\n\u003cp>Until recently, when Berkeley geophysicist Mark Richards \u003ca href=\"http://gsabulletin.gsapubs.org/content/early/2015/04/30/B31167.1.abstract\">offered this idea\u003c/a>: “I realized that the size of the impact is likely large enough to have triggered volcanic systems around the planet.”\u003c/p>\n\u003cp>\u003cstrong>Bigger Than Big\u003c/strong>\u003c/p>\n\u003cp>Richards calculates that the energy of a rock the size of Mount Everest slamming down from space was enough to unleash a magnitude 11 quake. That is not a typo. When I told Richards I thought the scale only went to 10, he told me that’s actually not true.\u003c/p>\n\u003cp>In earthquake terms, higher than 10 is a nightmare. Such a quake would be hundreds of times worse than the “big one” that hit San Francisco in 1906. Richards says it would’ve rattled the globe – even the volcanoes on the other side of the world in India.\u003c/p>\n\u003cfigure id=\"attachment_124232\" class=\"wp-caption alignleft\" style=\"max-width: 414px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/07/IMG_8537-e1437167252247.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\" wp-image-124232\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/07/IMG_8537-e1437167252247-800x738.jpg\" alt=\"A relative to the present day Komodo dragon, the owner of this skull (left) sported flippers and could grow more than 20 feet long. To the right in Charles Marshall's lab sits an Allosaurus foot.\" width=\"414\" height=\"382\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/IMG_8537-e1437167252247-800x738.jpg 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/IMG_8537-e1437167252247-400x369.jpg 400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/IMG_8537-e1437167252247-1440x1329.jpg 1440w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/IMG_8537-e1437167252247-1400x1292.jpg 1400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/IMG_8537-e1437167252247-1180x1089.jpg 1180w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/IMG_8537-e1437167252247-960x886.jpg 960w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/IMG_8537-e1437167252247.jpg 2007w\" sizes=\"(max-width: 414px) 100vw, 414px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">A relative to the present day Komodo dragon, the owner of this skull (left) sported flippers and could grow more than 20 feet long. To the right in Charles Marshall’s lab sits an Allosaurus foot. \u003ccite>(Daniel Potter/KQED)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>“So the idea is that system may have been kicked into high gear by the impact.”\u003c/p>\n\u003cp>Richards is careful to say that if he’s right, and the two events are connected, we still don’t know precisely what killed the dinosaurs. Rather, the proposal points the way toward a new investigation, says Paul Renne, director of the \u003ca href=\"http://www.bgc.org/\">Berkeley Geochronology Center\u003c/a> and coauthor of Richards’ paper.\u003c/p>\n\u003cp>“We just have to abandon the idea that it’s one or the other,” Renne said.\u003c/p>\n\u003cp>Both the impact itself and a wave of volcanism would have the potential to unleash massive outpourings of noxious gases, resulting in wild swings in temperature.\u003c/p>\n\u003cp>One factor might’ve been a release of CO2, say from so much vaporized limestone, resulting, along with other greenhouse gases, in a long-term warming effect.\u003c/p>\n\u003cfigure id=\"attachment_124230\" class=\"wp-caption alignright\" style=\"max-width: 530px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/07/4DPotter1.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\" wp-image-124230\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/07/4DPotter1-800x600.jpg\" alt=\"India’s Deccan Traps, described by geologists as a “large igneous province,” were formed over thousands of years as layer upon layer of lava flowed out and cooled, right around the same time the dinosaurs died.\" width=\"530\" height=\"397\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/4DPotter1-800x600.jpg 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/4DPotter1-400x300.jpg 400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/4DPotter1-1440x1080.jpg 1440w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/4DPotter1-1400x1050.jpg 1400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/4DPotter1-1180x885.jpg 1180w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/4DPotter1-960x720.jpg 960w\" sizes=\"(max-width: 530px) 100vw, 530px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">India’s Deccan Traps, described by geologists as a “large igneous province,” were formed over hundreds of thousands of years as layer upon layer of lava flowed out and cooled, right around the same time the dinosaurs died. \u003ccite>(Paul Renne/BGC)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>Renne says there could’ve also been an abundance of sulfate aerosols, “which, if they get up into the atmosphere, can actually reflect enough sunlight it results in cooling.”\u003c/p>\n\u003cp>In fact, one could argue for a double event – sudden cooling first, followed by a long, hot period from the greenhouse effect. Whether the dinosaurs died in a single bad weekend, or the lifetime of an animal as the food web collapsed, or several millenia, remains unclear.\u003c/p>\n\u003cp>“The potential effects of either an impact or massive volcanism in many respects can be the same. The symptoms would be indistinguishable,” Renne says.\u003c/p>\n\u003cp>\u003cstrong>Increasing Precision\u003c/strong>\u003c/p>\n\u003cp>To better understand the impact and its possible connection to the eruptions in India, the next step will be establishing a narrower range of dates. For Renne, this entails using a basement room full of mass spectrometers to test rocks from the Deccan Traps. Canvas sacks full of such rocks are heaped in the hallway outside his office.\u003c/p>\n\u003cp>“I’m a rock aficionado, and I have lots of beautiful rocks and big crystals. These are some of the ugliest rocks you’ll ever see,” Renne said, producing a sample that to my untrained eye might as well have been gravel from a nearby quarry.\u003c/p>\n\u003cfigure id=\"attachment_124234\" class=\"wp-caption alignleft\" style=\"max-width: 355px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/07/Skeletons.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\" wp-image-124234\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/07/Skeletons-800x1067.jpg\" alt=\"A fossilized Pteranodon swoops above Tyrannosaurus rex at the University of California Museum of Paleontology in Berkeley.\" width=\"355\" height=\"474\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/Skeletons-800x1067.jpg 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/Skeletons-400x533.jpg 400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/Skeletons-1440x1920.jpg 1440w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/Skeletons-1400x1867.jpg 1400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/Skeletons-1180x1573.jpg 1180w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/07/Skeletons-960x1280.jpg 960w\" sizes=\"(max-width: 355px) 100vw, 355px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">A fossilized Pteranodon swoops above Tyrannosaurus rex at the University of California Museum of Paleontology in Berkeley. \u003ccite>(Daniel Potter/KQED)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>Dating these rocks is a slow process, involving shipping a few dozen milligrams out of state to be irradiated and then sent back for testing. It can take months.\u003c/p>\n\u003cp>Nearby is a wood-paneled room that houses a magnetometer — another tool for dating prehistoric rocks. This is Courtney Sprain’s speciality; she’s a Ph.D. student who also coauthored Richards’ paper.\u003c/p>\n\u003cp>Sprain spends part of each summer in Montana gathering samples from coal beds, and told me by the end of each day she tends to resemble a chimneysweep.\u003c/p>\n\u003cp>When the Earth’s magnetic core shifts (we’re not sure why this happens), it leaves a record in the rocks. Sprain teases out these clues to refine the timescale.\u003c/p>\n\u003cp>“We’re getting precision of 20-thousand years,” she says, “whereas before it was 500-thousand, a million.”\u003c/p>\n\u003cp>Really, what would be ideal, if unrealistic, is precision down to what day of the week the impact occurred. But getting it under 10,000 years would be helpful.\u003c/p>\n\u003cp>Geologist Eldridge Moores, a distinguished professor emeritus at U.C. Davis, known for his role in the John McPhee book “Assembling California,” says it’s like a detective trying to figure out someone’s exact time of death.\u003c/p>\n\u003cp>“You have to know that – it’s essential information before you can answer the next question, which is why. The same is true with the dinosaurs.”\u003c/p>\n\u003cp>Moores was sitting with me at his house in Davis, a copy of Mark Richards’ paper on the dining room table before him, when I asked him the question: Do we know what killed the dinosaurs?\u003c/p>\n\u003cp>\u003c/p>\u003c/div>","attributes":{"named":{},"numeric":[]}},{"type":"component","content":"","name":"ad","attributes":{"named":{"label":"floatright"},"numeric":["floatright"]}},{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>He told me no — but he thinks we’re getting closer.\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/science/123833/if-you-think-you-understand-the-death-of-the-dinosaurs-youre-wrong","authors":["6609"],"categories":["science_30","science_31","science_38","science_40","science_43"],"tags":["science_2145","science_260","science_575","science_944"],"featImg":"science_124441","label":"science"},"science_73144":{"type":"posts","id":"science_73144","meta":{"index":"posts_1591205157","site":"science","id":"73144","score":null,"sort":[1435237216000]},"guestAuthors":[],"slug":"active-volcanoes-spotted-on-venus","title":"Active Volcanoes Spotted on Venus","publishDate":1435237216,"format":"standard","headTitle":"Active Volcanoes Spotted on Venus | KQED","labelTerm":{"site":"science"},"content":"\u003cp>Planetary scientists have found what they think is a smoking gun proving that the planet Venus is geologically alive—volcanoes in the act of erupting lava. Short-lived pulses of heat energy, sensed through the planet’s thick atmosphere by the Venus Express spacecraft, are explained as the red-hot glow of active pools and flows of molten rock.\u003c/p>\n\u003cp>Venus is often called our sister planet, being much like Earth in its size and rocky composition, but it’s more like hell than Earth. Its atmosphere is a thick blanket of carbon dioxide topped with a haze of sulfuric acid that completely hides the surface from view.\u003c/p>\n\u003cp>The greenhouse effect from this atmosphere makes Venus hotter than the fiercest pizza oven, at about 850 degrees Fahrenheit. The air pressure on the ground is like being 3,000 feet deep in the ocean, and the CO\u003csub>2\u003c/sub> gas is so thick that spacecraft have fallen through it to land without needing parachutes—although their electronics quickly failed in the searing heat.\u003c/p>\n\u003cp>Between 1975 and 1982, a handful of Soviet landers made \u003ca href=\"http://mentallandscape.com/C_CatalogVenus.htm\">the only visible-light images we have of the surface of Venus\u003c/a>. All the pictures show a landscape of volcanic rocks.\u003c/p>\n\u003cp>Between 1990 and 1994, the Magellan spacecraft used radar to map the surface of Venus in detail. We’ve learned that, other than some impact craters, the surface consists entirely of different kinds of lava. The volcanoes responsible range from little domes to sets of huge fractures thousands of miles long.\u003c/p>\n\u003cfigure id=\"attachment_74114\" class=\"wp-caption alignright\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/06/venus-lava-flows.png\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-74114\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/06/venus-lava-flows.png\" alt=\"Lava flows on Venus\" width=\"600\" height=\"419\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2015/06/venus-lava-flows.png 600w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/06/venus-lava-flows-400x279.png 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Lava flows on the east flank of the volcano Sapas Mons in a radar image from the Magellan mission. (NASA/JPL)\u003c/figcaption>\u003c/figure>\n\u003cp>So we know Venus is covered with lava, most of it looking fresh. The Soviet landers recorded lightning and thunder, \u003ca href=\"http://ww2.kqed.org/science/2015/03/05/volcanoes-and-lightning-make-tiny-glass-balls-together/\">typical in volcanic eruptions\u003c/a>. And satellites have detected short-lived pulses of sulfur gases in the atmosphere, also typical of eruptions. It’s a safe guess Venus didn’t stop all of its eruptions, forever, just yesterday.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>However, to be sure volcanism is really happening today on Venus, science wanted a clincher. In \u003ca href=\"http://onlinelibrary.wiley.com/doi/10.1002/2015GL064088/full\">a new paper\u003c/a> in the journal \u003ca href=\"http://agupubs.onlinelibrary.wiley.com/agu/journal/10.1002/%28ISSN%291944-8007/\">Geophysical Research Letters\u003c/a>, a team led by Eugene Shalygin of the \u003ca href=\"http://www.mps.mpg.de/en\">Max Planck Institute for Solar System Research\u003c/a> presents direct evidence of erupting lava in a large set of fissures named Ganis Chasma.\u003c/p>\n\u003cp>(A tip of the hat to Planetary Society ace reporter Emily Lakdawalla for noting that \u003ca href=\"http://www.planetary.org/blogs/emily-lakdawalla/2015/06181637-transient-hot-spots-on-venus.html\">the paper’s authors called Ganis Chasma by the wrong name\u003c/a>, confusing it with the nearby Ganiki Planitia.)\u003c/p>\n\u003cfigure id=\"attachment_73147\" class=\"wp-caption alignleft\" style=\"max-width: 364px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/06/venus-global.png\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\" wp-image-73147\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/06/venus-global-800x794.png\" alt=\"Venus location map\" width=\"364\" height=\"361\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2015/06/venus-global-800x794.png 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/06/venus-global-400x397.png 400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/06/venus-global-32x32.png 32w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/06/venus-global-64x64.png 64w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/06/venus-global-96x96.png 96w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/06/venus-global-128x128.png 128w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/06/venus-global-75x75.png 75w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/06/venus-global.png 816w\" sizes=\"(max-width: 364px) 100vw, 364px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Radar map of Venus showing the location of Ganis Chasma, a large set of fissures flanking the volcano Ozza Mons, itself part of the great Aphrodite Terra volcanic structure. (NASA/JPL)\u003c/figcaption>\u003c/figure>\n\u003cp>The evidence was recorded by an infrared camera on the spacecraft Venus Express, launched by the European Space Agency in 2005. Before ending its work late last year and burning up in the Venusian atmosphere, Venus Express used its camera to study the planet at night.\u003c/p>\n\u003cp>The orbiting camera was sensitive to infrared light at wavelengths at which Venus’s atmosphere is somewhat transparent, but the pictures were like watching a scene through heavy, blowing fog. Nevertheless, it detected four different places in Ganis Chasma that were slightly hotter than their surroundings. During earlier and later visits, these hot spots were absent.\u003c/p>\n\u003cp>Shalygin and his five coauthors systematically eliminated camera errors and other explanations. They calculated that a fairly small pool of lava, maybe the size of Hawaii’s Halemaumau crater, could look like a large patch of slightly warmer temperature when seen through the blurring atmosphere of Venus. A larger flow of lava, cooling down after its eruption, would do the same.\u003c/p>\n\u003cp>The Ganis Chasma eruptions appear to resemble basaltic fissure eruptions on Earth, like those of the volcanoes of Hawaii and Iceland. Here, lava flows may take years to cool down, but the hot spots on Venus disappeared in a matter of months. The authors speculate that the dense atmosphere cools the lava quickly, just as seawater does on Earth.\u003c/p>\n\u003cfigure id=\"attachment_73148\" class=\"wp-caption alignright\" style=\"max-width: 476px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/06/venus-volcs.png\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\" wp-image-73148\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/06/venus-volcs-800x450.png\" alt=\"Eruptive hot spots, Ganis Chasma, Venus\" width=\"476\" height=\"268\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2015/06/venus-volcs-800x450.png 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/06/venus-volcs-400x225.png 400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/06/venus-volcs.png 900w\" sizes=\"(max-width: 476px) 100vw, 476px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Hot spots on Ganis Chasma recorded by Venus Express. The spots lie exactly where eruptions are expected. (Shalygin/American Geophysical Union)\u003c/figcaption>\u003c/figure>\n\u003cp>The authors recommend that we keep a close eye on Ganis Chasma and Atla Regio, the larger volcanic region of which it’s a part. Of course, there are no spacecraft at Venus at the moment. Twenty years after the Magellan mission, our current radar technology \u003ca href=\"http://www.planetary.org/blogs/guest-blogs/van-kane/20150302-understanding-venus.html\">could map Venus as well as we’re mapping Mars\u003c/a> in visible light.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>But scientists have had no luck getting a new radar mapping mission off the ground. Venus researchers, like all scientists who rely on spacecraft missions, play a high-stakes gambling game as they make funding proposals to two major sponsors: NASA and the European Space Agency. ESA just finished choosing its next set of medium-class missions, and Venus lost out in that round. Now NASA is considering 28 proposals for its next round of Discovery-class missions, and there are said to be \u003ca href=\"http://www.thespacereview.com/article/2722/1\">four Venus proposals\u003c/a> in play there.\u003c/p>\n\n","blocks":[],"excerpt":"Spacecraft captures evidence of molten lava, clinching the argument that Venus is geologically alive.","status":"publish","parent":0,"modified":1704931651,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":16,"wordCount":854},"headData":{"title":"Active Volcanoes Spotted on Venus | KQED","description":"Spacecraft captures evidence of molten lava, clinching the argument that Venus is geologically alive.","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":"","schema":{"@context":"http://schema.org","@type":"Article","headline":"Active Volcanoes Spotted on Venus","datePublished":"2015-06-25T13:00:16.000Z","dateModified":"2024-01-11T00:07:31.000Z","image":"https://cdn.kqed.org/wp-content/uploads/2020/02/KQED-OG-Image@1x.png"}},"sticky":false,"path":"/science/73144/active-volcanoes-spotted-on-venus","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cp>Planetary scientists have found what they think is a smoking gun proving that the planet Venus is geologically alive—volcanoes in the act of erupting lava. Short-lived pulses of heat energy, sensed through the planet’s thick atmosphere by the Venus Express spacecraft, are explained as the red-hot glow of active pools and flows of molten rock.\u003c/p>\n\u003cp>Venus is often called our sister planet, being much like Earth in its size and rocky composition, but it’s more like hell than Earth. Its atmosphere is a thick blanket of carbon dioxide topped with a haze of sulfuric acid that completely hides the surface from view.\u003c/p>\n\u003cp>The greenhouse effect from this atmosphere makes Venus hotter than the fiercest pizza oven, at about 850 degrees Fahrenheit. The air pressure on the ground is like being 3,000 feet deep in the ocean, and the CO\u003csub>2\u003c/sub> gas is so thick that spacecraft have fallen through it to land without needing parachutes—although their electronics quickly failed in the searing heat.\u003c/p>\n\u003cp>Between 1975 and 1982, a handful of Soviet landers made \u003ca href=\"http://mentallandscape.com/C_CatalogVenus.htm\">the only visible-light images we have of the surface of Venus\u003c/a>. All the pictures show a landscape of volcanic rocks.\u003c/p>\n\u003cp>Between 1990 and 1994, the Magellan spacecraft used radar to map the surface of Venus in detail. We’ve learned that, other than some impact craters, the surface consists entirely of different kinds of lava. The volcanoes responsible range from little domes to sets of huge fractures thousands of miles long.\u003c/p>\n\u003cfigure id=\"attachment_74114\" class=\"wp-caption alignright\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/06/venus-lava-flows.png\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-74114\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/06/venus-lava-flows.png\" alt=\"Lava flows on Venus\" width=\"600\" height=\"419\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2015/06/venus-lava-flows.png 600w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/06/venus-lava-flows-400x279.png 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Lava flows on the east flank of the volcano Sapas Mons in a radar image from the Magellan mission. (NASA/JPL)\u003c/figcaption>\u003c/figure>\n\u003cp>So we know Venus is covered with lava, most of it looking fresh. The Soviet landers recorded lightning and thunder, \u003ca href=\"http://ww2.kqed.org/science/2015/03/05/volcanoes-and-lightning-make-tiny-glass-balls-together/\">typical in volcanic eruptions\u003c/a>. And satellites have detected short-lived pulses of sulfur gases in the atmosphere, also typical of eruptions. It’s a safe guess Venus didn’t stop all of its eruptions, forever, just yesterday.\u003c/p>\n\u003cp>\u003c/p>\u003c/div>","attributes":{"named":{},"numeric":[]}},{"type":"component","content":"","name":"ad","attributes":{"named":{"label":"fullwidth"},"numeric":["fullwidth"]}},{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>However, to be sure volcanism is really happening today on Venus, science wanted a clincher. In \u003ca href=\"http://onlinelibrary.wiley.com/doi/10.1002/2015GL064088/full\">a new paper\u003c/a> in the journal \u003ca href=\"http://agupubs.onlinelibrary.wiley.com/agu/journal/10.1002/%28ISSN%291944-8007/\">Geophysical Research Letters\u003c/a>, a team led by Eugene Shalygin of the \u003ca href=\"http://www.mps.mpg.de/en\">Max Planck Institute for Solar System Research\u003c/a> presents direct evidence of erupting lava in a large set of fissures named Ganis Chasma.\u003c/p>\n\u003cp>(A tip of the hat to Planetary Society ace reporter Emily Lakdawalla for noting that \u003ca href=\"http://www.planetary.org/blogs/emily-lakdawalla/2015/06181637-transient-hot-spots-on-venus.html\">the paper’s authors called Ganis Chasma by the wrong name\u003c/a>, confusing it with the nearby Ganiki Planitia.)\u003c/p>\n\u003cfigure id=\"attachment_73147\" class=\"wp-caption alignleft\" style=\"max-width: 364px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/06/venus-global.png\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\" wp-image-73147\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/06/venus-global-800x794.png\" alt=\"Venus location map\" width=\"364\" height=\"361\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2015/06/venus-global-800x794.png 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/06/venus-global-400x397.png 400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/06/venus-global-32x32.png 32w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/06/venus-global-64x64.png 64w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/06/venus-global-96x96.png 96w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/06/venus-global-128x128.png 128w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/06/venus-global-75x75.png 75w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/06/venus-global.png 816w\" sizes=\"(max-width: 364px) 100vw, 364px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Radar map of Venus showing the location of Ganis Chasma, a large set of fissures flanking the volcano Ozza Mons, itself part of the great Aphrodite Terra volcanic structure. (NASA/JPL)\u003c/figcaption>\u003c/figure>\n\u003cp>The evidence was recorded by an infrared camera on the spacecraft Venus Express, launched by the European Space Agency in 2005. Before ending its work late last year and burning up in the Venusian atmosphere, Venus Express used its camera to study the planet at night.\u003c/p>\n\u003cp>The orbiting camera was sensitive to infrared light at wavelengths at which Venus’s atmosphere is somewhat transparent, but the pictures were like watching a scene through heavy, blowing fog. Nevertheless, it detected four different places in Ganis Chasma that were slightly hotter than their surroundings. During earlier and later visits, these hot spots were absent.\u003c/p>\n\u003cp>Shalygin and his five coauthors systematically eliminated camera errors and other explanations. They calculated that a fairly small pool of lava, maybe the size of Hawaii’s Halemaumau crater, could look like a large patch of slightly warmer temperature when seen through the blurring atmosphere of Venus. A larger flow of lava, cooling down after its eruption, would do the same.\u003c/p>\n\u003cp>The Ganis Chasma eruptions appear to resemble basaltic fissure eruptions on Earth, like those of the volcanoes of Hawaii and Iceland. Here, lava flows may take years to cool down, but the hot spots on Venus disappeared in a matter of months. The authors speculate that the dense atmosphere cools the lava quickly, just as seawater does on Earth.\u003c/p>\n\u003cfigure id=\"attachment_73148\" class=\"wp-caption alignright\" style=\"max-width: 476px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/06/venus-volcs.png\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\" wp-image-73148\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/06/venus-volcs-800x450.png\" alt=\"Eruptive hot spots, Ganis Chasma, Venus\" width=\"476\" height=\"268\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2015/06/venus-volcs-800x450.png 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/06/venus-volcs-400x225.png 400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/06/venus-volcs.png 900w\" sizes=\"(max-width: 476px) 100vw, 476px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Hot spots on Ganis Chasma recorded by Venus Express. The spots lie exactly where eruptions are expected. (Shalygin/American Geophysical Union)\u003c/figcaption>\u003c/figure>\n\u003cp>The authors recommend that we keep a close eye on Ganis Chasma and Atla Regio, the larger volcanic region of which it’s a part. Of course, there are no spacecraft at Venus at the moment. Twenty years after the Magellan mission, our current radar technology \u003ca href=\"http://www.planetary.org/blogs/guest-blogs/van-kane/20150302-understanding-venus.html\">could map Venus as well as we’re mapping Mars\u003c/a> in visible light.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>But scientists have had no luck getting a new radar mapping mission off the ground. Venus researchers, like all scientists who rely on spacecraft missions, play a high-stakes gambling game as they make funding proposals to two major sponsors: NASA and the European Space Agency. ESA just finished choosing its next set of medium-class missions, and Venus lost out in that round. Now NASA is considering 28 proposals for its next round of Discovery-class missions, and there are said to be \u003ca href=\"http://www.thespacereview.com/article/2722/1\">four Venus proposals\u003c/a> in play there.\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/science/73144/active-volcanoes-spotted-on-venus","authors":["6228"],"categories":["science_28","science_38"],"tags":["science_5195","science_944"],"featImg":"science_73146","label":"science"},"science_29080":{"type":"posts","id":"science_29080","meta":{"index":"posts_1591205157","site":"science","id":"29080","score":null,"sort":[1428591622000]},"guestAuthors":[],"slug":"the-great-1815-tambora-eruption-what-if-this-volcano-blew-today","title":"The Great 1815 Tambora Eruption: What if This Volcano Blew Today?","publishDate":1428591622,"format":"aside","headTitle":"The Great 1815 Tambora Eruption: What if This Volcano Blew Today? | KQED","labelTerm":{"site":"science"},"content":"\u003cfigure id=\"attachment_29081\" class=\"wp-caption aligncenter\" style=\"max-width: 800px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/04/tambora.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/04/tambora.jpg\" alt=\"Tambora today\" width=\"800\" height=\"449\" class=\"size-full wp-image-29081\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">When Tambora blew its top, 200 years ago this week, it left a smoking caldera behind that measures 6 kilometers across. (Jialiang Gao/Wikimedia)\u003c/figcaption>\u003c/figure>\n\u003cp>Tambora was once a tall and graceful mountain, as high as Hawaii’s great volcanoes, with a shape as classic as Fujiyama’s. Then, in \u003ca href=\"http://en.wikipedia.org/wiki/1815_eruption_of_Mount_Tambora\">a series of great eruptions\u003c/a> 200 years ago this week, it lost more than one-third of its height and covered a wide swath of today’s Indonesia in choking, toxic ash. It was the most powerful eruption of the last 1000 years, as far as we can tell—our knowledge is far from complete.\u003c/p>\n\u003cp>At the time, no one in the world was called a scientist. Electricity was a laboratory curiosity. The steam engine was bleeding-edge technology. Indonesia did not have a volcano agency, and it took months before ships brought word from the colonial Dutch East Indies to the rest of the world.\u003c/p>\n\u003cp>The news that emerged was apocalyptic. The eruption’s roar was heard a thousand miles away. The sun was entirely blotted out for days within about 400 miles of the volcano. Acid rain and layers of fine ash killed the crops, causing widespread famine and disease. Tens of thousands of people were sickened by caustic ash and sulfuric gases. Great sea waves had flooded harbors and coastlines across the East Indies.\u003c/p>\n\u003cp>Fine ash particles and clouds of sulfuric acid droplets were injected nearly 30 miles up into the stratosphere and carried around the world. The summer of 1815 was marked by persistent red skies and cold days in Europe, North America and China. The weather was even worse in 1816, recorded by history as the year without a summer. Famine in Europe continued for several years more. The decade of the 1810s, as a result, is the coldest on record.\u003c/p>\n\u003cp>Volcanologists rank Tambora’s eruption as a category 7 in their \u003ca href=\"http://volcanoes.usgs.gov/images/pglossary/vei.php\">Volcanic Eruptivity Index scale\u003c/a>. It’s the only clear-cut example on the books—so far. \u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>Americans might picture this eruption happening in, say, the Pacific Northwest states among the Cascades volcanoes. Imagine the Mount St. Helens eruption of 1980, multiplied by 100 times. We have a fairly good idea of what happened, because \u003ca href=\"http://volcanoes.usgs.gov/volcanoes/crater_lake/crater_lake_geo_hist_135.html\">it really did happen about 7700 years ago\u003c/a> to a volcano in southern Oregon called Mount Mazama. The remains of that peak are now the center of \u003ca href=\"http://www.nps.gov/crla/index.htm\">Crater Lake National Park\u003c/a>.\u003c/p>\n\u003cp>Another Tambora will happen one day, as surely as Earth is an active planet. Eruptions that size are estimated to occur roughly every thousand years, on average. The next one could happen to some other lovely large volcano tomorrow. What will be different the next time?\u003c/p>\n\u003cul>\n\u003cli>We’ll have a better idea of the coming eruption in advance. The eruption of Bardarbunga last year, in Iceland, was a good example. In the weeks beforehand, scientists followed the magma as it moved underground and shared their data online. One by one, major volcanoes like Fujiyama are being studied with \u003ca href=\"http://ww2.kqed.org/science/2015/02/06/scientists-tune-in-to-the-earths-ambient-hum/\">ambient seismic techniques\u003c/a>. As volcano scientists learn more about their subject, our foresight will increase.\u003c/li>\n\u003cli>We’ll have a better idea of the eruption’s effects. \u003ca href=\"https://eos.org/project-updates/fire-in-the-hole-recreating-volcanic-eruptions-with-cannon-blasts\">Ingenious experiments\u003c/a> are helping us define fast ways to predict things like ashfall and plug the information into robust weather models. With sound methods in place, for instance, airlines can safely avoid \u003ca href=\"http://en.wikipedia.org/wiki/British_Airways_Flight_9\">engine-killing ash clouds\u003c/a>.\u003c/li>\n\u003cli>Word will get out fast. Today satellites, seismic networks and \u003ca href=\"http://science.kqed.org/quest/2013/02/21/infrasound-takes-a-bow/\">infrasound observatories\u003c/a> will help us characterize the eruption within hours. Even before live video links are re-established from the scene, we’ll have a good idea of what’s happened.\u003c/li>\n\u003cli>\nThe world will help with rescue, relief and recovery. The United Nations, the Red Cross/Red Crescent, \u003ca href=\"http://www.directrelief.org/tag/volcano/\">Direct Relief\u003c/a> and many more agencies like them did not exist in 1815.\u003c/li>\n\u003c/ul>\n\u003cp>\u003c/p>\n\u003cp>What will be the same?\u003c/p>\n\u003cul>\n\u003cli>Many thousands of people will die. The local inhabitants, whoever they are, will take the brunt of the disaster. Nearly all of the world’s large volcanoes are in populated areas, and the world population has grown tenfold since 1815. No nation will ever be able to weather such an eruption with impunity. Total evacuation is impossible.\u003c/li>\n\u003cli>Effects will be felt for years and around the world. Neighboring nations will suffer as displaced people pour over their borders. (Consider how Mexico City being wiped out by Popocatépetl would affect the U.S.) Climate disturbance will combine with economic disruption to cause misery and political instability of global extent. It will hurt all of us.\u003c/li>\n\u003c/ul>\n\n","blocks":[],"excerpt":"Tambora brought the world a taste of apocalypse 200 years ago. Today we have better tools to monitor volcanoes like it, but the next eruption of its size will still challenge civilization.","status":"publish","parent":0,"modified":1704932020,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":10,"wordCount":769},"headData":{"title":"The Great 1815 Tambora Eruption: What if This Volcano Blew Today? | KQED","description":"Tambora brought the world a taste of apocalypse 200 years ago. Today we have better tools to monitor volcanoes like it, but the next eruption of its size will still challenge civilization.","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":"","schema":{"@context":"http://schema.org","@type":"Article","headline":"The Great 1815 Tambora Eruption: What if This Volcano Blew Today?","datePublished":"2015-04-09T15:00:22.000Z","dateModified":"2024-01-11T00:13:40.000Z","image":"https://cdn.kqed.org/wp-content/uploads/2020/02/KQED-OG-Image@1x.png"}},"sticky":false,"path":"/science/29080/the-great-1815-tambora-eruption-what-if-this-volcano-blew-today","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cfigure id=\"attachment_29081\" class=\"wp-caption aligncenter\" style=\"max-width: 800px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/04/tambora.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/04/tambora.jpg\" alt=\"Tambora today\" width=\"800\" height=\"449\" class=\"size-full wp-image-29081\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">When Tambora blew its top, 200 years ago this week, it left a smoking caldera behind that measures 6 kilometers across. (Jialiang Gao/Wikimedia)\u003c/figcaption>\u003c/figure>\n\u003cp>Tambora was once a tall and graceful mountain, as high as Hawaii’s great volcanoes, with a shape as classic as Fujiyama’s. Then, in \u003ca href=\"http://en.wikipedia.org/wiki/1815_eruption_of_Mount_Tambora\">a series of great eruptions\u003c/a> 200 years ago this week, it lost more than one-third of its height and covered a wide swath of today’s Indonesia in choking, toxic ash. It was the most powerful eruption of the last 1000 years, as far as we can tell—our knowledge is far from complete.\u003c/p>\n\u003cp>At the time, no one in the world was called a scientist. Electricity was a laboratory curiosity. The steam engine was bleeding-edge technology. Indonesia did not have a volcano agency, and it took months before ships brought word from the colonial Dutch East Indies to the rest of the world.\u003c/p>\n\u003cp>The news that emerged was apocalyptic. The eruption’s roar was heard a thousand miles away. The sun was entirely blotted out for days within about 400 miles of the volcano. Acid rain and layers of fine ash killed the crops, causing widespread famine and disease. Tens of thousands of people were sickened by caustic ash and sulfuric gases. Great sea waves had flooded harbors and coastlines across the East Indies.\u003c/p>\n\u003cp>Fine ash particles and clouds of sulfuric acid droplets were injected nearly 30 miles up into the stratosphere and carried around the world. The summer of 1815 was marked by persistent red skies and cold days in Europe, North America and China. The weather was even worse in 1816, recorded by history as the year without a summer. Famine in Europe continued for several years more. The decade of the 1810s, as a result, is the coldest on record.\u003c/p>\n\u003cp>Volcanologists rank Tambora’s eruption as a category 7 in their \u003ca href=\"http://volcanoes.usgs.gov/images/pglossary/vei.php\">Volcanic Eruptivity Index scale\u003c/a>. It’s the only clear-cut example on the books—so far. \u003c/p>\n\u003cp>\u003c/p>\u003c/div>","attributes":{"named":{},"numeric":[]}},{"type":"component","content":"","name":"ad","attributes":{"named":{"label":"fullwidth"},"numeric":["fullwidth"]}},{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>Americans might picture this eruption happening in, say, the Pacific Northwest states among the Cascades volcanoes. Imagine the Mount St. Helens eruption of 1980, multiplied by 100 times. We have a fairly good idea of what happened, because \u003ca href=\"http://volcanoes.usgs.gov/volcanoes/crater_lake/crater_lake_geo_hist_135.html\">it really did happen about 7700 years ago\u003c/a> to a volcano in southern Oregon called Mount Mazama. The remains of that peak are now the center of \u003ca href=\"http://www.nps.gov/crla/index.htm\">Crater Lake National Park\u003c/a>.\u003c/p>\n\u003cp>Another Tambora will happen one day, as surely as Earth is an active planet. Eruptions that size are estimated to occur roughly every thousand years, on average. The next one could happen to some other lovely large volcano tomorrow. What will be different the next time?\u003c/p>\n\u003cul>\n\u003cli>We’ll have a better idea of the coming eruption in advance. The eruption of Bardarbunga last year, in Iceland, was a good example. In the weeks beforehand, scientists followed the magma as it moved underground and shared their data online. One by one, major volcanoes like Fujiyama are being studied with \u003ca href=\"http://ww2.kqed.org/science/2015/02/06/scientists-tune-in-to-the-earths-ambient-hum/\">ambient seismic techniques\u003c/a>. As volcano scientists learn more about their subject, our foresight will increase.\u003c/li>\n\u003cli>We’ll have a better idea of the eruption’s effects. \u003ca href=\"https://eos.org/project-updates/fire-in-the-hole-recreating-volcanic-eruptions-with-cannon-blasts\">Ingenious experiments\u003c/a> are helping us define fast ways to predict things like ashfall and plug the information into robust weather models. With sound methods in place, for instance, airlines can safely avoid \u003ca href=\"http://en.wikipedia.org/wiki/British_Airways_Flight_9\">engine-killing ash clouds\u003c/a>.\u003c/li>\n\u003cli>Word will get out fast. Today satellites, seismic networks and \u003ca href=\"http://science.kqed.org/quest/2013/02/21/infrasound-takes-a-bow/\">infrasound observatories\u003c/a> will help us characterize the eruption within hours. Even before live video links are re-established from the scene, we’ll have a good idea of what’s happened.\u003c/li>\n\u003cli>\nThe world will help with rescue, relief and recovery. The United Nations, the Red Cross/Red Crescent, \u003ca href=\"http://www.directrelief.org/tag/volcano/\">Direct Relief\u003c/a> and many more agencies like them did not exist in 1815.\u003c/li>\n\u003c/ul>\n\u003cp>\u003c/p>\n\u003cp>What will be the same?\u003c/p>\n\u003cul>\n\u003cli>Many thousands of people will die. The local inhabitants, whoever they are, will take the brunt of the disaster. Nearly all of the world’s large volcanoes are in populated areas, and the world population has grown tenfold since 1815. No nation will ever be able to weather such an eruption with impunity. Total evacuation is impossible.\u003c/li>\n\u003cli>Effects will be felt for years and around the world. Neighboring nations will suffer as displaced people pour over their borders. (Consider how Mexico City being wiped out by Popocatépetl would affect the U.S.) Climate disturbance will combine with economic disruption to cause misery and political instability of global extent. It will hurt all of us.\u003c/li>\n\u003c/ul>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/science/29080/the-great-1815-tambora-eruption-what-if-this-volcano-blew-today","authors":["6228"],"categories":["science_35","science_38"],"tags":["science_1490","science_1999","science_944"],"featImg":"science_29081","label":"science"},"science_27882":{"type":"posts","id":"science_27882","meta":{"index":"posts_1591205157","site":"science","id":"27882","score":null,"sort":[1425607859000]},"guestAuthors":[],"slug":"volcanoes-and-lightning-make-tiny-glass-balls-together","title":"Scientists Discover Natural Glass Created by Volcanoes and Lightning","publishDate":1425607859,"format":"aside","headTitle":"Scientists Discover Natural Glass Created by Volcanoes and Lightning | KQED","labelTerm":{"site":"science"},"content":"\u003cfigure id=\"attachment_27883\" class=\"wp-caption aligncenter\" style=\"max-width: 800px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/03/galunggung-lightning-usgs.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/03/galunggung-lightning-usgs.jpg\" alt=\"Volcanic lightning can melt ash into tiny spheres of glass\" width=\"800\" height=\"450\" class=\"size-full wp-image-27883\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Volcanic lightning lashes the eruption cloud over Galunggung, in Indonesia, in this 1984 photo. This discharge of energy creates abundant tiny spheres of melted rock that mix with the ash as it settles earthward and enters the geologic cycle. (USGS) \u003ccite>(U.S. Geological Survey)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>Geologists are familiar with something most of us have never seen—spherules, or microscopic balls of natural glass that hide in sediments all over the world. A new study reports a previously unknown kind of spherule that’s forged during volcanic eruptions as lightning lashes roiling clouds of hot ash.\u003c/p>\n\u003cp>Glassy spherules occur in all kinds of places on Earth, and on the Moon, and we know several ways they’re created. Meteors make them as they burn up entering the atmosphere from space. Large meteor impacts make lots more spherules as they explode into fiery debris. The same impacts can melt the ground they strike and form \u003ca href=\"http://science.kqed.org/quest/2012/12/13/help-find-the-healdsburg-tektites/\">tektites\u003c/a>. The red-hot spray of exploding lava also can make spherules, called Pele’s spheres or achneliths. All of these spherule types are on the order of a millimeter across.\u003c/p>\n\u003cp>And we have lightning. Whether it strikes loose sediment or hard stone, lightning’s instantaneous heat, estimated at 30,000°C, can melt tubes and droplets of material into the curious features called \u003ca href=\"http://geology.about.com/od/climate_change/a/fulgurites.htm\">fulgurites\u003c/a>. Knowing this power of lightning, \u003ca href=\"http://geo.ua.edu/profile/genareau-kimberly-2/\">Kimberly Genareau\u003c/a>, a volcanologist at the University of Alabama, wondered what happens in eruption clouds of volcanic ash when lightning laces through them. What she learned is the subject of \u003ca href=\"http://geology.gsapubs.org/content/early/2015/02/26/G36255.1.abstract\">an open-access paper in the journal \u003ci>Geology\u003c/i>\u003c/a>.\u003c/p>\n\u003cp>She acquired ash from two eruptions known for their spectacular volcanic lightning displays, the 2009 eruption of Redoubt in Alaska and the 2010 eruption of Eyjafjallajokull in Iceland.\u003c/p>\n\u003cp>The ashes contained a noticeable share of glassy spherules, as much as a few percent. These looked different enough from other types of spherules for Genareau and her coauthors to declare them a new type with the workaday name of lightning-induced volcanic spherules, or LIVS.\u003c/p>\n\u003cfigure id=\"attachment_27884\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/03/LIVS.png\">\u003cimg loading=\"lazy\" decoding=\"async\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/03/LIVS.png\" alt=\"Lightning-induced volcanic spherules\" width=\"600\" height=\"248\" class=\"size-full wp-image-27884\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">LIVS from the Redoubt eruption of 2009; a singleton on the left and a cluster on the right. These are smaller than a human hair. (Genareau/GSA)\u003c/figcaption>\u003c/figure>\n\u003cp>To create spherules themselves in a laboratory setting, Genareau turned to industrial techniques. Volcanic ash does nasty things to human equipment. It scratches car windshields, clogs air filters and damages jet engines. Electrical substations rely on the insulating property of air to prevent short circuits between high-voltage fixtures, but volcanic ash mucks that up badly. \u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>Because electrical failures are a known problem after eruptions, engineers have a standard lab test for checking how high-voltage equipment performs when it’s covered in volcanic ash. It was a simple matter to adapt this test by sprinkling a large insulator with ground lava dust, wetting it, and then loading it with voltage until it zapped. This analog of natural lightning produced spherules, too.\u003c/p>\n\u003cfigure id=\"attachment_27885\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/03/pseudoLIVS.png\">\u003cimg loading=\"lazy\" decoding=\"async\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/03/pseudoLIVS.png\" alt=\"Pseudo-LIVS created in an electrical lab\" width=\"600\" height=\"251\" class=\"size-full wp-image-27885\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Pseudo-spherules from high-voltage flashover trials, a lab version of lightning-melted ash. (Genareau/GSA)\u003c/figcaption>\u003c/figure>\n\u003cp>This is a tidy piece of research that both describes a new type of natural particle and shows how to reproduce it without an erupting volcano.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>Whenever geologists detect something new in the present, they’re duty-bound to ask themselves, “What if this has gone on for millions and billions of years?” As we learn to better understand LIVS, we may find them where they’ve been hiding in plain sight, misidentified as some other kind of spherule. We now have another tool for studying prehistoric eruptions through their ash particles. And because lightning has been detected on other planets, too, who knows what mischief it’s been doing out there all this time?\u003c/p>\n\n","blocks":[],"excerpt":"Geologists are familiar with something most of us have never seen—spherules, or microscopic balls of natural glass that hide in sediments all over the world. A new study reports a previously unknown kind of spherule that’s forged during volcanic eruptions as lightning lashes roiling clouds of hot ash.","status":"publish","parent":0,"modified":1704932185,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":11,"wordCount":628},"headData":{"title":"Scientists Discover Natural Glass Created by Volcanoes and Lightning | KQED","description":"Geologists are familiar with something most of us have never seen—spherules, or microscopic balls of natural glass that hide in sediments all over the world. A new study reports a previously unknown kind of spherule that’s forged during volcanic eruptions as lightning lashes roiling clouds of hot ash.","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":"","schema":{"@context":"http://schema.org","@type":"Article","headline":"Scientists Discover Natural Glass Created by Volcanoes and Lightning","datePublished":"2015-03-06T02:10:59.000Z","dateModified":"2024-01-11T00:16:25.000Z","image":"https://cdn.kqed.org/wp-content/uploads/2020/02/KQED-OG-Image@1x.png"}},"sticky":false,"path":"/science/27882/volcanoes-and-lightning-make-tiny-glass-balls-together","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cfigure id=\"attachment_27883\" class=\"wp-caption aligncenter\" style=\"max-width: 800px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/03/galunggung-lightning-usgs.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/03/galunggung-lightning-usgs.jpg\" alt=\"Volcanic lightning can melt ash into tiny spheres of glass\" width=\"800\" height=\"450\" class=\"size-full wp-image-27883\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Volcanic lightning lashes the eruption cloud over Galunggung, in Indonesia, in this 1984 photo. This discharge of energy creates abundant tiny spheres of melted rock that mix with the ash as it settles earthward and enters the geologic cycle. (USGS) \u003ccite>(U.S. Geological Survey)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>Geologists are familiar with something most of us have never seen—spherules, or microscopic balls of natural glass that hide in sediments all over the world. A new study reports a previously unknown kind of spherule that’s forged during volcanic eruptions as lightning lashes roiling clouds of hot ash.\u003c/p>\n\u003cp>Glassy spherules occur in all kinds of places on Earth, and on the Moon, and we know several ways they’re created. Meteors make them as they burn up entering the atmosphere from space. Large meteor impacts make lots more spherules as they explode into fiery debris. The same impacts can melt the ground they strike and form \u003ca href=\"http://science.kqed.org/quest/2012/12/13/help-find-the-healdsburg-tektites/\">tektites\u003c/a>. The red-hot spray of exploding lava also can make spherules, called Pele’s spheres or achneliths. All of these spherule types are on the order of a millimeter across.\u003c/p>\n\u003cp>And we have lightning. Whether it strikes loose sediment or hard stone, lightning’s instantaneous heat, estimated at 30,000°C, can melt tubes and droplets of material into the curious features called \u003ca href=\"http://geology.about.com/od/climate_change/a/fulgurites.htm\">fulgurites\u003c/a>. Knowing this power of lightning, \u003ca href=\"http://geo.ua.edu/profile/genareau-kimberly-2/\">Kimberly Genareau\u003c/a>, a volcanologist at the University of Alabama, wondered what happens in eruption clouds of volcanic ash when lightning laces through them. What she learned is the subject of \u003ca href=\"http://geology.gsapubs.org/content/early/2015/02/26/G36255.1.abstract\">an open-access paper in the journal \u003ci>Geology\u003c/i>\u003c/a>.\u003c/p>\n\u003cp>She acquired ash from two eruptions known for their spectacular volcanic lightning displays, the 2009 eruption of Redoubt in Alaska and the 2010 eruption of Eyjafjallajokull in Iceland.\u003c/p>\n\u003cp>The ashes contained a noticeable share of glassy spherules, as much as a few percent. These looked different enough from other types of spherules for Genareau and her coauthors to declare them a new type with the workaday name of lightning-induced volcanic spherules, or LIVS.\u003c/p>\n\u003cfigure id=\"attachment_27884\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/03/LIVS.png\">\u003cimg loading=\"lazy\" decoding=\"async\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/03/LIVS.png\" alt=\"Lightning-induced volcanic spherules\" width=\"600\" height=\"248\" class=\"size-full wp-image-27884\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">LIVS from the Redoubt eruption of 2009; a singleton on the left and a cluster on the right. These are smaller than a human hair. (Genareau/GSA)\u003c/figcaption>\u003c/figure>\n\u003cp>To create spherules themselves in a laboratory setting, Genareau turned to industrial techniques. Volcanic ash does nasty things to human equipment. It scratches car windshields, clogs air filters and damages jet engines. Electrical substations rely on the insulating property of air to prevent short circuits between high-voltage fixtures, but volcanic ash mucks that up badly. \u003c/p>\n\u003cp>\u003c/p>\u003c/div>","attributes":{"named":{},"numeric":[]}},{"type":"component","content":"","name":"ad","attributes":{"named":{"label":"fullwidth"},"numeric":["fullwidth"]}},{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>Because electrical failures are a known problem after eruptions, engineers have a standard lab test for checking how high-voltage equipment performs when it’s covered in volcanic ash. It was a simple matter to adapt this test by sprinkling a large insulator with ground lava dust, wetting it, and then loading it with voltage until it zapped. This analog of natural lightning produced spherules, too.\u003c/p>\n\u003cfigure id=\"attachment_27885\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/03/pseudoLIVS.png\">\u003cimg loading=\"lazy\" decoding=\"async\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/03/pseudoLIVS.png\" alt=\"Pseudo-LIVS created in an electrical lab\" width=\"600\" height=\"251\" class=\"size-full wp-image-27885\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Pseudo-spherules from high-voltage flashover trials, a lab version of lightning-melted ash. (Genareau/GSA)\u003c/figcaption>\u003c/figure>\n\u003cp>This is a tidy piece of research that both describes a new type of natural particle and shows how to reproduce it without an erupting volcano.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>Whenever geologists detect something new in the present, they’re duty-bound to ask themselves, “What if this has gone on for millions and billions of years?” As we learn to better understand LIVS, we may find them where they’ve been hiding in plain sight, misidentified as some other kind of spherule. We now have another tool for studying prehistoric eruptions through their ash particles. And because lightning has been detected on other planets, too, who knows what mischief it’s been doing out there all this time?\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/science/27882/volcanoes-and-lightning-make-tiny-glass-balls-together","authors":["6228"],"categories":["science_38"],"tags":["science_1746","science_944"],"featImg":"science_27883","label":"science"},"science_25256":{"type":"posts","id":"science_25256","meta":{"index":"posts_1591205157","site":"science","id":"25256","score":null,"sort":[1418926172000]},"guestAuthors":[],"slug":"dinosaur-extinction-new-research-favors-volcanism-as-cause","title":"Dinosaur Extinction: New Research Favors Volcanism as Cause","publishDate":1418926172,"format":"aside","headTitle":"Dinosaur Extinction: New Research Favors Volcanism as Cause | KQED","labelTerm":{"site":"science"},"content":"\u003cfigure id=\"attachment_25257\" class=\"wp-caption aligncenter\" style=\"max-width: 800px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/12/western-ghats-hari-ratan.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/12/western-ghats-hari-ratan.jpg\" alt=\"Deccan Traps\" width=\"800\" height=\"450\" class=\"size-full wp-image-25257\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">The colossal lava beds of the Deccan Traps are well exposed in the Western Ghats range of western India. Many scientists blame them, not just the Chicxulub asteroid impact, for the demise of the dinosaurs in the so-called K-T extinction. (\u003ca href=\"https://www.flickr.com/photos/ratan/\">Hari Ratan\u003c/a>/\u003ca href=\"https://creativecommons.org/licenses/by-nc-nd/2.0/\">CC-BY-NC-ND\u003c/a>)\u003c/figcaption>\u003c/figure>\n\u003cp>What made the dinosaurs go extinct? This scientific question has been fraught with controversy since the 1800s. For a while, starting in the 1980s, it seemed like everybody had settled on one cause: an asteroid impact from outer space. That’s what the textbooks say nowadays and that’s “what everyone knows.” But researchers, most of whom have been ignored and even shouted down, have kept on collecting evidence that favors an alternative. The case for their favored cause—volcanism—is bolstered by \u003ca href=\"http://www.sciencemag.org/content/early/2014/12/10/science.aaa0118\">a paper in last week’s issue of the journal \u003ci>Science\u003c/i>\u003c/a>.\u003c/p>\n\u003cp>Dinosaur fossils appear in the rocks throughout the long Cretaceous Period, but disappear at its end approximately 66 million years ago (except for the birds, which live on today). It wasn’t just dinosaurs either: other land animals suffered too, and about half of all plant species disappeared. In the oceans, the large sea lizards known as mosasaurs vanished, along with the long-necked plesiosaurs and coiled shellfish known as ammonoids. Just as with land plants, the species of floating algae in the sea, the base of the ocean’s food web, were devastated.\u003c/p>\n\u003cp>Arguments have long raged over what caused this mass extinction, typically called the “K-T event” because it marks the boundary between the Cretaceous Period (marked “K” on geologic maps) and the Tertiary Period that followed. Changes in sea level, climate, and ocean chemistry were the preferred candidates for many decades, and studies have shown that each of these can be nasty enough to cause large waves of extinction. Other, more novel suggestions included waves of disease, bursts of supernova radiation and evolutionary chaos. \u003c/p>\n\u003cp>Around 1980, two new “bombshell” candidates arose: a gigantic episode of volcanic activity and a gigantic cosmic impact. The impact theory, invented at UC Berkeley, is \u003ca href=\"http://en.wikipedia.org/wiki/Cretaceous%E2%80%93Paleogene_extinction_event\">so well known\u003c/a> you can chat about it at parties. It’s plausible science and a great story besides. The main problem is that the K-T mass extinction appears to have started before the impact and continued after it.\u003c/p>\n\u003cp>The volcanic theory is just as plausible, especially after 30 years of research. Giant eruption episodes are blamed for causing several other mass extinctions. And lava flows built a stupendous pile of basalt the size of France, called the Deccan Traps, in the heart of India around the time of the K-T event. Large amounts of lava emit sulfur gases and carbon dioxide. Either of these gases could disturb global climate and the chemistry of the ocean. If enough lava were erupted all at once, the effects of both gases would look like an instantaneous blow in the geologic record. The main problem with the Deccan Traps is that its exact age and chronology are poorly known.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>The discussion is very complex, but the root difficulty is that in the record of the rocks, geologic time is extremely foreshortened. A bed of stone no thicker than a handspan can represent a hundred thousand years of time or more, and a massive layer hundreds of feet thick might have been the work of one catastrophic week. Microfossils are a well established yardstick in geologic time, but lava flows don’t have any. Magnetic techniques don’t work on every rock either. Isotopic methods that tell a rock’s age typically reach a precision as good as around 1 percent—but that still means uncertainties of a million years or so. \u003c/p>\n\u003cp>That’s where \u003ca href=\"http://www.sciencemag.org/content/early/2014/12/10/science.aaa0118\">the latest paper in \u003ci>Science\u003c/i>\u003c/a> comes in. \u003ca href=\"http://www.princeton.edu/geosciences/people/schoene/\">Blair Schoene\u003c/a> of Princeton University and four co-authors visited the Deccan Traps and managed to find examples of lava containing tiny crystals of the mineral zircon. These allowed them to date the rocks in Princeton’s newest lab using the uranium-lead method, the gold standard of isotopic dating. \u003c/p>\n\u003cp>Zircon is not found in basalt. Schoene’s team had to find microscopic crystals of it in scattered beds of volcanic ash, representing rare explosive eruptions of lava with a different composition. Zircon samples from high and low positions in the 10,000-foot lava pile enabled them to show that Deccan eruptions crossed the K-T boundary, lasting from about 250,000 years before it to 500,000 years afterward. \u003c/p>\n\u003cp>It’s a simple finding, but it means that the volcanism people have kicked down the door and taken seats at the table where the K-T event is being discussed. \u003c/p>\n\u003cp>The volcanic theorists have been gathering evidence for a long time. It shows that truly monstrous eruptions took place that sent lava flows entirely across the Indian subcontinent. The emissions of gases that accompanied those flows would have wrought havoc with the atmosphere, disturbed the ocean circulation, and made the extinctions of the time entirely plausible, even without a giant impact. The new dates for the volcanism jibe with microfossil evidence, making their case doubly strong.\u003c/p>\n\u003cp>Many of the impact theorists have shown a strong, almost visceral resistance to the volcanism argument. Indeed, at the meeting of the American Geophysical Union going on this week in San Francisco, a group of Berkeley scientists is presenting an argument that the worst of the Deccan eruptions was simply triggered by the impact, which leaves volcanism secondary and their favored theory supreme.\u003c/p>\n\u003cp>But the volcanic K-T hypothesis is useful science, even if it’s wrong, because today’s global warming is driven by the same processes—a geologically sudden blast of greenhouse gases. If we can model the K-T event in detail and find its predicted signs in the rocks, we can have more confidence in the models we use today to forecast global warming.\u003c/p>\n\u003cp>[ad floatright]\u003c/p>\n\u003cp>The demise of the dinosaurs could have resembled the assassination of Rasputin, who according to legend was poisoned, stabbed, shot and drowned. As one coauthor of the \u003ci>Science\u003c/i> paper, Gerta Keller, has put it \u003ca href=\"http://rock.geosociety.org/Store/detail.aspx?id=spe505\">in a recent book on the volcanic theory\u003c/a>, “Ultimately, the effects of volcanism, impacts, sea-level and climate changes (warming and cooling), ocean acidification, ocean anoxia, and atmospheric changes have to be considered in any extinction scenario in order to understand the causes and consequences of mass extinctions. Moreover, these data hold the keys to help us understand, and cope with, the looming environmental and extinction crises in the modern world.”\u003c/p>\n\n","blocks":[],"excerpt":"A new set of rock dates have pushed volcanism back into the debate over the extinction of the dinosaurs.","status":"publish","parent":0,"modified":1704932497,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":15,"wordCount":1120},"headData":{"title":"Dinosaur Extinction: New Research Favors Volcanism as Cause | KQED","description":"A new set of rock dates have pushed volcanism back into the debate over the extinction of the dinosaurs.","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":"","schema":{"@context":"http://schema.org","@type":"Article","headline":"Dinosaur Extinction: New Research Favors Volcanism as Cause","datePublished":"2014-12-18T18:09:32.000Z","dateModified":"2024-01-11T00:21:37.000Z","image":"https://cdn.kqed.org/wp-content/uploads/2020/02/KQED-OG-Image@1x.png"}},"sticky":false,"path":"/science/25256/dinosaur-extinction-new-research-favors-volcanism-as-cause","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cfigure id=\"attachment_25257\" class=\"wp-caption aligncenter\" style=\"max-width: 800px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/12/western-ghats-hari-ratan.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/12/western-ghats-hari-ratan.jpg\" alt=\"Deccan Traps\" width=\"800\" height=\"450\" class=\"size-full wp-image-25257\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">The colossal lava beds of the Deccan Traps are well exposed in the Western Ghats range of western India. Many scientists blame them, not just the Chicxulub asteroid impact, for the demise of the dinosaurs in the so-called K-T extinction. (\u003ca href=\"https://www.flickr.com/photos/ratan/\">Hari Ratan\u003c/a>/\u003ca href=\"https://creativecommons.org/licenses/by-nc-nd/2.0/\">CC-BY-NC-ND\u003c/a>)\u003c/figcaption>\u003c/figure>\n\u003cp>What made the dinosaurs go extinct? This scientific question has been fraught with controversy since the 1800s. For a while, starting in the 1980s, it seemed like everybody had settled on one cause: an asteroid impact from outer space. That’s what the textbooks say nowadays and that’s “what everyone knows.” But researchers, most of whom have been ignored and even shouted down, have kept on collecting evidence that favors an alternative. The case for their favored cause—volcanism—is bolstered by \u003ca href=\"http://www.sciencemag.org/content/early/2014/12/10/science.aaa0118\">a paper in last week’s issue of the journal \u003ci>Science\u003c/i>\u003c/a>.\u003c/p>\n\u003cp>Dinosaur fossils appear in the rocks throughout the long Cretaceous Period, but disappear at its end approximately 66 million years ago (except for the birds, which live on today). It wasn’t just dinosaurs either: other land animals suffered too, and about half of all plant species disappeared. In the oceans, the large sea lizards known as mosasaurs vanished, along with the long-necked plesiosaurs and coiled shellfish known as ammonoids. Just as with land plants, the species of floating algae in the sea, the base of the ocean’s food web, were devastated.\u003c/p>\n\u003cp>Arguments have long raged over what caused this mass extinction, typically called the “K-T event” because it marks the boundary between the Cretaceous Period (marked “K” on geologic maps) and the Tertiary Period that followed. Changes in sea level, climate, and ocean chemistry were the preferred candidates for many decades, and studies have shown that each of these can be nasty enough to cause large waves of extinction. Other, more novel suggestions included waves of disease, bursts of supernova radiation and evolutionary chaos. \u003c/p>\n\u003cp>Around 1980, two new “bombshell” candidates arose: a gigantic episode of volcanic activity and a gigantic cosmic impact. The impact theory, invented at UC Berkeley, is \u003ca href=\"http://en.wikipedia.org/wiki/Cretaceous%E2%80%93Paleogene_extinction_event\">so well known\u003c/a> you can chat about it at parties. It’s plausible science and a great story besides. The main problem is that the K-T mass extinction appears to have started before the impact and continued after it.\u003c/p>\n\u003cp>The volcanic theory is just as plausible, especially after 30 years of research. Giant eruption episodes are blamed for causing several other mass extinctions. And lava flows built a stupendous pile of basalt the size of France, called the Deccan Traps, in the heart of India around the time of the K-T event. Large amounts of lava emit sulfur gases and carbon dioxide. Either of these gases could disturb global climate and the chemistry of the ocean. If enough lava were erupted all at once, the effects of both gases would look like an instantaneous blow in the geologic record. The main problem with the Deccan Traps is that its exact age and chronology are poorly known.\u003c/p>\n\u003cp>\u003c/p>\u003c/div>","attributes":{"named":{},"numeric":[]}},{"type":"component","content":"","name":"ad","attributes":{"named":{"label":"fullwidth"},"numeric":["fullwidth"]}},{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>The discussion is very complex, but the root difficulty is that in the record of the rocks, geologic time is extremely foreshortened. A bed of stone no thicker than a handspan can represent a hundred thousand years of time or more, and a massive layer hundreds of feet thick might have been the work of one catastrophic week. Microfossils are a well established yardstick in geologic time, but lava flows don’t have any. Magnetic techniques don’t work on every rock either. Isotopic methods that tell a rock’s age typically reach a precision as good as around 1 percent—but that still means uncertainties of a million years or so. \u003c/p>\n\u003cp>That’s where \u003ca href=\"http://www.sciencemag.org/content/early/2014/12/10/science.aaa0118\">the latest paper in \u003ci>Science\u003c/i>\u003c/a> comes in. \u003ca href=\"http://www.princeton.edu/geosciences/people/schoene/\">Blair Schoene\u003c/a> of Princeton University and four co-authors visited the Deccan Traps and managed to find examples of lava containing tiny crystals of the mineral zircon. These allowed them to date the rocks in Princeton’s newest lab using the uranium-lead method, the gold standard of isotopic dating. \u003c/p>\n\u003cp>Zircon is not found in basalt. Schoene’s team had to find microscopic crystals of it in scattered beds of volcanic ash, representing rare explosive eruptions of lava with a different composition. Zircon samples from high and low positions in the 10,000-foot lava pile enabled them to show that Deccan eruptions crossed the K-T boundary, lasting from about 250,000 years before it to 500,000 years afterward. \u003c/p>\n\u003cp>It’s a simple finding, but it means that the volcanism people have kicked down the door and taken seats at the table where the K-T event is being discussed. \u003c/p>\n\u003cp>The volcanic theorists have been gathering evidence for a long time. It shows that truly monstrous eruptions took place that sent lava flows entirely across the Indian subcontinent. The emissions of gases that accompanied those flows would have wrought havoc with the atmosphere, disturbed the ocean circulation, and made the extinctions of the time entirely plausible, even without a giant impact. The new dates for the volcanism jibe with microfossil evidence, making their case doubly strong.\u003c/p>\n\u003cp>Many of the impact theorists have shown a strong, almost visceral resistance to the volcanism argument. Indeed, at the meeting of the American Geophysical Union going on this week in San Francisco, a group of Berkeley scientists is presenting an argument that the worst of the Deccan eruptions was simply triggered by the impact, which leaves volcanism secondary and their favored theory supreme.\u003c/p>\n\u003cp>But the volcanic K-T hypothesis is useful science, even if it’s wrong, because today’s global warming is driven by the same processes—a geologically sudden blast of greenhouse gases. If we can model the K-T event in detail and find its predicted signs in the rocks, we can have more confidence in the models we use today to forecast global warming.\u003c/p>\n\u003cp>\u003c/p>\u003c/div>","attributes":{"named":{},"numeric":[]}},{"type":"component","content":"","name":"ad","attributes":{"named":{"label":"floatright"},"numeric":["floatright"]}},{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>The demise of the dinosaurs could have resembled the assassination of Rasputin, who according to legend was poisoned, stabbed, shot and drowned. As one coauthor of the \u003ci>Science\u003c/i> paper, Gerta Keller, has put it \u003ca href=\"http://rock.geosociety.org/Store/detail.aspx?id=spe505\">in a recent book on the volcanic theory\u003c/a>, “Ultimately, the effects of volcanism, impacts, sea-level and climate changes (warming and cooling), ocean acidification, ocean anoxia, and atmospheric changes have to be considered in any extinction scenario in order to understand the causes and consequences of mass extinctions. Moreover, these data hold the keys to help us understand, and cope with, the looming environmental and extinction crises in the modern world.”\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/science/25256/dinosaur-extinction-new-research-favors-volcanism-as-cause","authors":["6228"],"categories":["science_38"],"tags":["science_2145","science_260","science_190","science_944"],"featImg":"science_25257","label":"science"},"science_23497":{"type":"posts","id":"science_23497","meta":{"index":"posts_1591205157","site":"science","id":"23497","score":null,"sort":[1415304611000]},"guestAuthors":[],"slug":"yosemites-tuolumne-meadows-a-long-standing-geological-puzzle","title":"Yosemite's Tuolumne Meadows: A Long-standing Geological Puzzle","publishDate":1415304611,"format":"aside","headTitle":"Yosemite’s Tuolumne Meadows: A Long-standing Geological Puzzle | KQED","labelTerm":{"term":3259,"site":"science"},"content":"\u003cfigure id=\"attachment_23500\" class=\"wp-caption aligncenter\" style=\"max-width: 800px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/11/tuolumnemeadows.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/11/tuolumnemeadows.jpg\" alt=\"Tuolumne Meadows\" width=\"800\" height=\"450\" class=\"size-full wp-image-23500\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Tuolumne Meadows is an unexpected kind of place. In a new study, geologists suggest that it exists because an accident of geologic history allowed glaciers to carve the exact same kind of rock into both flats and high blocks like Lembert Dome, shown here. (Andrew Alden photo)\u003c/figcaption>\u003c/figure>\n\u003cp>One of many iconic landscapes in Yosemite National Park is a wide-open grassy stretch mixed with high granite outcrops called Tuolumne Meadows. Millions of visitors have stopped there in wonder. Geologists love a good view as much as anyone, but sooner or later they ask themselves the strange but typical question, “How did this landscape happen?” \u003c/p>\n\u003cp>Tuolumne Meadows is a long-standing geological puzzle—a large relatively flat place in the midst of a rugged range. \u003c/p>\n\u003cfigure id=\"attachment_23502\" class=\"wp-caption aligncenter\" style=\"max-width: 550px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/11/tuolumnemeadowspng.png\">\u003cimg loading=\"lazy\" decoding=\"async\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/11/tuolumnemeadowspng.png\" alt=\"Tuolumne Meadows in Google Maps\" width=\"550\" height=\"325\" class=\"size-full wp-image-23502\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Tuolumne Meadows in Google Maps\u003c/figcaption>\u003c/figure>\n\u003cp>Like most of the high Sierra valleys, the Meadows were covered by ice age glaciers until very recently (in geologic time), just 12,000 years ago or so. So in the Sierra, the geologists’ question usually boils down to “How did the glaciers make this landscape?” At Tuolumne Meadows, their question is “How the heck?”\u003c/p>\n\u003cp>Tuolumne Meadows is geologically weird because it mixes a wide flat area, typical of weak bedrock, with big humps of clean strong stone, like Lembert Dome, exposed like sculpture in a gallery. But the whole area is in one large body of identical granite, the Cathedral Peak Granodiorite. (Granodiorite has a slightly different blend of minerals from true granite; only geologists notice. Most of the Sierra’s beautiful white “granite” is granodiorite.) The clean crags that Yosemite rock climbers love are cheek by jowl with flat, well-eroded meadows, all in the same rock. How did the glaciers carve the same stuff into such a variety of landforms?\u003c/p>\n\u003cp>Geologist Richard Becker and three colleagues have unraveled the puzzle in a new paper for \u003ci>GSA Today\u003c/i> (\u003ca href=\"http://www.geosociety.org/gsatoday/archive/24/11/abstract/i1052-5173-24-11-4.htm\">open access\u003c/a>). They say the key is the cracks in the granite.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>Long ago, for nearly a hundred million years, the land we know as the Sierra Nevada was a huge belt of volcanoes, similar to Japan today. Japan gets its volcanism as a result of plate tectonics. The Pacific plate is being pulled westward under Japan where it sinks from its own weight, and as the plate subducts, its material partially melts into water-rich, highly fluid magma that slowly moves upward to erupt in Fujiyama and hundreds of other volcanoes. \u003c/p>\n\u003cp>Deeper down, that same process creates bodies of slow-cooled granite. In California those granite bodies, which once fed magma and fluids to ancient volcanoes above them, have been uncovered by millions of years of erosion. The Cathedral Peak Granodiorite is a former intrusion of magma that solidified about 88.1 million years ago. \u003c/p>\n\u003cp>Soon afterward (85.4 million years ago) another body of granite pushed its way into the area, feeding its own generation of volcanoes as it came. Fluids rising from it through the older granite created peculiar clusters of cracks. Becker and his coauthors have described these in previous papers and given them the name of tabular fracture clusters, or TFCs.\u003c/p>\n\u003cfigure id=\"attachment_23503\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/11/tabular-fracture-cluster.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/11/tabular-fracture-cluster.jpg\" alt=\"Tabular fracture cluster\" width=\"600\" height=\"465\" class=\"size-full wp-image-23503\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Ryan Hollister’s students from Turlock High School walk in the glacially eroded trace of a tabular fracture cluster in the Bummers Flat Granodiorite near Chewing Gum Lake in the Emigrant Wilderness. (\u003ca href=\"http://www.mrhollisterphoto.com/\">Ryan Hollister\u003c/a>)\u003c/figcaption>\u003c/figure>\n\u003cp>TFCs are not like the typical cracks in granite, which are classified by geologists as joints. They’re shattered zones, tightly clustered bundles of cracks, that may be a meter wide.\u003c/p>\n\u003cfigure id=\"attachment_23504\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/11/TFC-landscape.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/11/TFC-landscape.jpg\" alt=\"TFCs in the landscape\" width=\"600\" height=\"474\" class=\"size-full wp-image-23504\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Area of abundant TFCs near Mosquito Lake, Emigrant Wilderness. Cracks in the background are joints. (\u003ca href=\"http://www.mrhollisterphoto.com/about.html\">Ryan Hollister\u003c/a>)\u003c/figcaption>\u003c/figure>\n\u003cp>The ice age glaciers found those fractures easy digging. Where TFCs are scattered, glaciers carved them into deep grooves. Where they’re closely spaced, glaciers could also break the hard rock between them and scrape the land down wholesale. Tuolumne Meadows has two large sets of abundant TFCs, arranged in different directions, that cut the granite into blocks as effectively as a knife slicing up a pan of brownies.\u003c/p>\n\u003cp>Just to make sure of their findings, Becker’s team examined another part of the Sierra, the Mono Recesses, where the granite is almost identical but where TFCs are rare. \u003c/p>\n\u003cfigure id=\"attachment_23505\" class=\"wp-caption aligncenter\" style=\"max-width: 550px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/11/monorecessespng.png\">\u003cimg loading=\"lazy\" decoding=\"async\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/11/monorecessespng.png\" alt=\"Mono Recesses in Google Maps\" width=\"550\" height=\"325\" class=\"size-full wp-image-23505\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Mono Recesses in Google Maps\u003c/figcaption>\u003c/figure>\n\u003cp>There the glaciers carved a textbook alpine terrain of narrow, U-shaped valleys—another climber’s playground—without wide meadows. \u003c/p>\n\u003cfigure id=\"attachment_23506\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/11/2nd-recess-mono-creek.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/11/2nd-recess-mono-creek.jpg\" alt=\"2nd Recess of Mono Creek\" width=\"600\" height=\"480\" class=\"size-full wp-image-23506\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">The Mono Recesses is underlain by the same granite as Tuolumne Meadows, only unfractured, yielding a typical landscape of U-shaped glacial valleys (\u003ca href=\"https://www.flickr.com/photos/mtnexplorer/\">Craig Taylor/\u003c/a>\u003ca href=\"https://creativecommons.org/licenses/by-nc-sa/2.0/\">CC-BY-NC-SA\u003c/a>)\u003c/figcaption>\u003c/figure>\n\u003cp>\u003c/p>\n\u003cp>It’s just as grand, but a different kind of beautiful. Deep events of 85 million years ago left tracks at Tuolumne Meadows that the glaciers followed as they carved a geological sculpture garden in the high Yosemite country.\u003c/p>\n\n","blocks":[],"excerpt":"The iconic Tuolumne Meadows, in the high Sierra, is a geological puzzle. A newly published study traces the roots of the meadows to an incident deep in time and deep below the ground.","status":"publish","parent":0,"modified":1704932643,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":15,"wordCount":810},"headData":{"title":"Yosemite's Tuolumne Meadows: A Long-standing Geological Puzzle | KQED","description":"The iconic Tuolumne Meadows, in the high Sierra, is a geological puzzle. A newly published study traces the roots of the meadows to an incident deep in time and deep below the ground.","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":"","schema":{"@context":"http://schema.org","@type":"Article","headline":"Yosemite's Tuolumne Meadows: A Long-standing Geological Puzzle","datePublished":"2014-11-06T20:10:11.000Z","dateModified":"2024-01-11T00:24:03.000Z","image":"https://cdn.kqed.org/wp-content/uploads/2020/02/KQED-OG-Image@1x.png"}},"sticky":false,"path":"/science/23497/yosemites-tuolumne-meadows-a-long-standing-geological-puzzle","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cfigure id=\"attachment_23500\" class=\"wp-caption aligncenter\" style=\"max-width: 800px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/11/tuolumnemeadows.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/11/tuolumnemeadows.jpg\" alt=\"Tuolumne Meadows\" width=\"800\" height=\"450\" class=\"size-full wp-image-23500\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Tuolumne Meadows is an unexpected kind of place. In a new study, geologists suggest that it exists because an accident of geologic history allowed glaciers to carve the exact same kind of rock into both flats and high blocks like Lembert Dome, shown here. (Andrew Alden photo)\u003c/figcaption>\u003c/figure>\n\u003cp>One of many iconic landscapes in Yosemite National Park is a wide-open grassy stretch mixed with high granite outcrops called Tuolumne Meadows. Millions of visitors have stopped there in wonder. Geologists love a good view as much as anyone, but sooner or later they ask themselves the strange but typical question, “How did this landscape happen?” \u003c/p>\n\u003cp>Tuolumne Meadows is a long-standing geological puzzle—a large relatively flat place in the midst of a rugged range. \u003c/p>\n\u003cfigure id=\"attachment_23502\" class=\"wp-caption aligncenter\" style=\"max-width: 550px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/11/tuolumnemeadowspng.png\">\u003cimg loading=\"lazy\" decoding=\"async\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/11/tuolumnemeadowspng.png\" alt=\"Tuolumne Meadows in Google Maps\" width=\"550\" height=\"325\" class=\"size-full wp-image-23502\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Tuolumne Meadows in Google Maps\u003c/figcaption>\u003c/figure>\n\u003cp>Like most of the high Sierra valleys, the Meadows were covered by ice age glaciers until very recently (in geologic time), just 12,000 years ago or so. So in the Sierra, the geologists’ question usually boils down to “How did the glaciers make this landscape?” At Tuolumne Meadows, their question is “How the heck?”\u003c/p>\n\u003cp>Tuolumne Meadows is geologically weird because it mixes a wide flat area, typical of weak bedrock, with big humps of clean strong stone, like Lembert Dome, exposed like sculpture in a gallery. But the whole area is in one large body of identical granite, the Cathedral Peak Granodiorite. (Granodiorite has a slightly different blend of minerals from true granite; only geologists notice. Most of the Sierra’s beautiful white “granite” is granodiorite.) The clean crags that Yosemite rock climbers love are cheek by jowl with flat, well-eroded meadows, all in the same rock. How did the glaciers carve the same stuff into such a variety of landforms?\u003c/p>\n\u003cp>Geologist Richard Becker and three colleagues have unraveled the puzzle in a new paper for \u003ci>GSA Today\u003c/i> (\u003ca href=\"http://www.geosociety.org/gsatoday/archive/24/11/abstract/i1052-5173-24-11-4.htm\">open access\u003c/a>). They say the key is the cracks in the granite.\u003c/p>\n\u003cp>\u003c/p>\u003c/div>","attributes":{"named":{},"numeric":[]}},{"type":"component","content":"","name":"ad","attributes":{"named":{"label":"fullwidth"},"numeric":["fullwidth"]}},{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>Long ago, for nearly a hundred million years, the land we know as the Sierra Nevada was a huge belt of volcanoes, similar to Japan today. Japan gets its volcanism as a result of plate tectonics. The Pacific plate is being pulled westward under Japan where it sinks from its own weight, and as the plate subducts, its material partially melts into water-rich, highly fluid magma that slowly moves upward to erupt in Fujiyama and hundreds of other volcanoes. \u003c/p>\n\u003cp>Deeper down, that same process creates bodies of slow-cooled granite. In California those granite bodies, which once fed magma and fluids to ancient volcanoes above them, have been uncovered by millions of years of erosion. The Cathedral Peak Granodiorite is a former intrusion of magma that solidified about 88.1 million years ago. \u003c/p>\n\u003cp>Soon afterward (85.4 million years ago) another body of granite pushed its way into the area, feeding its own generation of volcanoes as it came. Fluids rising from it through the older granite created peculiar clusters of cracks. Becker and his coauthors have described these in previous papers and given them the name of tabular fracture clusters, or TFCs.\u003c/p>\n\u003cfigure id=\"attachment_23503\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/11/tabular-fracture-cluster.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/11/tabular-fracture-cluster.jpg\" alt=\"Tabular fracture cluster\" width=\"600\" height=\"465\" class=\"size-full wp-image-23503\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Ryan Hollister’s students from Turlock High School walk in the glacially eroded trace of a tabular fracture cluster in the Bummers Flat Granodiorite near Chewing Gum Lake in the Emigrant Wilderness. (\u003ca href=\"http://www.mrhollisterphoto.com/\">Ryan Hollister\u003c/a>)\u003c/figcaption>\u003c/figure>\n\u003cp>TFCs are not like the typical cracks in granite, which are classified by geologists as joints. They’re shattered zones, tightly clustered bundles of cracks, that may be a meter wide.\u003c/p>\n\u003cfigure id=\"attachment_23504\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/11/TFC-landscape.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/11/TFC-landscape.jpg\" alt=\"TFCs in the landscape\" width=\"600\" height=\"474\" class=\"size-full wp-image-23504\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Area of abundant TFCs near Mosquito Lake, Emigrant Wilderness. Cracks in the background are joints. (\u003ca href=\"http://www.mrhollisterphoto.com/about.html\">Ryan Hollister\u003c/a>)\u003c/figcaption>\u003c/figure>\n\u003cp>The ice age glaciers found those fractures easy digging. Where TFCs are scattered, glaciers carved them into deep grooves. Where they’re closely spaced, glaciers could also break the hard rock between them and scrape the land down wholesale. Tuolumne Meadows has two large sets of abundant TFCs, arranged in different directions, that cut the granite into blocks as effectively as a knife slicing up a pan of brownies.\u003c/p>\n\u003cp>Just to make sure of their findings, Becker’s team examined another part of the Sierra, the Mono Recesses, where the granite is almost identical but where TFCs are rare. \u003c/p>\n\u003cfigure id=\"attachment_23505\" class=\"wp-caption aligncenter\" style=\"max-width: 550px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/11/monorecessespng.png\">\u003cimg loading=\"lazy\" decoding=\"async\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/11/monorecessespng.png\" alt=\"Mono Recesses in Google Maps\" width=\"550\" height=\"325\" class=\"size-full wp-image-23505\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Mono Recesses in Google Maps\u003c/figcaption>\u003c/figure>\n\u003cp>There the glaciers carved a textbook alpine terrain of narrow, U-shaped valleys—another climber’s playground—without wide meadows. \u003c/p>\n\u003cfigure id=\"attachment_23506\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/11/2nd-recess-mono-creek.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/11/2nd-recess-mono-creek.jpg\" alt=\"2nd Recess of Mono Creek\" width=\"600\" height=\"480\" class=\"size-full wp-image-23506\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">The Mono Recesses is underlain by the same granite as Tuolumne Meadows, only unfractured, yielding a typical landscape of U-shaped glacial valleys (\u003ca href=\"https://www.flickr.com/photos/mtnexplorer/\">Craig Taylor/\u003c/a>\u003ca href=\"https://creativecommons.org/licenses/by-nc-sa/2.0/\">CC-BY-NC-SA\u003c/a>)\u003c/figcaption>\u003c/figure>\n\u003cp>\u003c/p>\n\u003cp>It’s just as grand, but a different kind of beautiful. Deep events of 85 million years ago left tracks at Tuolumne Meadows that the glaciers followed as they carved a geological sculpture garden in the high Yosemite country.\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/science/23497/yosemites-tuolumne-meadows-a-long-standing-geological-puzzle","authors":["6228"],"series":["science_3259"],"categories":["science_38"],"tags":["science_591","science_109","science_944","science_159"],"featImg":"science_23500","label":"science_3259"},"science_17905":{"type":"posts","id":"science_17905","meta":{"index":"posts_1591205157","site":"science","id":"17905","score":null,"sort":[1401804005000]},"guestAuthors":[],"slug":"famous-sunset-paintings-reflect-key-air-pollution-events-from-the-past","title":"Famous Sunset Paintings Reflect Key Air Pollution Events From the Past","publishDate":1401804005,"format":"aside","headTitle":"Famous Sunset Paintings Reflect Key Air Pollution Events From the Past | KQED","labelTerm":{"site":"science"},"content":"\u003cfigure id=\"attachment_17934\" class=\"wp-caption alignleft\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/06/sf-sunset.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-17934\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/06/sf-sunset.jpg\" alt=\"San Francisco sunset\" width=\"640\" height=\"360\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">A San Francisco sunset. (KP Tripathi/\u003ca title=\"Flickr - KP Tripathi\" href=\"https://www.flickr.com/photos/kptripathi/\">Flickr\u003c/a>)\u003c/figcaption>\u003c/figure>\n\u003cp>Last month the Bay Area saw 2014’s first \u003ca title=\"SF Gate - Spare the Air\" href=\"http://blog.sfgate.com/stew/2014/05/12/spare-the-air-advisory-issued-for-bay-area/\">Spare the Air alert\u003c/a>, even as we face an extra-dry \u003ca title=\"NBC - Gov Warns of Fire Season\" href=\"http://www.nbcbayarea.com/news/local/Gov-Jerry-Brown-Says-California-Bracing-for-Its-Toughest-Fire-Season-259736811.html\">fire season\u003c/a> with prospects of worsening air quality. On the bright side, we’re in for some beautiful sunsets! Air pollution scatters light, producing vivid reds that have been faithfully captured by landscape painters over the last 500 years.\u003c/p>\n\u003cp>Researchers in Greece \u003ca title=\"J Atmos Chem Phys - Environmental Information in Paintings\" href=\"http://www.atmos-chem-phys.net/14/2987/2014/acp-14-2987-2014.pdf\">recently found\u003c/a> that sunset paintings by artists such as \u003ca title=\"J.M.W. Turner - Wikipedia\" href=\"http://en.wikipedia.org/wiki/J._M._W._Turner\">J.M.W. Turner\u003c/a> and \u003ca title=\"Edgar Degas\" href=\"http://www.edgar-degas.org/\">Edgar Degas\u003c/a> accurately reflect contemporary pollution events—specifically, the 54 major volcanic eruptions since 1522. As the industrial age dawned and man-made particles began to fill the air, the paintings tracked that too.\u003c/p>\n\u003cp>\u003cb>Volcano vs. Human\u003cbr>\n\u003c/b>\u003c/p>\n\u003cfigure id=\"attachment_17907\" class=\"wp-caption alignleft\" style=\"max-width: 206px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/05/degas-race-horses-206x162.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-medium wp-image-17907\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/05/degas-race-horses-206x162.jpg\" alt='Edgar Degas, \"Race Horses\"' width=\"206\" height=\"162\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">“Race Horses,” painted by Edgar Degas in 1885, shows a sky reddened by volcanic ash from Krakatoa.\u003c/figcaption>\u003c/figure>\n\u003cp>Volcanoes were polluting the air and altering the global climate long before we humans got in on the act—and they haven’t slowed down since our arrival. Fallout from the catastrophic \u003ca title=\"Wikipedia - 1883 Krakatoa\" href=\"http://en.wikipedia.org/wiki/1883_eruption_of_Krakatoa\">1883 explosion of Krakatoa\u003c/a> in Indonesia colored skies on the other side of the world and cooled the entire planet. But these dramatic effects are short-lived; after a few years the ash clears and the weather returns to normal.\u003c/p>\n\u003cp>Human air pollution is more insidious, a gradual accumulation of emissions rather than a great big geologic belch. But the changes wrought are harder to reverse. Generation after generation of city-dwellers suffer from breathing ground-level contaminants, while other chemicals contribute to the greenhouse effect and waft up to corrode the ozone layer.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>\u003ca title=\"Christos S. Zerefos\" href=\"http://www.zerefos.gr/en/\">Christos S. Zerefos\u003c/a>, a professor at the Academy of Athens who led the study on pollution in paintings, actually began his career researching \u003ca title=\"Ozone Depletion - Wikipedia\" href=\"http://en.wikipedia.org/wiki/Ozone_depletion\">ozone depletion\u003c/a>. His work helped bring the resulting increase in UV radiation to the world’s attention. This latest paper may seem whimsical by contrast, but in fact a new source of historical data could help guide today’s climate models.\u003c/p>\n\u003cp>\u003cb>Gleaning Science from Art\u003c/b>\u003c/p>\n\u003cfigure id=\"attachment_17908\" class=\"wp-caption alignright\" style=\"max-width: 219px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/05/greifswald-moonlight-219x162.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-medium wp-image-17908\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/05/greifswald-moonlight-219x162.jpg\" alt='\"Griefswald in the Moonlight,\" painted by Caspar David Friedrich' width=\"219\" height=\"162\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">“Griefswald in the Moonlight,” painted by Caspar David Friedrich in 1817, with averaged R/G ratios indicating air pollution levels. (Zerefos et al., 2014, Atmos. Chem. Phys.)\u003c/figcaption>\u003c/figure>\n\u003cp>How do you turn paintings into data? Zerefos and his colleagues started with a digitized version of each painting. They selected a rectangle of cloudless sky at the horizon, and calculated the average amount of red, green, and blue within. Then they divided red by green, because we humans recognize “redness” in part \u003ca title=\"Color vision opponent process - Wikipedia\" href=\"http://en.wikipedia.org/wiki/Opponent_process\">by contrasting it\u003c/a> with “greenness.”\u003c/p>\n\u003cp>This R/G ratio was then used to calculate pollution: specifically, how many tiny particles called aerosols are suspended in the air. Aerosols are produced both by nature (dust storms, volcanoes, wildfires) and by humans (cars, factories, land-clearing fires). Complicating matters is the fact that human-induced climate change can increase dust storms and wildfires . . . Fortunately, the causes don’t matter to the calculation.\u003c/p>\n\u003cp>\u003ca title=\"Aerosol Optical Depth - NASA\" href=\"http://earthobservatory.nasa.gov/GlobalMaps/view.php?d1=MODAL2_M_AER_OD\">Aerosol optical depth\u003c/a>, or AOD, simply measures how polluted the air is at a given time and place, regardless of the pollution’s origin. The researchers were able to use the R/G ratios from the sunset paintings to predict the AOD of the air at the time of painting: a redder sunset means a higher AOD.\u003c/p>\n\u003cp>\u003cb>Finding Proof in Ice and Dust\u003c/b>\u003c/p>\n\u003cp>These AOD values were then compared to independent measurements of atmospheric pollution that covered the same time range as the paintings, such as \u003ca title=\"Ice Cores 101\" href=\"http://climatechange.umaine.edu/icecores/IceCore/Ice_Core_101.html\">ice cores\u003c/a>. Aerosols are deposited in snow on glaciers, which turns into a new layer of ice. Drilling down from the surface to sample these deeper, older layers provides information about historical air quality—which matched the data from the paintings.\u003c/p>\n\u003cfigure id=\"attachment_17909\" class=\"wp-caption alignleft\" style=\"max-width: 242px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/05/1024px-Sakurajima_at_Sunset-242x162.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-medium wp-image-17909\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/05/1024px-Sakurajima_at_Sunset-242x162.jpg\" alt=\"Sakurajima, one of the most active volcanoes in the world\" width=\"242\" height=\"162\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Sakurajima, one of the most active volcanoes in the world. (Kimon Berlin/\u003ca title=\"Flickr - Kimon Berlin\" href=\"https://www.flickr.com/photos/kimon/\">Flickr\u003c/a>)\u003c/figcaption>\u003c/figure>\n\u003cp>Zerefos and his colleagues also tested their painting-to-pollution technique with a modern experiment. While a dust cloud from the Sahara was passing through the sky, they asked a contemporary landscape painter to record the sunset. He did it again after the dust cloud had passed. Although the artist was unaware of the atmospheric changes, the R/G ratios in his two paintings matched independent measurements of AOD during and after the dust cloud.\u003c/p>\n\u003cp>Paintings as a new source of historical data could help scientists better understand the effects of current and future pollution, including climate change. The amount of aerosols in the atmosphere is integral to climate models. A new way of estimating aerosols in the past might help make more accurate predictions for the future.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>And the fact that Edgar Degas accidentally encoded atmospheric data in “Race Horses” is just really darn cool.\u003c/p>\n\n","blocks":[],"excerpt":"Data about volcanic eruptions and industrial pollution are encoded in great works of art.","status":"publish","parent":0,"modified":1704933551,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":17,"wordCount":804},"headData":{"title":"Famous Sunset Paintings Reflect Key Air Pollution Events From the Past | KQED","description":"Data about volcanic eruptions and industrial pollution are encoded in great works of art.","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":"","schema":{"@context":"http://schema.org","@type":"Article","headline":"Famous Sunset Paintings Reflect Key Air Pollution Events From the Past","datePublished":"2014-06-03T14:00:05.000Z","dateModified":"2024-01-11T00:39:11.000Z","image":"https://cdn.kqed.org/wp-content/uploads/2020/02/KQED-OG-Image@1x.png"}},"sticky":false,"path":"/science/17905/famous-sunset-paintings-reflect-key-air-pollution-events-from-the-past","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cfigure id=\"attachment_17934\" class=\"wp-caption alignleft\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/06/sf-sunset.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-17934\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/06/sf-sunset.jpg\" alt=\"San Francisco sunset\" width=\"640\" height=\"360\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">A San Francisco sunset. (KP Tripathi/\u003ca title=\"Flickr - KP Tripathi\" href=\"https://www.flickr.com/photos/kptripathi/\">Flickr\u003c/a>)\u003c/figcaption>\u003c/figure>\n\u003cp>Last month the Bay Area saw 2014’s first \u003ca title=\"SF Gate - Spare the Air\" href=\"http://blog.sfgate.com/stew/2014/05/12/spare-the-air-advisory-issued-for-bay-area/\">Spare the Air alert\u003c/a>, even as we face an extra-dry \u003ca title=\"NBC - Gov Warns of Fire Season\" href=\"http://www.nbcbayarea.com/news/local/Gov-Jerry-Brown-Says-California-Bracing-for-Its-Toughest-Fire-Season-259736811.html\">fire season\u003c/a> with prospects of worsening air quality. On the bright side, we’re in for some beautiful sunsets! Air pollution scatters light, producing vivid reds that have been faithfully captured by landscape painters over the last 500 years.\u003c/p>\n\u003cp>Researchers in Greece \u003ca title=\"J Atmos Chem Phys - Environmental Information in Paintings\" href=\"http://www.atmos-chem-phys.net/14/2987/2014/acp-14-2987-2014.pdf\">recently found\u003c/a> that sunset paintings by artists such as \u003ca title=\"J.M.W. Turner - Wikipedia\" href=\"http://en.wikipedia.org/wiki/J._M._W._Turner\">J.M.W. Turner\u003c/a> and \u003ca title=\"Edgar Degas\" href=\"http://www.edgar-degas.org/\">Edgar Degas\u003c/a> accurately reflect contemporary pollution events—specifically, the 54 major volcanic eruptions since 1522. As the industrial age dawned and man-made particles began to fill the air, the paintings tracked that too.\u003c/p>\n\u003cp>\u003cb>Volcano vs. Human\u003cbr>\n\u003c/b>\u003c/p>\n\u003cfigure id=\"attachment_17907\" class=\"wp-caption alignleft\" style=\"max-width: 206px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/05/degas-race-horses-206x162.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-medium wp-image-17907\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/05/degas-race-horses-206x162.jpg\" alt='Edgar Degas, \"Race Horses\"' width=\"206\" height=\"162\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">“Race Horses,” painted by Edgar Degas in 1885, shows a sky reddened by volcanic ash from Krakatoa.\u003c/figcaption>\u003c/figure>\n\u003cp>Volcanoes were polluting the air and altering the global climate long before we humans got in on the act—and they haven’t slowed down since our arrival. Fallout from the catastrophic \u003ca title=\"Wikipedia - 1883 Krakatoa\" href=\"http://en.wikipedia.org/wiki/1883_eruption_of_Krakatoa\">1883 explosion of Krakatoa\u003c/a> in Indonesia colored skies on the other side of the world and cooled the entire planet. But these dramatic effects are short-lived; after a few years the ash clears and the weather returns to normal.\u003c/p>\n\u003cp>Human air pollution is more insidious, a gradual accumulation of emissions rather than a great big geologic belch. But the changes wrought are harder to reverse. Generation after generation of city-dwellers suffer from breathing ground-level contaminants, while other chemicals contribute to the greenhouse effect and waft up to corrode the ozone layer.\u003c/p>\n\u003cp>\u003c/p>\u003c/div>","attributes":{"named":{},"numeric":[]}},{"type":"component","content":"","name":"ad","attributes":{"named":{"label":"fullwidth"},"numeric":["fullwidth"]}},{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>\u003ca title=\"Christos S. Zerefos\" href=\"http://www.zerefos.gr/en/\">Christos S. Zerefos\u003c/a>, a professor at the Academy of Athens who led the study on pollution in paintings, actually began his career researching \u003ca title=\"Ozone Depletion - Wikipedia\" href=\"http://en.wikipedia.org/wiki/Ozone_depletion\">ozone depletion\u003c/a>. His work helped bring the resulting increase in UV radiation to the world’s attention. This latest paper may seem whimsical by contrast, but in fact a new source of historical data could help guide today’s climate models.\u003c/p>\n\u003cp>\u003cb>Gleaning Science from Art\u003c/b>\u003c/p>\n\u003cfigure id=\"attachment_17908\" class=\"wp-caption alignright\" style=\"max-width: 219px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/05/greifswald-moonlight-219x162.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-medium wp-image-17908\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/05/greifswald-moonlight-219x162.jpg\" alt='\"Griefswald in the Moonlight,\" painted by Caspar David Friedrich' width=\"219\" height=\"162\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">“Griefswald in the Moonlight,” painted by Caspar David Friedrich in 1817, with averaged R/G ratios indicating air pollution levels. (Zerefos et al., 2014, Atmos. Chem. Phys.)\u003c/figcaption>\u003c/figure>\n\u003cp>How do you turn paintings into data? Zerefos and his colleagues started with a digitized version of each painting. They selected a rectangle of cloudless sky at the horizon, and calculated the average amount of red, green, and blue within. Then they divided red by green, because we humans recognize “redness” in part \u003ca title=\"Color vision opponent process - Wikipedia\" href=\"http://en.wikipedia.org/wiki/Opponent_process\">by contrasting it\u003c/a> with “greenness.”\u003c/p>\n\u003cp>This R/G ratio was then used to calculate pollution: specifically, how many tiny particles called aerosols are suspended in the air. Aerosols are produced both by nature (dust storms, volcanoes, wildfires) and by humans (cars, factories, land-clearing fires). Complicating matters is the fact that human-induced climate change can increase dust storms and wildfires . . . Fortunately, the causes don’t matter to the calculation.\u003c/p>\n\u003cp>\u003ca title=\"Aerosol Optical Depth - NASA\" href=\"http://earthobservatory.nasa.gov/GlobalMaps/view.php?d1=MODAL2_M_AER_OD\">Aerosol optical depth\u003c/a>, or AOD, simply measures how polluted the air is at a given time and place, regardless of the pollution’s origin. The researchers were able to use the R/G ratios from the sunset paintings to predict the AOD of the air at the time of painting: a redder sunset means a higher AOD.\u003c/p>\n\u003cp>\u003cb>Finding Proof in Ice and Dust\u003c/b>\u003c/p>\n\u003cp>These AOD values were then compared to independent measurements of atmospheric pollution that covered the same time range as the paintings, such as \u003ca title=\"Ice Cores 101\" href=\"http://climatechange.umaine.edu/icecores/IceCore/Ice_Core_101.html\">ice cores\u003c/a>. Aerosols are deposited in snow on glaciers, which turns into a new layer of ice. Drilling down from the surface to sample these deeper, older layers provides information about historical air quality—which matched the data from the paintings.\u003c/p>\n\u003cfigure id=\"attachment_17909\" class=\"wp-caption alignleft\" style=\"max-width: 242px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/05/1024px-Sakurajima_at_Sunset-242x162.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-medium wp-image-17909\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2014/05/1024px-Sakurajima_at_Sunset-242x162.jpg\" alt=\"Sakurajima, one of the most active volcanoes in the world\" width=\"242\" height=\"162\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Sakurajima, one of the most active volcanoes in the world. (Kimon Berlin/\u003ca title=\"Flickr - Kimon Berlin\" href=\"https://www.flickr.com/photos/kimon/\">Flickr\u003c/a>)\u003c/figcaption>\u003c/figure>\n\u003cp>Zerefos and his colleagues also tested their painting-to-pollution technique with a modern experiment. While a dust cloud from the Sahara was passing through the sky, they asked a contemporary landscape painter to record the sunset. He did it again after the dust cloud had passed. Although the artist was unaware of the atmospheric changes, the R/G ratios in his two paintings matched independent measurements of AOD during and after the dust cloud.\u003c/p>\n\u003cp>Paintings as a new source of historical data could help scientists better understand the effects of current and future pollution, including climate change. The amount of aerosols in the atmosphere is integral to climate models. A new way of estimating aerosols in the past might help make more accurate predictions for the future.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>And the fact that Edgar Degas accidentally encoded atmospheric data in “Race Horses” is just really darn cool.\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/science/17905/famous-sunset-paintings-reflect-key-air-pollution-events-from-the-past","authors":["6324"],"categories":["science_31"],"tags":["science_505","science_635","science_194","science_944"],"featImg":"science_17934","label":"science"}},"programsReducer":{"possible":{"id":"possible","title":"Possible","info":"Possible is hosted by entrepreneur Reid Hoffman and writer Aria Finger. Together in Possible, Hoffman and Finger lead enlightening discussions about building a brighter collective future. The show features interviews with visionary guests like Trevor Noah, Sam Altman and Janette Sadik-Khan. Possible paints an optimistic portrait of the world we can create through science, policy, business, art and our shared humanity. It asks: What if everything goes right for once? How can we get there? 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You ask the questions. You decide what Bay Curious investigates. And you join us on the journey to find the answers.","imageSrc":"https://cdn.kqed.org/wp-content/uploads/2024/04/Bay-Curious-Podcast-Tile-703x703-1.jpg","imageAlt":"\"KQED Bay Curious","officialWebsiteLink":"/news/series/baycurious","meta":{"site":"news","source":"kqed","order":"4"},"link":"/podcasts/baycurious","subscribe":{"apple":"https://podcasts.apple.com/us/podcast/bay-curious/id1172473406","npr":"https://www.npr.org/podcasts/500557090/bay-curious","rss":"https://ww2.kqed.org/news/category/bay-curious-podcast/feed/podcast","google":"https://podcasts.google.com/feed/aHR0cHM6Ly93dzIua3FlZC5vcmcvbmV3cy9jYXRlZ29yeS9iYXktY3VyaW91cy1wb2RjYXN0L2ZlZWQvcG9kY2FzdA","stitcher":"https://www.stitcher.com/podcast/kqed/bay-curious","spotify":"https://open.spotify.com/show/6O76IdmhixfijmhTZLIJ8k"}},"bbc-world-service":{"id":"bbc-world-service","title":"BBC World Service","info":"The day's top stories from BBC News compiled twice daily in the week, once at weekends.","airtime":"MON-FRI 9pm-10pm, TUE-FRI 1am-2am","imageSrc":"https://cdn.kqed.org/wp-content/uploads/2024/04/BBC-World-Service-Podcast-Tile-360x360-1.jpg","officialWebsiteLink":"https://www.bbc.co.uk/sounds/play/live:bbc_world_service","meta":{"site":"news","source":"BBC World Service"},"link":"/radio/program/bbc-world-service","subscribe":{"apple":"https://itunes.apple.com/us/podcast/global-news-podcast/id135067274?mt=2","tuneIn":"https://tunein.com/radio/BBC-World-Service-p455581/","rss":"https://podcasts.files.bbci.co.uk/p02nq0gn.rss"}},"code-switch-life-kit":{"id":"code-switch-life-kit","title":"Code Switch / Life Kit","info":"\u003cem>Code Switch\u003c/em>, which listeners will hear in the first part of the hour, has fearless and much-needed conversations about race. Hosted by journalists of color, the show tackles the subject of race head-on, exploring how it impacts every part of society — from politics and pop culture to history, sports and more.\u003cbr />\u003cbr />\u003cem>Life Kit\u003c/em>, which will be in the second part of the hour, guides you through spaces and feelings no one prepares you for — from finances to mental health, from workplace microaggressions to imposter syndrome, from relationships to parenting. The show features experts with real world experience and shares their knowledge. Because everyone needs a little help being human.\u003cbr />\u003cbr />\u003ca href=\"https://www.npr.org/podcasts/510312/codeswitch\">\u003cem>Code Switch\u003c/em> offical site and podcast\u003c/a>\u003cbr />\u003ca href=\"https://www.npr.org/lifekit\">\u003cem>Life Kit\u003c/em> offical site and podcast\u003c/a>\u003cbr />","airtime":"SUN 9pm-10pm","imageSrc":"https://cdn.kqed.org/wp-content/uploads/2024/04/Code-Switch-Life-Kit-Podcast-Tile-360x360-1.jpg","meta":{"site":"radio","source":"npr"},"link":"/radio/program/code-switch-life-kit","subscribe":{"apple":"https://podcasts.apple.com/podcast/1112190608?mt=2&at=11l79Y&ct=nprdirectory","google":"https://podcasts.google.com/feed/aHR0cHM6Ly93d3cubnByLm9yZy9yc3MvcG9kY2FzdC5waHA_aWQ9NTEwMzEy","spotify":"https://open.spotify.com/show/3bExJ9JQpkwNhoHvaIIuyV","rss":"https://feeds.npr.org/510312/podcast.xml"}},"commonwealth-club":{"id":"commonwealth-club","title":"Commonwealth Club of California Podcast","info":"The Commonwealth Club of California is the nation's oldest and largest public affairs forum. As a non-partisan forum, The Club brings to the public airwaves diverse viewpoints on important topics. The Club's weekly radio broadcast - the oldest in the U.S., dating back to 1924 - is carried across the nation on public radio stations and is now podcasting. Our website archive features audio of our recent programs, as well as selected speeches from our long and distinguished history. This podcast feed is usually updated twice a week and is always un-edited.","airtime":"THU 10pm, FRI 1am","imageSrc":"https://cdn.kqed.org/wp-content/uploads/2024/04/Commonwealth-Club-Podcast-Tile-360x360-1.jpg","officialWebsiteLink":"https://www.commonwealthclub.org/podcasts","meta":{"site":"news","source":"Commonwealth Club of California"},"link":"/radio/program/commonwealth-club","subscribe":{"apple":"https://itunes.apple.com/us/podcast/commonwealth-club-of-california-podcast/id976334034?mt=2","google":"https://podcasts.google.com/feed/aHR0cDovL3d3dy5jb21tb253ZWFsdGhjbHViLm9yZy9hdWRpby9wb2RjYXN0L3dlZWtseS54bWw","tuneIn":"https://tunein.com/radio/Commonwealth-Club-of-California-p1060/"}},"considerthis":{"id":"considerthis","title":"Consider This","tagline":"Make sense of the day","info":"Make sense of the day. Every weekday afternoon, Consider This helps you consider the major stories of the day in less than 15 minutes, featuring the reporting and storytelling resources of NPR. Plus, KQED’s Bianca Taylor brings you the local KQED news you need to know.","imageSrc":"https://cdn.kqed.org/wp-content/uploads/2024/04/Consider-This-Podcast-Tile-703x703-1.jpg","imageAlt":"Consider This from NPR and KQED","officialWebsiteLink":"/podcasts/considerthis","meta":{"site":"news","source":"kqed","order":"7"},"link":"/podcasts/considerthis","subscribe":{"apple":"https://podcasts.apple.com/podcast/id1503226625?mt=2&at=11l79Y&ct=nprdirectory","npr":"https://rpb3r.app.goo.gl/coronavirusdaily","google":"https://podcasts.google.com/feed/aHR0cHM6Ly9mZWVkcy5ucHIub3JnLzUxMDM1NS9wb2RjYXN0LnhtbA","spotify":"https://open.spotify.com/show/3Z6JdCS2d0eFEpXHKI6WqH"}},"forum":{"id":"forum","title":"Forum","tagline":"The conversation starts here","info":"KQED’s live call-in program discussing local, state, national and international issues, as well as in-depth interviews.","airtime":"MON-FRI 9am-11am, 10pm-11pm","imageSrc":"https://cdn.kqed.org/wp-content/uploads/2024/04/Forum-Podcast-Tile-703x703-1.jpg","imageAlt":"KQED Forum with Mina Kim and Alexis Madrigal","officialWebsiteLink":"/forum","meta":{"site":"news","source":"kqed","order":"8"},"link":"/forum","subscribe":{"apple":"https://podcasts.apple.com/us/podcast/kqeds-forum/id73329719","google":"https://podcasts.google.com/feed/aHR0cHM6Ly9mZWVkcy5tZWdhcGhvbmUuZm0vS1FJTkM5NTU3MzgxNjMz","npr":"https://www.npr.org/podcasts/432307980/forum","stitcher":"https://www.stitcher.com/podcast/kqedfm-kqeds-forum-podcast","rss":"https://feeds.megaphone.fm/KQINC9557381633"}},"freakonomics-radio":{"id":"freakonomics-radio","title":"Freakonomics Radio","info":"Freakonomics Radio is a one-hour award-winning podcast and public-radio project hosted by Stephen Dubner, with co-author Steve Levitt as a regular guest. 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Hosted by Robin Young, Jeremy Hobson and Tonya Mosley.","airtime":"MON-THU 11am-12pm","imageSrc":"https://cdn.kqed.org/wp-content/uploads/2024/04/Here-And-Now-Podcast-Tile-360x360-1.jpg","officialWebsiteLink":"http://www.wbur.org/hereandnow","meta":{"site":"news","source":"npr"},"link":"/radio/program/here-and-now","subsdcribe":{"apple":"https://itunes.apple.com/WebObjects/MZStore.woa/wa/viewPodcast?mt=2&id=426698661","tuneIn":"https://tunein.com/radio/Here--Now-p211/","rss":"https://feeds.npr.org/510051/podcast.xml"}},"how-i-built-this":{"id":"how-i-built-this","title":"How I Built This with Guy Raz","info":"Guy Raz dives into the stories behind some of the world's best known companies. 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Hosts Ki Sung and Katrina Schwartz introduce listeners to educators, researchers, parents and students who are developing effective ways to improve how kids learn. We cover topics like how fed-up administrators are developing surprising tactics to deal with classroom disruptions; how listening to podcasts are helping kids develop reading skills; the consequences of overparenting; and why interdisciplinary learning can engage students on all ends of the traditional achievement spectrum. This podcast is part of the MindShift education site, a division of KQED News. KQED is an NPR/PBS member station based in San Francisco. You can also visit the MindShift website for episodes and supplemental blog posts or tweet us \u003ca href=\"https://twitter.com/MindShiftKQED\">@MindShiftKQED\u003c/a> or visit us at \u003ca href=\"/mindshift\">MindShift.KQED.org\u003c/a>","imageSrc":"https://cdn.kqed.org/wp-content/uploads/2024/04/Mindshift-Podcast-Tile-703x703-1.jpg","imageAlt":"KQED MindShift: How We Will Learn","officialWebsiteLink":"/mindshift/","meta":{"site":"news","source":"kqed","order":"2"},"link":"/podcasts/mindshift","subscribe":{"apple":"https://podcasts.apple.com/us/podcast/mindshift-podcast/id1078765985","google":"https://podcasts.google.com/feed/aHR0cHM6Ly9mZWVkcy5tZWdhcGhvbmUuZm0vS1FJTkM1NzY0NjAwNDI5","npr":"https://www.npr.org/podcasts/464615685/mind-shift-podcast","stitcher":"https://www.stitcher.com/podcast/kqed/stories-teachers-share","spotify":"https://open.spotify.com/show/0MxSpNYZKNprFLCl7eEtyx"}},"morning-edition":{"id":"morning-edition","title":"Morning Edition","info":"\u003cem>Morning Edition\u003c/em> takes listeners around the country and the world with multi-faceted stories and commentaries every weekday. Hosts Steve Inskeep, David Greene and Rachel Martin bring you the latest breaking news and features to prepare you for the day.","airtime":"MON-FRI 3am-9am","imageSrc":"https://cdn.kqed.org/wp-content/uploads/2024/04/Morning-Edition-Podcast-Tile-360x360-1.jpg","officialWebsiteLink":"https://www.npr.org/programs/morning-edition/","meta":{"site":"news","source":"npr"},"link":"/radio/program/morning-edition"},"onourwatch":{"id":"onourwatch","title":"On Our Watch","tagline":"Police secrets, unsealed","info":"For decades, the process for how police police themselves has been inconsistent – if not opaque. In some states, like California, these proceedings were completely hidden. After a new police transparency law unsealed scores of internal affairs files, our reporters set out to examine these cases and the shadow world of police discipline. 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