What Makes California's Quake Warning System So Timely?
Geological Outings Around the Bay: Los Trancos Open Space
Side Trips from Interstate 5: San Emigdio Mountains
What Shall We Do About Earthquake Weather?
Geological Outings Around the Bay: Fremont Peak
GeoZeum: A Personal Museum of Geology
QUEST Lab: The Shaking Table at UC Berkeley
Sponsored
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The story segments featured in each show are introduced by on-camera host, environmental journalist \u003ca href=\"http://science.kqed.org/quest/author/pssethi/\">Simran Sethi\u003c/a>. The series also includes half-hour specials that focus on a single topic.\r\n \r\nAll 2013-2014 television programs can be viewed online in their entirety or as individual segments by clicking on the titles and images listed below. The programs are also broadcast in each of our six PBS partner regions including \u003ca href=\"http://science.kqed.org/quest/stations/north-carolina/\">North Carolina\u003c/a>, \u003ca href=\"http://science.kqed.org/quest/stations/ohio/\">Ohio\u003c/a>, \u003ca href=\"http://science.kqed.org/quest/stations/nebraska/\">Nebraska\u003c/a>, \u003ca href=\"http://science.kqed.org/quest/stations/northern-california/\">Northern California\u003c/a> and the \u003ca href=\"http://science.kqed.org/quest/stations/northwest/\">Pacific Northwest\u003c/a>. Check local listings for broadcast dates and times.","avatar":"https://secure.gravatar.com/avatar/d3874a881a1fe56a99098a4feea236c8?s=600&d=blank&r=g","twitter":null,"facebook":null,"instagram":null,"linkedin":null,"sites":[{"site":"quest","roles":["editor"]}],"headData":{"title":"QUEST Staff | KQED","description":null,"ogImgSrc":"https://secure.gravatar.com/avatar/d3874a881a1fe56a99098a4feea236c8?s=600&d=blank&r=g","twImgSrc":"https://secure.gravatar.com/avatar/d3874a881a1fe56a99098a4feea236c8?s=600&d=blank&r=g"},"isLoading":false,"link":"/author/quest"}},"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":"home","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":"/"}},"quest_141904":{"type":"posts","id":"quest_141904","meta":{"index":"posts_1591205157","site":"quest","id":"141904","score":null,"sort":[1460707239000]},"guestAuthors":[],"slug":"san-francisco-bay-area-earthquakes-and-faults","title":"San Francisco Bay Area Earthquakes and Faults","publishDate":1460707239,"format":"video","headTitle":"QUEST | KQED Science","labelTerm":{"term":10627,"site":"quest"},"content":"\u003cp>Most earthquakes happen along plate boundaries. Many of these locations are also where mountain building or volcanic activity occurs. Certain areas, sometimes referred to as earthquake belts, are more prone to earthquakes. One belt runs northward through the western Pacific Ocean, across the Aleutian Islands, and then down the western coasts of North and South America. This belt includes the Bay Area faults and is called the “Ring of Fire.”\u003c/p>\n\u003cfigure id=\"attachment_141905\" class=\"wp-caption aligncenter\" style=\"max-width: 2304px\">\u003cimg class=\"wp-image-141905 size-full\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2016/04/BayAreaFaultPlanesLabeled.png\" alt=\"major Bay Area Faults\" width=\"2304\" height=\"3072\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2016/04/BayAreaFaultPlanesLabeled.png 2304w, https://ww2.kqed.org/app/uploads/sites/39/2016/04/BayAreaFaultPlanesLabeled-400x533.png 400w, https://ww2.kqed.org/app/uploads/sites/39/2016/04/BayAreaFaultPlanesLabeled-800x1067.png 800w, https://ww2.kqed.org/app/uploads/sites/39/2016/04/BayAreaFaultPlanesLabeled-768x1024.png 768w, https://ww2.kqed.org/app/uploads/sites/39/2016/04/BayAreaFaultPlanesLabeled-1440x1920.png 1440w, https://ww2.kqed.org/app/uploads/sites/39/2016/04/BayAreaFaultPlanesLabeled-1180x1573.png 1180w, https://ww2.kqed.org/app/uploads/sites/39/2016/04/BayAreaFaultPlanesLabeled-960x1280.png 960w\" sizes=\"(max-width: 2304px) 100vw, 2304px\">\u003cfigcaption class=\"wp-caption-text\">Major Bay Area Faults \u003ccite>((Courtesy of California Academy of Sciences))\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>The City of San Francisco experienced major earthquakes in 1906 and 1989 due to its location along the San Andreas fault. However, of the major fault systems in the Bay Area, the Hayward Fault is of most concern to geologists. Extending almost 40 miles from Fremont to San Pablo Bay, the Hayward Fault runs under some of the most densely populated areas in the country. More than two million people live and work along the fault. BART, major gas lines, schools, and trauma centers sit on or near the fault. The Hayward Fault is a prime candidate in Northern California for a magnitude 7 earthquake within the next 30 years.\u003c/p>\n\u003cp>[youtube https://www.youtube.com/watch?v=GhFMtCmHc9c&w=640&h=360]\u003c/p>\n\u003cp>Geologists have observed cracks and deformed curbs on sidewalks and streets in areas near the fault. These are evidence of creep, a phenomenon of slow movement on the surface of the ground even though deep beneath the surface the rock is stuck in place. When the rock that’s stuck builds up enough tension, the fault then ruptures, or slips, causing a major earthquake. The last major earthquake on the Hayward Fault was in 1868—more than 140 years ago—and historically, major earthquakes have occurred along that fault about every 140 years.\u003c/p>\n\u003chr>\n\u003cp>This post is part of \u003ca href=\"https://www.calacademy.org/earthquakes\">Exploring Earthquakes\u003c/a>, a rich collection of resources co-presented by the California Academy of Sciences and KQED. This material is also available as a free \u003ca href=\"https://itunes.apple.com/book/earthquake/id552255768?mt=11\">iBooks textbook\u003c/a> and \u003ca href=\"https://itunes.apple.com/us/course/earthquake/id552092722\">iTunes U course\u003c/a>.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>Don’t miss \u003ca href=\"https://www.calacademy.org/exhibits/earthquake-life-on-a-dynamic-planet\">Earthquake\u003c/a>, an interactive exhibit at the Academy exploring the seismic forces that impact us today and featuring the Shake House, an earthquake simulator.\u003c/p>\n\n","blocks":[],"excerpt":"Many faults run through the San Francisco Bay Area, making it prone to earthquakes. ","status":"publish","parent":0,"modified":1460684944,"stats":{"hasAudio":false,"hasVideo":true,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":8,"wordCount":367},"headData":{"title":"San Francisco Bay Area Earthquakes and Faults | KQED","description":"Many faults run through the San Francisco Bay Area, making it prone to earthquakes. ","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":"","schema":{"@context":"http://schema.org","@type":"Article","headline":"San Francisco Bay Area Earthquakes and Faults","datePublished":"2016-04-15T08:00:39.000Z","dateModified":"2016-04-15T01:49:04.000Z","image":"https://cdn.kqed.org/wp-content/uploads/2020/02/KQED-OG-Image@1x.png"}},"disqusIdentifier":"141904 http://ww2.kqed.org/quest/?p=141904","disqusUrl":"https://ww2.kqed.org/quest/2016/04/15/san-francisco-bay-area-earthquakes-and-faults/","disqusTitle":"San Francisco Bay Area Earthquakes and Faults","videoEmbed":"https://www.youtube.com/watch?v=m5xM-CTDLo0&index=1&list=PLS14biAqBAtE_wpsyXkZbbb7Wwq4DkUzw","path":"/quest/141904/san-francisco-bay-area-earthquakes-and-faults","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cp>Most earthquakes happen along plate boundaries. Many of these locations are also where mountain building or volcanic activity occurs. Certain areas, sometimes referred to as earthquake belts, are more prone to earthquakes. One belt runs northward through the western Pacific Ocean, across the Aleutian Islands, and then down the western coasts of North and South America. This belt includes the Bay Area faults and is called the “Ring of Fire.”\u003c/p>\n\u003cfigure id=\"attachment_141905\" class=\"wp-caption aligncenter\" style=\"max-width: 2304px\">\u003cimg class=\"wp-image-141905 size-full\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2016/04/BayAreaFaultPlanesLabeled.png\" alt=\"major Bay Area Faults\" width=\"2304\" height=\"3072\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2016/04/BayAreaFaultPlanesLabeled.png 2304w, https://ww2.kqed.org/app/uploads/sites/39/2016/04/BayAreaFaultPlanesLabeled-400x533.png 400w, https://ww2.kqed.org/app/uploads/sites/39/2016/04/BayAreaFaultPlanesLabeled-800x1067.png 800w, https://ww2.kqed.org/app/uploads/sites/39/2016/04/BayAreaFaultPlanesLabeled-768x1024.png 768w, https://ww2.kqed.org/app/uploads/sites/39/2016/04/BayAreaFaultPlanesLabeled-1440x1920.png 1440w, https://ww2.kqed.org/app/uploads/sites/39/2016/04/BayAreaFaultPlanesLabeled-1180x1573.png 1180w, https://ww2.kqed.org/app/uploads/sites/39/2016/04/BayAreaFaultPlanesLabeled-960x1280.png 960w\" sizes=\"(max-width: 2304px) 100vw, 2304px\">\u003cfigcaption class=\"wp-caption-text\">Major Bay Area Faults \u003ccite>((Courtesy of California Academy of Sciences))\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>The City of San Francisco experienced major earthquakes in 1906 and 1989 due to its location along the San Andreas fault. However, of the major fault systems in the Bay Area, the Hayward Fault is of most concern to geologists. Extending almost 40 miles from Fremont to San Pablo Bay, the Hayward Fault runs under some of the most densely populated areas in the country. More than two million people live and work along the fault. BART, major gas lines, schools, and trauma centers sit on or near the fault. The Hayward Fault is a prime candidate in Northern California for a magnitude 7 earthquake within the next 30 years.\u003c/p>\n\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/GhFMtCmHc9c'\n title='//www.youtube.com/embed/GhFMtCmHc9c'\n allowfullscreen='true'\n style='border:0;'>\u003c/iframe>\n \u003c/span>\n \u003c/span>\u003c/p>\u003cp>\u003c/p>\n\u003cp>Geologists have observed cracks and deformed curbs on sidewalks and streets in areas near the fault. These are evidence of creep, a phenomenon of slow movement on the surface of the ground even though deep beneath the surface the rock is stuck in place. When the rock that’s stuck builds up enough tension, the fault then ruptures, or slips, causing a major earthquake. The last major earthquake on the Hayward Fault was in 1868—more than 140 years ago—and historically, major earthquakes have occurred along that fault about every 140 years.\u003c/p>\n\u003chr>\n\u003cp>This post is part of \u003ca href=\"https://www.calacademy.org/earthquakes\">Exploring Earthquakes\u003c/a>, a rich collection of resources co-presented by the California Academy of Sciences and KQED. This material is also available as a free \u003ca href=\"https://itunes.apple.com/book/earthquake/id552255768?mt=11\">iBooks textbook\u003c/a> and \u003ca href=\"https://itunes.apple.com/us/course/earthquake/id552092722\">iTunes U course\u003c/a>.\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>\u003c/p>\n\u003cp>Don’t miss \u003ca href=\"https://www.calacademy.org/exhibits/earthquake-life-on-a-dynamic-planet\">Earthquake\u003c/a>, an interactive exhibit at the Academy exploring the seismic forces that impact us today and featuring the Shake House, an earthquake simulator.\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/quest/141904/san-francisco-bay-area-earthquakes-and-faults","authors":["10216"],"categories":["quest_11"],"tags":["quest_439","quest_909","quest_13461","quest_1080","quest_1325","quest_2484","quest_3071"],"collections":["quest_10627"],"featImg":"quest_141905","label":"quest_10627"},"quest_51772":{"type":"posts","id":"quest_51772","meta":{"index":"posts_1591205157","site":"quest","id":"51772","score":null,"sort":[1364493250000]},"guestAuthors":[],"slug":"the-rocks-of-devils-slide","title":"The Rocks of Devil's Slide","publishDate":1364493250,"format":"aside","headTitle":"QUEST | KQED Science","labelTerm":{"site":"quest"},"content":"\u003cp>With the opening of the Lantos Tunnel this week at the notorious Devil's Slide on state Route 1, the work is not finished. The winding, vertiginous old road and the 70 acres of land it sits on will be handed over to San Mateo County, which has pledged to give it a makeover and splice it into the \u003ca href=\"http://www.californiacoastaltrail.info/cms/pages/main/index.html\">California Coastal Trail\u003c/a>, adding a new attraction to the \u003ca href=\"http://www.devilsslidecoast.org/map/\">Devil's Slide Coast\u003c/a>. The facilities will include parking lots at each end, water, bathrooms, trash bins, rails and pedestrian crossings.\u003c/p>\n\u003cp>Hikers and bicyclists will be thrilled with the high views up and down the coast. They may feel a tickle as they look at the surf hundreds of feet below. And some of them will feel curiosity as they look inland at the sides of the road, about 1.3 miles of it, that they could never stop and see before.\u003c/p>\n\u003cp>This stretch of road passes through two very different sets of rocks. The south end is the granite of Montara Mountain; I showed you some of this \u003ca href=\"http://ww2.kqed.org/quest/2011/08/11/what-happens-to-old-quarries/\">at Quarry Park in El Granada\u003c/a>, a bit farther south, in 2011. It holds up the rugged headlands around the tunnel's mouth. It dates from Cretaceous time, just like the granite in the Sierra Nevada—and in fact it's the same stuff, ripped out of the range and pulled northward here by the San Andreas fault. The same granite is found as far north as Bodega Head and south to San Luis Obispo County (including \u003ca href=\"http://ww2.kqed.org/quest/2013/01/03/our-newest-national-park-pinnacles-national-monument/\">Pinnacles\u003c/a> and \u003ca href=\"http://ww2.kqed.org/quest/2011/11/03/geological-outings-around-the-bay-fremont-peak/\">Fremont Peak\u003c/a>, part of a sliver of tectonic plate that geologists know as the Salinian block.\u003c/p>\n\u003cfigure id=\"attachment_51773\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2013/03/28/the-rocks-of-devils-slide/devilslidesouth/\" rel=\"attachment wp-att-51773\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/03/devilslidesouth.jpg\" alt=\"Caltrans photo\" width=\"600\" height=\"400\" class=\"size-full wp-image-51773\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/03/devilslidesouth.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/03/devilslidesouth-400x267.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Caltrans\u003c/figcaption>\u003c/figure>\n\u003cp>The north end is a thick pile of mudstone that dates from Paleocene time, slightly younger than the granite. This is the material that gave Devil's Slide its name. It's been falling into the sea for untold centuries, including the last century in which we have been vainly putting roads across the cliffs. \u003c/p>\n\u003cfigure id=\"attachment_51774\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2013/03/28/the-rocks-of-devils-slide/devilslidewest/\" rel=\"attachment wp-att-51774\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/03/devilslidewest.jpg\" alt=\"Caltrans\" width=\"600\" height=\"445\" class=\"size-full wp-image-51774\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/03/devilslidewest.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/03/devilslidewest-400x297.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Caltrans\u003c/figcaption>\u003c/figure>\n\u003cp>The San Mateo County geologic map describes it as marine shale and sandstone with beds of conglomerate. The conglomerate is basically sandstone that includes \"angular boulders of granitic rock as long as 2 meters and smaller boulders, cobbles, and rounded pebbles of hornblende gneiss, muscovite gneiss and schist, Franciscan chert, quartzite, limestone, sandstone, and shale.\" That variety of material represents a long-vanished countryside rather like today's, with vigorous rivers that carried this coarse sedimentary material straight out to sea. \u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>The contact between the granite and the mudstone is an inactive fault. Both units are in the Salinian block. And now it's time to show them on the geologic map.\u003c/p>\n\u003cfigure id=\"attachment_51775\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2013/03/28/the-rocks-of-devils-slide/devilslidegeomap/\" rel=\"attachment wp-att-51775\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/03/devilslidegeomap.png\" alt=\"Kgr, granitic rocks of Montara Mountain; Tss, Paleocene sandstone and shale; fs and fg, Franciscan sedimentary rocks; blue, Franciscan limestone\" width=\"600\" height=\"450\" class=\"size-full wp-image-51775\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/03/devilslidegeomap.png 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/03/devilslidegeomap-400x300.png 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Major units: Kgr, granitic rocks of Montara Mountain; Tss, Paleocene sandstone and shale; fs and fg, Franciscan sedimentary rocks; blue, Franciscan limestone. The \"V\" signs mark the tunnel entrances.\u003c/figcaption>\u003c/figure>\n\u003cp>That fault contact will be an attraction for many geologists and students. Local researcher Kathleen Burnham describes what she looks forward to seeing here: \"Among the notable features now hazardous and difficult to access are bedding-plane trace fossils, vertical burrows filled with white carbonate, some isoclinal bedding folds, and the contact between the strata of Point San Pedro and the underlying Montara Granodiorite. The Devil's Slide project as a whole will greatly enhance accessibility of these spectacular outcrops when the project is finished, traffic diverted, and vehicles no longer whizzing by within inches.\"\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>The geologists at Caltrans have been good friends of the geological community. Now that the old roadbed is in the County's hands, let's hope they don't decide to hide these rocks. Who knows how long we have to enjoy them.\u003c/p>\n\n","blocks":[],"excerpt":"Lovers of geology look forward to inspecting the roadcut along old Route 1 at Devil's Slide next year.","status":"publish","parent":0,"modified":1366389174,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":10,"wordCount":611},"headData":{"title":"The Rocks of Devil's Slide | KQED","description":"Lovers of geology look forward to inspecting the roadcut along old Route 1 at Devil's Slide next year.","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":"","schema":{"@context":"http://schema.org","@type":"Article","headline":"The Rocks of Devil's Slide","datePublished":"2013-03-28T17:54:10.000Z","dateModified":"2013-04-19T16:32:54.000Z","image":"https://cdn.kqed.org/wp-content/uploads/2020/02/KQED-OG-Image@1x.png"}},"disqusIdentifier":"51772 http://science.kqed.org/quest/?p=51772","disqusUrl":"https://ww2.kqed.org/quest/2013/03/28/the-rocks-of-devils-slide/","disqusTitle":"The Rocks of Devil's Slide","path":"/quest/51772/the-rocks-of-devils-slide","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cp>With the opening of the Lantos Tunnel this week at the notorious Devil's Slide on state Route 1, the work is not finished. The winding, vertiginous old road and the 70 acres of land it sits on will be handed over to San Mateo County, which has pledged to give it a makeover and splice it into the \u003ca href=\"http://www.californiacoastaltrail.info/cms/pages/main/index.html\">California Coastal Trail\u003c/a>, adding a new attraction to the \u003ca href=\"http://www.devilsslidecoast.org/map/\">Devil's Slide Coast\u003c/a>. The facilities will include parking lots at each end, water, bathrooms, trash bins, rails and pedestrian crossings.\u003c/p>\n\u003cp>Hikers and bicyclists will be thrilled with the high views up and down the coast. They may feel a tickle as they look at the surf hundreds of feet below. And some of them will feel curiosity as they look inland at the sides of the road, about 1.3 miles of it, that they could never stop and see before.\u003c/p>\n\u003cp>This stretch of road passes through two very different sets of rocks. The south end is the granite of Montara Mountain; I showed you some of this \u003ca href=\"http://ww2.kqed.org/quest/2011/08/11/what-happens-to-old-quarries/\">at Quarry Park in El Granada\u003c/a>, a bit farther south, in 2011. It holds up the rugged headlands around the tunnel's mouth. It dates from Cretaceous time, just like the granite in the Sierra Nevada—and in fact it's the same stuff, ripped out of the range and pulled northward here by the San Andreas fault. The same granite is found as far north as Bodega Head and south to San Luis Obispo County (including \u003ca href=\"http://ww2.kqed.org/quest/2013/01/03/our-newest-national-park-pinnacles-national-monument/\">Pinnacles\u003c/a> and \u003ca href=\"http://ww2.kqed.org/quest/2011/11/03/geological-outings-around-the-bay-fremont-peak/\">Fremont Peak\u003c/a>, part of a sliver of tectonic plate that geologists know as the Salinian block.\u003c/p>\n\u003cfigure id=\"attachment_51773\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2013/03/28/the-rocks-of-devils-slide/devilslidesouth/\" rel=\"attachment wp-att-51773\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/03/devilslidesouth.jpg\" alt=\"Caltrans photo\" width=\"600\" height=\"400\" class=\"size-full wp-image-51773\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/03/devilslidesouth.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/03/devilslidesouth-400x267.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Caltrans\u003c/figcaption>\u003c/figure>\n\u003cp>The north end is a thick pile of mudstone that dates from Paleocene time, slightly younger than the granite. This is the material that gave Devil's Slide its name. It's been falling into the sea for untold centuries, including the last century in which we have been vainly putting roads across the cliffs. \u003c/p>\n\u003cfigure id=\"attachment_51774\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2013/03/28/the-rocks-of-devils-slide/devilslidewest/\" rel=\"attachment wp-att-51774\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/03/devilslidewest.jpg\" alt=\"Caltrans\" width=\"600\" height=\"445\" class=\"size-full wp-image-51774\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/03/devilslidewest.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/03/devilslidewest-400x297.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Caltrans\u003c/figcaption>\u003c/figure>\n\u003cp>The San Mateo County geologic map describes it as marine shale and sandstone with beds of conglomerate. The conglomerate is basically sandstone that includes \"angular boulders of granitic rock as long as 2 meters and smaller boulders, cobbles, and rounded pebbles of hornblende gneiss, muscovite gneiss and schist, Franciscan chert, quartzite, limestone, sandstone, and shale.\" That variety of material represents a long-vanished countryside rather like today's, with vigorous rivers that carried this coarse sedimentary material straight out to sea. \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 contact between the granite and the mudstone is an inactive fault. Both units are in the Salinian block. And now it's time to show them on the geologic map.\u003c/p>\n\u003cfigure id=\"attachment_51775\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2013/03/28/the-rocks-of-devils-slide/devilslidegeomap/\" rel=\"attachment wp-att-51775\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/03/devilslidegeomap.png\" alt=\"Kgr, granitic rocks of Montara Mountain; Tss, Paleocene sandstone and shale; fs and fg, Franciscan sedimentary rocks; blue, Franciscan limestone\" width=\"600\" height=\"450\" class=\"size-full wp-image-51775\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/03/devilslidegeomap.png 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/03/devilslidegeomap-400x300.png 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Major units: Kgr, granitic rocks of Montara Mountain; Tss, Paleocene sandstone and shale; fs and fg, Franciscan sedimentary rocks; blue, Franciscan limestone. The \"V\" signs mark the tunnel entrances.\u003c/figcaption>\u003c/figure>\n\u003cp>That fault contact will be an attraction for many geologists and students. Local researcher Kathleen Burnham describes what she looks forward to seeing here: \"Among the notable features now hazardous and difficult to access are bedding-plane trace fossils, vertical burrows filled with white carbonate, some isoclinal bedding folds, and the contact between the strata of Point San Pedro and the underlying Montara Granodiorite. The Devil's Slide project as a whole will greatly enhance accessibility of these spectacular outcrops when the project is finished, traffic diverted, and vehicles no longer whizzing by within inches.\"\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>The geologists at Caltrans have been good friends of the geological community. Now that the old roadbed is in the County's hands, let's hope they don't decide to hide these rocks. Who knows how long we have to enjoy them.\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/quest/51772/the-rocks-of-devils-slide","authors":["6228"],"categories":["quest_11"],"tags":["quest_11858","quest_11862","quest_10406","quest_11518","quest_3669","quest_11868","quest_2484"],"featImg":"quest_51776","label":"quest"},"quest_49223":{"type":"posts","id":"quest_49223","meta":{"index":"posts_1591205157","site":"quest","id":"49223","score":null,"sort":[1359663661000]},"guestAuthors":[],"slug":"what-makes-californias-quake-warning-system-so-timely","title":"What Makes California's Quake Warning System So Timely?","publishDate":1359663661,"format":"aside","headTitle":"QUEST | KQED Science","labelTerm":{"site":"quest"},"content":"\u003cfigure id=\"attachment_49224\" class=\"wp-caption alignleft\" style=\"max-width: 300px\">\u003ca href=\"http://ww2.kqed.org/quest/2013/01/31/what-makes-californias-quake-warning-system-so-timely/caleqwarningtop/\" rel=\"attachment wp-att-49224\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/01/CalEQwarningtop-300x169.jpg\" alt=\"The collapsed Cypress Viaduct was the site of the first earthquake early-warning system, in 1989. USGS photo by Howard Wilshire\" width=\"300\" height=\"169\" class=\"size-thumbnail wp-image-49224\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">The collapsed Cypress Viaduct in Oakland was the site of the first earthquake early-warning system, in 1989. USGS photo by Howard Wilshire\u003c/figcaption>\u003c/figure>\n\u003cp>Earlier this week, State Senator Alex Padilla went before the cameras with a group of earthquake scientists to kick-start California into building the world's best earthquake early-warning system. Does such a thing really work? And why should we start now?\u003c/p>\n\u003cp>Early-warning systems are not a scientific boondoggle; they really work. First things first, though: these do not predict earthquakes. Instead, they're automatic systems that detect quakes right at the epicenter, and measure their size almost instantly. With that information, they signal faraway users that strong shaking is on its way RIGHT NOW. You could call that a prediction if you like, an instant shaking prediction. But quake researchers are extremely allergic to the word \"prediction,\" so please call these warning systems. They're like the tsunami warning systems we're familiar with by now, only a lot faster.\u003c/p>\n\u003cp>The Bay Area had the world's first example back in 1989, in the aftermath of the Loma Prieta earthquake. It detected aftershocks. It consisted of a handful of seismographs around the epicenter in the Santa Cruz Mountains, a computer and a microwave radio network. When the computer got enough simultaneous signals from the seismographs, it considered that the detection of a large aftershock and sent out an alarm on the radio network. Crews who were taking down the wreckage of the Cypress Structure, 100 kilometers away, got about 20 seconds of warning to back off and get out. You can imagine how useful that system was to those workers, crude as it was.\u003c/p>\n\u003cp>Today much larger and better systems are at work around the world. Japan's is the most advanced—not so much scientifically, because every system's software uses the latest science, but in terms of being integrated into people's lives. If you saw it in action during the 2011 Tohoku earthquake, you can imagine one like it in California.\u003c/p>\n\u003cp>Senator Padilla's bill was triggered after one of his regular visits to Caltech. (He's an astronomy geek, it turns out.) While he was there, the earthquake people got hold of him and demonstrated the early-warning tools on the California Integrated Seismic Network (\u003ca href=\"http://www.cisn.org/\">CISN\u003c/a>), like the experimental \u003ca href=\"http://www.elarms.org/index.php\">ElarmS\u003c/a> project. The CISN people told him, as they've been telling anyone who will listen for ten years now, that they're ready to roll whenever the money can be found. Right now their research relies on a lean stream of funds from government projects and the Gordon and Betty Moore Foundation.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>Padilla's bill (\u003ca href=\"http://leginfo.legislature.ca.gov/faces/billNavClient.xhtml?bill_id=201320140SB135\">Senate Bill 135\u003c/a>) is mostly preamble with one new sentence for the Government Code that commits the Office of Emergency Services to work with the CISN partners to \"develop a comprehensive statewide earthquake early warning system in California.\" In the preamble is one unusual item: a reference to \u003ca href=\"http://www.nature.com/nature/journal/vaop/ncurrent/full/nature11703.html\">a dry scientific paper in \u003ci>Nature\u003c/i> last month\u003c/a>. The paper is also prominently featured in Padilla's news release about SB-135, which linked to a Caltech \u003ca href=\"http://www.caltech.edu/content/faulty-behavior\">press-office piece\u003c/a> on the paper.\u003c/p>\n\u003cp>Peggy Hellweg, the CISN point person at Cal Berkeley's Seismological Lab, explained where the paper fits in the larger story. Ever since the 1992 Landers quake in Southern California, she told me, a major weak point in our understanding of earthquake faults is how ruptures can expand beyond the limits we thought they had. At Landers, five separately mapped faults gave way at once in a single rupture. On the larger scale, both the giant 2004 Sumatra and 2011 Tohoku quakes ruptured fault segments that no one expected to fail. As for our own San Andreas fault system, we've always taken it as a given that the so-called creeping section, which runs between San Juan Bautista and Parkfield, separates northern and southern California. We don't expect a rupture on either the north or south end of the fault to rip through the creeping section, because its degree of creep—steady motion without earthquakes—would seem to preclude the more wrenching motion of a proper earthquake. It shouldn't have enough strain energy on it.\u003c/p>\n\u003cp>The \u003ci>Nature\u003c/i> paper combined simulations of faulting with lab tests of actual material drill-sampled from the fault zone that ruptured in the large 1999 Chi Chi earthquake in Taiwan. Its authors described scenarios in which ruptures advancing into a creeping fault, if they hit it just right, would set it off. In fact, that supposedly low-strain creeping section could release quite a lot of energy.\u003c/p>\n\u003cp>The authors suggested that creeping might be a temporary state between the relaxed state right after a quake (no energy) and the \"stuck\" state that most earthquake faults are in (lots of energy). \"Temporary\" in this case means centuries. If their work holds up and can be generalized, then it's plausible that the San Andreas fault could all go at once. \u003ca href=\"http://www.sciencenews.org/view/generic/id/347423/description/Quakes_may_bring_nearby_rocks_closer_to_rupture\">An article in \u003ci>Science News\u003c/i>\u003c/a> quotes some of the cautionary comments, which make the same points I would. \u003c/p>\n\u003cp>\u003c/p>\n\u003cp>It strikes me as unusual that such a scientific article would be used as a \"news hook\" to promote something as fundamental as a new statewide quake-warning system. Normally, in California, we would cite the latest awful earthquake, because that seems to focus people's attention better. But as Senator Padilla said, better to get a system in place before rather than after the next Big One. I absolutely support SB-135 anyway, regardless of this one paper.\u003c/p>\n\n","blocks":[],"excerpt":"In the age-old war between Northern and Southern California, a change in the science has changed the politics.","status":"publish","parent":0,"modified":1359666812,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":12,"wordCount":935},"headData":{"title":"What Makes California's Quake Warning System So Timely? | KQED","description":"In the age-old war between Northern and Southern California, a change in the science has changed the politics.","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":"","schema":{"@context":"http://schema.org","@type":"Article","headline":"What Makes California's Quake Warning System So Timely?","datePublished":"2013-01-31T20:21:01.000Z","dateModified":"2013-01-31T21:13:32.000Z","image":"https://cdn.kqed.org/wp-content/uploads/2020/02/KQED-OG-Image@1x.png"}},"disqusIdentifier":"49223 http://science.kqed.org/quest/?p=49223","disqusUrl":"https://ww2.kqed.org/quest/2013/01/31/what-makes-californias-quake-warning-system-so-timely/","disqusTitle":"What Makes California's Quake Warning System So Timely?","path":"/quest/49223/what-makes-californias-quake-warning-system-so-timely","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cfigure id=\"attachment_49224\" class=\"wp-caption alignleft\" style=\"max-width: 300px\">\u003ca href=\"http://ww2.kqed.org/quest/2013/01/31/what-makes-californias-quake-warning-system-so-timely/caleqwarningtop/\" rel=\"attachment wp-att-49224\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/01/CalEQwarningtop-300x169.jpg\" alt=\"The collapsed Cypress Viaduct was the site of the first earthquake early-warning system, in 1989. USGS photo by Howard Wilshire\" width=\"300\" height=\"169\" class=\"size-thumbnail wp-image-49224\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">The collapsed Cypress Viaduct in Oakland was the site of the first earthquake early-warning system, in 1989. USGS photo by Howard Wilshire\u003c/figcaption>\u003c/figure>\n\u003cp>Earlier this week, State Senator Alex Padilla went before the cameras with a group of earthquake scientists to kick-start California into building the world's best earthquake early-warning system. Does such a thing really work? And why should we start now?\u003c/p>\n\u003cp>Early-warning systems are not a scientific boondoggle; they really work. First things first, though: these do not predict earthquakes. Instead, they're automatic systems that detect quakes right at the epicenter, and measure their size almost instantly. With that information, they signal faraway users that strong shaking is on its way RIGHT NOW. You could call that a prediction if you like, an instant shaking prediction. But quake researchers are extremely allergic to the word \"prediction,\" so please call these warning systems. They're like the tsunami warning systems we're familiar with by now, only a lot faster.\u003c/p>\n\u003cp>The Bay Area had the world's first example back in 1989, in the aftermath of the Loma Prieta earthquake. It detected aftershocks. It consisted of a handful of seismographs around the epicenter in the Santa Cruz Mountains, a computer and a microwave radio network. When the computer got enough simultaneous signals from the seismographs, it considered that the detection of a large aftershock and sent out an alarm on the radio network. Crews who were taking down the wreckage of the Cypress Structure, 100 kilometers away, got about 20 seconds of warning to back off and get out. You can imagine how useful that system was to those workers, crude as it was.\u003c/p>\n\u003cp>Today much larger and better systems are at work around the world. Japan's is the most advanced—not so much scientifically, because every system's software uses the latest science, but in terms of being integrated into people's lives. If you saw it in action during the 2011 Tohoku earthquake, you can imagine one like it in California.\u003c/p>\n\u003cp>Senator Padilla's bill was triggered after one of his regular visits to Caltech. (He's an astronomy geek, it turns out.) While he was there, the earthquake people got hold of him and demonstrated the early-warning tools on the California Integrated Seismic Network (\u003ca href=\"http://www.cisn.org/\">CISN\u003c/a>), like the experimental \u003ca href=\"http://www.elarms.org/index.php\">ElarmS\u003c/a> project. The CISN people told him, as they've been telling anyone who will listen for ten years now, that they're ready to roll whenever the money can be found. Right now their research relies on a lean stream of funds from government projects and the Gordon and Betty Moore Foundation.\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>Padilla's bill (\u003ca href=\"http://leginfo.legislature.ca.gov/faces/billNavClient.xhtml?bill_id=201320140SB135\">Senate Bill 135\u003c/a>) is mostly preamble with one new sentence for the Government Code that commits the Office of Emergency Services to work with the CISN partners to \"develop a comprehensive statewide earthquake early warning system in California.\" In the preamble is one unusual item: a reference to \u003ca href=\"http://www.nature.com/nature/journal/vaop/ncurrent/full/nature11703.html\">a dry scientific paper in \u003ci>Nature\u003c/i> last month\u003c/a>. The paper is also prominently featured in Padilla's news release about SB-135, which linked to a Caltech \u003ca href=\"http://www.caltech.edu/content/faulty-behavior\">press-office piece\u003c/a> on the paper.\u003c/p>\n\u003cp>Peggy Hellweg, the CISN point person at Cal Berkeley's Seismological Lab, explained where the paper fits in the larger story. Ever since the 1992 Landers quake in Southern California, she told me, a major weak point in our understanding of earthquake faults is how ruptures can expand beyond the limits we thought they had. At Landers, five separately mapped faults gave way at once in a single rupture. On the larger scale, both the giant 2004 Sumatra and 2011 Tohoku quakes ruptured fault segments that no one expected to fail. As for our own San Andreas fault system, we've always taken it as a given that the so-called creeping section, which runs between San Juan Bautista and Parkfield, separates northern and southern California. We don't expect a rupture on either the north or south end of the fault to rip through the creeping section, because its degree of creep—steady motion without earthquakes—would seem to preclude the more wrenching motion of a proper earthquake. It shouldn't have enough strain energy on it.\u003c/p>\n\u003cp>The \u003ci>Nature\u003c/i> paper combined simulations of faulting with lab tests of actual material drill-sampled from the fault zone that ruptured in the large 1999 Chi Chi earthquake in Taiwan. Its authors described scenarios in which ruptures advancing into a creeping fault, if they hit it just right, would set it off. In fact, that supposedly low-strain creeping section could release quite a lot of energy.\u003c/p>\n\u003cp>The authors suggested that creeping might be a temporary state between the relaxed state right after a quake (no energy) and the \"stuck\" state that most earthquake faults are in (lots of energy). \"Temporary\" in this case means centuries. If their work holds up and can be generalized, then it's plausible that the San Andreas fault could all go at once. \u003ca href=\"http://www.sciencenews.org/view/generic/id/347423/description/Quakes_may_bring_nearby_rocks_closer_to_rupture\">An article in \u003ci>Science News\u003c/i>\u003c/a> quotes some of the cautionary comments, which make the same points I would. \u003c/p>\n\u003cp>\u003c/p>\n\u003cp>It strikes me as unusual that such a scientific article would be used as a \"news hook\" to promote something as fundamental as a new statewide quake-warning system. Normally, in California, we would cite the latest awful earthquake, because that seems to focus people's attention better. But as Senator Padilla said, better to get a system in place before rather than after the next Big One. I absolutely support SB-135 anyway, regardless of this one paper.\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/quest/49223/what-makes-californias-quake-warning-system-so-timely","authors":["6228"],"categories":["quest_11"],"tags":["quest_11711","quest_608","quest_11710","quest_946","quest_13202","quest_2484"],"featImg":"quest_49224","label":"quest"},"quest_47096":{"type":"posts","id":"quest_47096","meta":{"index":"posts_1591205157","site":"quest","id":"47096","score":null,"sort":[1353010347000]},"guestAuthors":[],"slug":"geological-outings-around-the-bay-los-trancos-open-space","title":"Geological Outings Around the Bay: Los Trancos Open Space","publishDate":1353010347,"format":"standard","headTitle":"QUEST | KQED Science","labelTerm":{"site":"quest"},"content":"\u003cfigure id=\"attachment_47107\" class=\"wp-caption alignleft\" style=\"max-width: 300px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/11/15/geological-outings-around-the-bay-los-trancos-open-space/trancoscongl/\" rel=\"attachment wp-att-47107\">\u003cimg class=\"size-full wp-image-47107\" title=\"trancoscongl\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/11/trancoscongl.jpg\" alt=\"\" width=\"300\" height=\"216\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">While you're visiting the San Andreas fault, don't overlook the local rock, an excellent conglomerate. Photos by Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>Due south of Stanford, way up in the high hills, Los Trancos Open Space Preserve offers an excellent place to study the San Andreas fault. The preserve has a well-annotated trail that will show you good examples of the odd landforms and disturbances found all along the fault from Point Arena to the Salton Sea. \u003ca href=\"http://ww2.kqed.org/quest/science-hike/san-andreas-fault-trail-exploration/\">Craig Rosa presented this trail for KQED QUEST\u003c/a> a few years ago, and I can't improve on that. But since that time, geologists have gained a thrilling new tool for seeing landscapes: lidar mapping.\u003c/p>\n\u003cp>Lidar is laser-based radar. An airplane-mounted laser sprays the ground with tiny, precise laser pulses, and the time it takes for the light to return is measured. Our equipment is good enough to turn those times into distances, with precisions measured in centimeters. Every one of those millions of measurements—distances and GPS positions—is painstakingly recorded and poured into a database called a point cloud. It's a cloud because it's a blurry mixture of returns from treetops, shrubbery, buildings, flying birds and whatnot as well as the ground surface. But all that cruft can be digitally removed to show only what geologists care about: the bare land. (Foresters, on the other hand, love the way you can extract the treetops and map the woods itself.)\u003c/p>\n\u003cp>Here's what Los Trancos looks like in Google Maps. The San Andreas fault trail runs through thick oak woods in the valley of Los Trancos Creek. The fault itself runs from an inch right of the top-left corner to an inch left of the bottom-right corner.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/11/15/geological-outings-around-the-bay-los-trancos-open-space/trancosgm/\" rel=\"attachment wp-att-47109\">\u003cimg class=\"aligncenter size-full wp-image-47109\" title=\"trancosGM\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/11/trancosGM.jpg\" alt=\"\" width=\"600\" height=\"500\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/11/trancosGM.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/11/trancosGM-400x333.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>See it? Not really. The fault trace was mapped by people in boots, with the help of historical photos that showed the rips in the ground from the 1906 earthquake. Now have a look at the digital elevation model built from lidar data and digitally illuminated from the left.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/11/15/geological-outings-around-the-bay-los-trancos-open-space/trancosdem2/\" rel=\"attachment wp-att-47108\">\u003cimg class=\"aligncenter size-full wp-image-47108\" title=\"trancosdem2\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/11/trancosdem2.gif\" alt=\"\" width=\"600\" height=\"500\">\u003c/a>\u003c/p>\n\u003cp>This is what makes geologists use forbidden words like \"revolutionary\" when they give talks about lidar. To their trained eyes, this image has all kinds of information in it. It shows the stuff we've already mapped, plus many more subtle features we could go back and look for.\u003c/p>\n\u003cp>To me, most obviously, this image shows disorganized landslide topography along the western, uphill side of the fault trace. It suggests to me that one of the exhibits along the fault trail may need to be corrected: station 8 has a set of posts in the ground marking \"a minor fault,\" but it is much more likely to be a landslide scar. Check it out yourself on the ground and see what you think.\u003c/p>\n\u003cp>You can play with the lidar data yourself, using Google Earth and getting the data from the \u003ca href=\"http://calm.geo.berkeley.edu/ncalm/ddc.html\">National Center for Airborne Laser Mapping\u003c/a>. I did that to make the image below, which is from a higher elevation and tilted counterclockwise a bit.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/11/15/geological-outings-around-the-bay-los-trancos-open-space/trancosdem1/\" rel=\"attachment wp-att-47097\">\u003cimg class=\"aligncenter size-full wp-image-47097\" title=\"trancosdem1\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/11/trancosdem1.gif\" alt=\"\" width=\"640\" height=\"360\">\u003c/a>\u003c/p>\n\u003cp>We can see the fault cross Page Mill Road and head down behind Black Mountain along the headwaters of Stevens Creek. The fault guides Stevens and Los Trancos creeks right up to the road where the land forms a saddle, at the center of the image. This view looks down to that saddle.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/11/15/geological-outings-around-the-bay-los-trancos-open-space/trancos-saddle/\" rel=\"attachment wp-att-47110\">\u003cimg class=\"aligncenter size-full wp-image-47110\" title=\"trancos-saddle\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/11/trancos-saddle.jpg\" alt=\"\" width=\"600\" height=\"439\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/11/trancos-saddle.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/11/trancos-saddle-400x293.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>And if you cross the road to the Monte Bello Open Space Preserve, you can follow the fault into the heart of the Santa Cruz Mountains.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/11/15/geological-outings-around-the-bay-los-trancos-open-space/trancosviewsouth/\" rel=\"attachment wp-att-47106\">\u003cimg class=\"aligncenter size-full wp-image-47106\" title=\"trancosviewsouth\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/11/trancosviewsouth.jpg\" alt=\"\" width=\"600\" height=\"388\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/11/trancosviewsouth.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/11/trancosviewsouth-400x259.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>That's the fault coming in from the left in the strip of woods, then curving slightly to the left and exiting the horizon where the mountains are lowest. The highest of those distant peaks is Loma Prieta itself, which gave its name to the October 1989 earthquake by virtue of being the nearest notable landmark. Consider this picture an invitation to blaze your own self-educational trail along the fault.\u003c/p>\n\n","blocks":[],"excerpt":"Lidar mapping unveils one of the Bay Area's best places to visit the San Andreas fault.","status":"publish","parent":0,"modified":1475696902,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":17,"wordCount":659},"headData":{"title":"Geological Outings Around the Bay: Los Trancos Open Space | KQED","description":"Lidar mapping unveils one of the Bay Area's best places to visit the San Andreas fault.","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":"","schema":{"@context":"http://schema.org","@type":"Article","headline":"Geological Outings Around the Bay: Los Trancos Open Space","datePublished":"2012-11-15T20:12:27.000Z","dateModified":"2016-10-05T19:48:22.000Z","image":"https://cdn.kqed.org/wp-content/uploads/2020/02/KQED-OG-Image@1x.png"}},"disqusIdentifier":"47096 http://science.kqed.org/quest/?p=47096","disqusUrl":"https://ww2.kqed.org/quest/2012/11/15/geological-outings-around-the-bay-los-trancos-open-space/","disqusTitle":"Geological Outings Around the Bay: Los Trancos Open Space","path":"/quest/47096/geological-outings-around-the-bay-los-trancos-open-space","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cfigure id=\"attachment_47107\" class=\"wp-caption alignleft\" style=\"max-width: 300px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/11/15/geological-outings-around-the-bay-los-trancos-open-space/trancoscongl/\" rel=\"attachment wp-att-47107\">\u003cimg class=\"size-full wp-image-47107\" title=\"trancoscongl\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/11/trancoscongl.jpg\" alt=\"\" width=\"300\" height=\"216\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">While you're visiting the San Andreas fault, don't overlook the local rock, an excellent conglomerate. Photos by Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>Due south of Stanford, way up in the high hills, Los Trancos Open Space Preserve offers an excellent place to study the San Andreas fault. The preserve has a well-annotated trail that will show you good examples of the odd landforms and disturbances found all along the fault from Point Arena to the Salton Sea. \u003ca href=\"http://ww2.kqed.org/quest/science-hike/san-andreas-fault-trail-exploration/\">Craig Rosa presented this trail for KQED QUEST\u003c/a> a few years ago, and I can't improve on that. But since that time, geologists have gained a thrilling new tool for seeing landscapes: lidar mapping.\u003c/p>\n\u003cp>Lidar is laser-based radar. An airplane-mounted laser sprays the ground with tiny, precise laser pulses, and the time it takes for the light to return is measured. Our equipment is good enough to turn those times into distances, with precisions measured in centimeters. Every one of those millions of measurements—distances and GPS positions—is painstakingly recorded and poured into a database called a point cloud. It's a cloud because it's a blurry mixture of returns from treetops, shrubbery, buildings, flying birds and whatnot as well as the ground surface. But all that cruft can be digitally removed to show only what geologists care about: the bare land. (Foresters, on the other hand, love the way you can extract the treetops and map the woods itself.)\u003c/p>\n\u003cp>Here's what Los Trancos looks like in Google Maps. The San Andreas fault trail runs through thick oak woods in the valley of Los Trancos Creek. The fault itself runs from an inch right of the top-left corner to an inch left of the bottom-right corner.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/11/15/geological-outings-around-the-bay-los-trancos-open-space/trancosgm/\" rel=\"attachment wp-att-47109\">\u003cimg class=\"aligncenter size-full wp-image-47109\" title=\"trancosGM\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/11/trancosGM.jpg\" alt=\"\" width=\"600\" height=\"500\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/11/trancosGM.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/11/trancosGM-400x333.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>See it? Not really. The fault trace was mapped by people in boots, with the help of historical photos that showed the rips in the ground from the 1906 earthquake. Now have a look at the digital elevation model built from lidar data and digitally illuminated from the left.\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 href=\"http://ww2.kqed.org/quest/2012/11/15/geological-outings-around-the-bay-los-trancos-open-space/trancosdem2/\" rel=\"attachment wp-att-47108\">\u003cimg class=\"aligncenter size-full wp-image-47108\" title=\"trancosdem2\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/11/trancosdem2.gif\" alt=\"\" width=\"600\" height=\"500\">\u003c/a>\u003c/p>\n\u003cp>This is what makes geologists use forbidden words like \"revolutionary\" when they give talks about lidar. To their trained eyes, this image has all kinds of information in it. It shows the stuff we've already mapped, plus many more subtle features we could go back and look for.\u003c/p>\n\u003cp>To me, most obviously, this image shows disorganized landslide topography along the western, uphill side of the fault trace. It suggests to me that one of the exhibits along the fault trail may need to be corrected: station 8 has a set of posts in the ground marking \"a minor fault,\" but it is much more likely to be a landslide scar. Check it out yourself on the ground and see what you think.\u003c/p>\n\u003cp>You can play with the lidar data yourself, using Google Earth and getting the data from the \u003ca href=\"http://calm.geo.berkeley.edu/ncalm/ddc.html\">National Center for Airborne Laser Mapping\u003c/a>. I did that to make the image below, which is from a higher elevation and tilted counterclockwise a bit.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/11/15/geological-outings-around-the-bay-los-trancos-open-space/trancosdem1/\" rel=\"attachment wp-att-47097\">\u003cimg class=\"aligncenter size-full wp-image-47097\" title=\"trancosdem1\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/11/trancosdem1.gif\" alt=\"\" width=\"640\" height=\"360\">\u003c/a>\u003c/p>\n\u003cp>We can see the fault cross Page Mill Road and head down behind Black Mountain along the headwaters of Stevens Creek. The fault guides Stevens and Los Trancos creeks right up to the road where the land forms a saddle, at the center of the image. This view looks down to that saddle.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/11/15/geological-outings-around-the-bay-los-trancos-open-space/trancos-saddle/\" rel=\"attachment wp-att-47110\">\u003cimg class=\"aligncenter size-full wp-image-47110\" title=\"trancos-saddle\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/11/trancos-saddle.jpg\" alt=\"\" width=\"600\" height=\"439\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/11/trancos-saddle.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/11/trancos-saddle-400x293.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>And if you cross the road to the Monte Bello Open Space Preserve, you can follow the fault into the heart of the Santa Cruz Mountains.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/11/15/geological-outings-around-the-bay-los-trancos-open-space/trancosviewsouth/\" rel=\"attachment wp-att-47106\">\u003cimg class=\"aligncenter size-full wp-image-47106\" title=\"trancosviewsouth\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/11/trancosviewsouth.jpg\" alt=\"\" width=\"600\" height=\"388\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/11/trancosviewsouth.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/11/trancosviewsouth-400x259.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>That's the fault coming in from the left in the strip of woods, then curving slightly to the left and exiting the horizon where the mountains are lowest. The highest of those distant peaks is Loma Prieta itself, which gave its name to the October 1989 earthquake by virtue of being the nearest notable landmark. Consider this picture an invitation to blaze your own self-educational trail along the fault.\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/quest/47096/geological-outings-around-the-bay-los-trancos-open-space","authors":["6228"],"categories":["quest_11"],"tags":["quest_11608","quest_11607","quest_13","quest_2484"],"featImg":"quest_47097","label":"quest"},"quest_44500":{"type":"posts","id":"quest_44500","meta":{"index":"posts_1591205157","site":"quest","id":"44500","score":null,"sort":[1348168065000]},"guestAuthors":[],"slug":"side-trips-from-interstate-5-san-emigdio-mountains","title":"Side Trips from Interstate 5: San Emigdio Mountains","publishDate":1348168065,"format":"aside","headTitle":"QUEST | KQED Science","labelTerm":{"site":"quest"},"content":"\u003cfigure id=\"attachment_44505\" class=\"wp-caption alignleft\" style=\"max-width: 300px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/09/20/side-trips-from-interstate-5-san-emigdio-mountains/emigdio-top/\" rel=\"attachment wp-att-44505\">\u003cimg class=\"size-thumbnail wp-image-44505\" title=\"emigdio-top\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/09/emigdio-top-300x169.jpg\" alt=\"\" width=\"300\" height=\"169\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">The southern wall of the Great Valley is worth passing through instead of passing by. Photos by Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>With all the construction going on south of Bakersfield on I-5, now is a time to seriously consider a scenic detour of two hours or so that avoids the congestion.\u003c/p>\n\u003cp>The key points are the little towns of Maricopa and Lebec, and the road between them is named Cerro Noroeste Road at its west end and Frazier Mountain Park Road at its east end. I've marked it with asterisks in this Google Maps clipping. How you get to Maricopa is up to you: state route 33 gets you there from Coalinga, as does state route 58 from Buttonwillow. Another road goes through the Elk Hills if you have extra time.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/09/20/side-trips-from-interstate-5-san-emigdio-mountains/emigdiotopo/\" rel=\"attachment wp-att-44506\">\u003cimg class=\"aligncenter size-full wp-image-44506\" title=\"emigdiotopo\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/09/emigdiotopo.jpg\" alt=\"\" width=\"640\" height=\"550\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/09/emigdiotopo.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2012/09/emigdiotopo-400x344.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003c/p>\n\u003cp>The geologic overlay (from the \u003ca href=\"http://www.quake.ca.gov/gmaps/GMC/stategeologicmap.html\">interactive state geologic map\u003c/a>) shows that this road threads along the part of the San Andreas fault called the Great Bend. Compressive forces across the fault here have pushed up the land into mountain ranges, the San Emigdio range on the north and the Transverse Ranges on the south.\u003c/p>\n\u003cfigure id=\"attachment_44504\" class=\"wp-caption aligncenter\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/09/20/side-trips-from-interstate-5-san-emigdio-mountains/emigdiogeo/\" rel=\"attachment wp-att-44504\">\u003cimg class=\"size-full wp-image-44504\" title=\"emigdiogeo\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/09/emigdiogeo.png\" alt=\"\" width=\"640\" height=\"550\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/09/emigdiogeo.png 640w, https://ww2.kqed.org/app/uploads/sites/39/2012/09/emigdiogeo-400x344.png 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Pink is Sierra Nevada granite, brown is Precambrian rocks, other colors are mostly young (Tertiary) sedimentary and volcanic rocks.\u003c/figcaption>\u003c/figure>\n\u003cp>I'll show you the sights from the southbound perspective. The San Emigdios get their name from the patron saint of earthquakes, and this area was badly shaken by the enormous 1857 earthquake that \u003ca href=\"http://geology.about.com/od/geology_ca/ig/saf1857/\">ruptured the ground from Parkfield to El Cajon\u003c/a>.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>Haze often hides the range, but as you approach the west side of the Great Valley it emerges over the arid oil-producing country around Taft.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/09/20/side-trips-from-interstate-5-san-emigdio-mountains/emig-taftview/\" rel=\"attachment wp-att-44509\">\u003cimg class=\"aligncenter size-full wp-image-44509\" title=\"emig-taftview\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/09/emig-taftview.jpg\" alt=\"\" width=\"600\" height=\"414\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-taftview.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-taftview-400x276.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>Cerro Noroeste Road begins as a turnoff from state route 33/166 just west of the fault trace. If you take an early opportunity to \u003ca href=\"http://geology.about.com/od/geology_ca/ig/saf1857/saf1857norosag.htm\">look north\u003c/a>, you can follow the fault's path into the Carrizo Plain. The road ascends to a ridge with spectacular views. Northward you'll see a kaleidoscope of vegetation and lithology on the Great Valley's south edge.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/09/20/side-trips-from-interstate-5-san-emigdio-mountains/emig-lithline/\" rel=\"attachment wp-att-44507\">\u003cimg class=\"aligncenter size-full wp-image-44507\" title=\"emig-lithline\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/09/emig-lithline.jpg\" alt=\"\" width=\"600\" height=\"450\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-lithline.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-lithline-400x300.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>Southward is a succession of Transverse Range ridges that includes the Sierra Madre, San Rafael and Santa Ynez mountains, the last of which overlooks the Santa Barbara coast.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/09/20/side-trips-from-interstate-5-san-emigdio-mountains/emig-cerrosouth/\" rel=\"attachment wp-att-44501\">\u003cimg class=\"aligncenter size-full wp-image-44501\" title=\"emig-cerrosouth\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/09/emig-cerrosouth.jpg\" alt=\"\" width=\"600\" height=\"396\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-cerrosouth.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-cerrosouth-400x264.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>In springtime, the vegetation includes some choice vernal pools. This was in late May.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/09/20/side-trips-from-interstate-5-san-emigdio-mountains/emig-vernalpool/\" rel=\"attachment wp-att-44510\">\u003cimg class=\"aligncenter size-full wp-image-44510\" title=\"emig-vernalpool\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/09/emig-vernalpool.jpg\" alt=\"\" width=\"600\" height=\"420\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-vernalpool.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-vernalpool-400x280.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>The high point of the road is Apache Saddle, just over 6000 feet. This is also the highest point on the San Andreas fault. On the other side is the resort area from Pine Mountain Club to Lake of the Woods to Frazier Park, right off I-5. If you take the time to explore, you'll find that the rocks are very different on opposite sides of the fault—that's because the southern side has been carried hundreds of miles west past the northern side, one earthquake at a time, for some 25 million years and counting. This is the view of the fault valley from Mount Pinos; the highest peak is Mount San Emigdio, flagship peak of the range.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/09/20/side-trips-from-interstate-5-san-emigdio-mountains/emig-pinosview/\" rel=\"attachment wp-att-44508\">\u003cimg class=\"aligncenter size-full wp-image-44508\" title=\"emig-pinosview\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/09/emig-pinosview.jpg\" alt=\"\" width=\"600\" height=\"387\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-pinosview.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-pinosview-400x258.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>(I showed you \u003ca href=\"http://ww2.kqed.org/quest/2012/03/29/californias-and-the-worlds-oldest-rocks/\">California's oldest rocks\u003c/a> from Mount Pinos a few months ago.)\u003c/p>\n\u003cp>The fault valley itself is a dramatic showcase of tectonic features if you know what you're looking at. Its inhabitants sprawl around the fault trace, as they do almost everywhere. This view is looking west in Pine Mountain Club.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/09/20/side-trips-from-interstate-5-san-emigdio-mountains/emig-cerrovalleywest/\" rel=\"attachment wp-att-44502\">\u003cimg class=\"aligncenter size-full wp-image-44502\" title=\"emig-cerrovalleywest\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/09/emig-cerrovalleywest.jpg\" alt=\"\" width=\"600\" height=\"389\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-cerrovalleywest.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-cerrovalleywest-400x259.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>Farther along, you'll drive through Cuddy Valley. This photo was taken in March.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/09/20/side-trips-from-interstate-5-san-emigdio-mountains/emig-cuddyvalley/\" rel=\"attachment wp-att-44503\">\u003cimg class=\"aligncenter size-full wp-image-44503\" title=\"emig-cuddyvalley\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/09/emig-cuddyvalley.jpg\" alt=\"\" width=\"600\" height=\"413\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-cuddyvalley.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-cuddyvalley-400x275.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>The fault trace runs along the foot of the hills on the opposite side. At the far end is \u003ca href=\"http://geology.about.com/od/geology_ca/ig/saf1857/saf1857cuddysag.htm\">a prominent sag pond\u003c/a>, formed where two fault strands allow the ground to subside between them. The large peak is Frazier Mountain, which you can drive up if you return for a longer visit. And why wouldn't you? It beats creeping up the Grapevine.\u003c/p>\n\n","blocks":[],"excerpt":"Journeying through the Great Valley's southern rampart is time better spent than inching up the Grapevine.","status":"publish","parent":0,"modified":1349809142,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":23,"wordCount":635},"headData":{"title":"Side Trips from Interstate 5: San Emigdio Mountains | KQED","description":"Journeying through the Great Valley's southern rampart is time better spent than inching up the Grapevine.","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":"","schema":{"@context":"http://schema.org","@type":"Article","headline":"Side Trips from Interstate 5: San Emigdio Mountains","datePublished":"2012-09-20T19:07:45.000Z","dateModified":"2012-10-09T18:59:02.000Z","image":"https://cdn.kqed.org/wp-content/uploads/2020/02/KQED-OG-Image@1x.png"}},"disqusIdentifier":"44500 http://science.kqed.org/quest/?p=44500","disqusUrl":"https://ww2.kqed.org/quest/2012/09/20/side-trips-from-interstate-5-san-emigdio-mountains/","disqusTitle":"Side Trips from Interstate 5: San Emigdio Mountains","path":"/quest/44500/side-trips-from-interstate-5-san-emigdio-mountains","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cfigure id=\"attachment_44505\" class=\"wp-caption alignleft\" style=\"max-width: 300px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/09/20/side-trips-from-interstate-5-san-emigdio-mountains/emigdio-top/\" rel=\"attachment wp-att-44505\">\u003cimg class=\"size-thumbnail wp-image-44505\" title=\"emigdio-top\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/09/emigdio-top-300x169.jpg\" alt=\"\" width=\"300\" height=\"169\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">The southern wall of the Great Valley is worth passing through instead of passing by. Photos by Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>With all the construction going on south of Bakersfield on I-5, now is a time to seriously consider a scenic detour of two hours or so that avoids the congestion.\u003c/p>\n\u003cp>The key points are the little towns of Maricopa and Lebec, and the road between them is named Cerro Noroeste Road at its west end and Frazier Mountain Park Road at its east end. I've marked it with asterisks in this Google Maps clipping. How you get to Maricopa is up to you: state route 33 gets you there from Coalinga, as does state route 58 from Buttonwillow. Another road goes through the Elk Hills if you have extra time.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/09/20/side-trips-from-interstate-5-san-emigdio-mountains/emigdiotopo/\" rel=\"attachment wp-att-44506\">\u003cimg class=\"aligncenter size-full wp-image-44506\" title=\"emigdiotopo\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/09/emigdiotopo.jpg\" alt=\"\" width=\"640\" height=\"550\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/09/emigdiotopo.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2012/09/emigdiotopo-400x344.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003c/p>\n\u003cp>The geologic overlay (from the \u003ca href=\"http://www.quake.ca.gov/gmaps/GMC/stategeologicmap.html\">interactive state geologic map\u003c/a>) shows that this road threads along the part of the San Andreas fault called the Great Bend. Compressive forces across the fault here have pushed up the land into mountain ranges, the San Emigdio range on the north and the Transverse Ranges on the south.\u003c/p>\n\u003cfigure id=\"attachment_44504\" class=\"wp-caption aligncenter\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/09/20/side-trips-from-interstate-5-san-emigdio-mountains/emigdiogeo/\" rel=\"attachment wp-att-44504\">\u003cimg class=\"size-full wp-image-44504\" title=\"emigdiogeo\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/09/emigdiogeo.png\" alt=\"\" width=\"640\" height=\"550\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/09/emigdiogeo.png 640w, https://ww2.kqed.org/app/uploads/sites/39/2012/09/emigdiogeo-400x344.png 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Pink is Sierra Nevada granite, brown is Precambrian rocks, other colors are mostly young (Tertiary) sedimentary and volcanic rocks.\u003c/figcaption>\u003c/figure>\n\u003cp>I'll show you the sights from the southbound perspective. The San Emigdios get their name from the patron saint of earthquakes, and this area was badly shaken by the enormous 1857 earthquake that \u003ca href=\"http://geology.about.com/od/geology_ca/ig/saf1857/\">ruptured the ground from Parkfield to El Cajon\u003c/a>.\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>Haze often hides the range, but as you approach the west side of the Great Valley it emerges over the arid oil-producing country around Taft.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/09/20/side-trips-from-interstate-5-san-emigdio-mountains/emig-taftview/\" rel=\"attachment wp-att-44509\">\u003cimg class=\"aligncenter size-full wp-image-44509\" title=\"emig-taftview\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/09/emig-taftview.jpg\" alt=\"\" width=\"600\" height=\"414\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-taftview.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-taftview-400x276.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>Cerro Noroeste Road begins as a turnoff from state route 33/166 just west of the fault trace. If you take an early opportunity to \u003ca href=\"http://geology.about.com/od/geology_ca/ig/saf1857/saf1857norosag.htm\">look north\u003c/a>, you can follow the fault's path into the Carrizo Plain. The road ascends to a ridge with spectacular views. Northward you'll see a kaleidoscope of vegetation and lithology on the Great Valley's south edge.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/09/20/side-trips-from-interstate-5-san-emigdio-mountains/emig-lithline/\" rel=\"attachment wp-att-44507\">\u003cimg class=\"aligncenter size-full wp-image-44507\" title=\"emig-lithline\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/09/emig-lithline.jpg\" alt=\"\" width=\"600\" height=\"450\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-lithline.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-lithline-400x300.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>Southward is a succession of Transverse Range ridges that includes the Sierra Madre, San Rafael and Santa Ynez mountains, the last of which overlooks the Santa Barbara coast.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/09/20/side-trips-from-interstate-5-san-emigdio-mountains/emig-cerrosouth/\" rel=\"attachment wp-att-44501\">\u003cimg class=\"aligncenter size-full wp-image-44501\" title=\"emig-cerrosouth\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/09/emig-cerrosouth.jpg\" alt=\"\" width=\"600\" height=\"396\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-cerrosouth.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-cerrosouth-400x264.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>In springtime, the vegetation includes some choice vernal pools. This was in late May.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/09/20/side-trips-from-interstate-5-san-emigdio-mountains/emig-vernalpool/\" rel=\"attachment wp-att-44510\">\u003cimg class=\"aligncenter size-full wp-image-44510\" title=\"emig-vernalpool\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/09/emig-vernalpool.jpg\" alt=\"\" width=\"600\" height=\"420\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-vernalpool.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-vernalpool-400x280.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>The high point of the road is Apache Saddle, just over 6000 feet. This is also the highest point on the San Andreas fault. On the other side is the resort area from Pine Mountain Club to Lake of the Woods to Frazier Park, right off I-5. If you take the time to explore, you'll find that the rocks are very different on opposite sides of the fault—that's because the southern side has been carried hundreds of miles west past the northern side, one earthquake at a time, for some 25 million years and counting. This is the view of the fault valley from Mount Pinos; the highest peak is Mount San Emigdio, flagship peak of the range.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/09/20/side-trips-from-interstate-5-san-emigdio-mountains/emig-pinosview/\" rel=\"attachment wp-att-44508\">\u003cimg class=\"aligncenter size-full wp-image-44508\" title=\"emig-pinosview\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/09/emig-pinosview.jpg\" alt=\"\" width=\"600\" height=\"387\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-pinosview.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-pinosview-400x258.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>(I showed you \u003ca href=\"http://ww2.kqed.org/quest/2012/03/29/californias-and-the-worlds-oldest-rocks/\">California's oldest rocks\u003c/a> from Mount Pinos a few months ago.)\u003c/p>\n\u003cp>The fault valley itself is a dramatic showcase of tectonic features if you know what you're looking at. Its inhabitants sprawl around the fault trace, as they do almost everywhere. This view is looking west in Pine Mountain Club.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/09/20/side-trips-from-interstate-5-san-emigdio-mountains/emig-cerrovalleywest/\" rel=\"attachment wp-att-44502\">\u003cimg class=\"aligncenter size-full wp-image-44502\" title=\"emig-cerrovalleywest\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/09/emig-cerrovalleywest.jpg\" alt=\"\" width=\"600\" height=\"389\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-cerrovalleywest.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-cerrovalleywest-400x259.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>Farther along, you'll drive through Cuddy Valley. This photo was taken in March.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/09/20/side-trips-from-interstate-5-san-emigdio-mountains/emig-cuddyvalley/\" rel=\"attachment wp-att-44503\">\u003cimg class=\"aligncenter size-full wp-image-44503\" title=\"emig-cuddyvalley\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/09/emig-cuddyvalley.jpg\" alt=\"\" width=\"600\" height=\"413\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-cuddyvalley.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/09/emig-cuddyvalley-400x275.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>The fault trace runs along the foot of the hills on the opposite side. At the far end is \u003ca href=\"http://geology.about.com/od/geology_ca/ig/saf1857/saf1857cuddysag.htm\">a prominent sag pond\u003c/a>, formed where two fault strands allow the ground to subside between them. The large peak is Frazier Mountain, which you can drive up if you return for a longer visit. And why wouldn't you? It beats creeping up the Grapevine.\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/quest/44500/side-trips-from-interstate-5-san-emigdio-mountains","authors":["6228"],"categories":["quest_11"],"tags":["quest_10760","quest_13202","quest_2484","quest_2630","quest_11472"],"featImg":"quest_44505","label":"quest"},"quest_41494":{"type":"posts","id":"quest_41494","meta":{"index":"posts_1591205157","site":"quest","id":"41494","score":null,"sort":[1343327215000]},"guestAuthors":[],"slug":"what-shall-we-do-about-earthquake-weather","title":"What Shall We Do About Earthquake Weather?","publishDate":1343327215,"format":"standard","headTitle":"QUEST | KQED Science","labelTerm":{"site":"quest"},"content":"\u003cfigure id=\"attachment_41495\" class=\"wp-caption alignleft\" style=\"max-width: 300px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/07/26/what-shall-we-do-about-earthquake-weather/eqweather/\" rel=\"attachment wp-att-41495\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/07/EQweather-300x169.jpg\" alt=\"\" title=\"EQweather\" width=\"300\" height=\"169\" class=\"size-thumbnail wp-image-41495\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">The San Andreas fault trace is marked on a road near Fort Ross. Photo by Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>We in the Bay Area, like most Californians, have always lived under the chronic threat of earthquakes. We know about it from personal experience and, farther back, from history. The government works against this threat in the sensible ways: building codes, zoning ordinances, scientific research, insurance mandates.\u003c/p>\n\u003cp>The rest of us have folkways organized around our local hazard. \"Drop, cover and hold on\" is a good one that we teach all of our kids. \"Stand in a doorway\" has been officially phased out—that works only in a traditional adobe building—but it's nearly as stubborn as the old adobes themselves.\u003c/p>\n\u003cp>The folk notion of \"earthquake weather\" centers around a belief that hot, still weather foreshadows an earthquake. It seems to be rooted in our culture as deeply as the ancient Greeks. Science established long ago that earthquakes have no statistical relation to the weather. Yet just last week one of the smartest, most competent people I know said in an online exchange, \"I've been worrying about earthquakes since the period of extreme stillness started yesterday.\" \u003c/p>\n\u003cp>I look around and wonder, too, when the weather gets weird. Something deeper is going on, something that I think we can't help doing. To talk about it I must turn to mythic, not scientific language. When the wind dies, the world is obviously holding its breath. What does the world await? The sky above is clear; there are no surface hazards nearby; it must be something below about to happen.\u003c/p>\n\u003cp>Scientists consider \"earthquake weather\" one of many misconceptions to be ruthlessly stamped out. (See attempts by the \u003ca href=\"http://www.consrv.ca.gov/index/Earthquakes/Pages/qh_earthquakes_myths.aspx\">California Department of Conservation\u003c/a>, the \u003ca href=\"http://www.scec.org/education/public/allmyths.html\">Southern California Earthquake Center\u003c/a> and the \u003ca href=\"http://earthquake.usgs.gov/learn/faq/?categoryID=6\">U.S. Geological Survey\u003c/a>.) But physics cannot displace psychology. I think that hot, still weather is so unusual in California that it allows our latent anxieties, whatever they are, to rise and demand attention. \u003ci>Something feels strange: is it related to my ongoing dread? Yes, that must be it. I will be vigilant. Now I feel a bit more in control.\u003c/i>\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>Earthquakes are a chronic, uncontrollable threat; maybe it's natural to contemplate them only on sanctioned occasions, the way we contemplate death at funerals. If \"earthquake weather\" is one way of doing this together, then at least that's an arbitrary habit—a folkway—we can share in full awareness of its arbitrariness. I suggest that the best way to talk about \"earthquake weather\" is to always begin with the words, \"I know it's silly of me, but . . .\" Because it \u003ci>isn't\u003c/i> sensible to hold on to unsupported ideas, but that's what we do, even adults. We can't outgrow what is inherent. So let's harness the habit in the service of awareness.\u003c/p>\n\n","blocks":[],"excerpt":"If we can't shake this discredited notion, let's speak it instead with a smile.","status":"publish","parent":0,"modified":1344279325,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":8,"wordCount":478},"headData":{"title":"What Shall We Do About Earthquake Weather? | KQED","description":"If we can't shake this discredited notion, let's speak it instead with a smile.","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":"","schema":{"@context":"http://schema.org","@type":"Article","headline":"What Shall We Do About Earthquake Weather?","datePublished":"2012-07-26T18:26:55.000Z","dateModified":"2012-08-06T18:55:25.000Z","image":"https://cdn.kqed.org/wp-content/uploads/2020/02/KQED-OG-Image@1x.png"}},"disqusIdentifier":"41494 http://science.kqed.org/quest/?p=41494","disqusUrl":"https://ww2.kqed.org/quest/2012/07/26/what-shall-we-do-about-earthquake-weather/","disqusTitle":"What Shall We Do About Earthquake Weather?","path":"/quest/41494/what-shall-we-do-about-earthquake-weather","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cfigure id=\"attachment_41495\" class=\"wp-caption alignleft\" style=\"max-width: 300px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/07/26/what-shall-we-do-about-earthquake-weather/eqweather/\" rel=\"attachment wp-att-41495\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/07/EQweather-300x169.jpg\" alt=\"\" title=\"EQweather\" width=\"300\" height=\"169\" class=\"size-thumbnail wp-image-41495\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">The San Andreas fault trace is marked on a road near Fort Ross. Photo by Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>We in the Bay Area, like most Californians, have always lived under the chronic threat of earthquakes. We know about it from personal experience and, farther back, from history. The government works against this threat in the sensible ways: building codes, zoning ordinances, scientific research, insurance mandates.\u003c/p>\n\u003cp>The rest of us have folkways organized around our local hazard. \"Drop, cover and hold on\" is a good one that we teach all of our kids. \"Stand in a doorway\" has been officially phased out—that works only in a traditional adobe building—but it's nearly as stubborn as the old adobes themselves.\u003c/p>\n\u003cp>The folk notion of \"earthquake weather\" centers around a belief that hot, still weather foreshadows an earthquake. It seems to be rooted in our culture as deeply as the ancient Greeks. Science established long ago that earthquakes have no statistical relation to the weather. Yet just last week one of the smartest, most competent people I know said in an online exchange, \"I've been worrying about earthquakes since the period of extreme stillness started yesterday.\" \u003c/p>\n\u003cp>I look around and wonder, too, when the weather gets weird. Something deeper is going on, something that I think we can't help doing. To talk about it I must turn to mythic, not scientific language. When the wind dies, the world is obviously holding its breath. What does the world await? The sky above is clear; there are no surface hazards nearby; it must be something below about to happen.\u003c/p>\n\u003cp>Scientists consider \"earthquake weather\" one of many misconceptions to be ruthlessly stamped out. (See attempts by the \u003ca href=\"http://www.consrv.ca.gov/index/Earthquakes/Pages/qh_earthquakes_myths.aspx\">California Department of Conservation\u003c/a>, the \u003ca href=\"http://www.scec.org/education/public/allmyths.html\">Southern California Earthquake Center\u003c/a> and the \u003ca href=\"http://earthquake.usgs.gov/learn/faq/?categoryID=6\">U.S. Geological Survey\u003c/a>.) But physics cannot displace psychology. I think that hot, still weather is so unusual in California that it allows our latent anxieties, whatever they are, to rise and demand attention. \u003ci>Something feels strange: is it related to my ongoing dread? Yes, that must be it. I will be vigilant. Now I feel a bit more in control.\u003c/i>\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>\u003c/p>\n\u003cp>Earthquakes are a chronic, uncontrollable threat; maybe it's natural to contemplate them only on sanctioned occasions, the way we contemplate death at funerals. If \"earthquake weather\" is one way of doing this together, then at least that's an arbitrary habit—a folkway—we can share in full awareness of its arbitrariness. I suggest that the best way to talk about \"earthquake weather\" is to always begin with the words, \"I know it's silly of me, but . . .\" Because it \u003ci>isn't\u003c/i> sensible to hold on to unsupported ideas, but that's what we do, even adults. We can't outgrow what is inherent. So let's harness the habit in the service of awareness.\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/quest/41494/what-shall-we-do-about-earthquake-weather","authors":["6228"],"categories":["quest_11"],"tags":["quest_11318","quest_11317","quest_909","quest_10188","quest_13202","quest_2484"],"featImg":"quest_41495","label":"quest"},"quest_26772":{"type":"posts","id":"quest_26772","meta":{"index":"posts_1591205157","site":"quest","id":"26772","score":null,"sort":[1320349149000]},"guestAuthors":[],"slug":"geological-outings-around-the-bay-fremont-peak","title":"Geological Outings Around the Bay: Fremont Peak","publishDate":1320349149,"format":"standard","headTitle":"QUEST | KQED Science","labelTerm":{"site":"quest"},"content":"\u003cfigure id=\"attachment_26775\" class=\"wp-caption alignnone\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/11/fremonttop.jpg\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/11/fremonttop.jpg\" alt=\"\" title=\"fremonttop\" width=\"640\" height=\"360\" class=\"size-full wp-image-26775\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/11/fremonttop.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/11/fremonttop-400x225.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Fremont Peak is renowned for its views of Monterey Bay to the west and the Hollister Valley to the east. All photos by Andrew Alden.\u003c/figcaption>\u003c/figure>\n\u003cp>I often think of the Bay Area as a series of regions dominated by a particular mountain. San Francisco is under the sway of Mount Tamalpais, of course, and the East Bay is Mount Diablo territory. Farther south the skylines feature Black Mountain on the west and Mission Peak on the east, then Loma Prieta and Mount Hamilton respectively. And the area stretching from Gilroy to Monterey is the land of Fremont Peak. It makes a good focus for a day trip.\u003c/p>\n\u003cp>Let's have a look at the area in the online \u003ca href=\"http://www.quake.ca.gov/gmaps/RGM/monterey/monterey.html\">Geologic Map of the Monterey Quadrangle\u003c/a>.\u003c/p>\n\u003cfigure id=\"attachment_26774\" class=\"wp-caption alignleft\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/11/03/geological-outings-around-the-bay-fremont-peak/fremontpkmap/\" rel=\"attachment wp-att-26774\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/11/fremontpkmap.png\" alt=\"\" title=\"fremontpkmap\" width=\"640\" height=\"500\" class=\"size-full wp-image-26774\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/11/fremontpkmap.png 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/11/fremontpkmap-400x313.png 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Map from California Department of Conservation\u003c/figcaption>\u003c/figure>\n\u003cp>The San Andreas fault slashes across the area southwest of Hollister. To its east are young (Miocene and Pliocene, 7 to 4 million years old) sedimentary rocks that correlate with the huge young sequences in the Central Valley. To its west (on the north side) are older sedimentary rocks mostly dating from the Eocene and Oligocene epochs around 35 million years old. The southern part of the map area, where Fremont Peak lies, is granite and related rocks making up the Gabilan Range. You reach the peak through the town of San Juan Bautista, located directly under the \"San Andreas fault\" label.\u003c/p>\n\u003cp>If you have the time to find Anzar Road, north of San Juan Bautista, pay a visit to Anzar Lake, one of the best-developed sag ponds on the San Andreas fault. These form where fault movement causes the ground to sink below the water table.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/11/03/geological-outings-around-the-bay-fremont-peak/fremanzarlake/\" rel=\"attachment wp-att-26773\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/11/fremanzarlake.jpg\" alt=\"\" title=\"fremanzarlake\" width=\"600\" height=\"412\" class=\"aligncenter size-full wp-image-26773\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/11/fremanzarlake.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2011/11/fremanzarlake-400x275.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>Anzar Road runs right along the fault trace pointing straight toward San Juan Bautista, where the old Spanish mission sits next to the fault overlooking the fertile soils that once formed the bottom of ancient Lake San Benito. The uplifted ground here made a desirable location, but the mission has suffered several large earthquakes during its history. The town is a good place to acquire lunch, visit the \u003ca href=\"http://ww2.kqed.org/quest/2011/09/29/geozeum-a-personal-museum-of-geology/\">GeoZeum\u003c/a>, and admire Fremont Peak from below.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/11/03/geological-outings-around-the-bay-fremont-peak/fremsjbmission/\" rel=\"attachment wp-att-26780\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/11/fremSJBmission.jpg\" alt=\"\" title=\"fremSJBmission\" width=\"600\" height=\"376\" class=\"aligncenter size-full wp-image-26780\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/11/fremSJBmission.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2011/11/fremSJBmission-400x251.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>Fremont Peak, formerly known as Gabilan Peak, is the centerpiece of \u003ca href=\"http://www.parks.ca.gov/?page_id=564\">Fremont Peak State Park\u003c/a>. The road up the mountain offers eastward views over Hollister Valley to the southern Diablo Range. The vegetation changes as you leave the sedimentary rocks and enter the granite zone. The granite of the Gabilan Range is part of the geologic province called Salinia. It's a segment of the Sierra Nevada that has been carried northward along the San Andreas fault. Other pieces of Salinia occur in the Santa Cruz Mountains, Point Reyes, and as far north as Bodega Head in Sonoma County.\u003c/p>\n\u003cfigure id=\"attachment_26776\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/11/03/geological-outings-around-the-bay-fremont-peak/frempkeast/\" rel=\"attachment wp-att-26776\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/11/frempkeast.jpg\" alt=\"\" title=\"frempkeast\" width=\"600\" height=\"418\" class=\"size-full wp-image-26776\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/11/frempkeast.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2011/11/frempkeast-400x279.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">The San Andreas fault runs in front of the chaparral-covered hill at center. Note the change in vegetation as the bedrock changes.\u003c/figcaption>\u003c/figure>\n\u003cp>The peak itself is not made up of granite, but rather of the much older metamorphic rocks that lay on top when the granite was emplaced from below. The most distinctive of these rocks is marble. The rock has been so thoroughly squeezed that it contains no fossils from which to determine its age. On the map it's the blue zone labeled \"PzMz\" or Paleozoic-Mesozoic, the scientific version of \"beats me.\"\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/11/03/geological-outings-around-the-bay-fremont-peak/frempkmarble/\" rel=\"attachment wp-att-26777\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/11/frempkmarble.jpg\" alt=\"\" title=\"frempkmarble\" width=\"600\" height=\"399\" class=\"aligncenter size-full wp-image-26777\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/11/frempkmarble.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2011/11/frempkmarble-400x266.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>The peak itself bears a plaque commemorating the famous stunt pulled by Captain John C. Frémont to taunt the Mexican authorities in early 1846, raising the American flag within sight of the capital in Monterey and Mexican troops gathered to the east. He soon took the flag down, blaming the bad weather, but his point had been made: the United States was coming into the country. The peak itself is a tumble of big marble boulders, worth a close look even if the views are good.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/11/03/geological-outings-around-the-bay-fremont-peak/frempkplaque/\" rel=\"attachment wp-att-26778\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/11/frempkplaque.jpg\" alt=\"\" title=\"frempkplaque\" width=\"500\" height=\"365\" class=\"aligncenter size-full wp-image-26778\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/11/frempkplaque.jpg 500w, https://ww2.kqed.org/app/uploads/sites/39/2011/11/frempkplaque-400x292.jpg 400w\" sizes=\"(max-width: 500px) 100vw, 500px\">\u003c/a>\u003c/p>\n\u003cp>On a clear day the whole sweep of Monterey Bay is visible. The western spine of the mountain consists of marble and beautifully displays the difference that topography makes to plant communities. The cool, sheltered north face is forest while the south face is parched grasslands and wildflowers.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/11/03/geological-outings-around-the-bay-fremont-peak/frempkwest/\" rel=\"attachment wp-att-26779\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/11/frempkwest.jpg\" alt=\"\" title=\"frempkwest\" width=\"600\" height=\"371\" class=\"aligncenter size-full wp-image-26779\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/11/frempkwest.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2011/11/frempkwest-400x247.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>The rock is riddled with small barite mines, and visitors with black lights will get a nice show inside them. At night, the park allows stargazers to \u003ca href=\"http://isthe.com/chongo/fpo/index.html\">view the sky through a 30-inch telescope\u003c/a>.\u003c/p>\n\n","blocks":[],"excerpt":"Fremont Peak oversees a large region of the Coast Ranges between Monterey and Hollister. When you pay it a visit, be sure to look around your feet too.","status":"publish","parent":0,"modified":1326779168,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":17,"wordCount":721},"headData":{"title":"Geological Outings Around the Bay: Fremont Peak | KQED","description":"Fremont Peak oversees a large region of the Coast Ranges between Monterey and Hollister. When you pay it a visit, be sure to look around your feet too.","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":"","schema":{"@context":"http://schema.org","@type":"Article","headline":"Geological Outings Around the Bay: Fremont Peak","datePublished":"2011-11-03T19:39:09.000Z","dateModified":"2012-01-17T05:46:08.000Z","image":"https://cdn.kqed.org/wp-content/uploads/2020/02/KQED-OG-Image@1x.png"}},"disqusIdentifier":"26772 http://science.kqed.org/quest/?p=26772","disqusUrl":"https://ww2.kqed.org/quest/2011/11/03/geological-outings-around-the-bay-fremont-peak/","disqusTitle":"Geological Outings Around the Bay: Fremont Peak","path":"/quest/26772/geological-outings-around-the-bay-fremont-peak","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cfigure id=\"attachment_26775\" class=\"wp-caption alignnone\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/11/fremonttop.jpg\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/11/fremonttop.jpg\" alt=\"\" title=\"fremonttop\" width=\"640\" height=\"360\" class=\"size-full wp-image-26775\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/11/fremonttop.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/11/fremonttop-400x225.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Fremont Peak is renowned for its views of Monterey Bay to the west and the Hollister Valley to the east. All photos by Andrew Alden.\u003c/figcaption>\u003c/figure>\n\u003cp>I often think of the Bay Area as a series of regions dominated by a particular mountain. San Francisco is under the sway of Mount Tamalpais, of course, and the East Bay is Mount Diablo territory. Farther south the skylines feature Black Mountain on the west and Mission Peak on the east, then Loma Prieta and Mount Hamilton respectively. And the area stretching from Gilroy to Monterey is the land of Fremont Peak. It makes a good focus for a day trip.\u003c/p>\n\u003cp>Let's have a look at the area in the online \u003ca href=\"http://www.quake.ca.gov/gmaps/RGM/monterey/monterey.html\">Geologic Map of the Monterey Quadrangle\u003c/a>.\u003c/p>\n\u003cfigure id=\"attachment_26774\" class=\"wp-caption alignleft\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/11/03/geological-outings-around-the-bay-fremont-peak/fremontpkmap/\" rel=\"attachment wp-att-26774\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/11/fremontpkmap.png\" alt=\"\" title=\"fremontpkmap\" width=\"640\" height=\"500\" class=\"size-full wp-image-26774\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/11/fremontpkmap.png 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/11/fremontpkmap-400x313.png 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Map from California Department of Conservation\u003c/figcaption>\u003c/figure>\n\u003cp>The San Andreas fault slashes across the area southwest of Hollister. To its east are young (Miocene and Pliocene, 7 to 4 million years old) sedimentary rocks that correlate with the huge young sequences in the Central Valley. To its west (on the north side) are older sedimentary rocks mostly dating from the Eocene and Oligocene epochs around 35 million years old. The southern part of the map area, where Fremont Peak lies, is granite and related rocks making up the Gabilan Range. You reach the peak through the town of San Juan Bautista, located directly under the \"San Andreas fault\" label.\u003c/p>\n\u003cp>If you have the time to find Anzar Road, north of San Juan Bautista, pay a visit to Anzar Lake, one of the best-developed sag ponds on the San Andreas fault. These form where fault movement causes the ground to sink below the water table.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/11/03/geological-outings-around-the-bay-fremont-peak/fremanzarlake/\" rel=\"attachment wp-att-26773\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/11/fremanzarlake.jpg\" alt=\"\" title=\"fremanzarlake\" width=\"600\" height=\"412\" class=\"aligncenter size-full wp-image-26773\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/11/fremanzarlake.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2011/11/fremanzarlake-400x275.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\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>Anzar Road runs right along the fault trace pointing straight toward San Juan Bautista, where the old Spanish mission sits next to the fault overlooking the fertile soils that once formed the bottom of ancient Lake San Benito. The uplifted ground here made a desirable location, but the mission has suffered several large earthquakes during its history. The town is a good place to acquire lunch, visit the \u003ca href=\"http://ww2.kqed.org/quest/2011/09/29/geozeum-a-personal-museum-of-geology/\">GeoZeum\u003c/a>, and admire Fremont Peak from below.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/11/03/geological-outings-around-the-bay-fremont-peak/fremsjbmission/\" rel=\"attachment wp-att-26780\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/11/fremSJBmission.jpg\" alt=\"\" title=\"fremSJBmission\" width=\"600\" height=\"376\" class=\"aligncenter size-full wp-image-26780\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/11/fremSJBmission.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2011/11/fremSJBmission-400x251.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>Fremont Peak, formerly known as Gabilan Peak, is the centerpiece of \u003ca href=\"http://www.parks.ca.gov/?page_id=564\">Fremont Peak State Park\u003c/a>. The road up the mountain offers eastward views over Hollister Valley to the southern Diablo Range. The vegetation changes as you leave the sedimentary rocks and enter the granite zone. The granite of the Gabilan Range is part of the geologic province called Salinia. It's a segment of the Sierra Nevada that has been carried northward along the San Andreas fault. Other pieces of Salinia occur in the Santa Cruz Mountains, Point Reyes, and as far north as Bodega Head in Sonoma County.\u003c/p>\n\u003cfigure id=\"attachment_26776\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/11/03/geological-outings-around-the-bay-fremont-peak/frempkeast/\" rel=\"attachment wp-att-26776\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/11/frempkeast.jpg\" alt=\"\" title=\"frempkeast\" width=\"600\" height=\"418\" class=\"size-full wp-image-26776\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/11/frempkeast.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2011/11/frempkeast-400x279.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">The San Andreas fault runs in front of the chaparral-covered hill at center. Note the change in vegetation as the bedrock changes.\u003c/figcaption>\u003c/figure>\n\u003cp>The peak itself is not made up of granite, but rather of the much older metamorphic rocks that lay on top when the granite was emplaced from below. The most distinctive of these rocks is marble. The rock has been so thoroughly squeezed that it contains no fossils from which to determine its age. On the map it's the blue zone labeled \"PzMz\" or Paleozoic-Mesozoic, the scientific version of \"beats me.\"\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/11/03/geological-outings-around-the-bay-fremont-peak/frempkmarble/\" rel=\"attachment wp-att-26777\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/11/frempkmarble.jpg\" alt=\"\" title=\"frempkmarble\" width=\"600\" height=\"399\" class=\"aligncenter size-full wp-image-26777\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/11/frempkmarble.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2011/11/frempkmarble-400x266.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>The peak itself bears a plaque commemorating the famous stunt pulled by Captain John C. Frémont to taunt the Mexican authorities in early 1846, raising the American flag within sight of the capital in Monterey and Mexican troops gathered to the east. He soon took the flag down, blaming the bad weather, but his point had been made: the United States was coming into the country. The peak itself is a tumble of big marble boulders, worth a close look even if the views are good.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/11/03/geological-outings-around-the-bay-fremont-peak/frempkplaque/\" rel=\"attachment wp-att-26778\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/11/frempkplaque.jpg\" alt=\"\" title=\"frempkplaque\" width=\"500\" height=\"365\" class=\"aligncenter size-full wp-image-26778\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/11/frempkplaque.jpg 500w, https://ww2.kqed.org/app/uploads/sites/39/2011/11/frempkplaque-400x292.jpg 400w\" sizes=\"(max-width: 500px) 100vw, 500px\">\u003c/a>\u003c/p>\n\u003cp>On a clear day the whole sweep of Monterey Bay is visible. The western spine of the mountain consists of marble and beautifully displays the difference that topography makes to plant communities. The cool, sheltered north face is forest while the south face is parched grasslands and wildflowers.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/11/03/geological-outings-around-the-bay-fremont-peak/frempkwest/\" rel=\"attachment wp-att-26779\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/11/frempkwest.jpg\" alt=\"\" title=\"frempkwest\" width=\"600\" height=\"371\" class=\"aligncenter size-full wp-image-26779\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/11/frempkwest.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2011/11/frempkwest-400x247.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>The rock is riddled with small barite mines, and visitors with black lights will get a nice show inside them. At night, the park allows stargazers to \u003ca href=\"http://isthe.com/chongo/fpo/index.html\">view the sky through a 30-inch telescope\u003c/a>.\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/quest/26772/geological-outings-around-the-bay-fremont-peak","authors":["6228"],"categories":["quest_3","quest_11"],"tags":["quest_13192","quest_10404","quest_10406","quest_10405","quest_13202","quest_2484","quest_10238"],"featImg":"quest_26775","label":"quest"},"quest_25495":{"type":"posts","id":"quest_25495","meta":{"index":"posts_1591205157","site":"quest","id":"25495","score":null,"sort":[1317308429000]},"guestAuthors":[],"slug":"geozeum-a-personal-museum-of-geology","title":"GeoZeum: A Personal Museum of Geology","publishDate":1317308429,"format":"standard","headTitle":"QUEST | KQED Science","labelTerm":{"site":"quest"},"content":"\u003cfigure id=\"attachment_25496\" class=\"wp-caption alignleft\" style=\"max-width: 300px\">\u003ca href=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/09/geozeumtop.jpg\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/09/geozeumtop-300x169.jpg\" alt=\"\" title=\"geozeumtop\" width=\"300\" height=\"169\" class=\"size-thumbnail wp-image-25496\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">GeoZeum is a brand-new boutique education center of geology in historic—and geologically rich—San Juan Bautista. Photos by Andrew Alden.\u003c/figcaption>\u003c/figure>\n\u003cp>Most of us have a retirement dream: What would we do once our daily grind is over? Retired geologists I know indulge their devotion to poetry, photography, winemaking, philosophy, or Burning Man. A common idea is to open a little rock shop. Phil Stoffer is a born teacher with a huge rock collection, and his retirement project is to run a little museum in San Juan Bautista, a superb place to personally introduce the pleasures and treasures of Earth science to all comers. \"It's all about keeping geology going,\" he says. I have seen nothing like it before.\u003c/p>\n\u003cp>Stoffer has dipped into a lot of the geologist's typical career options: mining, oil and gas, scientific librarian, college instructor, and website creator and field hand for the U.S. Geological Survey. He's collected rocks and fossils and photographed geology in all fifty states. All of that, experience and photos and specimens, is the nucleus of Stoffer's \u003ca href=\"http://www.geozeum.com/\">GeoZeum\u003c/a>, just a short stroll from the San Andreas fault and, of course, on the Web.\u003c/p>\n\u003cfigure id=\"attachment_25497\" class=\"wp-caption aligncenter\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/09/29/geozeum-a-personal-museum-of-geology/geozeumrox/\" rel=\"attachment wp-att-25497\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/09/geozeumrox.jpg\" alt=\"\" title=\"geozeumrox\" width=\"640\" height=\"360\" class=\"size-full wp-image-25497\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/09/geozeumrox.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/09/geozeumrox-400x225.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Some of the best rocks in GeoZeum are found near San Juan Bautista.\u003c/figcaption>\u003c/figure>\n\u003cp>GeoZeum has shelves of rocks, minerals and fossils. It also has tables covered with them, meant to be handled. It has an earthquake machine and a tsunami tank. It has big 3D photos of landforms and glasses to view them with. It even has a closet filled with fluorescent minerals. A lapidary lab is in the planning stage. And the key ingredient is the owner, eager to show and tell.\u003c/p>\n\u003cp>A project like GeoZeum relies on a lot of synergy. First, there's the Spanish mission in San Juan Bautista. California's unique \u003ca href=\"http://www.cuca.k12.ca.us/lessons/missions/contents/index.html\">4th-grade curriculum emphasizing the missions\u003c/a> brings busloads of children to San Juan Bautista. \u003ca href=\"http://www.san-juan-bautista.ca.us/\">The city itself is a draw for tourists\u003c/a>, too. The mission owes its very location to the scarp raised along the San Andreas fault, and more than any other California mission its history is tied to earthquakes.\u003c/p>\n\u003cfigure id=\"attachment_25498\" class=\"wp-caption aligncenter\" style=\"max-width: 500px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/09/29/geozeum-a-personal-museum-of-geology/geozeumsjbmission/\" rel=\"attachment wp-att-25498\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/09/geozeumSJBmission.jpg\" alt=\"\" title=\"geozeumSJBmission\" width=\"500\" height=\"350\" class=\"aligncenter size-full wp-image-25498\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/09/geozeumSJBmission.jpg 500w, https://ww2.kqed.org/app/uploads/sites/39/2011/09/geozeumSJBmission-400x280.jpg 400w\" sizes=\"(max-width: 500px) 100vw, 500px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">The San Andreas fault runs along the foot of the rise on which the San Juan Bautista mission sits. GeoZeum's Phil Stoffer leads walks here every weekend.\u003c/figcaption>\u003c/figure>\n\u003cp>Second, GeoZeum shares a building with \u003ca href=\"http://www.topsarockshop.com/index.htm\">TOPS A Rock Shop\u003c/a>, an uncommonly well-stocked example of its genre. TOPS will be a natural gathering place for the rock-and-mineral club that Stoffer is launching.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>Third, San Juan Bautista is a remarkable nexus of geological sites every bit as interesting as the Bay Area. Indeed, just a million years ago you could say the area \u003ci>was\u003c/i> the Bay Area, because the rivers of the Central Valley reached the Pacific through here. The area is full of mines and quarries, several earthquake faults, and diverse packages of rocks that those faults have carried here from far away. The GeoZeum website has a lot of maps and other material about the area.\u003c/p>\n\u003cp>One of Stoffer's favorite places is the riverbed of the San Benito River, where the gravel contains an enormous variety of rock types. But when I visited him earlier this week, we went instead to Gabilan (Fremont) Peak and explored some old barite mines in the ancient marble that makes up the mountaintop. We brought along ultraviolet flashlights and admired the veins of blue and yellow fluorescence in the mine passages. Stoffer has dozens of ideas like these for geologic walks.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/09/29/geozeum-a-personal-museum-of-geology/geozeumsteps/\" rel=\"attachment wp-att-25499\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/09/geozeumsteps.jpg\" alt=\"\" title=\"geozeumsteps\" width=\"500\" height=\"410\" class=\"aligncenter size-full wp-image-25499\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/09/geozeumsteps.jpg 500w, https://ww2.kqed.org/app/uploads/sites/39/2011/09/geozeumsteps-400x328.jpg 400w\" sizes=\"(max-width: 500px) 100vw, 500px\">\u003c/a>\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>GeoZeum is already operating Thursday through Sunday, but its formal Grand Opening is October 15. Stoffer will welcome you to his museum, whether you're a kid, a fellow retired geologist or anything between. Just look for the dinosaur tracks on the sidewalk.\u003c/p>\n\n","blocks":[],"excerpt":"GeoZeum is something between a rock shop and a discovery museum in historic—and geologically rich—San Juan Bautista.","status":"publish","parent":0,"modified":1317853304,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":11,"wordCount":631},"headData":{"title":"GeoZeum: A Personal Museum of Geology | KQED","description":"GeoZeum is something between a rock shop and a discovery museum in historic—and geologically rich—San Juan Bautista.","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":"","schema":{"@context":"http://schema.org","@type":"Article","headline":"GeoZeum: A Personal Museum of Geology","datePublished":"2011-09-29T15:00:29.000Z","dateModified":"2011-10-05T22:21:44.000Z","image":"https://cdn.kqed.org/wp-content/uploads/2020/02/KQED-OG-Image@1x.png"}},"disqusIdentifier":"25495 http://science.kqed.org/quest/?p=25495","disqusUrl":"https://ww2.kqed.org/quest/2011/09/29/geozeum-a-personal-museum-of-geology/","disqusTitle":"GeoZeum: A Personal Museum of Geology","path":"/quest/25495/geozeum-a-personal-museum-of-geology","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cfigure id=\"attachment_25496\" class=\"wp-caption alignleft\" style=\"max-width: 300px\">\u003ca href=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/09/geozeumtop.jpg\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/09/geozeumtop-300x169.jpg\" alt=\"\" title=\"geozeumtop\" width=\"300\" height=\"169\" class=\"size-thumbnail wp-image-25496\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">GeoZeum is a brand-new boutique education center of geology in historic—and geologically rich—San Juan Bautista. Photos by Andrew Alden.\u003c/figcaption>\u003c/figure>\n\u003cp>Most of us have a retirement dream: What would we do once our daily grind is over? Retired geologists I know indulge their devotion to poetry, photography, winemaking, philosophy, or Burning Man. A common idea is to open a little rock shop. Phil Stoffer is a born teacher with a huge rock collection, and his retirement project is to run a little museum in San Juan Bautista, a superb place to personally introduce the pleasures and treasures of Earth science to all comers. \"It's all about keeping geology going,\" he says. I have seen nothing like it before.\u003c/p>\n\u003cp>Stoffer has dipped into a lot of the geologist's typical career options: mining, oil and gas, scientific librarian, college instructor, and website creator and field hand for the U.S. Geological Survey. He's collected rocks and fossils and photographed geology in all fifty states. All of that, experience and photos and specimens, is the nucleus of Stoffer's \u003ca href=\"http://www.geozeum.com/\">GeoZeum\u003c/a>, just a short stroll from the San Andreas fault and, of course, on the Web.\u003c/p>\n\u003cfigure id=\"attachment_25497\" class=\"wp-caption aligncenter\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/09/29/geozeum-a-personal-museum-of-geology/geozeumrox/\" rel=\"attachment wp-att-25497\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/09/geozeumrox.jpg\" alt=\"\" title=\"geozeumrox\" width=\"640\" height=\"360\" class=\"size-full wp-image-25497\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/09/geozeumrox.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/09/geozeumrox-400x225.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Some of the best rocks in GeoZeum are found near San Juan Bautista.\u003c/figcaption>\u003c/figure>\n\u003cp>GeoZeum has shelves of rocks, minerals and fossils. It also has tables covered with them, meant to be handled. It has an earthquake machine and a tsunami tank. It has big 3D photos of landforms and glasses to view them with. It even has a closet filled with fluorescent minerals. A lapidary lab is in the planning stage. And the key ingredient is the owner, eager to show and tell.\u003c/p>\n\u003cp>A project like GeoZeum relies on a lot of synergy. First, there's the Spanish mission in San Juan Bautista. California's unique \u003ca href=\"http://www.cuca.k12.ca.us/lessons/missions/contents/index.html\">4th-grade curriculum emphasizing the missions\u003c/a> brings busloads of children to San Juan Bautista. \u003ca href=\"http://www.san-juan-bautista.ca.us/\">The city itself is a draw for tourists\u003c/a>, too. The mission owes its very location to the scarp raised along the San Andreas fault, and more than any other California mission its history is tied to earthquakes.\u003c/p>\n\u003cfigure id=\"attachment_25498\" class=\"wp-caption aligncenter\" style=\"max-width: 500px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/09/29/geozeum-a-personal-museum-of-geology/geozeumsjbmission/\" rel=\"attachment wp-att-25498\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/09/geozeumSJBmission.jpg\" alt=\"\" title=\"geozeumSJBmission\" width=\"500\" height=\"350\" class=\"aligncenter size-full wp-image-25498\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/09/geozeumSJBmission.jpg 500w, https://ww2.kqed.org/app/uploads/sites/39/2011/09/geozeumSJBmission-400x280.jpg 400w\" sizes=\"(max-width: 500px) 100vw, 500px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">The San Andreas fault runs along the foot of the rise on which the San Juan Bautista mission sits. GeoZeum's Phil Stoffer leads walks here every weekend.\u003c/figcaption>\u003c/figure>\n\u003cp>Second, GeoZeum shares a building with \u003ca href=\"http://www.topsarockshop.com/index.htm\">TOPS A Rock Shop\u003c/a>, an uncommonly well-stocked example of its genre. TOPS will be a natural gathering place for the rock-and-mineral club that Stoffer is launching.\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>Third, San Juan Bautista is a remarkable nexus of geological sites every bit as interesting as the Bay Area. Indeed, just a million years ago you could say the area \u003ci>was\u003c/i> the Bay Area, because the rivers of the Central Valley reached the Pacific through here. The area is full of mines and quarries, several earthquake faults, and diverse packages of rocks that those faults have carried here from far away. The GeoZeum website has a lot of maps and other material about the area.\u003c/p>\n\u003cp>One of Stoffer's favorite places is the riverbed of the San Benito River, where the gravel contains an enormous variety of rock types. But when I visited him earlier this week, we went instead to Gabilan (Fremont) Peak and explored some old barite mines in the ancient marble that makes up the mountaintop. We brought along ultraviolet flashlights and admired the veins of blue and yellow fluorescence in the mine passages. Stoffer has dozens of ideas like these for geologic walks.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/09/29/geozeum-a-personal-museum-of-geology/geozeumsteps/\" rel=\"attachment wp-att-25499\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/09/geozeumsteps.jpg\" alt=\"\" title=\"geozeumsteps\" width=\"500\" height=\"410\" class=\"aligncenter size-full wp-image-25499\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/09/geozeumsteps.jpg 500w, https://ww2.kqed.org/app/uploads/sites/39/2011/09/geozeumsteps-400x328.jpg 400w\" sizes=\"(max-width: 500px) 100vw, 500px\">\u003c/a>\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>GeoZeum is already operating Thursday through Sunday, but its formal Grand Opening is October 15. Stoffer will welcome you to his museum, whether you're a kid, a fellow retired geologist or anything between. Just look for the dinosaur tracks on the sidewalk.\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/quest/25495/geozeum-a-personal-museum-of-geology","authors":["6228"],"categories":["quest_11"],"tags":["quest_1897","quest_13202","quest_2447","quest_2484","quest_10238"],"featImg":"quest_25496","label":"quest"},"quest_24405":{"type":"posts","id":"quest_24405","meta":{"index":"posts_1591205157","site":"quest","id":"24405","score":null,"sort":[1316545241000]},"guestAuthors":[],"slug":"the-shaking-table-at-uc-berkeley","title":"QUEST Lab: The Shaking Table at UC Berkeley","publishDate":1316545241,"format":"video","headTitle":"QUEST Lab | QUEST | KQED Science","labelTerm":{"term":13256,"site":"quest"},"content":"\u003cp>In 2008, I produced a QUEST TV feature story called, \"Hayward Fault: Predictable Peril\" (UPDATED: \u003ca href=\"http://ww2.kqed.org/quest/2015/10/14/the-hayward-fault-predictable-peril/\">The Hayward Fault: Overdue for Disaster\u003c/a>). The story focused on the earthquake fault that runs from San Jose in the south to San Pablo Bay in the East Bay of the San Francisco Bay Area. A magnitude 7 earthquake occurred along this fault in 1868 that killed several people and destroyed buildings throughout the East Bay as well as in San Francisco. The 1868 quake was referred to as 'the great earthquake' prior to the epic 1906 earthquake that happened along the San Andreas fault. \u003c/p>\n\u003cp>The gist of the 2008 TV story was that geologists are now able to use special paleoseismic techniques to analyze earthquake faults and determine their seismic history over several thousand years. By noticing patterns in earthquake activity over long periods of time, they can also make predictions about when major events are likely to happen in the future. They determined that a major event of 6.8 or higher happens every 140 years or so on the Hayward Fault. It's been 143 since the last one. \u003c/p>\n\u003cfigure id=\"attachment_24808\" class=\"wp-caption alignleft\" style=\"max-width: 300px\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/09/Shaking-Table_Khalid_6401-300x169.jpg\" alt=\"\" title=\"Shaking Table_Khalid_640\" width=\"300\" height=\"169\" class=\"size-thumbnail wp-image-24808\">\u003cfigcaption class=\"wp-caption-text\">Engineer Khalid Mosalam\u003c/figcaption>\u003c/figure>\n\u003cp>A 2003 report by the USGS found that there is a \u003ca href=\"http://earthquake.usgs.gov/regional/nca/wg02/results.php\">62% probability of at least one magnitude 6.7 or greater earthquake in the 3-decade interval 2003-2032 within the San Francisco Bay region\u003c/a>. With odds like this, I'm grateful that there are people like Khalid Mosalam and his colleagues at the Pacific Earthquake Engineering Research Center's Shaking Table Laboratory who dedicate their careers to learning how to make the built environment that we live in, work in and travel on more safe in an earthquake. \u003c/p>\n\u003cp>I'd included about a minute of video from the Shaking Table Lab in the 2008 piece but I always regretted that I wasn't able to show more of this facility. So when we started putting together an entire episode focused around the theme of earthquakes, I thought a short segment about the Shaking Table would be perfect for this show. \u003c/p>\n\u003cfigure id=\"attachment_24812\" class=\"wp-caption alignright\" style=\"max-width: 300px\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/09/Shaking-Table_electric_640-300x169.jpg\" alt=\"\" title=\"Shaking Table_electric_640\" width=\"300\" height=\"169\" class=\"size-thumbnail wp-image-24812\">\u003cfigcaption class=\"wp-caption-text\">Substation equipment getting shaken up on the table\u003c/figcaption>\u003c/figure>\n\u003cp>When we were there shooting in 2008, they were testing some electrical substation switches which were interesting but definitely not as dramatic as some of the other structures they build and shake in three axes, often until collapse. The generous engineers at PEER were able to provide us some videos of other structures they tested including a two story house, a masonry wall and a bridge pier support. The 20' x 20' table is one of the largest in the world to be able to move in three directions (translation and rotation) so, according to Mosalam, it's an extremely important piece of equipment at UC Berkeley and has contributed to important research that will result in people being safer when the next 'big one' hits. \u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\u003cp>\u003c/p>\n","blocks":[],"excerpt":"Khalid Mosalam and his colleagues at the Pacific Earthquake Engineering Research Center's Shaking Table Laboratory are helping to make communities safer in an earthquake. \r\n","status":"publish","parent":0,"modified":1460742884,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":7,"wordCount":478},"headData":{"title":"QUEST Lab: The Shaking Table at UC Berkeley | KQED","description":"Khalid Mosalam and his colleagues at the Pacific Earthquake Engineering Research Center's Shaking Table Laboratory are helping to make communities safer in an earthquake. \r\n","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":"","schema":{"@context":"http://schema.org","@type":"Article","headline":"QUEST Lab: The Shaking Table at UC Berkeley","datePublished":"2011-09-20T19:00:41.000Z","dateModified":"2016-04-15T17:54:44.000Z","image":"https://cdn.kqed.org/wp-content/uploads/2020/02/KQED-OG-Image@1x.png"}},"disqusIdentifier":"24405 http://science.kqed.org/quest/?p=24405","disqusUrl":"https://ww2.kqed.org/quest/2011/09/20/the-shaking-table-at-uc-berkeley/","disqusTitle":"QUEST Lab: The Shaking Table at UC Berkeley","videoEmbed":"https://www.youtube.com/watch?v=dW5Hxeg7vsc","path":"/quest/24405/the-shaking-table-at-uc-berkeley","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cp>In 2008, I produced a QUEST TV feature story called, \"Hayward Fault: Predictable Peril\" (UPDATED: \u003ca href=\"http://ww2.kqed.org/quest/2015/10/14/the-hayward-fault-predictable-peril/\">The Hayward Fault: Overdue for Disaster\u003c/a>). The story focused on the earthquake fault that runs from San Jose in the south to San Pablo Bay in the East Bay of the San Francisco Bay Area. A magnitude 7 earthquake occurred along this fault in 1868 that killed several people and destroyed buildings throughout the East Bay as well as in San Francisco. The 1868 quake was referred to as 'the great earthquake' prior to the epic 1906 earthquake that happened along the San Andreas fault. \u003c/p>\n\u003cp>The gist of the 2008 TV story was that geologists are now able to use special paleoseismic techniques to analyze earthquake faults and determine their seismic history over several thousand years. By noticing patterns in earthquake activity over long periods of time, they can also make predictions about when major events are likely to happen in the future. They determined that a major event of 6.8 or higher happens every 140 years or so on the Hayward Fault. It's been 143 since the last one. \u003c/p>\n\u003cfigure id=\"attachment_24808\" class=\"wp-caption alignleft\" style=\"max-width: 300px\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/09/Shaking-Table_Khalid_6401-300x169.jpg\" alt=\"\" title=\"Shaking Table_Khalid_640\" width=\"300\" height=\"169\" class=\"size-thumbnail wp-image-24808\">\u003cfigcaption class=\"wp-caption-text\">Engineer Khalid Mosalam\u003c/figcaption>\u003c/figure>\n\u003cp>A 2003 report by the USGS found that there is a \u003ca href=\"http://earthquake.usgs.gov/regional/nca/wg02/results.php\">62% probability of at least one magnitude 6.7 or greater earthquake in the 3-decade interval 2003-2032 within the San Francisco Bay region\u003c/a>. With odds like this, I'm grateful that there are people like Khalid Mosalam and his colleagues at the Pacific Earthquake Engineering Research Center's Shaking Table Laboratory who dedicate their careers to learning how to make the built environment that we live in, work in and travel on more safe in an earthquake. \u003c/p>\n\u003cp>I'd included about a minute of video from the Shaking Table Lab in the 2008 piece but I always regretted that I wasn't able to show more of this facility. So when we started putting together an entire episode focused around the theme of earthquakes, I thought a short segment about the Shaking Table would be perfect for this show. \u003c/p>\n\u003cfigure id=\"attachment_24812\" class=\"wp-caption alignright\" style=\"max-width: 300px\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/09/Shaking-Table_electric_640-300x169.jpg\" alt=\"\" title=\"Shaking Table_electric_640\" width=\"300\" height=\"169\" class=\"size-thumbnail wp-image-24812\">\u003cfigcaption class=\"wp-caption-text\">Substation equipment getting shaken up on the table\u003c/figcaption>\u003c/figure>\n\u003cp>When we were there shooting in 2008, they were testing some electrical substation switches which were interesting but definitely not as dramatic as some of the other structures they build and shake in three axes, often until collapse. The generous engineers at PEER were able to provide us some videos of other structures they tested including a two story house, a masonry wall and a bridge pier support. The 20' x 20' table is one of the largest in the world to be able to move in three directions (translation and rotation) so, according to Mosalam, it's an extremely important piece of equipment at UC Berkeley and has contributed to important research that will result in people being safer when the next 'big one' hits. \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>\u003cp>\u003c/p>\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/quest/24405/the-shaking-table-at-uc-berkeley","authors":["209"],"series":["quest_13256"],"categories":["quest_8","quest_11","quest_3233"],"tags":["quest_3923","quest_814","quest_907","quest_13197","quest_1080","quest_13200","quest_1325","quest_3351","quest_2141","quest_10188","quest_2349","quest_13","quest_2484","quest_10187","quest_2893"],"featImg":"quest_24804","label":"quest_13256"}},"programsReducer":{"possible":{"id":"possible","title":"Possible","info":"Possible is hosted by entrepreneur Reid Hoffman and writer Aria Finger. 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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. 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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. 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