Geological Outings Around the Bay: San Bruno Mountain
Geological Outings Around the Bay: Sunol Regional Wilderness
Side Trips from Interstate 5: Stony Creek Valley
Geological Outings Around the Bay: New Almaden
Geological Outings Around the Bay: Albany Hill
Geological Outings Around the Bay: The Great Slickenside of Corona Heights
Geological Outings Around the Bay: Stinson Beach
Geological Outings Around the Bay: Marin Headlands
Calera Limestone, a Gift from the Ancient Pacific
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Roadbuilders and railroad companies had to cut their way around this peak, which walls off San Francisco from the San Mateo Peninsula. Ranchers found no forage on it, and urbanizers made little headway on its rugged slopes. Megalomaniac planners once proposed blowing it up and using it as fill to turn the whole Bay into \"made land\" à la Foster City. And I'm sure the airline pilots at SFO would rather it weren't there either.\u003c/p>\n\u003cp>But three sets of users benefit from the mountain today. A quarry on its north side, in Brisbane, produces crushed rock. Several large broadcasting towers serve the city and peninsula from its long ridgetop. And the rest of us can hike this distinctive place in peace and relative quiet because San Bruno Mountain is a \u003ca href=\"http://www.parks.ca.gov/?page_id=518\">state park\u003c/a> that happens to be \u003ca href=\"http://www.co.sanmateo.ca.us/portal/site/parks/menuitem.f13bead76123ee4482439054d17332a0/?vgnextoid=cb7bc8909231e110VgnVCM1000001d37230aRCRD\">run by San Mateo County\u003c/a>.\u003c/p>\n\u003cp>The mountain serves as an island of habitat for some of the Bay Area's most iconic vegetation. As usual, the park literature will give you lots of detail on the plants and little about the rocks. But here's what we know, starting with the bedrock map (excerpted from the San Mateo County geologic map).\u003c/p>\n\u003cfigure id=\"attachment_49032\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2013/01/24/geological-outings-around-the-bay-san-bruno-mountain/sanbrunogeo600/\" rel=\"attachment wp-att-49032\">\u003cimg class=\"size-full wp-image-49032\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/01/sanbrunogeo600.png\" alt=\"Relevant map units: KJs, San Bruno Mountain sandstone; fs, fsr, Franciscan sandstone and sheared rock (melange); Qc, Colma Formation; Qcl, colluvium (debris); Qhaf, alluvial (stream) sediment; af, artificial fill. San Andreas fault at lower left corner.\" width=\"600\" height=\"500\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/01/sanbrunogeo600.png 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/01/sanbrunogeo600-400x333.png 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Relevant map units: KJs, San Bruno Mountain sandstone; fs, fsr, Franciscan sandstone and sheared rock (melange); Qc, Colma Formation; Qcl, colluvium (debris); Qhaf, alluvial (stream) sediment; af, artificial fill. San Andreas fault at lower left corner.\u003c/figcaption>\u003c/figure>\n\u003cp>The rock is composed of the coarse, raw sandstone known as \u003ca href=\"http://geology.about.com/od/rocks/ig/sedrockindex/rocpicgraywacke.htm\">graywacke\u003c/a> along with some finer-grained shale. It's strongly layered, as seen in this roadcut on the Bay side along Bayshore Boulevard.\u003c/p>\n\u003cfigure id=\"attachment_49036\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2013/01/24/geological-outings-around-the-bay-san-bruno-mountain/sanbrunomtn-outcrop/\" rel=\"attachment wp-att-49036\">\u003cimg class=\"size-full wp-image-49036\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/01/sanbrunomtn-outcrop.jpg\" alt=\"Photos by Andrew Alden\" width=\"600\" height=\"382\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/01/sanbrunomtn-outcrop.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/01/sanbrunomtn-outcrop-400x255.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Photos by Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>Here's a piece of it close up. The fresh rock, like you get in quarries, is gray, but at the surface it's brown because of iron oxides that form by weathering.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2013/01/24/geological-outings-around-the-bay-san-bruno-mountain/sanbrunomtn-handspec/\" rel=\"attachment wp-att-49035\">\u003cimg class=\"aligncenter size-full wp-image-49035\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/01/sanbrunomtn-handspec.jpg\" alt=\"sanbrunomtn-handspec\" width=\"600\" height=\"429\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/01/sanbrunomtn-handspec.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/01/sanbrunomtn-handspec-400x286.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>The sandstone has a lot of rock particles (lithics) in it, which are rich in iron and which break down readily under surface conditions. The thin brown crust is made of manganese oxides and is coating the surface of a fracture. As you turn pieces of it in the sunlight, you'll see tiny glittering flakes of white mica in it. Under the microscope it displays metamorphic minerals like pumpellyite, showing that the stone was subjected to heat and pressure after it formed.\u003c/p>\n\u003cp>This body of stone is classified as part of the Franciscan Complex, and correlated rocks (the San Bruno Mountain terrane) run north through western San Francisco, including Land's End. The Marin hills from \u003ca href=\"http://ww2.kqed.org/quest/2011/06/23/geological-outings-around-the-bay-stinson-beach/\">Stinson Beach\u003c/a> to southern Tomales Bay, across from Inverness, also are part of it. It has no fossils in it, but the experts say it formed in a marine setting.\u003c/p>\n\u003cp>A paper published in November 2012 (Dumitru et al., \u003ci>Geology\u003c/i>) assigned this rock an Early Eocene date (53-49 million years ago) and concluded that its sand came in a huge flood of sediment from Idaho, where vigorous volcanism was going on at the time. This was not what anyone thought. Most Franciscan sandstones, which are older, are thought to arise from the Californian upheavals in the Sierra Nevada region. Since that time the sandstone was heated and intruded by dikes of lava around 14-12 million years ago, while it was being manhandled by the San Andreas fault system like the rest of the Coast Ranges.\u003c/p>\n\u003cp>But knowing all that doesn't make San Bruno Mountain any more beautiful. And even on hazy days when the amazing view around is occluded, you can still admire the mountain itself.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2013/01/24/geological-outings-around-the-bay-san-bruno-mountain/sanbrunomtn-top/\" rel=\"attachment wp-att-49031\">\u003cimg class=\"aligncenter size-full wp-image-49031\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/01/sanbrunomtn-top.jpg\" alt=\"sanbrunomtn-top\" width=\"640\" height=\"360\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/01/sanbrunomtn-top.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2013/01/sanbrunomtn-top-400x225.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003c/p>\n\u003cp>Wrapping around the mountain's west side is the Colma Formation, which underlies the cemeteries of Colma and surroundings. This is a package of ice age sand, about 125,000 years old, that is the remains of the seashore at a time when the polar ice caps were even smaller than they are today. The ocean was about 10 meters higher than today, and sands from this time are found in the East Bay, all over San Francisco, and up and down the Pacific coast on \u003ca href=\"http://ww2.kqed.org/quest/2011/03/03/geological-outings-around-the-bay-pebble-beach/\">wave-cut platforms\u003c/a>. This map shows the situation at the time the Colma Formation was laid down.\u003c/p>\n\u003cfigure id=\"attachment_49033\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2013/01/24/geological-outings-around-the-bay-san-bruno-mountain/sanbrunomtn-bay125ka/\" rel=\"attachment wp-att-49033\">\u003cimg class=\"size-full wp-image-49033\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/01/sanbrunomtn-bay125ka.gif\" alt=\"US Geological Survey illustration\" width=\"600\" height=\"400\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">US Geological Survey illustration\u003c/figcaption>\u003c/figure>\n\u003cp>Much of the Colma Formation is recycled sand from the earlier Merced Formation, but surely the rain and waves here added lots of brown sand from San Bruno Mountain, too. You can see the Colma sands at the far west end of the park, in Daly City at the place on the geologic map where the third question mark sits marking the Hillside fault. This is an exposure in Hillside Park.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2013/01/24/geological-outings-around-the-bay-san-bruno-mountain/sanbrunomtn-sand/\" rel=\"attachment wp-att-49037\">\u003cimg class=\"aligncenter size-full wp-image-49037\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/01/sanbrunomtn-sand.jpg\" alt=\"sanbrunomtn-sand\" width=\"600\" height=\"450\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/01/sanbrunomtn-sand.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/01/sanbrunomtn-sand-400x300.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>Like the sandstone of San Bruno Mountain, this sand has a large proportion of lithics, accounting for its dark color. The area looks and feels just like beach dunes, but it's some 400 feet above the sea today. That is a testimony to the geologically rapid disruption of the Bay Area's land by the San Andreas fault system. Nearby is a small patch of dune habitat that San Bruno Mountain Watch is \u003ca href=\"http://www.mountainwatch.org/daly-city-dunes/\">keeping an eye on\u003c/a>.\u003c/p>\n\u003cp>Now is a good time to start visiting San Bruno Mountain instead of driving around it. The wildflower season is just starting, heralded by this ceanothus.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2013/01/24/geological-outings-around-the-bay-san-bruno-mountain/sanbrunomtn-cean/\" rel=\"attachment wp-att-49034\">\u003cimg class=\"aligncenter size-full wp-image-49034\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/01/sanbrunomtn-cean.jpg\" alt=\"sanbrunomtn-cean\" width=\"600\" height=\"448\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/01/sanbrunomtn-cean.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/01/sanbrunomtn-cean-400x299.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\n","blocks":[],"excerpt":"There is no Bay Area peak more central than San Bruno Mountain, and it's remarkably unspoiled.","status":"publish","parent":0,"modified":1475696828,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":19,"wordCount":888},"headData":{"title":"Geological Outings Around the Bay: San Bruno Mountain | KQED","description":"There is no Bay Area peak more central than San Bruno Mountain, and it's remarkably unspoiled.","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":""},"disqusIdentifier":"49030 http://science.kqed.org/quest/?p=49030","disqusUrl":"https://ww2.kqed.org/quest/2013/01/24/geological-outings-around-the-bay-san-bruno-mountain/","disqusTitle":"Geological Outings Around the Bay: San Bruno Mountain","path":"/quest/49030/geological-outings-around-the-bay-san-bruno-mountain","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cp>San Bruno Mountain has been in the way for a long time. Roadbuilders and railroad companies had to cut their way around this peak, which walls off San Francisco from the San Mateo Peninsula. Ranchers found no forage on it, and urbanizers made little headway on its rugged slopes. Megalomaniac planners once proposed blowing it up and using it as fill to turn the whole Bay into \"made land\" à la Foster City. And I'm sure the airline pilots at SFO would rather it weren't there either.\u003c/p>\n\u003cp>But three sets of users benefit from the mountain today. A quarry on its north side, in Brisbane, produces crushed rock. Several large broadcasting towers serve the city and peninsula from its long ridgetop. And the rest of us can hike this distinctive place in peace and relative quiet because San Bruno Mountain is a \u003ca href=\"http://www.parks.ca.gov/?page_id=518\">state park\u003c/a> that happens to be \u003ca href=\"http://www.co.sanmateo.ca.us/portal/site/parks/menuitem.f13bead76123ee4482439054d17332a0/?vgnextoid=cb7bc8909231e110VgnVCM1000001d37230aRCRD\">run by San Mateo County\u003c/a>.\u003c/p>\n\u003cp>The mountain serves as an island of habitat for some of the Bay Area's most iconic vegetation. As usual, the park literature will give you lots of detail on the plants and little about the rocks. But here's what we know, starting with the bedrock map (excerpted from the San Mateo County geologic map).\u003c/p>\n\u003cfigure id=\"attachment_49032\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2013/01/24/geological-outings-around-the-bay-san-bruno-mountain/sanbrunogeo600/\" rel=\"attachment wp-att-49032\">\u003cimg class=\"size-full wp-image-49032\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/01/sanbrunogeo600.png\" alt=\"Relevant map units: KJs, San Bruno Mountain sandstone; fs, fsr, Franciscan sandstone and sheared rock (melange); Qc, Colma Formation; Qcl, colluvium (debris); Qhaf, alluvial (stream) sediment; af, artificial fill. San Andreas fault at lower left corner.\" width=\"600\" height=\"500\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/01/sanbrunogeo600.png 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/01/sanbrunogeo600-400x333.png 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Relevant map units: KJs, San Bruno Mountain sandstone; fs, fsr, Franciscan sandstone and sheared rock (melange); Qc, Colma Formation; Qcl, colluvium (debris); Qhaf, alluvial (stream) sediment; af, artificial fill. San Andreas fault at lower left corner.\u003c/figcaption>\u003c/figure>\n\u003cp>The rock is composed of the coarse, raw sandstone known as \u003ca href=\"http://geology.about.com/od/rocks/ig/sedrockindex/rocpicgraywacke.htm\">graywacke\u003c/a> along with some finer-grained shale. It's strongly layered, as seen in this roadcut on the Bay side along Bayshore Boulevard.\u003c/p>\n\u003cfigure id=\"attachment_49036\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2013/01/24/geological-outings-around-the-bay-san-bruno-mountain/sanbrunomtn-outcrop/\" rel=\"attachment wp-att-49036\">\u003cimg class=\"size-full wp-image-49036\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/01/sanbrunomtn-outcrop.jpg\" alt=\"Photos by Andrew Alden\" width=\"600\" height=\"382\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/01/sanbrunomtn-outcrop.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/01/sanbrunomtn-outcrop-400x255.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Photos by Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>Here's a piece of it close up. The fresh rock, like you get in quarries, is gray, but at the surface it's brown because of iron oxides that form by weathering.\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/2013/01/24/geological-outings-around-the-bay-san-bruno-mountain/sanbrunomtn-handspec/\" rel=\"attachment wp-att-49035\">\u003cimg class=\"aligncenter size-full wp-image-49035\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/01/sanbrunomtn-handspec.jpg\" alt=\"sanbrunomtn-handspec\" width=\"600\" height=\"429\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/01/sanbrunomtn-handspec.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/01/sanbrunomtn-handspec-400x286.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>The sandstone has a lot of rock particles (lithics) in it, which are rich in iron and which break down readily under surface conditions. The thin brown crust is made of manganese oxides and is coating the surface of a fracture. As you turn pieces of it in the sunlight, you'll see tiny glittering flakes of white mica in it. Under the microscope it displays metamorphic minerals like pumpellyite, showing that the stone was subjected to heat and pressure after it formed.\u003c/p>\n\u003cp>This body of stone is classified as part of the Franciscan Complex, and correlated rocks (the San Bruno Mountain terrane) run north through western San Francisco, including Land's End. The Marin hills from \u003ca href=\"http://ww2.kqed.org/quest/2011/06/23/geological-outings-around-the-bay-stinson-beach/\">Stinson Beach\u003c/a> to southern Tomales Bay, across from Inverness, also are part of it. It has no fossils in it, but the experts say it formed in a marine setting.\u003c/p>\n\u003cp>A paper published in November 2012 (Dumitru et al., \u003ci>Geology\u003c/i>) assigned this rock an Early Eocene date (53-49 million years ago) and concluded that its sand came in a huge flood of sediment from Idaho, where vigorous volcanism was going on at the time. This was not what anyone thought. Most Franciscan sandstones, which are older, are thought to arise from the Californian upheavals in the Sierra Nevada region. Since that time the sandstone was heated and intruded by dikes of lava around 14-12 million years ago, while it was being manhandled by the San Andreas fault system like the rest of the Coast Ranges.\u003c/p>\n\u003cp>But knowing all that doesn't make San Bruno Mountain any more beautiful. And even on hazy days when the amazing view around is occluded, you can still admire the mountain itself.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2013/01/24/geological-outings-around-the-bay-san-bruno-mountain/sanbrunomtn-top/\" rel=\"attachment wp-att-49031\">\u003cimg class=\"aligncenter size-full wp-image-49031\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/01/sanbrunomtn-top.jpg\" alt=\"sanbrunomtn-top\" width=\"640\" height=\"360\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/01/sanbrunomtn-top.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2013/01/sanbrunomtn-top-400x225.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003c/p>\n\u003cp>Wrapping around the mountain's west side is the Colma Formation, which underlies the cemeteries of Colma and surroundings. This is a package of ice age sand, about 125,000 years old, that is the remains of the seashore at a time when the polar ice caps were even smaller than they are today. The ocean was about 10 meters higher than today, and sands from this time are found in the East Bay, all over San Francisco, and up and down the Pacific coast on \u003ca href=\"http://ww2.kqed.org/quest/2011/03/03/geological-outings-around-the-bay-pebble-beach/\">wave-cut platforms\u003c/a>. This map shows the situation at the time the Colma Formation was laid down.\u003c/p>\n\u003cfigure id=\"attachment_49033\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2013/01/24/geological-outings-around-the-bay-san-bruno-mountain/sanbrunomtn-bay125ka/\" rel=\"attachment wp-att-49033\">\u003cimg class=\"size-full wp-image-49033\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/01/sanbrunomtn-bay125ka.gif\" alt=\"US Geological Survey illustration\" width=\"600\" height=\"400\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">US Geological Survey illustration\u003c/figcaption>\u003c/figure>\n\u003cp>Much of the Colma Formation is recycled sand from the earlier Merced Formation, but surely the rain and waves here added lots of brown sand from San Bruno Mountain, too. You can see the Colma sands at the far west end of the park, in Daly City at the place on the geologic map where the third question mark sits marking the Hillside fault. This is an exposure in Hillside Park.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2013/01/24/geological-outings-around-the-bay-san-bruno-mountain/sanbrunomtn-sand/\" rel=\"attachment wp-att-49037\">\u003cimg class=\"aligncenter size-full wp-image-49037\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/01/sanbrunomtn-sand.jpg\" alt=\"sanbrunomtn-sand\" width=\"600\" height=\"450\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/01/sanbrunomtn-sand.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/01/sanbrunomtn-sand-400x300.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>Like the sandstone of San Bruno Mountain, this sand has a large proportion of lithics, accounting for its dark color. The area looks and feels just like beach dunes, but it's some 400 feet above the sea today. That is a testimony to the geologically rapid disruption of the Bay Area's land by the San Andreas fault system. Nearby is a small patch of dune habitat that San Bruno Mountain Watch is \u003ca href=\"http://www.mountainwatch.org/daly-city-dunes/\">keeping an eye on\u003c/a>.\u003c/p>\n\u003cp>Now is a good time to start visiting San Bruno Mountain instead of driving around it. The wildflower season is just starting, heralded by this ceanothus.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2013/01/24/geological-outings-around-the-bay-san-bruno-mountain/sanbrunomtn-cean/\" rel=\"attachment wp-att-49034\">\u003cimg class=\"aligncenter size-full wp-image-49034\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/01/sanbrunomtn-cean.jpg\" alt=\"sanbrunomtn-cean\" width=\"600\" height=\"448\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/01/sanbrunomtn-cean.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/01/sanbrunomtn-cean-400x299.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/quest/49030/geological-outings-around-the-bay-san-bruno-mountain","authors":["6228"],"categories":["quest_11"],"tags":["quest_11699","quest_11697","quest_11698","quest_3580","quest_13","quest_11696"],"featImg":"quest_49031","label":"quest"},"quest_41176":{"type":"posts","id":"quest_41176","meta":{"index":"posts_1591205157","site":"quest","id":"41176","score":null,"sort":[1342730570000]},"guestAuthors":[],"slug":"geological-outings-around-the-bay-sunol-regional-wilderness","title":"Geological Outings Around the Bay: Sunol Regional Wilderness","publishDate":1342730570,"format":"standard","headTitle":"QUEST | KQED Science","labelTerm":{"site":"quest"},"content":"\u003cfigure id=\"attachment_41178\" class=\"wp-caption aligncenter\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/07/19/geological-outings-around-the-bay-sunol-regional-wilderness/sunoltop/\" rel=\"attachment wp-att-41178\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/07/sunoltop.jpg\" alt=\"\" title=\"sunoltop\" width=\"640\" height=\"360\" class=\"size-full wp-image-41178\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunoltop.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunoltop-400x225.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Flag Hill, made up of fossiliferous sandstone of the Briones Formation, overlooks the Sunol Regional Wilderness. Photos by Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>The \u003ca href=\"http://www.ebparks.org/parks/sunol/\">Sunol Regional Wilderness\u003c/a>, part of the \u003ca href=\"http://www.ebparks.org/\">East Bay Regional Park District\u003c/a>, is a great place for many different students of nature and lovers of the outdoors. Here's how it looks to geology aficionados.\u003c/p>\n\u003cp>The park is near the village of Sunol, south of where state route 84 meets Interstate 680. As you approach the park on Calaveras Road, you are driving pretty much directly on the Calaveras fault, which stretches from the Hollister area north past Pleasanton. It's due east of Fremont, behind Mission and Monument Peaks. That set of mountains is a splinter of crustal rocks raised by the interaction of the Calaveras and Hayward faults on either side.\u003c/p>\n\u003cp>The park's bedrock geology is a mixture of relatively young marine sandstone and metamorphic rocks of the much older Franciscan Complex (map from \u003ca href=\"http://pubs.usgs.gov/of/1996/of96-252/almap.pdf\">USGS OF96-252\u003c/a>).\u003c/p>\n\u003cfigure id=\"attachment_41181\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/07/19/geological-outings-around-the-bay-sunol-regional-wilderness/sunolmap2/\" rel=\"attachment wp-att-41181\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/07/sunolmap2.png\" alt=\"\" title=\"sunolmap2\" width=\"600\" height=\"450\" class=\"size-full wp-image-41181\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunolmap2.png 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunolmap2-400x300.png 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Sunol Regional Wilderness is east of the Calaveras fault. LY, Little Yosemite; FH, Flag Hill; P, southern parking lot. Tan colors are young sandstones of the Briones Formation and related units; green is Great Valley Sequence sandstone of Cretaceous age; blues and purples are Franciscan rocks including melange, graywacke (sandstone) and serpentinite.\u003c/figcaption>\u003c/figure>\n\u003cp>The area, like the rest of the Bay Area, has a complex and continuing history of uplift and erosion and sideways movement on our major strike-slip faults. There are occasional bedrock terraces like this one that mark previous levels of Alameda Creek, at times when it had the leisure to cut its streambed wide into the surrounding hills.\u003c/p>\n\u003cfigure id=\"attachment_41185\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/07/19/geological-outings-around-the-bay-sunol-regional-wilderness/sunolterrace/\" rel=\"attachment wp-att-41185\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/07/sunolterrace.jpg\" alt=\"\" title=\"sunolterrace\" width=\"600\" height=\"424\" class=\"size-full wp-image-41185\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunolterrace.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunolterrace-400x283.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Beneath a thin veneer of stream gravel lies solid bedrock: a stream-cut platform.\u003c/figcaption>\u003c/figure>\n\u003cp>The eastern part of the park is archetypical Franciscan melange country, like that found up and down the Diablo Range. Melange is an intimate mixture of sandstone, basalt, chert and serpentinite, the four major Franciscan rock types. The land it underlies is an intricate set of slopes and peaks, laced with old and young landslide scars and dotted with \"knockers\" of resistant rock.\u003c/p>\n\u003cfigure id=\"attachment_41180\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/07/19/geological-outings-around-the-bay-sunol-regional-wilderness/sunolknocker/\" rel=\"attachment wp-att-41180\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/07/sunolknocker.jpg\" alt=\"\" title=\"sunolknocker\" width=\"600\" height=\"450\" class=\"size-full wp-image-41180\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunolknocker.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunolknocker-400x300.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Melange country, with the Mission Hills beyond the Calaveras fault. Note the radio towers of Monument and Mission Peaks.\u003c/figcaption>\u003c/figure>\n\u003cp>Some of the complexity underneath can be seen in this detailed geologic map prepared by Franciscan specialist John Wakabayashi of Cal State Fresno (\u003ca href=\"http://sanjoaquingeologicalsociety.org/presentation/2011SJGSMelanges_sm.ppt\">from a 2011 Powerpoint presentation\u003c/a>).\u003c/p>\n\u003cfigure id=\"attachment_41182\" class=\"wp-caption aligncenter\" style=\"max-width: 697px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/07/19/geological-outings-around-the-bay-sunol-regional-wilderness/sunolmap/\" rel=\"attachment wp-att-41182\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/07/sunolmap.png\" alt=\"\" title=\"sunolmap\" width=\"697\" height=\"715\" class=\"size-full wp-image-41182\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunolmap.png 697w, https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunolmap-400x410.png 400w, https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunolmap-32x32.png 32w\" sizes=\"(max-width: 697px) 100vw, 697px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Click the map for the full-size version.\u003c/figcaption>\u003c/figure>\n\u003cp>Serpentinite and related high-grade metamorphic rocks thread through the land like the dark in a marble cake. The photo doesn't do justice to the blue of the serpentinite in this exposure. \u003c/p>\n\u003cfigure id=\"attachment_41184\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/07/19/geological-outings-around-the-bay-sunol-regional-wilderness/sunolserp/\" rel=\"attachment wp-att-41184\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/07/sunolserp.jpg\" alt=\"\" title=\"sunolserp\" width=\"600\" height=\"400\" class=\"size-full wp-image-41184\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunolserp.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunolserp-400x267.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Upper reaches of the \"W\" Tree Rock Scramble.\u003c/figcaption>\u003c/figure>\n\u003cp>If you take yourself off the trail into these hills, watch for snakes and poison oak, but also be on the lookout for beauties like this garnet amphibolite among the knockers. It's just as blue as new jeans. (Admire it, but don't hammer it. Collecting is forbidden in all parks.)\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/07/19/geological-outings-around-the-bay-sunol-regional-wilderness/sunolamph/\" rel=\"attachment wp-att-41179\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/07/sunolamph.jpg\" alt=\"\" title=\"sunolamph\" width=\"600\" height=\"425\" class=\"aligncenter size-full wp-image-41179\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunolamph.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunolamph-400x283.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>The details and structures of Sunol's rocks are yielding new insights to students of the Franciscan. That is scientifically important because the Franciscan is a major part of the subduction zone in California, which in turn is the world's best example of subduction-related rocks. Sunol, therefore, is a star player at the frontier of plate tectonics itself.\u003c/p>\n\n","blocks":[],"excerpt":"The Franciscan rocks of Sunol Regional Wilderness are star players at the frontier of plate tectonics.","status":"publish","parent":0,"modified":1344279280,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":12,"wordCount":558},"headData":{"title":"Geological Outings Around the Bay: Sunol Regional Wilderness | KQED","description":"The Franciscan rocks of Sunol Regional Wilderness are star players at the frontier of plate tectonics.","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":""},"disqusIdentifier":"41176 http://science.kqed.org/quest/?p=41176","disqusUrl":"https://ww2.kqed.org/quest/2012/07/19/geological-outings-around-the-bay-sunol-regional-wilderness/","disqusTitle":"Geological Outings Around the Bay: Sunol Regional Wilderness","path":"/quest/41176/geological-outings-around-the-bay-sunol-regional-wilderness","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cfigure id=\"attachment_41178\" class=\"wp-caption aligncenter\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/07/19/geological-outings-around-the-bay-sunol-regional-wilderness/sunoltop/\" rel=\"attachment wp-att-41178\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/07/sunoltop.jpg\" alt=\"\" title=\"sunoltop\" width=\"640\" height=\"360\" class=\"size-full wp-image-41178\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunoltop.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunoltop-400x225.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Flag Hill, made up of fossiliferous sandstone of the Briones Formation, overlooks the Sunol Regional Wilderness. Photos by Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>The \u003ca href=\"http://www.ebparks.org/parks/sunol/\">Sunol Regional Wilderness\u003c/a>, part of the \u003ca href=\"http://www.ebparks.org/\">East Bay Regional Park District\u003c/a>, is a great place for many different students of nature and lovers of the outdoors. Here's how it looks to geology aficionados.\u003c/p>\n\u003cp>The park is near the village of Sunol, south of where state route 84 meets Interstate 680. As you approach the park on Calaveras Road, you are driving pretty much directly on the Calaveras fault, which stretches from the Hollister area north past Pleasanton. It's due east of Fremont, behind Mission and Monument Peaks. That set of mountains is a splinter of crustal rocks raised by the interaction of the Calaveras and Hayward faults on either side.\u003c/p>\n\u003cp>The park's bedrock geology is a mixture of relatively young marine sandstone and metamorphic rocks of the much older Franciscan Complex (map from \u003ca href=\"http://pubs.usgs.gov/of/1996/of96-252/almap.pdf\">USGS OF96-252\u003c/a>).\u003c/p>\n\u003cfigure id=\"attachment_41181\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/07/19/geological-outings-around-the-bay-sunol-regional-wilderness/sunolmap2/\" rel=\"attachment wp-att-41181\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/07/sunolmap2.png\" alt=\"\" title=\"sunolmap2\" width=\"600\" height=\"450\" class=\"size-full wp-image-41181\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunolmap2.png 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunolmap2-400x300.png 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Sunol Regional Wilderness is east of the Calaveras fault. LY, Little Yosemite; FH, Flag Hill; P, southern parking lot. Tan colors are young sandstones of the Briones Formation and related units; green is Great Valley Sequence sandstone of Cretaceous age; blues and purples are Franciscan rocks including melange, graywacke (sandstone) and serpentinite.\u003c/figcaption>\u003c/figure>\n\u003cp>The area, like the rest of the Bay Area, has a complex and continuing history of uplift and erosion and sideways movement on our major strike-slip faults. There are occasional bedrock terraces like this one that mark previous levels of Alameda Creek, at times when it had the leisure to cut its streambed wide into the surrounding hills.\u003c/p>\n\u003cfigure id=\"attachment_41185\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/07/19/geological-outings-around-the-bay-sunol-regional-wilderness/sunolterrace/\" rel=\"attachment wp-att-41185\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/07/sunolterrace.jpg\" alt=\"\" title=\"sunolterrace\" width=\"600\" height=\"424\" class=\"size-full wp-image-41185\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunolterrace.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunolterrace-400x283.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Beneath a thin veneer of stream gravel lies solid bedrock: a stream-cut platform.\u003c/figcaption>\u003c/figure>\n\u003cp>The eastern part of the park is archetypical Franciscan melange country, like that found up and down the Diablo Range. Melange is an intimate mixture of sandstone, basalt, chert and serpentinite, the four major Franciscan rock types. The land it underlies is an intricate set of slopes and peaks, laced with old and young landslide scars and dotted with \"knockers\" of resistant rock.\u003c/p>\n\u003cfigure id=\"attachment_41180\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/07/19/geological-outings-around-the-bay-sunol-regional-wilderness/sunolknocker/\" rel=\"attachment wp-att-41180\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/07/sunolknocker.jpg\" alt=\"\" title=\"sunolknocker\" width=\"600\" height=\"450\" class=\"size-full wp-image-41180\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunolknocker.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunolknocker-400x300.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Melange country, with the Mission Hills beyond the Calaveras fault. Note the radio towers of Monument and Mission Peaks.\u003c/figcaption>\u003c/figure>\n\u003cp>Some of the complexity underneath can be seen in this detailed geologic map prepared by Franciscan specialist John Wakabayashi of Cal State Fresno (\u003ca href=\"http://sanjoaquingeologicalsociety.org/presentation/2011SJGSMelanges_sm.ppt\">from a 2011 Powerpoint presentation\u003c/a>).\u003c/p>\n\u003cfigure id=\"attachment_41182\" class=\"wp-caption aligncenter\" style=\"max-width: 697px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/07/19/geological-outings-around-the-bay-sunol-regional-wilderness/sunolmap/\" rel=\"attachment wp-att-41182\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/07/sunolmap.png\" alt=\"\" title=\"sunolmap\" width=\"697\" height=\"715\" class=\"size-full wp-image-41182\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunolmap.png 697w, https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunolmap-400x410.png 400w, https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunolmap-32x32.png 32w\" sizes=\"(max-width: 697px) 100vw, 697px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Click the map for the full-size version.\u003c/figcaption>\u003c/figure>\n\u003cp>Serpentinite and related high-grade metamorphic rocks thread through the land like the dark in a marble cake. The photo doesn't do justice to the blue of the serpentinite in this exposure. \u003c/p>\n\u003cfigure id=\"attachment_41184\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/07/19/geological-outings-around-the-bay-sunol-regional-wilderness/sunolserp/\" rel=\"attachment wp-att-41184\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/07/sunolserp.jpg\" alt=\"\" title=\"sunolserp\" width=\"600\" height=\"400\" class=\"size-full wp-image-41184\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunolserp.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunolserp-400x267.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Upper reaches of the \"W\" Tree Rock Scramble.\u003c/figcaption>\u003c/figure>\n\u003cp>If you take yourself off the trail into these hills, watch for snakes and poison oak, but also be on the lookout for beauties like this garnet amphibolite among the knockers. It's just as blue as new jeans. (Admire it, but don't hammer it. Collecting is forbidden in all parks.)\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/2012/07/19/geological-outings-around-the-bay-sunol-regional-wilderness/sunolamph/\" rel=\"attachment wp-att-41179\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/07/sunolamph.jpg\" alt=\"\" title=\"sunolamph\" width=\"600\" height=\"425\" class=\"aligncenter size-full wp-image-41179\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunolamph.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/07/sunolamph-400x283.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>The details and structures of Sunol's rocks are yielding new insights to students of the Franciscan. That is scientifically important because the Franciscan is a major part of the subduction zone in California, which in turn is the world's best example of subduction-related rocks. Sunol, therefore, is a star player at the frontier of plate tectonics itself.\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/quest/41176/geological-outings-around-the-bay-sunol-regional-wilderness","authors":["6228"],"categories":["quest_11"],"tags":["quest_3492","quest_3580","quest_13200","quest_13202","quest_3747","quest_2589","quest_2590","quest_9979"],"featImg":"quest_41178","label":"quest"},"quest_40264":{"type":"posts","id":"quest_40264","meta":{"index":"posts_1591205157","site":"quest","id":"40264","score":null,"sort":[1340910402000]},"guestAuthors":[],"slug":"side-trips-from-interstate-5-stony-creek-valley","title":"Side Trips from Interstate 5: Stony Creek Valley","publishDate":1340910402,"format":"standard","headTitle":"QUEST | KQED Science","labelTerm":{"site":"quest"},"content":"\u003cp>Anyone looking at the Sacramento Valley in a satellite view surely wonders about the eastern edge of the Coast Range, a belt of striking corrugated terrain running up the west side from the Bay Area almost all the way to Redding. I'm here to tell you that it's extremely picturesque country. Geologically, it consists of the thick, tilted-up Great Valley Sequence of sedimentary rocks and the older, underlying Franciscan Complex metamorphic rocks farther west.\u003c/p>\n\u003cp>As you go north on I-5 you pass four towns that I think of as the four W's: Winters, Woodland, Williams and Willows. Today's sample of this district is a loop into the corrugated country starting at Willows and ending back at I-5 in Orland or Corning; take your choice. Here's the route (created on \u003ca href=\"http://www.gmap-pedometer.com/\">gmap-pedometer.com\u003c/a>):\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/06/28/side-trips-from-interstate-5-stony-creek-valley/stonycrvlymaptopo/\" rel=\"attachment wp-att-40265\">\u003cimg class=\"aligncenter size-full wp-image-40265\" title=\"stonycrvlymaptopo\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/06/stonycrvlymaptopo.png\" alt=\"\" width=\"496\" height=\"420\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycrvlymaptopo.png 496w, https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycrvlymaptopo-400x339.png 400w\" sizes=\"(max-width: 496px) 100vw, 496px\">\u003c/a>\u003c/p>\n\u003cp>And here's the geology en route (created from the \u003ca href=\"http://www.quake.ca.gov/gmaps/GMC/stategeologicmap.html\">interactive state geologic map\u003c/a>):\u003c/p>\n\u003cfigure id=\"attachment_40276\" class=\"wp-caption aligncenter\" style=\"max-width: 500px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/06/28/side-trips-from-interstate-5-stony-creek-valley/stonycrvlymapgeo/\" rel=\"attachment wp-att-40276\">\u003cimg class=\"size-full wp-image-40276\" title=\"stonycrvlymapgeo\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/06/stonycrvlymapgeo.png\" alt=\"\" width=\"500\" height=\"420\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycrvlymapgeo.png 500w, https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycrvlymapgeo-400x336.png 400w\" sizes=\"(max-width: 500px) 100vw, 500px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">A belt of serpentinite (purple) separates Franciscan metamorphic rocks on the west from Great Valley Sequence sedimentary rocks on the east (J, Jurassic; Kl and Ku, lower and upper Cretaceous). Overlain on these are Tertiary volcaniclastic and volcanic rocks (Tvp and Tv) and younger outwash deposits (QPc). Pink lines mark structures: anticlines and synclines.\u003c/figcaption>\u003c/figure>\n\u003cp>State route 162 leads west from Willows into the series of ridges formed by the uptilted Great Valley Sequence rocks. These are the same formations, of the same age, that \u003ca href=\"http://ww2.kqed.org/quest/2012/01/26/geological-outings-around-the-bay-mount-vaca-and-the-monticello-dam/\">I showed you north of Fairfield\u003c/a>.\u003c/p>\n\u003cfigure id=\"attachment_40266\" class=\"wp-caption aligncenter\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/06/28/side-trips-from-interstate-5-stony-creek-valley/stonycreekvalley1/\" rel=\"attachment wp-att-40266\">\u003cimg class=\"size-full wp-image-40266\" title=\"stonycreekvalley1\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/06/stonycreekvalley1.jpg\" alt=\"\" width=\"640\" height=\"360\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley1.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley1-400x225.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">All photos by Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>Beyond a series of these ridges is a long valley underlain by fine-grained Jurassic rocks, the oldest part of the Great Valley Sequence. The valley is punctuated by \u003ca href=\"http://geology.about.com/od/structureslandforms/ig/erosional/hogback.htm\">hogback ridges\u003c/a> that affect the course of the roads. Parts of the valley have been turned into reservoirs, like Stony Gorge Reservoir.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/06/28/side-trips-from-interstate-5-stony-creek-valley/stonycreekvalley02/\" rel=\"attachment wp-att-40267\">\u003cimg class=\"aligncenter size-full wp-image-40267\" title=\"stonycreekvalley02\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/06/stonycreekvalley02.jpg\" alt=\"\" width=\"600\" height=\"400\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley02.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley02-400x267.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>A new reservoir is planned south of here around the settlement of Sites that will be used to regulate streamflow in the northern Sacramento Valley and allow older structures to be modified.\u003c/p>\n\u003cp>Eventually route 162 crosses Stony Creek, where the Great Valley Sequence rocks are spectacularly exposed in a washboard streambed.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/06/28/side-trips-from-interstate-5-stony-creek-valley/stonycreekvalley03/\" rel=\"attachment wp-att-40268\">\u003cimg class=\"aligncenter size-full wp-image-40268\" title=\"stonycreekvalley03\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/06/stonycreekvalley03.jpg\" alt=\"\" width=\"600\" height=\"470\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley03.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley03-400x313.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>Turn north here on 162 and follow the river, taking note of the different levels of stream terraces built when Stony Creek had not eroded as far down as it has today.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/06/28/side-trips-from-interstate-5-stony-creek-valley/stonycreekvalley04/\" rel=\"attachment wp-att-40269\">\u003cimg class=\"aligncenter size-full wp-image-40269\" title=\"stonycreekvalley04\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/06/stonycreekvalley04.jpg\" alt=\"\" width=\"600\" height=\"391\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley04.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley04-400x261.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>When 162 turns west again, continue north on county road 306. (At the moment, the route on 162 through the Coast Range to Covelo is closed.) In late April when I visited, the countryside was a picture-postcard experience.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/06/28/side-trips-from-interstate-5-stony-creek-valley/stonycreekvalley05/\" rel=\"attachment wp-att-40270\">\u003cimg class=\"aligncenter size-full wp-image-40270\" title=\"stonycreekvalley05\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/06/stonycreekvalley05.jpg\" alt=\"\" width=\"600\" height=\"441\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley05.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley05-400x294.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>If you like, take 162 a ways into the Franciscan country, or for a more intimate experience take county road 313 west instead, a well-graded dirt road just three miles to the north. (That's the spur shown on the route map.) In clear weather, vistas spread out as you rise. Here's the view south down the valley of Stony Creek:\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/06/28/side-trips-from-interstate-5-stony-creek-valley/stonycreekvalley06/\" rel=\"attachment wp-att-40271\">\u003cimg class=\"aligncenter size-full wp-image-40271\" title=\"stonycreekvalley06\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/06/stonycreekvalley06.jpg\" alt=\"\" width=\"600\" height=\"467\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley06.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley06-400x311.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>And here's the view northeast toward the Great Valley over the sawtooth ridges of Great Valley Sequence rocks:\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/06/28/side-trips-from-interstate-5-stony-creek-valley/stonycreekvalley07/\" rel=\"attachment wp-att-40272\">\u003cimg class=\"aligncenter size-full wp-image-40272\" title=\"stonycreekvalley07\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/06/stonycreekvalley07.jpg\" alt=\"\" width=\"600\" height=\"434\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley07.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley07-400x289.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>Ahead is the rugged topography held up by the Franciscan Complex. Note how the vegetation has changed as well as the bones of the land. The highest peak is Red Mountain. The contact between these two highly contrasting geologic provinces is the Coast Range thrust, which has tilted up the rocks on the east side like a pet pushing under a bedsheet.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/06/28/side-trips-from-interstate-5-stony-creek-valley/stonycreekvalley08/\" rel=\"attachment wp-att-40273\">\u003cimg class=\"aligncenter size-full wp-image-40273\" title=\"stonycreekvalley08\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/06/stonycreekvalley08.jpg\" alt=\"\" width=\"600\" height=\"450\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley08.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley08-400x300.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>Watch the roadcuts, too, for exposures of \u003ca href=\"http://ww2.kqed.org/quest/2010/08/05/learn-the-facts-about-serpentinite-before-its-removed-as-californias-state-rock/\">serpentinite\u003c/a>, or \u003ca href=\"http://geology.about.com/od/rocks/ig/metrockindex/rocpicschist.htm\">schist\u003c/a> like this:\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/06/28/side-trips-from-interstate-5-stony-creek-valley/stonycreekvalley09/\" rel=\"attachment wp-att-40274\">\u003cimg class=\"aligncenter size-full wp-image-40274\" title=\"stonycreekvalley09\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/06/stonycreekvalley09.jpg\" alt=\"\" width=\"600\" height=\"498\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley09.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley09-400x332.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>Step out and collect a specimen or two if you like; this is public land. Chrome ore was mined around here, in and around the serpentinite belt. The tiny settlement of Chrome marks the site of one former mine.\u003c/p>\n\u003cp>Road 306 butts into Newville Road, and that's where you turn back toward the freeway. But there's one more attraction as you go forward through geologic time into the Sacramento Valley: the unexpected Black Butte. This is a segment of a huge lava flow, the \u003ca href=\"http://myweb.csuchico.edu/~rteasdale/Lovejoy.html\">Lovejoy Basalt\u003c/a>, that once crossed the Valley from a source in the northern Sierra Nevada, reaching from here south to Vacaville. Black Butte was raised by a fault, sparing it from erosional destruction. The lake around it is artificial, and the whole is a splendid park.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/06/28/side-trips-from-interstate-5-stony-creek-valley/stonycreekvalley10/\" rel=\"attachment wp-att-40275\">\u003cimg class=\"aligncenter size-full wp-image-40275\" title=\"stonycreekvalley10\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/06/stonycreekvalley10.jpg\" alt=\"\" width=\"600\" height=\"450\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley10.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley10-400x300.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>To get to Corning requires a short backtrack to Black Butte Road, which crosses orchard lands and offers low-key views (which I believe will show Mount Shasta on clear days). You may also take a shorter side trip starting in Orland that visits Black Butte alone. But once you get behind the curtain of those serrated Great Valley Sequence hills, you'll never look at this stretch of I-5 the same way again.\u003c/p>\n\n","blocks":[],"excerpt":"Visit some classic rocks in the little-trafficked country lying just over the hills of the western Sacramento Valley.","status":"publish","parent":0,"modified":1341603816,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":28,"wordCount":787},"headData":{"title":"Side Trips from Interstate 5: Stony Creek Valley | KQED","description":"Visit some classic rocks in the little-trafficked country lying just over the hills of the western Sacramento Valley.","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":""},"disqusIdentifier":"40264 http://science.kqed.org/quest/?p=40264","disqusUrl":"https://ww2.kqed.org/quest/2012/06/28/side-trips-from-interstate-5-stony-creek-valley/","disqusTitle":"Side Trips from Interstate 5: Stony Creek Valley","path":"/quest/40264/side-trips-from-interstate-5-stony-creek-valley","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cp>Anyone looking at the Sacramento Valley in a satellite view surely wonders about the eastern edge of the Coast Range, a belt of striking corrugated terrain running up the west side from the Bay Area almost all the way to Redding. I'm here to tell you that it's extremely picturesque country. Geologically, it consists of the thick, tilted-up Great Valley Sequence of sedimentary rocks and the older, underlying Franciscan Complex metamorphic rocks farther west.\u003c/p>\n\u003cp>As you go north on I-5 you pass four towns that I think of as the four W's: Winters, Woodland, Williams and Willows. Today's sample of this district is a loop into the corrugated country starting at Willows and ending back at I-5 in Orland or Corning; take your choice. Here's the route (created on \u003ca href=\"http://www.gmap-pedometer.com/\">gmap-pedometer.com\u003c/a>):\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/06/28/side-trips-from-interstate-5-stony-creek-valley/stonycrvlymaptopo/\" rel=\"attachment wp-att-40265\">\u003cimg class=\"aligncenter size-full wp-image-40265\" title=\"stonycrvlymaptopo\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/06/stonycrvlymaptopo.png\" alt=\"\" width=\"496\" height=\"420\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycrvlymaptopo.png 496w, https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycrvlymaptopo-400x339.png 400w\" sizes=\"(max-width: 496px) 100vw, 496px\">\u003c/a>\u003c/p>\n\u003cp>And here's the geology en route (created from the \u003ca href=\"http://www.quake.ca.gov/gmaps/GMC/stategeologicmap.html\">interactive state geologic map\u003c/a>):\u003c/p>\n\u003cfigure id=\"attachment_40276\" class=\"wp-caption aligncenter\" style=\"max-width: 500px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/06/28/side-trips-from-interstate-5-stony-creek-valley/stonycrvlymapgeo/\" rel=\"attachment wp-att-40276\">\u003cimg class=\"size-full wp-image-40276\" title=\"stonycrvlymapgeo\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/06/stonycrvlymapgeo.png\" alt=\"\" width=\"500\" height=\"420\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycrvlymapgeo.png 500w, https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycrvlymapgeo-400x336.png 400w\" sizes=\"(max-width: 500px) 100vw, 500px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">A belt of serpentinite (purple) separates Franciscan metamorphic rocks on the west from Great Valley Sequence sedimentary rocks on the east (J, Jurassic; Kl and Ku, lower and upper Cretaceous). Overlain on these are Tertiary volcaniclastic and volcanic rocks (Tvp and Tv) and younger outwash deposits (QPc). Pink lines mark structures: anticlines and synclines.\u003c/figcaption>\u003c/figure>\n\u003cp>State route 162 leads west from Willows into the series of ridges formed by the uptilted Great Valley Sequence rocks. These are the same formations, of the same age, that \u003ca href=\"http://ww2.kqed.org/quest/2012/01/26/geological-outings-around-the-bay-mount-vaca-and-the-monticello-dam/\">I showed you north of Fairfield\u003c/a>.\u003c/p>\n\u003cfigure id=\"attachment_40266\" class=\"wp-caption aligncenter\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/06/28/side-trips-from-interstate-5-stony-creek-valley/stonycreekvalley1/\" rel=\"attachment wp-att-40266\">\u003cimg class=\"size-full wp-image-40266\" title=\"stonycreekvalley1\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/06/stonycreekvalley1.jpg\" alt=\"\" width=\"640\" height=\"360\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley1.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley1-400x225.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">All photos by Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>Beyond a series of these ridges is a long valley underlain by fine-grained Jurassic rocks, the oldest part of the Great Valley Sequence. The valley is punctuated by \u003ca href=\"http://geology.about.com/od/structureslandforms/ig/erosional/hogback.htm\">hogback ridges\u003c/a> that affect the course of the roads. Parts of the valley have been turned into reservoirs, like Stony Gorge Reservoir.\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/2012/06/28/side-trips-from-interstate-5-stony-creek-valley/stonycreekvalley02/\" rel=\"attachment wp-att-40267\">\u003cimg class=\"aligncenter size-full wp-image-40267\" title=\"stonycreekvalley02\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/06/stonycreekvalley02.jpg\" alt=\"\" width=\"600\" height=\"400\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley02.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley02-400x267.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>A new reservoir is planned south of here around the settlement of Sites that will be used to regulate streamflow in the northern Sacramento Valley and allow older structures to be modified.\u003c/p>\n\u003cp>Eventually route 162 crosses Stony Creek, where the Great Valley Sequence rocks are spectacularly exposed in a washboard streambed.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/06/28/side-trips-from-interstate-5-stony-creek-valley/stonycreekvalley03/\" rel=\"attachment wp-att-40268\">\u003cimg class=\"aligncenter size-full wp-image-40268\" title=\"stonycreekvalley03\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/06/stonycreekvalley03.jpg\" alt=\"\" width=\"600\" height=\"470\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley03.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley03-400x313.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>Turn north here on 162 and follow the river, taking note of the different levels of stream terraces built when Stony Creek had not eroded as far down as it has today.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/06/28/side-trips-from-interstate-5-stony-creek-valley/stonycreekvalley04/\" rel=\"attachment wp-att-40269\">\u003cimg class=\"aligncenter size-full wp-image-40269\" title=\"stonycreekvalley04\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/06/stonycreekvalley04.jpg\" alt=\"\" width=\"600\" height=\"391\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley04.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley04-400x261.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>When 162 turns west again, continue north on county road 306. (At the moment, the route on 162 through the Coast Range to Covelo is closed.) In late April when I visited, the countryside was a picture-postcard experience.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/06/28/side-trips-from-interstate-5-stony-creek-valley/stonycreekvalley05/\" rel=\"attachment wp-att-40270\">\u003cimg class=\"aligncenter size-full wp-image-40270\" title=\"stonycreekvalley05\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/06/stonycreekvalley05.jpg\" alt=\"\" width=\"600\" height=\"441\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley05.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley05-400x294.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>If you like, take 162 a ways into the Franciscan country, or for a more intimate experience take county road 313 west instead, a well-graded dirt road just three miles to the north. (That's the spur shown on the route map.) In clear weather, vistas spread out as you rise. Here's the view south down the valley of Stony Creek:\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/06/28/side-trips-from-interstate-5-stony-creek-valley/stonycreekvalley06/\" rel=\"attachment wp-att-40271\">\u003cimg class=\"aligncenter size-full wp-image-40271\" title=\"stonycreekvalley06\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/06/stonycreekvalley06.jpg\" alt=\"\" width=\"600\" height=\"467\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley06.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley06-400x311.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>And here's the view northeast toward the Great Valley over the sawtooth ridges of Great Valley Sequence rocks:\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/06/28/side-trips-from-interstate-5-stony-creek-valley/stonycreekvalley07/\" rel=\"attachment wp-att-40272\">\u003cimg class=\"aligncenter size-full wp-image-40272\" title=\"stonycreekvalley07\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/06/stonycreekvalley07.jpg\" alt=\"\" width=\"600\" height=\"434\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley07.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley07-400x289.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>Ahead is the rugged topography held up by the Franciscan Complex. Note how the vegetation has changed as well as the bones of the land. The highest peak is Red Mountain. The contact between these two highly contrasting geologic provinces is the Coast Range thrust, which has tilted up the rocks on the east side like a pet pushing under a bedsheet.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/06/28/side-trips-from-interstate-5-stony-creek-valley/stonycreekvalley08/\" rel=\"attachment wp-att-40273\">\u003cimg class=\"aligncenter size-full wp-image-40273\" title=\"stonycreekvalley08\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/06/stonycreekvalley08.jpg\" alt=\"\" width=\"600\" height=\"450\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley08.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley08-400x300.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>Watch the roadcuts, too, for exposures of \u003ca href=\"http://ww2.kqed.org/quest/2010/08/05/learn-the-facts-about-serpentinite-before-its-removed-as-californias-state-rock/\">serpentinite\u003c/a>, or \u003ca href=\"http://geology.about.com/od/rocks/ig/metrockindex/rocpicschist.htm\">schist\u003c/a> like this:\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/06/28/side-trips-from-interstate-5-stony-creek-valley/stonycreekvalley09/\" rel=\"attachment wp-att-40274\">\u003cimg class=\"aligncenter size-full wp-image-40274\" title=\"stonycreekvalley09\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/06/stonycreekvalley09.jpg\" alt=\"\" width=\"600\" height=\"498\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley09.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley09-400x332.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>Step out and collect a specimen or two if you like; this is public land. Chrome ore was mined around here, in and around the serpentinite belt. The tiny settlement of Chrome marks the site of one former mine.\u003c/p>\n\u003cp>Road 306 butts into Newville Road, and that's where you turn back toward the freeway. But there's one more attraction as you go forward through geologic time into the Sacramento Valley: the unexpected Black Butte. This is a segment of a huge lava flow, the \u003ca href=\"http://myweb.csuchico.edu/~rteasdale/Lovejoy.html\">Lovejoy Basalt\u003c/a>, that once crossed the Valley from a source in the northern Sierra Nevada, reaching from here south to Vacaville. Black Butte was raised by a fault, sparing it from erosional destruction. The lake around it is artificial, and the whole is a splendid park.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/06/28/side-trips-from-interstate-5-stony-creek-valley/stonycreekvalley10/\" rel=\"attachment wp-att-40275\">\u003cimg class=\"aligncenter size-full wp-image-40275\" title=\"stonycreekvalley10\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/06/stonycreekvalley10.jpg\" alt=\"\" width=\"600\" height=\"450\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley10.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/06/stonycreekvalley10-400x300.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>To get to Corning requires a short backtrack to Black Butte Road, which crosses orchard lands and offers low-key views (which I believe will show Mount Shasta on clear days). You may also take a shorter side trip starting in Orland that visits Black Butte alone. But once you get behind the curtain of those serrated Great Valley Sequence hills, you'll never look at this stretch of I-5 the same way again.\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/quest/40264/side-trips-from-interstate-5-stony-creek-valley","authors":["6228"],"categories":["quest_11"],"tags":["quest_3580","quest_13200","quest_10648","quest_10760","quest_3653","quest_13202","quest_11247"],"featImg":"quest_40266","label":"quest"},"quest_33174":{"type":"posts","id":"quest_33174","meta":{"index":"posts_1591205157","site":"quest","id":"33174","score":null,"sort":[1331827215000]},"guestAuthors":[],"slug":"geological-outings-around-the-bay-new-almaden","title":"Geological Outings Around the Bay: New Almaden","publishDate":1331827215,"format":"standard","headTitle":"QUEST | KQED Science","labelTerm":{"site":"quest"},"content":"\u003cfigure id=\"attachment_33179\" class=\"wp-caption alignleft\" style=\"max-width: 300px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/03/15/geological-outings-around-the-bay-new-almaden/newalmaden/\" rel=\"attachment wp-att-33179\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/newalmaden-300x169.jpg\" alt=\"\" title=\"newalmaden\" width=\"300\" height=\"169\" class=\"size-thumbnail wp-image-33179\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">View west from Almaden Quicksilver County Park toward Loma Prieta, highest peak of the Sierra Azul. All photos by Andrew Alden.\u003c/figcaption>\u003c/figure>\n\u003cp>In the foothills due south of San Jose sit the remnants of California's first mining bonanza, the New Almaden mercury district. Today \u003ca href=\"http://www.newalmaden.org/AQSPark/index.html\">Almaden Quicksilver County Park\u003c/a> is a rugged playground for hikers, bicyclists and equestrians, but lovers of geology and mines have a special kind of fun there.\u003c/p>\n\u003cp>The first Californians mined a deep-red ore they called \u003ci>mohetka\u003c/i> in the heights of Los Capitancillos Ridge. Like other ancient peoples around the world, they used it as a pigment. In 1845 a Mexican visitor recognized the substance as cinnabar or mercury ore. Soon afterward the New World's richest quicksilver mining district began production, supplying the mercury for the refiners of the California Gold Rush. Its name, New Almaden, echoed the famous Almadén mines of Spain. A hundred years later, the mines had yielded mercury in the amount of more than a million flasksa volume of the liquid metal weighing 76 pounds. Although mining ended in the 1970s, geologists believe that much undiscovered ore remains.\u003c/p>\n\u003cp>Let's look at the geologic map of the area (derived from \u003ca href=\"http://pubs.usgs.gov/of/1998/of98-795/\">USGS Map OF-98-975\u003c/a>). \u003c/p>\n\u003cfigure id=\"attachment_33181\" class=\"wp-caption aligncenter\" style=\"max-width: 627px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/03/15/geological-outings-around-the-bay-new-almaden/newalmadengeomap/\" rel=\"attachment wp-att-33181\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/newalmadengeomap.png\" alt=\"\" title=\"newalmadengeomap\" width=\"627\" height=\"472\" class=\"size-full wp-image-33181\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/newalmadengeomap.png 627w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/newalmadengeomap-400x301.png 400w\" sizes=\"(max-width: 627px) 100vw, 627px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">The New Almaden district runs northwest on Los Capitancillos Ridge from the village of New Almaden. Asterisks mark the four park entrances. Franciscan rock units are fm, melange; fpv, volcanics; gs, greenstone; pink, serpentinite; yellow, silica-carbonate rock; orange, chert. Units with names starting Q, T or K are younger.\u003c/figcaption>\u003c/figure>\n\u003cp>It's kind of a mess, and the details are in the caption, but basically Los Capitancillos Ridge is like many other \u003ca href=\"http://ww2.kqed.org/quest/2011/07/21/bay-area-mercury/\">Bay Area mercury sites\u003c/a>, an intricate mixture of \u003ca href=\"http://ww2.kqed.org/quest/2011/04/21/geological-outings-around-the-bay-marin-headlands/\">Franciscan rocks\u003c/a> and serpentinite that has been kneaded and heated and injected with metal-bearing fluids. These fluids, derived from magma intrusions, replaced the minerals in the serpentinite and turned it into silica-carbonate rock. The cinnabar lodes, in turn, were emplaced in and near the silica-carbonates. As you hike about the ridge, keep an eye underfoot for the widespread \u003ca href=\"http://geology.about.com/od/more_metrocks/ig/serpentinites/\">serpentinite\u003c/a>.\u003c/p>\n\u003cfigure id=\"attachment_33182\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/03/15/geological-outings-around-the-bay-new-almaden/newalmadenserpentine/\" rel=\"attachment wp-att-33182\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/newalmadenserpentine.jpg\" alt=\"\" title=\"newalmadenserpentine\" width=\"600\" height=\"438\" class=\"size-full wp-image-33182\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/newalmadenserpentine.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/newalmadenserpentine-400x292.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Serpentinite boulders in a streambed.\u003c/figcaption>\u003c/figure>\n\u003cp>Among other things, the park contains mines and machinery spanning a century of progress from traditional techniques of medieval origin to modern American facilities. One mine entrance, the San Cristobal tunnel, has been kept open for a short distance.\u003c/p>\n\u003cfigure id=\"attachment_33175\" class=\"wp-caption aligncenter\" style=\"max-width: 500px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/03/15/geological-outings-around-the-bay-new-almaden/sancristobal/\" rel=\"attachment wp-att-33175\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/sancristobal.jpg\" alt=\"\" title=\"sancristobal\" width=\"500\" height=\"402\" class=\"size-full wp-image-33175\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/sancristobal.jpg 500w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/sancristobal-400x322.jpg 400w\" sizes=\"(max-width: 500px) 100vw, 500px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">San Cristobal tunnel, first opened in 1866.\u003c/figcaption>\u003c/figure>\n\u003cp>Go on in and look for the veins in the walls. These are typically filled with quartz or dolomite. \u003c/p>\n\u003cfigure id=\"attachment_33184\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/03/15/geological-outings-around-the-bay-new-almaden/newalmadenveins/\" rel=\"attachment wp-att-33184\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/newalmadenveins.jpg\" alt=\"\" title=\"newalmadenveins\" width=\"600\" height=\"450\" class=\"size-full wp-image-33184\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/newalmadenveins.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/newalmadenveins-400x300.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Veins in the San Cristobal tunnel.\u003c/figcaption>\u003c/figure>\n\u003cp>Another worthwhile spot is the site of the Buena Vista shaft, the deepest in the district. The foundation of the pumphouse is constructed of large blocks of local sandstone and Sierran granite. It was abandoned in 1893.\u003c/p>\n\u003cfigure id=\"attachment_33180\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/03/15/geological-outings-around-the-bay-new-almaden/newalmadenfoundation/\" rel=\"attachment wp-att-33180\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/newalmadenfoundation.jpg\" alt=\"\" title=\"newalmadenfoundation\" width=\"600\" height=\"486\" class=\"size-full wp-image-33180\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/newalmadenfoundation.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/newalmadenfoundation-400x324.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">The Buena Vista shaft mainly served to dewater the hills and allow neighboring mines to go deeper in search of cinnabar. \u003c/figcaption>\u003c/figure>\n\u003cp>Nearby are extensive piles of mine tailings. Although this shaft produced only minor amounts of ore, the rocks themselves are interesting. Remember that collecting rocks and minerals is forbidden. A ranger told me that if people kept taking things home with them, eventually there would be no tailings left. I don't see the problem with that, and \u003ca href=\"http://ww2.kqed.org/quest/2011/11/17/fossil-collecting-in-the-bay-area/\">if I could make the rules I would give rockhounds access\u003c/a> to limited parts of the park.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/03/15/geological-outings-around-the-bay-new-almaden/newalmadentailings/\" rel=\"attachment wp-att-33183\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/newalmadentailings.jpg\" alt=\"\" title=\"newalmadentailings\" width=\"600\" height=\"450\" class=\"aligncenter size-full wp-image-33183\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/newalmadentailings.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/newalmadentailings-400x300.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>Don't miss the views of the surrounding territory. The top photo of this post shows the view west to the Sierra Azul, and to the east are views of the Santa Teresa Hills and Diablo Range.\u003c/p>\n\u003cfigure id=\"attachment_33178\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/03/15/geological-outings-around-the-bay-new-almaden/hamilton/\" rel=\"attachment wp-att-33178\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/hamilton.jpg\" alt=\"\" title=\"hamilton\" width=\"600\" height=\"463\" class=\"size-full wp-image-33178\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/hamilton.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/hamilton-400x309.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Mount Hamilton's observatories stand out beyond the lower Santa Teresa Hills, site of more mercury mines and sandstone quarries.\u003c/figcaption>\u003c/figure>\n\u003cp>The mining museum housed in the Casa Grande, the old manager's residence built in 1854, is full of exhibits and is well worth a visit if you can be there during its brief open hours.\u003c/p>\n\u003cfigure id=\"attachment_33176\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/03/15/geological-outings-around-the-bay-new-almaden/casagrande/\" rel=\"attachment wp-att-33176\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/casagrande.jpg\" alt=\"\" title=\"casagrande\" width=\"600\" height=\"459\" class=\"size-full wp-image-33176\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/casagrande.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/casagrande-400x306.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">The Casa Grande has rooms full of period furnishings as well as the Quicksilver Mining Museum.\u003c/figcaption>\u003c/figure>\n\u003cp>The little museum shop has cinnabar from the Guadalupe Mine for sale. This is the only way you can acquire New Almaden specimens today, unless a dealer is selling off a historic collection at a \u003ca href=\"http://ww2.kqed.org/quest/2011/08/18/theres-nothing-like-a-rock-show/\">rock and mineral show\u003c/a>.\u003c/p>\n\u003cfigure id=\"attachment_33177\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/03/15/geological-outings-around-the-bay-new-almaden/guadalupecinnabar/\" rel=\"attachment wp-att-33177\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/guadalupecinnabar.jpg\" alt=\"\" title=\"guadalupecinnabar\" width=\"600\" height=\"487\" class=\"size-full wp-image-33177\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/guadalupecinnabar.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/guadalupecinnabar-400x325.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">New Almaden cinnabar is notable for its tiny crystals that give the ore a glittering appearance.\u003c/figcaption>\u003c/figure>\n\u003cp>\u003c/p>\n\u003cp>The definitive source for historic and geologic information on the area is the classic \u003ca href=\"http://openlibrary.org/books/OL7034975M/Geology_and_quicksilver_deposits_of_the_New_Almaden_District_Santa_Clara_County_California\">US Geological Survey Professional Paper 360\u003c/a>, \"Geology and Quicksilver Deposits of the New Almaden District.\"\u003c/p>\n\n","blocks":[],"excerpt":"The New Almaden area looms large in Gold Rush history. Today it's an open-air museum of California mining practices and quicksilver geology.","status":"publish","parent":0,"modified":1332966126,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":15,"wordCount":754},"headData":{"title":"Geological Outings Around the Bay: New Almaden | KQED","description":"The New Almaden area looms large in Gold Rush history. Today it's an open-air museum of California mining practices and quicksilver geology.","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":""},"disqusIdentifier":"33174 http://science.kqed.org/quest/?p=33174","disqusUrl":"https://ww2.kqed.org/quest/2012/03/15/geological-outings-around-the-bay-new-almaden/","disqusTitle":"Geological Outings Around the Bay: New Almaden","path":"/quest/33174/geological-outings-around-the-bay-new-almaden","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cfigure id=\"attachment_33179\" class=\"wp-caption alignleft\" style=\"max-width: 300px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/03/15/geological-outings-around-the-bay-new-almaden/newalmaden/\" rel=\"attachment wp-att-33179\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/newalmaden-300x169.jpg\" alt=\"\" title=\"newalmaden\" width=\"300\" height=\"169\" class=\"size-thumbnail wp-image-33179\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">View west from Almaden Quicksilver County Park toward Loma Prieta, highest peak of the Sierra Azul. All photos by Andrew Alden.\u003c/figcaption>\u003c/figure>\n\u003cp>In the foothills due south of San Jose sit the remnants of California's first mining bonanza, the New Almaden mercury district. Today \u003ca href=\"http://www.newalmaden.org/AQSPark/index.html\">Almaden Quicksilver County Park\u003c/a> is a rugged playground for hikers, bicyclists and equestrians, but lovers of geology and mines have a special kind of fun there.\u003c/p>\n\u003cp>The first Californians mined a deep-red ore they called \u003ci>mohetka\u003c/i> in the heights of Los Capitancillos Ridge. Like other ancient peoples around the world, they used it as a pigment. In 1845 a Mexican visitor recognized the substance as cinnabar or mercury ore. Soon afterward the New World's richest quicksilver mining district began production, supplying the mercury for the refiners of the California Gold Rush. Its name, New Almaden, echoed the famous Almadén mines of Spain. A hundred years later, the mines had yielded mercury in the amount of more than a million flasksa volume of the liquid metal weighing 76 pounds. Although mining ended in the 1970s, geologists believe that much undiscovered ore remains.\u003c/p>\n\u003cp>Let's look at the geologic map of the area (derived from \u003ca href=\"http://pubs.usgs.gov/of/1998/of98-795/\">USGS Map OF-98-975\u003c/a>). \u003c/p>\n\u003cfigure id=\"attachment_33181\" class=\"wp-caption aligncenter\" style=\"max-width: 627px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/03/15/geological-outings-around-the-bay-new-almaden/newalmadengeomap/\" rel=\"attachment wp-att-33181\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/newalmadengeomap.png\" alt=\"\" title=\"newalmadengeomap\" width=\"627\" height=\"472\" class=\"size-full wp-image-33181\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/newalmadengeomap.png 627w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/newalmadengeomap-400x301.png 400w\" sizes=\"(max-width: 627px) 100vw, 627px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">The New Almaden district runs northwest on Los Capitancillos Ridge from the village of New Almaden. Asterisks mark the four park entrances. Franciscan rock units are fm, melange; fpv, volcanics; gs, greenstone; pink, serpentinite; yellow, silica-carbonate rock; orange, chert. Units with names starting Q, T or K are younger.\u003c/figcaption>\u003c/figure>\n\u003cp>It's kind of a mess, and the details are in the caption, but basically Los Capitancillos Ridge is like many other \u003ca href=\"http://ww2.kqed.org/quest/2011/07/21/bay-area-mercury/\">Bay Area mercury sites\u003c/a>, an intricate mixture of \u003ca href=\"http://ww2.kqed.org/quest/2011/04/21/geological-outings-around-the-bay-marin-headlands/\">Franciscan rocks\u003c/a> and serpentinite that has been kneaded and heated and injected with metal-bearing fluids. These fluids, derived from magma intrusions, replaced the minerals in the serpentinite and turned it into silica-carbonate rock. The cinnabar lodes, in turn, were emplaced in and near the silica-carbonates. As you hike about the ridge, keep an eye underfoot for the widespread \u003ca href=\"http://geology.about.com/od/more_metrocks/ig/serpentinites/\">serpentinite\u003c/a>.\u003c/p>\n\u003cfigure id=\"attachment_33182\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/03/15/geological-outings-around-the-bay-new-almaden/newalmadenserpentine/\" rel=\"attachment wp-att-33182\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/newalmadenserpentine.jpg\" alt=\"\" title=\"newalmadenserpentine\" width=\"600\" height=\"438\" class=\"size-full wp-image-33182\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/newalmadenserpentine.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/newalmadenserpentine-400x292.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Serpentinite boulders in a streambed.\u003c/figcaption>\u003c/figure>\n\u003cp>Among other things, the park contains mines and machinery spanning a century of progress from traditional techniques of medieval origin to modern American facilities. One mine entrance, the San Cristobal tunnel, has been kept open for a short distance.\u003c/p>\n\u003cfigure id=\"attachment_33175\" class=\"wp-caption aligncenter\" style=\"max-width: 500px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/03/15/geological-outings-around-the-bay-new-almaden/sancristobal/\" rel=\"attachment wp-att-33175\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/sancristobal.jpg\" alt=\"\" title=\"sancristobal\" width=\"500\" height=\"402\" class=\"size-full wp-image-33175\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/sancristobal.jpg 500w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/sancristobal-400x322.jpg 400w\" sizes=\"(max-width: 500px) 100vw, 500px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">San Cristobal tunnel, first opened in 1866.\u003c/figcaption>\u003c/figure>\n\u003cp>Go on in and look for the veins in the walls. These are typically filled with quartz or dolomite. \u003c/p>\n\u003cfigure id=\"attachment_33184\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/03/15/geological-outings-around-the-bay-new-almaden/newalmadenveins/\" rel=\"attachment wp-att-33184\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/newalmadenveins.jpg\" alt=\"\" title=\"newalmadenveins\" width=\"600\" height=\"450\" class=\"size-full wp-image-33184\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/newalmadenveins.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/newalmadenveins-400x300.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Veins in the San Cristobal tunnel.\u003c/figcaption>\u003c/figure>\n\u003cp>Another worthwhile spot is the site of the Buena Vista shaft, the deepest in the district. The foundation of the pumphouse is constructed of large blocks of local sandstone and Sierran granite. It was abandoned in 1893.\u003c/p>\n\u003cfigure id=\"attachment_33180\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/03/15/geological-outings-around-the-bay-new-almaden/newalmadenfoundation/\" rel=\"attachment wp-att-33180\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/newalmadenfoundation.jpg\" alt=\"\" title=\"newalmadenfoundation\" width=\"600\" height=\"486\" class=\"size-full wp-image-33180\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/newalmadenfoundation.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/newalmadenfoundation-400x324.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">The Buena Vista shaft mainly served to dewater the hills and allow neighboring mines to go deeper in search of cinnabar. \u003c/figcaption>\u003c/figure>\n\u003cp>Nearby are extensive piles of mine tailings. Although this shaft produced only minor amounts of ore, the rocks themselves are interesting. Remember that collecting rocks and minerals is forbidden. A ranger told me that if people kept taking things home with them, eventually there would be no tailings left. I don't see the problem with that, and \u003ca href=\"http://ww2.kqed.org/quest/2011/11/17/fossil-collecting-in-the-bay-area/\">if I could make the rules I would give rockhounds access\u003c/a> to limited parts of the park.\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/2012/03/15/geological-outings-around-the-bay-new-almaden/newalmadentailings/\" rel=\"attachment wp-att-33183\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/newalmadentailings.jpg\" alt=\"\" title=\"newalmadentailings\" width=\"600\" height=\"450\" class=\"aligncenter size-full wp-image-33183\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/newalmadentailings.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/newalmadentailings-400x300.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>Don't miss the views of the surrounding territory. The top photo of this post shows the view west to the Sierra Azul, and to the east are views of the Santa Teresa Hills and Diablo Range.\u003c/p>\n\u003cfigure id=\"attachment_33178\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/03/15/geological-outings-around-the-bay-new-almaden/hamilton/\" rel=\"attachment wp-att-33178\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/hamilton.jpg\" alt=\"\" title=\"hamilton\" width=\"600\" height=\"463\" class=\"size-full wp-image-33178\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/hamilton.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/hamilton-400x309.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Mount Hamilton's observatories stand out beyond the lower Santa Teresa Hills, site of more mercury mines and sandstone quarries.\u003c/figcaption>\u003c/figure>\n\u003cp>The mining museum housed in the Casa Grande, the old manager's residence built in 1854, is full of exhibits and is well worth a visit if you can be there during its brief open hours.\u003c/p>\n\u003cfigure id=\"attachment_33176\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/03/15/geological-outings-around-the-bay-new-almaden/casagrande/\" rel=\"attachment wp-att-33176\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/casagrande.jpg\" alt=\"\" title=\"casagrande\" width=\"600\" height=\"459\" class=\"size-full wp-image-33176\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/casagrande.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/casagrande-400x306.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">The Casa Grande has rooms full of period furnishings as well as the Quicksilver Mining Museum.\u003c/figcaption>\u003c/figure>\n\u003cp>The little museum shop has cinnabar from the Guadalupe Mine for sale. This is the only way you can acquire New Almaden specimens today, unless a dealer is selling off a historic collection at a \u003ca href=\"http://ww2.kqed.org/quest/2011/08/18/theres-nothing-like-a-rock-show/\">rock and mineral show\u003c/a>.\u003c/p>\n\u003cfigure id=\"attachment_33177\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/03/15/geological-outings-around-the-bay-new-almaden/guadalupecinnabar/\" rel=\"attachment wp-att-33177\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/guadalupecinnabar.jpg\" alt=\"\" title=\"guadalupecinnabar\" width=\"600\" height=\"487\" class=\"size-full wp-image-33177\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/guadalupecinnabar.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/guadalupecinnabar-400x325.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">New Almaden cinnabar is notable for its tiny crystals that give the ore a glittering appearance.\u003c/figcaption>\u003c/figure>\n\u003cp>\u003c/p>\n\u003cp>The definitive source for historic and geologic information on the area is the classic \u003ca href=\"http://openlibrary.org/books/OL7034975M/Geology_and_quicksilver_deposits_of_the_New_Almaden_District_Santa_Clara_County_California\">US Geological Survey Professional Paper 360\u003c/a>, \"Geology and Quicksilver Deposits of the New Almaden District.\"\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/quest/33174/geological-outings-around-the-bay-new-almaden","authors":["6228"],"categories":["quest_11"],"tags":["quest_10819","quest_3580","quest_1791","quest_1834","quest_9890","quest_13202","quest_2590","quest_3820"],"featImg":"quest_33179","label":"quest"},"quest_25770":{"type":"posts","id":"quest_25770","meta":{"index":"posts_1591205157","site":"quest","id":"25770","score":null,"sort":[1318531732000]},"guestAuthors":[],"slug":"geological-outings-around-the-bay-albany-hill","title":"Geological Outings Around the Bay: Albany Hill","publishDate":1318531732,"format":"standard","headTitle":"QUEST | KQED Science","labelTerm":{"site":"quest"},"content":"\u003cfigure id=\"attachment_25773\" class=\"wp-caption aligncenter\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/10/13/geological-outings-around-the-bay-albany-hill/elcerritobart/\" rel=\"attachment wp-att-25773\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/10/elcerritobart.jpg\" alt=\"\" title=\"elcerritobart\" width=\"640\" height=\"360\" class=\"size-full wp-image-25773\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/10/elcerritobart.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/10/elcerritobart-400x225.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Photos by Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>This is the classic view of Albany Hill from the El Cerrito BART station. With the sun behind it, you can see that much of the hill's apparent size is due to a high hairstyle of eucalyptus trees. Beneath them is an isolated body of Franciscan sandstone dating from late in the Cretaceous Period, about 70 to 83 million years old.\u003c/p>\n\u003cp>Many Bay Area landmarks had different names before the Gold Rush. Albany Hill was first named \"Cerrito de San Antonio\" by the Peralta family. Afterward it became El Cerrito, \"little hill,\" and got its current name just a century ago when the city of Albany incorporated. During those years it served first as a rock quarry and the site of an explosives factory (when the eucalyptus forest was planted, as \u003ca href=\"http://ww2.kqed.org/quest/2011/10/06/geological-outings-around-the-bay-point-pinole-and-the-hayward-fault/\">at Pinole Point\u003c/a>, to muffle accidents) and later as a fine place to build homes and apartment buildings. Today much of it is preserved in Albany Hill Park in a benign stasis.\u003c/p>\n\u003cp>Albany Hill appears on the geologic map as a patch of unit Kfn, Franciscan rocks of the Novato Quarry terrane.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/10/13/geological-outings-around-the-bay-albany-hill/elcerritomap/\" rel=\"attachment wp-att-25775\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/10/elcerritomap-566x360.png\" alt=\"\" title=\"elcerritomap\" width=\"566\" height=\"360\" class=\"size-large wp-image-25775\">\u003c/a>\u003c/p>\n\u003cp>The line labeled \"A\" marks part of cross-section AA' that conveniently starts right at Albany Hill.\u003c/p>\n\u003cfigure id=\"attachment_25771\" class=\"wp-caption aligncenter\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/10/13/geological-outings-around-the-bay-albany-hill/elcerritoxsec/\" rel=\"attachment wp-att-25771\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/10/elcerritoxsec.png\" alt=\"\" title=\"elcerritoxsec\" width=\"640\" height=\"410\" class=\"size-full wp-image-25771\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/10/elcerritoxsec.png 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/10/elcerritoxsec-400x256.png 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Cross-section showing interpreted structure beneath the map; the portion shown in the map segment reaches to the \"Qls\" symbol (landslide deposits).\u003c/figcaption>\u003c/figure>\n\u003cp>To visit the rocks of Albany Hill, park along Taft Avenue, which runs up the east side of the hill. The street boasts an extensive roadcut where you can inspect and sample the rock. It's a hard, massive, medium-grained sandstone that has undergone some metamorphism. This has wiped out any original structural features that may have been there, such as bedding and erosion marks. This isn't the dramatic stuff of \u003ca href=\"http://ww2.kqed.org/quest/2011/03/24/geological-outings-around-the-bay-shell-beach/\">Pebble Beach\u003c/a>.\u003c/p>\n\u003cfigure id=\"attachment_25777\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/10/13/geological-outings-around-the-bay-albany-hill/elcerritoweathered/\" rel=\"attachment wp-att-25777\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/10/elcerritoweathered.jpg\" alt=\"\" title=\"elcerritoweathered\" width=\"600\" height=\"450\" class=\"size-full wp-image-25777\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/10/elcerritoweathered.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2011/10/elcerritoweathered-400x300.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Weathered sandstone of Albany Hill in Taft Avenue roadcut. The light patch is rich in calcite.\u003c/figcaption>\u003c/figure>\n\u003cp>Up at the end of Taft is a parking area for Albany Hill Park. Enjoy the woods and the views and watch for the occasional outcrops underfoot. In many of these, foot traffic exposes the sandstone's true tan color.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>The map shows two other exposures of this rock nearby. The one at Point Isabel is almost entirely covered today, but at Fleming Point, behind the racetrack stands at Golden Gate Fields, years of (again) explosives manufacturing and quarrying have left it well exposed.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/10/13/geological-outings-around-the-bay-albany-hill/elcerr-flemingpoint/\" rel=\"attachment wp-att-25772\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/10/elcerr-flemingpoint.jpg\" alt=\"\" title=\"elcerr-flemingpoint\" width=\"600\" height=\"364\" class=\"aligncenter size-full wp-image-25772\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/10/elcerr-flemingpoint.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2011/10/elcerr-flemingpoint-400x243.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>These three outcrops are part of a longer discontinuous belt of rocks of the Novato Quarry terrane. It runs from Piedmont on the south to Point Richmond, to Novato across the Bay, and beyond in patches all the way to Bodega Head.\u003c/p>\n\u003cp>While you're on this side of the freeway, take a hike out the Albany Bulb, an artificial peninsula studded with anonymous art works. There you can see the \u003ci>other\u003c/i> classic view of Albany Hill, sitting in front of the much younger rocks of the Berkeley Hills.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/10/13/geological-outings-around-the-bay-albany-hill/elcerritobulb/\" rel=\"attachment wp-att-25774\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/10/elcerritobulb.jpg\" alt=\"\" title=\"elcerritobulb\" width=\"600\" height=\"419\" class=\"aligncenter size-full wp-image-25774\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/10/elcerritobulb.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2011/10/elcerritobulb-400x279.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\n","blocks":[],"excerpt":"Among the commuters who pass it twice a day, surely thousands of people wonder about that dramatic little hill next to I-80/580 just north of Berkeley. Wonder no more.","status":"publish","parent":0,"modified":1325109122,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":14,"wordCount":495},"headData":{"title":"Geological Outings Around the Bay: Albany Hill | KQED","description":"Among the commuters who pass it twice a day, surely thousands of people wonder about that dramatic little hill next to I-80/580 just north of Berkeley. Wonder no more.","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":""},"disqusIdentifier":"25770 http://science.kqed.org/quest/?p=25770","disqusUrl":"https://ww2.kqed.org/quest/2011/10/13/geological-outings-around-the-bay-albany-hill/","disqusTitle":"Geological Outings Around the Bay: Albany Hill","path":"/quest/25770/geological-outings-around-the-bay-albany-hill","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cfigure id=\"attachment_25773\" class=\"wp-caption aligncenter\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/10/13/geological-outings-around-the-bay-albany-hill/elcerritobart/\" rel=\"attachment wp-att-25773\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/10/elcerritobart.jpg\" alt=\"\" title=\"elcerritobart\" width=\"640\" height=\"360\" class=\"size-full wp-image-25773\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/10/elcerritobart.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/10/elcerritobart-400x225.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Photos by Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>This is the classic view of Albany Hill from the El Cerrito BART station. With the sun behind it, you can see that much of the hill's apparent size is due to a high hairstyle of eucalyptus trees. Beneath them is an isolated body of Franciscan sandstone dating from late in the Cretaceous Period, about 70 to 83 million years old.\u003c/p>\n\u003cp>Many Bay Area landmarks had different names before the Gold Rush. Albany Hill was first named \"Cerrito de San Antonio\" by the Peralta family. Afterward it became El Cerrito, \"little hill,\" and got its current name just a century ago when the city of Albany incorporated. During those years it served first as a rock quarry and the site of an explosives factory (when the eucalyptus forest was planted, as \u003ca href=\"http://ww2.kqed.org/quest/2011/10/06/geological-outings-around-the-bay-point-pinole-and-the-hayward-fault/\">at Pinole Point\u003c/a>, to muffle accidents) and later as a fine place to build homes and apartment buildings. Today much of it is preserved in Albany Hill Park in a benign stasis.\u003c/p>\n\u003cp>Albany Hill appears on the geologic map as a patch of unit Kfn, Franciscan rocks of the Novato Quarry terrane.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/10/13/geological-outings-around-the-bay-albany-hill/elcerritomap/\" rel=\"attachment wp-att-25775\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/10/elcerritomap-566x360.png\" alt=\"\" title=\"elcerritomap\" width=\"566\" height=\"360\" class=\"size-large wp-image-25775\">\u003c/a>\u003c/p>\n\u003cp>The line labeled \"A\" marks part of cross-section AA' that conveniently starts right at Albany Hill.\u003c/p>\n\u003cfigure id=\"attachment_25771\" class=\"wp-caption aligncenter\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/10/13/geological-outings-around-the-bay-albany-hill/elcerritoxsec/\" rel=\"attachment wp-att-25771\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/10/elcerritoxsec.png\" alt=\"\" title=\"elcerritoxsec\" width=\"640\" height=\"410\" class=\"size-full wp-image-25771\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/10/elcerritoxsec.png 640w, https://ww2.kqed.org/app/uploads/sites/39/2011/10/elcerritoxsec-400x256.png 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Cross-section showing interpreted structure beneath the map; the portion shown in the map segment reaches to the \"Qls\" symbol (landslide deposits).\u003c/figcaption>\u003c/figure>\n\u003cp>To visit the rocks of Albany Hill, park along Taft Avenue, which runs up the east side of the hill. The street boasts an extensive roadcut where you can inspect and sample the rock. It's a hard, massive, medium-grained sandstone that has undergone some metamorphism. This has wiped out any original structural features that may have been there, such as bedding and erosion marks. This isn't the dramatic stuff of \u003ca href=\"http://ww2.kqed.org/quest/2011/03/24/geological-outings-around-the-bay-shell-beach/\">Pebble Beach\u003c/a>.\u003c/p>\n\u003cfigure id=\"attachment_25777\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2011/10/13/geological-outings-around-the-bay-albany-hill/elcerritoweathered/\" rel=\"attachment wp-att-25777\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/10/elcerritoweathered.jpg\" alt=\"\" title=\"elcerritoweathered\" width=\"600\" height=\"450\" class=\"size-full wp-image-25777\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/10/elcerritoweathered.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2011/10/elcerritoweathered-400x300.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Weathered sandstone of Albany Hill in Taft Avenue roadcut. The light patch is rich in calcite.\u003c/figcaption>\u003c/figure>\n\u003cp>Up at the end of Taft is a parking area for Albany Hill Park. Enjoy the woods and the views and watch for the occasional outcrops underfoot. In many of these, foot traffic exposes the sandstone's true tan color.\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 map shows two other exposures of this rock nearby. The one at Point Isabel is almost entirely covered today, but at Fleming Point, behind the racetrack stands at Golden Gate Fields, years of (again) explosives manufacturing and quarrying have left it well exposed.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/10/13/geological-outings-around-the-bay-albany-hill/elcerr-flemingpoint/\" rel=\"attachment wp-att-25772\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/10/elcerr-flemingpoint.jpg\" alt=\"\" title=\"elcerr-flemingpoint\" width=\"600\" height=\"364\" class=\"aligncenter size-full wp-image-25772\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/10/elcerr-flemingpoint.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2011/10/elcerr-flemingpoint-400x243.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>These three outcrops are part of a longer discontinuous belt of rocks of the Novato Quarry terrane. It runs from Piedmont on the south to Point Richmond, to Novato across the Bay, and beyond in patches all the way to Bodega Head.\u003c/p>\n\u003cp>While you're on this side of the freeway, take a hike out the Albany Bulb, an artificial peninsula studded with anonymous art works. There you can see the \u003ci>other\u003c/i> classic view of Albany Hill, sitting in front of the much younger rocks of the Berkeley Hills.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2011/10/13/geological-outings-around-the-bay-albany-hill/elcerritobulb/\" rel=\"attachment wp-att-25774\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/10/elcerritobulb.jpg\" alt=\"\" title=\"elcerritobulb\" width=\"600\" height=\"419\" class=\"aligncenter size-full wp-image-25774\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2011/10/elcerritobulb.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2011/10/elcerritobulb-400x279.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/quest/25770/geological-outings-around-the-bay-albany-hill","authors":["6228"],"categories":["quest_11"],"tags":["quest_10260","quest_10261","quest_10262","quest_1025","quest_3580","quest_10263","quest_13202","quest_2447","quest_3747","quest_8739"],"featImg":"quest_25773","label":"quest"},"quest_15607":{"type":"posts","id":"quest_15607","meta":{"index":"posts_1591205157","site":"quest","id":"15607","score":null,"sort":[1310066425000]},"guestAuthors":[],"slug":"geological-outings-around-the-bay-the-great-slickenside-of-corona-heights","title":"Geological Outings Around the Bay: The Great Slickenside of Corona Heights","publishDate":1310066425,"format":"standard","headTitle":"QUEST | KQED Science","labelTerm":{"site":"quest"},"content":"\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/coronatop.jpg\" alt=\"corona heights\" class=\"alignleft size-full\">\u003cem>\u003csup>Sutro Tower and the gnarled chert of the Marin Headlandsterrane are parts of a splendid spectacle at San Francisco's Corona Heights. Photos by Andrew Alden.\u003c/sup>\u003c/em>\u003c/span>\u003c/p>\n\u003cp>San Francisco is \"America's Favorite City\" for many great reasons. Geologists have their own list of reasons to love it, many of which are Franciscan—by which we mean the peculiar association of rocks found up and down the Coast Ranges. Corona Heights is a small hill west of the Castro district that features some of these rocks, but one of its main attractions is a world-class slickenside.\u003c/p>\n\u003cp>\u003c!--more-->\u003c/p>\n\u003cp>You get to Corona Heights by walking about a mile west from the 16th/Mission BART station, or by taking the F line up Market Street to the Noe or Sanchez stops. Here's the hill as seen from 16th Street. You can't miss it.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/corona1.jpg\" alt=\"corona heights\">\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>Corona Heights is a hardworking hill that formerly yielded clay and chert. Years of quarrying have accentuated its rugged appearance and left splendid exposures of the bedrock. Along the way, if you keep an eye on appearances of old concrete (doesn't everybody?), you may spot the old chert aggregate around the neighborhood.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/corona2.jpg\" alt=\"chert aggregate\">\u003c/p>\n\u003cp>Corona Heights, like Bernal Heights to the southeast, is an island of resistant chert that is part of the dismembered \u003ca href=\"http://www.kqed.org/quest/blog/2011/04/21/geological-outings-around-the-bay-marin-headlands/\">Marin Headlands terrane\u003c/a>. It houses a fine playground and the \u003ca href=\"http://www.randallmuseum.org/\">Randall Museum\u003c/a>. It has a \u003ca href=\"http://sfnaturalareas.org/pages/1\">dedicated group doing habitat restoration\u003c/a>. But we're here to see the slickenside.\u003c/p>\n\u003cp>A slickenside is the polished surface that is created along a fault as the rocks rub against each other. They are common in faulted rocks, but only in patches the size of your hand. (I showed you some in \u003ca href=\"http://www.kqed.org/quest/blog/2011/04/14/calera-limestone-a-gift-from-the-ancient-pacific/\">the Calera Limestone\u003c/a>.) Larger ones are rarer. Quarrying at Corona Heights uncovered one the size of a big front yard, one of the world's largest exposures. To see it, start at Castro and 15th, go uphill on 15th and turn left on Beaver Street. Again, you can't miss it.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/corona3.jpg\" alt=\"slickenside\">\u003c/p>\n\u003cp>The site is also a playground, named for Sidney Peixotto. If you continue up 15th Street instead, you'll see the exposure this way.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/corona4.jpg\" alt=\"playground and slickenside\">\u003c/p>\n\u003cp>But the real joy of the thing comes at close hand, where you can feel the mirror-smooth surface that only a hard stone like chert can provide.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/corona5.jpg\" alt=\"fault polish\">\u003c/p>\n\u003cp>Surfaces like this are of scientific interest, although the data base is still scant. UC Santa Cruz researcher James Kirkpatrick has surveyed this site by lidar. He and others hope that close analysis can tell us more about how faults behave in detail. That's an advanced topic; the rest of us can \u003ca href=\"http://www.geocaching.com/seek/cache_details.aspx?guid=52f407dc-3635-46b9-89e5-1564c28b4578\">collect the geocache at this spot\u003c/a>.\u003c/p>\n\u003cp>Afterward is a good time to climb to the top of the hill and take in one of the city's best views. On a clear day you can see \u003ca href=\"http://www.kqed.org/quest/blog/2011/06/02/mount-diablo-views/\">Mount Diablo\u003c/a> (click for a 1000-pixel version).\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/coronapan.jpg\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/coronapan.jpg\" width=\"500\" alt=\"panorama\">\u003c/a>\u003c/p>\n\u003cp>\u003c/p>\n\u003cp> 37.7654 -122.4373\u003c/p>\n\n","blocks":[],"excerpt":"Everyone loves San Francisco, but geologists love it for reasons others don't, such as its gigantic slickenside.","status":"publish","parent":0,"modified":1443830584,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":20,"wordCount":489},"headData":{"title":"Geological Outings Around the Bay: The Great Slickenside of Corona Heights | KQED","description":"","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":""},"disqusIdentifier":"15607 http://www.kqed.org/quest/blog/?p=15607","disqusUrl":"https://ww2.kqed.org/quest/2011/07/07/geological-outings-around-the-bay-the-great-slickenside-of-corona-heights/","disqusTitle":"Geological Outings Around the Bay: The Great Slickenside of Corona Heights","path":"/quest/15607/geological-outings-around-the-bay-the-great-slickenside-of-corona-heights","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/coronatop.jpg\" alt=\"corona heights\" class=\"alignleft size-full\">\u003cem>\u003csup>Sutro Tower and the gnarled chert of the Marin Headlandsterrane are parts of a splendid spectacle at San Francisco's Corona Heights. Photos by Andrew Alden.\u003c/sup>\u003c/em>\u003c/span>\u003c/p>\n\u003cp>San Francisco is \"America's Favorite City\" for many great reasons. Geologists have their own list of reasons to love it, many of which are Franciscan—by which we mean the peculiar association of rocks found up and down the Coast Ranges. Corona Heights is a small hill west of the Castro district that features some of these rocks, but one of its main attractions is a world-class slickenside.\u003c/p>\n\u003cp>\u003c!--more-->\u003c/p>\n\u003cp>You get to Corona Heights by walking about a mile west from the 16th/Mission BART station, or by taking the F line up Market Street to the Noe or Sanchez stops. Here's the hill as seen from 16th Street. You can't miss it.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/corona1.jpg\" alt=\"corona heights\">\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>Corona Heights is a hardworking hill that formerly yielded clay and chert. Years of quarrying have accentuated its rugged appearance and left splendid exposures of the bedrock. Along the way, if you keep an eye on appearances of old concrete (doesn't everybody?), you may spot the old chert aggregate around the neighborhood.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/corona2.jpg\" alt=\"chert aggregate\">\u003c/p>\n\u003cp>Corona Heights, like Bernal Heights to the southeast, is an island of resistant chert that is part of the dismembered \u003ca href=\"http://www.kqed.org/quest/blog/2011/04/21/geological-outings-around-the-bay-marin-headlands/\">Marin Headlands terrane\u003c/a>. It houses a fine playground and the \u003ca href=\"http://www.randallmuseum.org/\">Randall Museum\u003c/a>. It has a \u003ca href=\"http://sfnaturalareas.org/pages/1\">dedicated group doing habitat restoration\u003c/a>. But we're here to see the slickenside.\u003c/p>\n\u003cp>A slickenside is the polished surface that is created along a fault as the rocks rub against each other. They are common in faulted rocks, but only in patches the size of your hand. (I showed you some in \u003ca href=\"http://www.kqed.org/quest/blog/2011/04/14/calera-limestone-a-gift-from-the-ancient-pacific/\">the Calera Limestone\u003c/a>.) Larger ones are rarer. Quarrying at Corona Heights uncovered one the size of a big front yard, one of the world's largest exposures. To see it, start at Castro and 15th, go uphill on 15th and turn left on Beaver Street. Again, you can't miss it.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/corona3.jpg\" alt=\"slickenside\">\u003c/p>\n\u003cp>The site is also a playground, named for Sidney Peixotto. If you continue up 15th Street instead, you'll see the exposure this way.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/corona4.jpg\" alt=\"playground and slickenside\">\u003c/p>\n\u003cp>But the real joy of the thing comes at close hand, where you can feel the mirror-smooth surface that only a hard stone like chert can provide.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/corona5.jpg\" alt=\"fault polish\">\u003c/p>\n\u003cp>Surfaces like this are of scientific interest, although the data base is still scant. UC Santa Cruz researcher James Kirkpatrick has surveyed this site by lidar. He and others hope that close analysis can tell us more about how faults behave in detail. That's an advanced topic; the rest of us can \u003ca href=\"http://www.geocaching.com/seek/cache_details.aspx?guid=52f407dc-3635-46b9-89e5-1564c28b4578\">collect the geocache at this spot\u003c/a>.\u003c/p>\n\u003cp>Afterward is a good time to climb to the top of the hill and take in one of the city's best views. On a clear day you can see \u003ca href=\"http://www.kqed.org/quest/blog/2011/06/02/mount-diablo-views/\">Mount Diablo\u003c/a> (click for a 1000-pixel version).\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/coronapan.jpg\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/07/coronapan.jpg\" width=\"500\" alt=\"panorama\">\u003c/a>\u003c/p>\n\u003cp>\u003c/p>\n\u003cp> 37.7654 -122.4373\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/quest/15607/geological-outings-around-the-bay-the-great-slickenside-of-corona-heights","authors":["6228"],"categories":["quest_11"],"tags":["quest_3507","quest_1080","quest_3580","quest_3592","quest_3724","quest_2486","quest_3764"],"featImg":"quest_15608","label":"quest"},"quest_15399":{"type":"posts","id":"quest_15399","meta":{"index":"posts_1591205157","site":"quest","id":"15399","score":null,"sort":[1308855976000]},"guestAuthors":[],"slug":"geological-outings-around-the-bay-stinson-beach","title":"Geological Outings Around the Bay: Stinson Beach","publishDate":1308855976,"format":"standard","headTitle":"QUEST | KQED Science","labelTerm":{"site":"quest"},"content":"\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinsontop2.jpg\" alt=\"stinson beach\" class=\"alignleft size-full\">\u003cem>\u003csup>If you can tear your eyes off the sea and sky, Stinson Beach offers a geological feast in its sediments, rocks and structure. Photos by Andrew Alden.\u003c/sup>\u003c/em>\u003c/span>\u003c/p>\n\u003cp>Even if geology weren't a factor, Stinson Beach would be among my top Bay Area beaches: it's small enough to thoroughly explore but large enough to take up a day, it offers shelter and plenty of wildlife, it has nearby places to eat and drink, and feels far from the workaday world without being a huge deal to get to.\u003c/p>\n\u003cp>But with me, geology is always a factor. Let's take in the scene.\u003c/p>\n\u003cp>\u003c!--more-->\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson12.jpg\" alt=\"stinson beach view\">\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>Stinson Beach is on Route 1 just north of San Francisco. You can drive there or take a bus, but either way what you see as you come in from the south is a lovely arc of sand. In the distance is the Point Reyes Peninsula with the low tableland of Bolinas on the left (a wave-cut platform) and the highlands of Point Reyes on the right. All of that land is on the Pacific plate and lies across the San Andreas fault. The fault runs just offshore, touching land in the center distance at the end of the beach and exiting the photo at upper right. Have a look at the geologic map.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinsonmap2.png\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinsonmap2.png\" width=\"500\" alt=\"geologic map\">\u003c/a>\u003c/p>\n\u003cp>\u003csub>Click the map for a larger version. Abbreviations: mt, marine terrace, Tms, Tertiary (Miocene) sedimentary rocks; QTs, Pliocene-Pleistocene sedimentary rocks; Kfs, Franciscan sandstone; sp, serpentinite; fc, Franciscan chert; ls, landslide deposits. From \u003ca href=\"http://geomaps.wr.usgs.gov/sfgeo/geologic/docs/Marin_County.kmz\">Marin County section\u003c/a> (KMZ file) of the USGS \u003ca href=\"http://geomaps.wr.usgs.gov/sfgeo/geologic/details.html\">Bay Area Geologic Map\u003c/a>.\u003c/sub>\u003c/p>\n\u003cp>Everything on the east side of the fault belongs to the Franciscan Complex, a big, sloppy geologic unit that includes bodies of sandstone, chert, shale, volcanic rocks and serpentinite. Parts of it are so mixed up that geologists have thrown up their hands and called it melange (\u003ca href=\"http://ww2.kqed.org/quest/2011/03/24/geological-outings-around-the-bay-shell-beach/\">which I featured in this post\u003c/a>).\u003c/p>\n\u003cp>If you're drawn to that great plate boundary, walk to the north end of the beach. The waves hit the beach here at an angle, sweeping the sand into crosshatches.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson22.jpg\" alt=\"sand waves\">\u003c/p>\n\u003cp>At the end of the beach is a tidal waterway leading to Bolinas Lagoon. There the repetitive wash of the tides builds symmetrical ripples like this.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson32.jpg\" alt=\"ripples\">\u003c/p>\n\u003cp>You won't see the fault here unless it happens to rupture while you're visiting, which is extremely unlikely. But if that happens, take pictures because the waves will swiftly erase the evidence. The lagoon is a feeding ground for all sorts of seabirds as well as the town's sheltered anchorage.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson42.jpg\" alt=\"bolinas lagoon\">\u003c/p>\n\u003cp>As you head south back down the beach, notice the terrace at the base of the hills, where many residences in the town of Stinson Beach sit. This is probably the same type of wave-cut platform that appears up and down the California coast (like \u003ca href=\"http://ww2.kqed.org/quest/2011/03/03/geological-outings-around-the-bay-pebble-beach/\">Pebble Beach\u003c/a>).\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson52.jpg\" alt=\"wave-cut platform\">\u003c/p>\n\u003cp>The beach's south end is a pile of boulders that have eroded from the geological plum-pudding of the Franciscan melange. The distant peninsula is the toe of an ancient landslide, one of many in this shaken-and-stirred area.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson62.jpg\" alt=\"boulders\">\u003c/p>\n\u003cp>Some of the boulders are straightforward rocks with a single composition, while others like this one are themselves melanges of many different ingredients.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson72.jpg\" alt=\"melange\">\u003c/p>\n\u003cp>Close up, you may be able to pick out every rock type found in the Franciscan—assembled in a single boulder!\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson82.jpg\" alt=\"melange\">\u003c/p>\n\u003cp>If you visited the \u003ca href=\"http://ww2.kqed.org/quest/2011/04/21/geological-outings-around-the-bay-marin-headlands/\">rocks of the Marin Headlands\u003c/a> a few weeks earlier, you'll recognize the Franciscan ribbon chert here, too, although it's green rather than red. That is due to the low-grade metamorphism that has affected the entire Franciscan in most of Marin.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson92.jpg\" alt=\"green chert\">\u003c/p>\n\u003cp>While you're studying these rocks, take a look at the cliff behind them, which is an intimate mixture of rocks and matrix that keeps crumbling into the waves to yield Stinson Beach's abundance of fresh, dark sand. \u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson992.jpg\" alt=\"folded chert\">\u003c/p>\n\u003cp>I always stay til sundown.\u003c/p>\n\u003cp>What are your top Bay Area beaches, and why?\u003c/p>\n\u003cp>\u003c/p>\n\u003cp> 37.899 -122.645\u003c/p>\n\n","blocks":[],"excerpt":"Even if geology weren't a factor, Stinson Beach would be among my top Bay Area beaches. But with me, geology is always a factor. Let's take in the scene.","status":"publish","parent":0,"modified":1311135088,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":32,"wordCount":666},"headData":{"title":"Geological Outings Around the Bay: Stinson Beach | KQED","description":"","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":""},"disqusIdentifier":"15399 http://www.kqed.org/quest/blog/?p=15399","disqusUrl":"https://ww2.kqed.org/quest/2011/06/23/geological-outings-around-the-bay-stinson-beach/","disqusTitle":"Geological Outings Around the Bay: Stinson Beach","path":"/quest/15399/geological-outings-around-the-bay-stinson-beach","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinsontop2.jpg\" alt=\"stinson beach\" class=\"alignleft size-full\">\u003cem>\u003csup>If you can tear your eyes off the sea and sky, Stinson Beach offers a geological feast in its sediments, rocks and structure. Photos by Andrew Alden.\u003c/sup>\u003c/em>\u003c/span>\u003c/p>\n\u003cp>Even if geology weren't a factor, Stinson Beach would be among my top Bay Area beaches: it's small enough to thoroughly explore but large enough to take up a day, it offers shelter and plenty of wildlife, it has nearby places to eat and drink, and feels far from the workaday world without being a huge deal to get to.\u003c/p>\n\u003cp>But with me, geology is always a factor. Let's take in the scene.\u003c/p>\n\u003cp>\u003c!--more-->\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson12.jpg\" alt=\"stinson beach view\">\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>Stinson Beach is on Route 1 just north of San Francisco. You can drive there or take a bus, but either way what you see as you come in from the south is a lovely arc of sand. In the distance is the Point Reyes Peninsula with the low tableland of Bolinas on the left (a wave-cut platform) and the highlands of Point Reyes on the right. All of that land is on the Pacific plate and lies across the San Andreas fault. The fault runs just offshore, touching land in the center distance at the end of the beach and exiting the photo at upper right. Have a look at the geologic map.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinsonmap2.png\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinsonmap2.png\" width=\"500\" alt=\"geologic map\">\u003c/a>\u003c/p>\n\u003cp>\u003csub>Click the map for a larger version. Abbreviations: mt, marine terrace, Tms, Tertiary (Miocene) sedimentary rocks; QTs, Pliocene-Pleistocene sedimentary rocks; Kfs, Franciscan sandstone; sp, serpentinite; fc, Franciscan chert; ls, landslide deposits. From \u003ca href=\"http://geomaps.wr.usgs.gov/sfgeo/geologic/docs/Marin_County.kmz\">Marin County section\u003c/a> (KMZ file) of the USGS \u003ca href=\"http://geomaps.wr.usgs.gov/sfgeo/geologic/details.html\">Bay Area Geologic Map\u003c/a>.\u003c/sub>\u003c/p>\n\u003cp>Everything on the east side of the fault belongs to the Franciscan Complex, a big, sloppy geologic unit that includes bodies of sandstone, chert, shale, volcanic rocks and serpentinite. Parts of it are so mixed up that geologists have thrown up their hands and called it melange (\u003ca href=\"http://ww2.kqed.org/quest/2011/03/24/geological-outings-around-the-bay-shell-beach/\">which I featured in this post\u003c/a>).\u003c/p>\n\u003cp>If you're drawn to that great plate boundary, walk to the north end of the beach. The waves hit the beach here at an angle, sweeping the sand into crosshatches.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson22.jpg\" alt=\"sand waves\">\u003c/p>\n\u003cp>At the end of the beach is a tidal waterway leading to Bolinas Lagoon. There the repetitive wash of the tides builds symmetrical ripples like this.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson32.jpg\" alt=\"ripples\">\u003c/p>\n\u003cp>You won't see the fault here unless it happens to rupture while you're visiting, which is extremely unlikely. But if that happens, take pictures because the waves will swiftly erase the evidence. The lagoon is a feeding ground for all sorts of seabirds as well as the town's sheltered anchorage.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson42.jpg\" alt=\"bolinas lagoon\">\u003c/p>\n\u003cp>As you head south back down the beach, notice the terrace at the base of the hills, where many residences in the town of Stinson Beach sit. This is probably the same type of wave-cut platform that appears up and down the California coast (like \u003ca href=\"http://ww2.kqed.org/quest/2011/03/03/geological-outings-around-the-bay-pebble-beach/\">Pebble Beach\u003c/a>).\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson52.jpg\" alt=\"wave-cut platform\">\u003c/p>\n\u003cp>The beach's south end is a pile of boulders that have eroded from the geological plum-pudding of the Franciscan melange. The distant peninsula is the toe of an ancient landslide, one of many in this shaken-and-stirred area.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson62.jpg\" alt=\"boulders\">\u003c/p>\n\u003cp>Some of the boulders are straightforward rocks with a single composition, while others like this one are themselves melanges of many different ingredients.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson72.jpg\" alt=\"melange\">\u003c/p>\n\u003cp>Close up, you may be able to pick out every rock type found in the Franciscan—assembled in a single boulder!\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson82.jpg\" alt=\"melange\">\u003c/p>\n\u003cp>If you visited the \u003ca href=\"http://ww2.kqed.org/quest/2011/04/21/geological-outings-around-the-bay-marin-headlands/\">rocks of the Marin Headlands\u003c/a> a few weeks earlier, you'll recognize the Franciscan ribbon chert here, too, although it's green rather than red. That is due to the low-grade metamorphism that has affected the entire Franciscan in most of Marin.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson92.jpg\" alt=\"green chert\">\u003c/p>\n\u003cp>While you're studying these rocks, take a look at the cliff behind them, which is an intimate mixture of rocks and matrix that keeps crumbling into the waves to yield Stinson Beach's abundance of fresh, dark sand. \u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/06/stinson992.jpg\" alt=\"folded chert\">\u003c/p>\n\u003cp>I always stay til sundown.\u003c/p>\n\u003cp>What are your top Bay Area beaches, and why?\u003c/p>\n\u003cp>\u003c/p>\n\u003cp> 37.899 -122.645\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/quest/15399/geological-outings-around-the-bay-stinson-beach","authors":["6228"],"categories":["quest_11"],"tags":["quest_294","quest_3489","quest_3580","quest_1608","quest_3706","quest_2447","quest_2484","quest_3783"],"featImg":"quest_15411","label":"quest"},"quest_13980":{"type":"posts","id":"quest_13980","meta":{"index":"posts_1591205157","site":"quest","id":"13980","score":null,"sort":[1303415507000]},"guestAuthors":[],"slug":"geological-outings-around-the-bay-marin-headlands","title":"Geological Outings Around the Bay: Marin Headlands","publishDate":1303415507,"format":"standard","headTitle":"QUEST | KQED Science","labelTerm":{"site":"quest"},"content":"\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/mheadthumb2.jpg\" alt=\"marin headlands\" class=\"alignleft size-full\">\u003cem>\u003csup>A ridge of deep-sea chert sets off the Golden Gate and its signature bridge. Photos by Andrew Alden except where noted.\u003c/sup>\u003c/em>\u003c/span>\u003c/p>\n\u003cp>Thousands of people, tourists and locals alike, come here to gaze over the Golden Gate. But if you turn your back to it, the Marin Headlands are a textbook location to see some classic rocks of the Franciscan Complex. Rocks like these set apart the landscapes that incorporate them, literally shaping San Francisco's worldview.\u003c/p>\n\u003cp>The Marin Headlands have such a distinctive set of Franciscan rocks that their geologic package is named the Marin Headlands terrane, a geologist's word that means a well-defined piece of land and the closely related rocks that underlie it. The Franciscan has about a dozen terranes represented in the Bay Area, and while the Marin Headlands terrane appears in several places, this is where to see it best.\u003c/p>\n\u003cp>\u003c!--more-->\u003c/p>\n\u003cp>The Headlands couldn't be easier to get to—the entrance is just north of the Golden Gate Bridge. Head west and start on Conzelman Road, and stop at the first turnout (Battery Spencer) if you can find a parking spot; if there isn't try the next, because all display the same rocks. The roadcuts on Conzelman Road have just been renewed as the roadway is improved, so it's a great time to study them. (Road work goes on during the week; check \u003ca href=\"http://www.projectheadlands.gov/\">projectheadlands.gov\u003c/a> for updates.) Here's what you'll be looking at. Remember that no hammering or collecting is allowed in the \u003ca href=\"http://www.nps.gov/goga/marin-headlands.htm\">Golden Gate National Recreation Area\u003c/a>.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/mheadconz12.jpg\" alt=\"conzelman road chert\">\u003c/p>\n\u003cp>The reddish-brown, swirly rock is ribbon chert. This hard sedimentary stone started out in the Pacific as deep-sea clay full of the microscopic shells of radiolarians, lying on the volcanic rocks of the seafloor. It was once flat beds, but as the seafloor was subducted beneath California the chert was crumpled into a picturesque state.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/mheadconz22.jpg\" alt=\"folded ribbon chert\">\u003c/p>\n\u003cp>The crust itself was also crumpled, sliced into ribbons and stacked up. That accounts for the look of the geologic map of the Headlands (click it to see it bigger).\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/mheadmap2.jpg\" width=\"500\" alt=\"marin headlands geologic map\">\u003cbr>\n\u003csub>\u003ci>From \u003ca href=\"http://pubs.usgs.gov/sim/2006/2918/\">USGS Scientific Investigations Map 2918\u003c/a>\u003c/i>\u003c/sub>\u003c/p>\n\u003cp>The map depicts three main rock types from the Franciscan: the oldest lava of the ancient seabed of Jurassic age (Jfv), the deep-sea chert that sifted down onto it over a period of some 100 million years (JKfc), and the sandstone that collected on top of that as the seafloor approached California during the Cretaceous Period (Kfs). Melange, as I've explained \u003ca href=\"http://ww2.kqed.org/quest/2011/03/24/geological-outings-around-the-bay-shell-beach/\">in my post about Shell Beach\u003c/a>, is an intimate mixture of all three (and more) Franciscan rock types. Alluvium is the young sediment that lies in river valleys.\u003c/p>\n\u003cp>The lava that once underlay the chert now crops out next to it. At the end of Conzelman Road, at Point Bonita (south of the \"Kfs\" label), there's a spot where you can see spectacularly preserved pillow lava, looking as pristine as it did 150 million years ago when it erupted into the deep sea.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/mheadpillows2.jpg\" alt=\"pillow lava\">\u003cbr>\n\u003csub>\u003ci>Photo courtesy \u003ca href=\"http://www.flickr.com/photos/edbierman/\">Ed Bierman\u003c/a> of Flickr under Creative Commons license\u003c/i>\u003c/sub>\u003c/p>\n\u003cp>You can see this lava close up on the south end of Rodeo Beach (northwest of \"Kfs\") in its mildly metamorphosed form known as greenstone. \u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/mheadgreenstone2.jpg\" alt=\"rodeo beach greenstone\">\u003c/p>\n\u003cp>While you're at the beach, take care NOT to resist the excellent pebbles, sourced from the whole range of the Franciscan. I'm told that Kirby Cove's pebble beach is just as good.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/mheadpebbles2.jpg\" alt=\"rodeo beach pebbles\">\u003c/p>\n\u003cp>If you're up for some hiking, there's a lot more to see. For instance, north of Rodeo Beach the view up the coast shows off the sandstone and melange.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/mheadnorth2.jpg\" alt=\"marin coast\">\u003c/p>\n\u003cp>And if you keep your eyes on the ground, you may spot black manganese minerals coating the chert. Parts of the Headlands were exploited for this strategic mineral during World War II. The most likely source for the material is the formation of manganese nodules, back when this chert was abyssal mud. To impress your friends, be sure to call out, \"Look! Psilomelane!\" when you find some. That's the name of this sooty-looking mixture of manganese oxides.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/mheadmang2.jpg\" alt=\"psilomelane\">\u003c/p>\n\u003cp>If you still must admire the Golden Gate instead of the rocks, let my colleague Brian Romans show you \u003ca href=\"http://ww2.kqed.org/quest/2010/10/14/sand-waves-and-the-golden-gate/\">some of the wonderful geology under that impressive strait\u003c/a>.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp> 37.829 -122.483\u003c/p>\n\n","blocks":[],"excerpt":"The Marin Headlands are a textbook location to see some classic rocks of the Franciscan Complex, rocks that literally shape San Francisco's worldview.","status":"publish","parent":0,"modified":1343973965,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":25,"wordCount":714},"headData":{"title":"Geological Outings Around the Bay: Marin Headlands | KQED","description":"","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":""},"disqusIdentifier":"13980 http://www.kqed.org/quest/blog/?p=13980","disqusUrl":"https://ww2.kqed.org/quest/2011/04/21/geological-outings-around-the-bay-marin-headlands/","disqusTitle":"Geological Outings Around the Bay: Marin Headlands","path":"/quest/13980/geological-outings-around-the-bay-marin-headlands","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/mheadthumb2.jpg\" alt=\"marin headlands\" class=\"alignleft size-full\">\u003cem>\u003csup>A ridge of deep-sea chert sets off the Golden Gate and its signature bridge. Photos by Andrew Alden except where noted.\u003c/sup>\u003c/em>\u003c/span>\u003c/p>\n\u003cp>Thousands of people, tourists and locals alike, come here to gaze over the Golden Gate. But if you turn your back to it, the Marin Headlands are a textbook location to see some classic rocks of the Franciscan Complex. Rocks like these set apart the landscapes that incorporate them, literally shaping San Francisco's worldview.\u003c/p>\n\u003cp>The Marin Headlands have such a distinctive set of Franciscan rocks that their geologic package is named the Marin Headlands terrane, a geologist's word that means a well-defined piece of land and the closely related rocks that underlie it. The Franciscan has about a dozen terranes represented in the Bay Area, and while the Marin Headlands terrane appears in several places, this is where to see it best.\u003c/p>\n\u003cp>\u003c!--more-->\u003c/p>\n\u003cp>The Headlands couldn't be easier to get to—the entrance is just north of the Golden Gate Bridge. Head west and start on Conzelman Road, and stop at the first turnout (Battery Spencer) if you can find a parking spot; if there isn't try the next, because all display the same rocks. The roadcuts on Conzelman Road have just been renewed as the roadway is improved, so it's a great time to study them. (Road work goes on during the week; check \u003ca href=\"http://www.projectheadlands.gov/\">projectheadlands.gov\u003c/a> for updates.) Here's what you'll be looking at. Remember that no hammering or collecting is allowed in the \u003ca href=\"http://www.nps.gov/goga/marin-headlands.htm\">Golden Gate National Recreation Area\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>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/mheadconz12.jpg\" alt=\"conzelman road chert\">\u003c/p>\n\u003cp>The reddish-brown, swirly rock is ribbon chert. This hard sedimentary stone started out in the Pacific as deep-sea clay full of the microscopic shells of radiolarians, lying on the volcanic rocks of the seafloor. It was once flat beds, but as the seafloor was subducted beneath California the chert was crumpled into a picturesque state.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/mheadconz22.jpg\" alt=\"folded ribbon chert\">\u003c/p>\n\u003cp>The crust itself was also crumpled, sliced into ribbons and stacked up. That accounts for the look of the geologic map of the Headlands (click it to see it bigger).\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/mheadmap2.jpg\" width=\"500\" alt=\"marin headlands geologic map\">\u003cbr>\n\u003csub>\u003ci>From \u003ca href=\"http://pubs.usgs.gov/sim/2006/2918/\">USGS Scientific Investigations Map 2918\u003c/a>\u003c/i>\u003c/sub>\u003c/p>\n\u003cp>The map depicts three main rock types from the Franciscan: the oldest lava of the ancient seabed of Jurassic age (Jfv), the deep-sea chert that sifted down onto it over a period of some 100 million years (JKfc), and the sandstone that collected on top of that as the seafloor approached California during the Cretaceous Period (Kfs). Melange, as I've explained \u003ca href=\"http://ww2.kqed.org/quest/2011/03/24/geological-outings-around-the-bay-shell-beach/\">in my post about Shell Beach\u003c/a>, is an intimate mixture of all three (and more) Franciscan rock types. Alluvium is the young sediment that lies in river valleys.\u003c/p>\n\u003cp>The lava that once underlay the chert now crops out next to it. At the end of Conzelman Road, at Point Bonita (south of the \"Kfs\" label), there's a spot where you can see spectacularly preserved pillow lava, looking as pristine as it did 150 million years ago when it erupted into the deep sea.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/mheadpillows2.jpg\" alt=\"pillow lava\">\u003cbr>\n\u003csub>\u003ci>Photo courtesy \u003ca href=\"http://www.flickr.com/photos/edbierman/\">Ed Bierman\u003c/a> of Flickr under Creative Commons license\u003c/i>\u003c/sub>\u003c/p>\n\u003cp>You can see this lava close up on the south end of Rodeo Beach (northwest of \"Kfs\") in its mildly metamorphosed form known as greenstone. \u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/mheadgreenstone2.jpg\" alt=\"rodeo beach greenstone\">\u003c/p>\n\u003cp>While you're at the beach, take care NOT to resist the excellent pebbles, sourced from the whole range of the Franciscan. I'm told that Kirby Cove's pebble beach is just as good.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/mheadpebbles2.jpg\" alt=\"rodeo beach pebbles\">\u003c/p>\n\u003cp>If you're up for some hiking, there's a lot more to see. For instance, north of Rodeo Beach the view up the coast shows off the sandstone and melange.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/mheadnorth2.jpg\" alt=\"marin coast\">\u003c/p>\n\u003cp>And if you keep your eyes on the ground, you may spot black manganese minerals coating the chert. Parts of the Headlands were exploited for this strategic mineral during World War II. The most likely source for the material is the formation of manganese nodules, back when this chert was abyssal mud. To impress your friends, be sure to call out, \"Look! Psilomelane!\" when you find some. That's the name of this sooty-looking mixture of manganese oxides.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/mheadmang2.jpg\" alt=\"psilomelane\">\u003c/p>\n\u003cp>If you still must admire the Golden Gate instead of the rocks, let my colleague Brian Romans show you \u003ca href=\"http://ww2.kqed.org/quest/2010/10/14/sand-waves-and-the-golden-gate/\">some of the wonderful geology under that impressive strait\u003c/a>.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp> 37.829 -122.483\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/quest/13980/geological-outings-around-the-bay-marin-headlands","authors":["6228"],"categories":["quest_11"],"tags":["quest_3507","quest_3580","quest_1237","quest_1738","quest_3747","quest_3820"],"featImg":"quest_14006","label":"quest"},"quest_19212":{"type":"posts","id":"quest_19212","meta":{"index":"posts_1591205157","site":"quest","id":"19212","score":null,"sort":[1302809442000]},"guestAuthors":[],"slug":"calera-limestone-a-gift-from-the-ancient-pacific","title":"Calera Limestone, a Gift from the Ancient Pacific","publishDate":1302809442,"format":"standard","headTitle":"QUEST | KQED Science","labelTerm":{"site":"quest"},"content":"\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/calerathumb.jpg\" alt=\"calera limestone\" class=\"alignleft size-full\">\u003cem>\u003csup>A disjointed body of rock called the Calera Limestone shows its typical colors, white to gray to black, at Rockaway Beach south of Pacifica. It has an interesting history and prehistory. Photos by Andrew Alden except where otherwise noted.\u003c/sup>\u003c/em>\u003c/span>\u003c/p>\n\u003cp>Limestone has always been a useful rock, but we have relatively little of it around here. The first settlers sought it out to burn, because roasted limestone becomes lime, the crucial ingredient in mortar. Small operators would stake a claim on an outcrop of limestone, build a lime kiln, and supply local customers as long as the rock or the fuel (local firewood) held out. \u003c/p>\n\u003cp>Today many country roads around here still bear the name \"Limekiln.\" And one of the Bay Area's more interesting rocks is a limestone named for the Spanish word for limekiln, \u003ci>calera\u003c/i>.\u003c/p>\n\u003cp>\u003c!--more-->\u003c/p>\n\u003cp>The Calera Limestone was named in 1914. Its so-called type locality, the place where its formal description was taken, was a quarry on a hill just north of Rockaway Beach south of Pacifica. The name comes from Calera Valley, from which we can presume that a limekiln operated there before the gold rush. \u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>The former quarry is in the Golden Gate National Recreation Area today, and that's where my photos come from. Limestone stands out from other rocks in its color palette, usually white and gray.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/caleraquarry.jpg\" alt=\"rockaway quarry\">\u003c/p>\n\u003cp>The quarry exposure shows that the limestone beds are tilted almost upright. Studies of microfossils date the Calera at 88 to 105 million years old, in the middle of the long Cretaceous Period. Parts of the limestone are quite dark, thanks to a few percent of organic matter.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/calerabeds.jpg\" alt=\"limestone bedding\">\u003c/p>\n\u003cp>The Calera Limestone is not a big, thick bed of stone; rather, it's one ingredient in the disjointed Franciscan Complex that I described at \u003ca href=\"http://ww2.kqed.org/quest/2011/03/24/geological-outings-around-the-bay-shell-beach/\">Shell Beach\u003c/a>. It's found in pods, lenses and stringers along the San Andreas fault between Pacifica and Gilroy in a group of Franciscan rocks called the Permanente terrane. Indeed, more of this terrane occurs at Parkfield, some 350 kilometers south of here. \u003c/p>\n\u003cp>Fault motion over the last 25 million years or so has carried this limestone north to the ocean's edge today, one earthquake at a time. You can see signs of the disruption in the rocks of Rockaway Quarry.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/calerabrec.jpg\" alt=\"brecciation\">\u003c/p>\n\u003cp>The natural process that shattered and recemented this rock is called brecciation. If you see a rock like this, with jagged pieces in a finer groundmass, you may call it breccia (BRET-cha).\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/caleraslick.jpg\" alt=\"slickenside\">\u003c/p>\n\u003cp>Another sign of disruption is this slickenside, the polished surface made by faulting. It's not often found in limestone, but the Rockaway Quarry has good examples.\u003c/p>\n\u003cp>Another body of Calera Limestone crops out west of Cupertino, where Henry Kaiser began his entry into the concrete business in 1939 with a quarry. Whereas the Rockaway Quarry produced mainly crushed rock, the Permanente Quarry (now the \u003ca href=\"http://www.lehighpermanente.com/#/henry-kaiser/4537948194\">Lehigh Permanente Quarry\u003c/a>) processes high-quality limestone into portland cement. \u003ca href=\"http://ww2.kqed.org/quest/2008/04/04/cement-a-dirty-business/\">QUEST featured this quarry in 2008\u003c/a>, including this picture of the excavation. It supplies about half of the Bay Area's cement today.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/calerapermanente.jpg\" alt=\"permanente quarry\">\u003cbr>\n\u003csub>\u003ci>Photo courtesy \u003ca href=\"http://www.flickr.com/people/kqedquest/\">KQED QUEST\u003c/a> under Creative Commons license\u003c/i>\u003c/sub>\u003c/p>\n\u003cp>Geologists have studied the Calera Limestone for many years, taking advantage of the excellent exposures in the quarry. They have learned that the limestone formed in tropical seas, far from land, as the calcium carbonate shells of microorganisms rained onto the seafloor from highly productive surface waters. The waters were shallow for an ocean basin, which means that the limestone formed on a sunken volcanic plateau or ridge rather than the flat deep seafloor. The typical limestone of the Midwest is very different, having formed in huge sheets in very shallow waters when the sea was much higher than today. In geo-speak, they are epicontinental whereas the Calera is pelagic.\u003c/p>\n\u003cp>The Calera Limestone plateau was carried by plate-tectonic motion from the tropical Pacific and plastered onto North America, where it remained without being pulled downward by subduction. The Calera is in pieces today not because it was torn apart during subduction, but because it formed in separate basins on a volcanic plateau and was torn apart much later by the San Andreas fault. \u003c/p>\n\u003cp>The upshot is that this limestone carries a precious record of conditions in the shallow Cretaceous tropical Pacific, a place and time for which we have little other evidence because subduction has removed the deep seafloor rocks. Those dark streaks in the limestone, rich in organic matter, record periods when the world ocean went stagnant and dead. They match well with similar rocks from other ocean basins, enabling us to place a signpost in time from a world now lost.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/caleraclass.jpg\" alt=\"calera limestone\">\u003cbr>\n\u003csub>\u003cem>Students and professional groups visit the Permanente Quarry for open-air lessons. Photo courtesy \u003ca href=\"http://www.flickr.com/people/paleololigo/\">Penny Higgins\u003c/a> of Flickr under Creative Commons license.\u003c/em>\u003c/sub>\u003c/p>\n\u003cp>\u003c/p>\n\u003cp> 37.614 -122.494\u003c/p>\n\n","blocks":[],"excerpt":"This humble stone is both economically and scientifically valuable, not just a mainstay of the concrete supply but a signpost in time from a world now lost.","status":"publish","parent":0,"modified":1311134731,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":24,"wordCount":801},"headData":{"title":"Calera Limestone, a Gift from the Ancient Pacific | KQED","description":"","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":""},"disqusIdentifier":"19212 http://www.kqed.org/quest/blog/?p=13777","disqusUrl":"https://ww2.kqed.org/quest/2011/04/14/calera-limestone-a-gift-from-the-ancient-pacific/","disqusTitle":"Calera Limestone, a Gift from the Ancient Pacific","path":"/quest/19212/calera-limestone-a-gift-from-the-ancient-pacific","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cp>\u003cspan class=\"left\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/calerathumb.jpg\" alt=\"calera limestone\" class=\"alignleft size-full\">\u003cem>\u003csup>A disjointed body of rock called the Calera Limestone shows its typical colors, white to gray to black, at Rockaway Beach south of Pacifica. It has an interesting history and prehistory. Photos by Andrew Alden except where otherwise noted.\u003c/sup>\u003c/em>\u003c/span>\u003c/p>\n\u003cp>Limestone has always been a useful rock, but we have relatively little of it around here. The first settlers sought it out to burn, because roasted limestone becomes lime, the crucial ingredient in mortar. Small operators would stake a claim on an outcrop of limestone, build a lime kiln, and supply local customers as long as the rock or the fuel (local firewood) held out. \u003c/p>\n\u003cp>Today many country roads around here still bear the name \"Limekiln.\" And one of the Bay Area's more interesting rocks is a limestone named for the Spanish word for limekiln, \u003ci>calera\u003c/i>.\u003c/p>\n\u003cp>\u003c!--more-->\u003c/p>\n\u003cp>The Calera Limestone was named in 1914. Its so-called type locality, the place where its formal description was taken, was a quarry on a hill just north of Rockaway Beach south of Pacifica. The name comes from Calera Valley, from which we can presume that a limekiln operated there before the gold rush. \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 former quarry is in the Golden Gate National Recreation Area today, and that's where my photos come from. Limestone stands out from other rocks in its color palette, usually white and gray.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/caleraquarry.jpg\" alt=\"rockaway quarry\">\u003c/p>\n\u003cp>The quarry exposure shows that the limestone beds are tilted almost upright. Studies of microfossils date the Calera at 88 to 105 million years old, in the middle of the long Cretaceous Period. Parts of the limestone are quite dark, thanks to a few percent of organic matter.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/calerabeds.jpg\" alt=\"limestone bedding\">\u003c/p>\n\u003cp>The Calera Limestone is not a big, thick bed of stone; rather, it's one ingredient in the disjointed Franciscan Complex that I described at \u003ca href=\"http://ww2.kqed.org/quest/2011/03/24/geological-outings-around-the-bay-shell-beach/\">Shell Beach\u003c/a>. It's found in pods, lenses and stringers along the San Andreas fault between Pacifica and Gilroy in a group of Franciscan rocks called the Permanente terrane. Indeed, more of this terrane occurs at Parkfield, some 350 kilometers south of here. \u003c/p>\n\u003cp>Fault motion over the last 25 million years or so has carried this limestone north to the ocean's edge today, one earthquake at a time. You can see signs of the disruption in the rocks of Rockaway Quarry.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/calerabrec.jpg\" alt=\"brecciation\">\u003c/p>\n\u003cp>The natural process that shattered and recemented this rock is called brecciation. If you see a rock like this, with jagged pieces in a finer groundmass, you may call it breccia (BRET-cha).\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/caleraslick.jpg\" alt=\"slickenside\">\u003c/p>\n\u003cp>Another sign of disruption is this slickenside, the polished surface made by faulting. It's not often found in limestone, but the Rockaway Quarry has good examples.\u003c/p>\n\u003cp>Another body of Calera Limestone crops out west of Cupertino, where Henry Kaiser began his entry into the concrete business in 1939 with a quarry. Whereas the Rockaway Quarry produced mainly crushed rock, the Permanente Quarry (now the \u003ca href=\"http://www.lehighpermanente.com/#/henry-kaiser/4537948194\">Lehigh Permanente Quarry\u003c/a>) processes high-quality limestone into portland cement. \u003ca href=\"http://ww2.kqed.org/quest/2008/04/04/cement-a-dirty-business/\">QUEST featured this quarry in 2008\u003c/a>, including this picture of the excavation. It supplies about half of the Bay Area's cement today.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/calerapermanente.jpg\" alt=\"permanente quarry\">\u003cbr>\n\u003csub>\u003ci>Photo courtesy \u003ca href=\"http://www.flickr.com/people/kqedquest/\">KQED QUEST\u003c/a> under Creative Commons license\u003c/i>\u003c/sub>\u003c/p>\n\u003cp>Geologists have studied the Calera Limestone for many years, taking advantage of the excellent exposures in the quarry. They have learned that the limestone formed in tropical seas, far from land, as the calcium carbonate shells of microorganisms rained onto the seafloor from highly productive surface waters. The waters were shallow for an ocean basin, which means that the limestone formed on a sunken volcanic plateau or ridge rather than the flat deep seafloor. The typical limestone of the Midwest is very different, having formed in huge sheets in very shallow waters when the sea was much higher than today. In geo-speak, they are epicontinental whereas the Calera is pelagic.\u003c/p>\n\u003cp>The Calera Limestone plateau was carried by plate-tectonic motion from the tropical Pacific and plastered onto North America, where it remained without being pulled downward by subduction. The Calera is in pieces today not because it was torn apart during subduction, but because it formed in separate basins on a volcanic plateau and was torn apart much later by the San Andreas fault. \u003c/p>\n\u003cp>The upshot is that this limestone carries a precious record of conditions in the shallow Cretaceous tropical Pacific, a place and time for which we have little other evidence because subduction has removed the deep seafloor rocks. Those dark streaks in the limestone, rich in organic matter, record periods when the world ocean went stagnant and dead. They match well with similar rocks from other ocean basins, enabling us to place a signpost in time from a world now lost.\u003c/p>\n\u003cp>\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2011/04/caleraclass.jpg\" alt=\"calera limestone\">\u003cbr>\n\u003csub>\u003cem>Students and professional groups visit the Permanente Quarry for open-air lessons. Photo courtesy \u003ca href=\"http://www.flickr.com/people/paleololigo/\">Penny Higgins\u003c/a> of Flickr under Creative Commons license.\u003c/em>\u003c/sub>\u003c/p>\n\u003cp>\u003c/p>\n\u003cp> 37.614 -122.494\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/quest/19212/calera-limestone-a-gift-from-the-ancient-pacific","authors":["6228"],"categories":["quest_8","quest_9","quest_11"],"tags":["quest_3494","quest_531","quest_3535","quest_3580","quest_1311","quest_1556","quest_3637","quest_3638","quest_3639","quest_3657","quest_3724","quest_2484","quest_3764"],"featImg":"quest_13784","label":"quest"}},"programsReducer":{"possible":{"id":"possible","title":"Possible","info":"Possible is hosted by entrepreneur Reid Hoffman and writer Aria Finger. Together in Possible, Hoffman and Finger lead enlightening discussions about building a brighter collective future. The show features interviews with visionary guests like Trevor Noah, Sam Altman and Janette Sadik-Khan. Possible paints an optimistic portrait of the world we can create through science, policy, business, art and our shared humanity. It asks: What if everything goes right for once? How can we get there? Each episode also includes a short fiction story generated by advanced AI GPT-4, serving as a thought-provoking springboard to speculate how humanity could leverage technology for good.","airtime":"SUN 2pm","imageSrc":"https://cdn.kqed.org/wp-content/uploads/2023/08/possible-5gxfizEbKOJ-pbF5ASgxrs_.1400x1400.jpg","officialWebsiteLink":"https://www.possible.fm/","meta":{"site":"news","source":"Possible"},"link":"/radio/program/possible","subscribe":{"apple":"https://podcasts.apple.com/us/podcast/possible/id1677184070","spotify":"https://open.spotify.com/show/730YpdUSNlMyPQwNnyjp4k"}},"1a":{"id":"1a","title":"1A","info":"1A is home to the national conversation. 1A brings on great guests and frames the best debate in ways that make you think, share and engage.","airtime":"MON-THU 11pm-12am","imageSrc":"https://ww2.kqed.org/radio/wp-content/uploads/sites/50/2018/04/1a.jpg","officialWebsiteLink":"https://the1a.org/","meta":{"site":"news","source":"npr"},"link":"/radio/program/1a","subscribe":{"npr":"https://rpb3r.app.goo.gl/RBrW","apple":"https://itunes.apple.com/WebObjects/MZStore.woa/wa/viewPodcast?s=143441&mt=2&id=1188724250&at=11l79Y&ct=nprdirectory","tuneIn":"https://tunein.com/radio/1A-p947376/","rss":"https://feeds.npr.org/510316/podcast.xml"}},"all-things-considered":{"id":"all-things-considered","title":"All Things Considered","info":"Every weekday, \u003cem>All Things Considered\u003c/em> hosts Robert Siegel, Audie Cornish, Ari Shapiro, and Kelly McEvers present the program's trademark mix of news, interviews, commentaries, reviews, and offbeat features. Michel Martin hosts on the weekends.","airtime":"MON-FRI 1pm-2pm, 4:30pm-6:30pm\u003cbr />SAT-SUN 5pm-6pm","imageSrc":"https://cdn.kqed.org/wp-content/uploads/2021/10/ATC_1400.jpg","officialWebsiteLink":"https://www.npr.org/programs/all-things-considered/","meta":{"site":"news","source":"npr"},"link":"/radio/program/all-things-considered"},"american-suburb-podcast":{"id":"american-suburb-podcast","title":"American Suburb: The Podcast","tagline":"The flip side of gentrification, told through one town","info":"Gentrification is changing cities across America, forcing people from neighborhoods they have long called home. Call them the displaced. Now those priced out of the Bay Area are looking for a better life in an unlikely place. American Suburb follows this migration to one California town along the Delta, 45 miles from San Francisco. But is this once sleepy suburb ready for them?","imageSrc":"https://ww2.kqed.org/news/wp-content/uploads/sites/10/powerpress/1440_0018_AmericanSuburb_iTunesTile_01.jpg","officialWebsiteLink":"/news/series/american-suburb-podcast","meta":{"site":"news","source":"kqed","order":"13"},"link":"/news/series/american-suburb-podcast/","subscribe":{"npr":"https://rpb3r.app.goo.gl/RBrW","apple":"https://itunes.apple.com/WebObjects/MZStore.woa/wa/viewPodcast?mt=2&id=1287748328","tuneIn":"https://tunein.com/radio/American-Suburb-p1086805/","rss":"https://ww2.kqed.org/news/series/american-suburb-podcast/feed/podcast","google":"https://podcasts.google.com/feed/aHR0cHM6Ly9mZWVkcy5tZWdhcGhvbmUuZm0vS1FJTkMzMDExODgxNjA5"}},"baycurious":{"id":"baycurious","title":"Bay Curious","tagline":"Exploring the Bay Area, one question at a time","info":"KQED’s new podcast, Bay Curious, gets to the bottom of the mysteries — both profound and peculiar — that give the Bay Area its unique identity. And we’ll do it with your help! You ask the questions. You decide what Bay Curious investigates. 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We cover topics like how fed-up administrators are developing surprising tactics to deal with classroom disruptions; how listening to podcasts are helping kids develop reading skills; the consequences of overparenting; and why interdisciplinary learning can engage students on all ends of the traditional achievement spectrum. This podcast is part of the MindShift education site, a division of KQED News. KQED is an NPR/PBS member station based in San Francisco. 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Hosts Steve Inskeep, David Greene and Rachel Martin bring you the latest breaking news and features to prepare you for the day.","airtime":"MON-FRI 3am-9am","imageSrc":"https://ww2.kqed.org/app/uploads/2021/10/ME_1400.jpg","officialWebsiteLink":"https://www.npr.org/programs/morning-edition/","meta":{"site":"news","source":"npr"},"link":"/radio/program/morning-edition"},"onourwatch":{"id":"onourwatch","title":"On Our Watch","tagline":"Police secrets, unsealed","info":"For decades, the process for how police police themselves has been inconsistent – if not opaque. In some states, like California, these proceedings were completely hidden. After a new police transparency law unsealed scores of internal affairs files, our reporters set out to examine these cases and the shadow world of police discipline. On Our Watch brings listeners into the rooms where officers are questioned and witnesses are interrogated to find out who this system is really protecting. Is it the officers, or the public they've sworn to serve?","imageSrc":"https://cdn.kqed.org/wp-content/uploads/2024/01/OOW_Tile_Final.png","imageAlt":"On Our Watch from NPR and KQED","officialWebsiteLink":"/podcasts/onourwatch","meta":{"site":"news","source":"kqed","order":"1"},"link":"/podcasts/onourwatch","subscribe":{"apple":"https://podcasts.apple.com/podcast/id1567098962","google":"https://podcasts.google.com/feed/aHR0cHM6Ly9mZWVkcy5ucHIub3JnLzUxMDM2MC9wb2RjYXN0LnhtbD9zYz1nb29nbGVwb2RjYXN0cw","npr":"https://rpb3r.app.goo.gl/onourwatch","spotify":"https://open.spotify.com/show/0OLWoyizopu6tY1XiuX70x","tuneIn":"https://tunein.com/radio/On-Our-Watch-p1436229/","stitcher":"https://www.stitcher.com/show/on-our-watch","rss":"https://feeds.npr.org/510360/podcast.xml"}},"on-the-media":{"id":"on-the-media","title":"On The Media","info":"Our weekly podcast explores how the media 'sausage' is made, casts an incisive eye on fluctuations in the marketplace of ideas, and examines threats to the freedom of information and expression in America and abroad. 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