Side Trips from Interstate 5: Panoche and Tumey Hills
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accelerated erosion in the bed of Cache Creek testifies to a big change upstream: a switch in the drainage of Clear Lake. 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Her science radio stories appear on KQED and NPR.\r\n\r\nEmail her at astanden@kqed.org","avatar":"https://secure.gravatar.com/avatar/3d021b72de685a788b0487b059d0a6a1?s=600&d=blank&r=g","twitter":null,"facebook":null,"instagram":null,"linkedin":null,"sites":[{"site":"news","roles":["subscriber"]},{"site":"futureofyou","roles":["subscriber"]},{"site":"stateofhealth","roles":["subscriber"]},{"site":"science","roles":["editor"]},{"site":"quest","roles":["subscriber"]}],"headData":{"title":"Amy Standen | KQED","description":null,"ogImgSrc":"https://secure.gravatar.com/avatar/3d021b72de685a788b0487b059d0a6a1?s=600&d=blank&r=g","twImgSrc":"https://secure.gravatar.com/avatar/3d021b72de685a788b0487b059d0a6a1?s=600&d=blank&r=g"},"isLoading":false,"link":"/author/amystanden"},"andrew-alden":{"type":"authors","id":"6228","meta":{"index":"authors_1591205172","id":"6228","found":true},"name":"Andrew Alden","firstName":"Andrew","lastName":"Alden","slug":"andrew-alden","email":"alden@andrew-alden.com","display_author_email":false,"staff_mastheads":[],"title":null,"bio":"Andrew Alden earned his geology degree at the University of New Hampshire and moved back to the Bay Area to work at the U.S. Geological Survey for six years. He has \u003ca href=\"http://geology.about.com/\">written on geology for About.com\u003c/a> since its founding in 1997. In 2007, he started the Oakland Geology blog, which won recognition as \"Best of the East Bay\" from the \u003ci>East Bay Express\u003c/i> in 2010. 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From on high, and on the geologic map, the Kettleman Hills are a dramatic and obvious example of an anticlinal arch. The center is uplifted and dissected by erosion, so that the insides are the older rocks.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2013/02/28/side-trips-from-interstate-5-kettleman-hills/kethillsgeomap/\" rel=\"attachment wp-att-50107\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/02/kethillsgeomap.png\" alt=\"kethillsgeomap\" width=\"600\" height=\"400\" class=\"aligncenter size-full wp-image-50107\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillsgeomap.png 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillsgeomap-400x267.png 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>These hills drew the attention of oil drillers early on, but their holes came up dry until October 3rd, 1928, when a well struck a highly overpressured reservoir some 7000 feet down. A gusher resulted that lasted for three years. Oil production from the field was so great that the market was depressed and several other oil-producing states grumbled about the lack of regulation in California. \u003c/p>\n\u003cfigure id=\"attachment_50111\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2013/02/28/side-trips-from-interstate-5-kettleman-hills/kethillswellhead/\" rel=\"attachment wp-att-50111\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/02/kethillswellhead.jpg\" alt=\"Massive Christmas tree of well controls used in the Kettleman Hills North Dome oil field\" width=\"600\" height=\"468\" class=\"size-full wp-image-50111\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillswellhead.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillswellhead-400x312.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Massive \"Christmas tree\" of well controls used in the Kettleman Hills North Dome oil field. Photo courtesy {link url=\"http://www.flickr.com/photos/bilbord99/\"}Bill Mulder{/link} of flickr under Creative Commons license\u003c/figcaption>\u003c/figure>\n\u003cp>The town of Avenal arose with the oil boom, along with a host of businesses based on petroleum. \u003c/p>\n\u003cfigure id=\"attachment_50104\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2013/02/28/side-trips-from-interstate-5-kettleman-hills/kettlemanking/\" rel=\"attachment wp-att-50104\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/02/kettlemanking.png\" alt=\"This company was later acquired by Beacon.\" width=\"600\" height=\"453\" class=\"size-full wp-image-50104\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/02/kettlemanking.png 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/02/kettlemanking-400x302.png 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">This company was later acquired by Beacon. Photo courtesy {link url=\"http://www.flickr.com/photos/thomashawk/\"}Thomas Hawk{/link} of Flickr under Creative Commons license\u003c/figcaption>\u003c/figure>\n\u003cp>The classic geologic treatment of the Kettleman Hills oil field was issued in 1940 by the U.S. Geological Survey as \u003ca href=\"http://pubs.er.usgs.gov/publication/pp195\">Professional Paper 195\u003c/a>. \u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>Today the field is almost played out, although you can never discount new advances that might revive it. But the hills remain, blooming every spring. And the roadcuts, where you can access them, are still \u003ca href=\"http://inyo.coffeecup.com/site/kh/kettleman.html\">full of fossils\u003c/a>.\u003c/p>\n\u003cfigure id=\"attachment_50109\" class=\"wp-caption aligncenter\" style=\"max-width: 500px\">\u003ca href=\"http://ww2.kqed.org/quest/2013/02/28/side-trips-from-interstate-5-kettleman-hills/kethillssanddollar/\" rel=\"attachment wp-att-50109\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/02/kethillssanddollar.jpg\" alt=\"The sand dollar Dendraster gibbsi\" width=\"500\" height=\"484\" class=\"size-full wp-image-50109\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillssanddollar.jpg 500w, https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillssanddollar-400x387.jpg 400w, https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillssanddollar-32x32.jpg 32w\" sizes=\"(max-width: 500px) 100vw, 500px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">The sand dollar Dendraster gibbsi, 43 millimeters across, from the interior of the Kettleman Hills. Photo courtesy {link url=\"http://www.flickr.com/photos/jsjgeology/\"}James St. John{/link} of Flickr under Creative Commons license\u003c/figcaption>\u003c/figure>\n\u003cp>You can cross the hills in three places, two of them busy highways: the Avenal cutoff in the north and state route 41 in the middle. I've tried looking for places to pull over on these roads and it basically shouldn't be done. Take the third way, farther south starting at the Utica Avenue exit; head west and then immediately south on 25th Avenue, taking it all the way to Twisselman Road and back to the freeway.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2013/02/28/side-trips-from-interstate-5-kettleman-hills/kethillsroutemap/\" rel=\"attachment wp-att-50108\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/02/kethillsroutemap.png\" alt=\"kethillsroutemap\" width=\"600\" height=\"425\" class=\"aligncenter size-full wp-image-50108\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillsroutemap.png 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillsroutemap-400x283.png 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>The edge of the hills is marked by the California Aqueduct, which is always worth contemplating.\u003c/p>\n\u003cfigure id=\"attachment_50106\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2013/02/28/side-trips-from-interstate-5-kettleman-hills/kethillsaqueduct/\" rel=\"attachment wp-att-50106\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/02/kethillsaqueduct.jpg\" alt=\"Photos by Andrew Alden\" width=\"600\" height=\"362\" class=\"size-full wp-image-50106\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillsaqueduct.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillsaqueduct-400x241.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>There are a few roadcuts worth checking out. They all seem to be full of fossils dating from the Pleistocene, when the Central Valley was an arm of the sea. With the compression of the Coast Ranges, outlying folds in the crust of the San Joaquin Valley were pushed up into anticlines which formed traps for huge amounts of oil and gas.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2013/02/28/side-trips-from-interstate-5-kettleman-hills/kethillfossils/\" rel=\"attachment wp-att-50105\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/02/kethillfossils.jpg\" alt=\"kethillfossils\" width=\"600\" height=\"400\" class=\"aligncenter size-full wp-image-50105\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillfossils.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillfossils-400x267.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>Where Devil's Den Road splits off is the gap between the Middle and South Domes of the Kettleman Hills. East of there was the shoreline of Tulare Lake, an inland sea that was drained away long ago by the farms and cities of the Great Valley. Imagine the effect it must have had on the local climate here. This countryside, at its best, is worlds away from I-5.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2013/02/28/side-trips-from-interstate-5-kettleman-hills/kethillstop/\" rel=\"attachment wp-att-50110\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/02/kethillstop.jpg\" alt=\"kethillstop\" width=\"640\" height=\"360\" class=\"aligncenter size-full wp-image-50110\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillstop.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillstop-400x225.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>Remember, the point of a side trip is not to rush—plenty of opportunity for that on the freeway—and be ready to stop and smell the flowers, or at least sniff the breeze.\u003c/p>\n\n","blocks":[],"excerpt":"This side trip takes you into the quiet range of hills that runs along the freeway south of Coalinga.","status":"publish","parent":0,"modified":1362707277,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":16,"wordCount":568},"headData":{"title":"Side Trips from Interstate 5: Kettleman Hills | KQED","description":"This side trip takes you into the quiet range of hills that runs along the freeway south of Coalinga.","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":"","schema":{"@context":"http://schema.org","@type":"Article","headline":"Side Trips from Interstate 5: Kettleman Hills","datePublished":"2013-02-28T19:59:35.000Z","dateModified":"2013-03-08T01:47:57.000Z","image":"https://cdn.kqed.org/wp-content/uploads/2020/02/KQED-OG-Image@1x.png"}},"disqusIdentifier":"50103 http://science.kqed.org/quest/?p=50103","disqusUrl":"https://ww2.kqed.org/quest/2013/02/28/side-trips-from-interstate-5-kettleman-hills/","disqusTitle":"Side Trips from Interstate 5: Kettleman Hills","path":"/quest/50103/side-trips-from-interstate-5-kettleman-hills","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cp>As you head south on I-5 past Coalinga, the road runs just east of a long range of hills. From on high, and on the geologic map, the Kettleman Hills are a dramatic and obvious example of an anticlinal arch. The center is uplifted and dissected by erosion, so that the insides are the older rocks.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2013/02/28/side-trips-from-interstate-5-kettleman-hills/kethillsgeomap/\" rel=\"attachment wp-att-50107\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/02/kethillsgeomap.png\" alt=\"kethillsgeomap\" width=\"600\" height=\"400\" class=\"aligncenter size-full wp-image-50107\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillsgeomap.png 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillsgeomap-400x267.png 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>These hills drew the attention of oil drillers early on, but their holes came up dry until October 3rd, 1928, when a well struck a highly overpressured reservoir some 7000 feet down. A gusher resulted that lasted for three years. Oil production from the field was so great that the market was depressed and several other oil-producing states grumbled about the lack of regulation in California. \u003c/p>\n\u003cfigure id=\"attachment_50111\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2013/02/28/side-trips-from-interstate-5-kettleman-hills/kethillswellhead/\" rel=\"attachment wp-att-50111\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/02/kethillswellhead.jpg\" alt=\"Massive Christmas tree of well controls used in the Kettleman Hills North Dome oil field\" width=\"600\" height=\"468\" class=\"size-full wp-image-50111\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillswellhead.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillswellhead-400x312.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Massive \"Christmas tree\" of well controls used in the Kettleman Hills North Dome oil field. Photo courtesy {link url=\"http://www.flickr.com/photos/bilbord99/\"}Bill Mulder{/link} of flickr under Creative Commons license\u003c/figcaption>\u003c/figure>\n\u003cp>The town of Avenal arose with the oil boom, along with a host of businesses based on petroleum. \u003c/p>\n\u003cfigure id=\"attachment_50104\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2013/02/28/side-trips-from-interstate-5-kettleman-hills/kettlemanking/\" rel=\"attachment wp-att-50104\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/02/kettlemanking.png\" alt=\"This company was later acquired by Beacon.\" width=\"600\" height=\"453\" class=\"size-full wp-image-50104\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/02/kettlemanking.png 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/02/kettlemanking-400x302.png 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">This company was later acquired by Beacon. Photo courtesy {link url=\"http://www.flickr.com/photos/thomashawk/\"}Thomas Hawk{/link} of Flickr under Creative Commons license\u003c/figcaption>\u003c/figure>\n\u003cp>The classic geologic treatment of the Kettleman Hills oil field was issued in 1940 by the U.S. Geological Survey as \u003ca href=\"http://pubs.er.usgs.gov/publication/pp195\">Professional Paper 195\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>Today the field is almost played out, although you can never discount new advances that might revive it. But the hills remain, blooming every spring. And the roadcuts, where you can access them, are still \u003ca href=\"http://inyo.coffeecup.com/site/kh/kettleman.html\">full of fossils\u003c/a>.\u003c/p>\n\u003cfigure id=\"attachment_50109\" class=\"wp-caption aligncenter\" style=\"max-width: 500px\">\u003ca href=\"http://ww2.kqed.org/quest/2013/02/28/side-trips-from-interstate-5-kettleman-hills/kethillssanddollar/\" rel=\"attachment wp-att-50109\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/02/kethillssanddollar.jpg\" alt=\"The sand dollar Dendraster gibbsi\" width=\"500\" height=\"484\" class=\"size-full wp-image-50109\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillssanddollar.jpg 500w, https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillssanddollar-400x387.jpg 400w, https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillssanddollar-32x32.jpg 32w\" sizes=\"(max-width: 500px) 100vw, 500px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">The sand dollar Dendraster gibbsi, 43 millimeters across, from the interior of the Kettleman Hills. Photo courtesy {link url=\"http://www.flickr.com/photos/jsjgeology/\"}James St. John{/link} of Flickr under Creative Commons license\u003c/figcaption>\u003c/figure>\n\u003cp>You can cross the hills in three places, two of them busy highways: the Avenal cutoff in the north and state route 41 in the middle. I've tried looking for places to pull over on these roads and it basically shouldn't be done. Take the third way, farther south starting at the Utica Avenue exit; head west and then immediately south on 25th Avenue, taking it all the way to Twisselman Road and back to the freeway.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2013/02/28/side-trips-from-interstate-5-kettleman-hills/kethillsroutemap/\" rel=\"attachment wp-att-50108\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/02/kethillsroutemap.png\" alt=\"kethillsroutemap\" width=\"600\" height=\"425\" class=\"aligncenter size-full wp-image-50108\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillsroutemap.png 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillsroutemap-400x283.png 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>The edge of the hills is marked by the California Aqueduct, which is always worth contemplating.\u003c/p>\n\u003cfigure id=\"attachment_50106\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2013/02/28/side-trips-from-interstate-5-kettleman-hills/kethillsaqueduct/\" rel=\"attachment wp-att-50106\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/02/kethillsaqueduct.jpg\" alt=\"Photos by Andrew Alden\" width=\"600\" height=\"362\" class=\"size-full wp-image-50106\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillsaqueduct.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillsaqueduct-400x241.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>There are a few roadcuts worth checking out. They all seem to be full of fossils dating from the Pleistocene, when the Central Valley was an arm of the sea. With the compression of the Coast Ranges, outlying folds in the crust of the San Joaquin Valley were pushed up into anticlines which formed traps for huge amounts of oil and gas.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2013/02/28/side-trips-from-interstate-5-kettleman-hills/kethillfossils/\" rel=\"attachment wp-att-50105\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/02/kethillfossils.jpg\" alt=\"kethillfossils\" width=\"600\" height=\"400\" class=\"aligncenter size-full wp-image-50105\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillfossils.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillfossils-400x267.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>Where Devil's Den Road splits off is the gap between the Middle and South Domes of the Kettleman Hills. East of there was the shoreline of Tulare Lake, an inland sea that was drained away long ago by the farms and cities of the Great Valley. Imagine the effect it must have had on the local climate here. This countryside, at its best, is worlds away from I-5.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2013/02/28/side-trips-from-interstate-5-kettleman-hills/kethillstop/\" rel=\"attachment wp-att-50110\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2013/02/kethillstop.jpg\" alt=\"kethillstop\" width=\"640\" height=\"360\" class=\"aligncenter size-full wp-image-50110\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillstop.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2013/02/kethillstop-400x225.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>Remember, the point of a side trip is not to rush—plenty of opportunity for that on the freeway—and be ready to stop and smell the flowers, or at least sniff the breeze.\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/quest/50103/side-trips-from-interstate-5-kettleman-hills","authors":["6228"],"categories":["quest_11"],"tags":["quest_639","quest_13200","quest_11797","quest_9804","quest_2057","quest_2169","quest_13202"],"featImg":"quest_50110","label":"quest"},"quest_43267":{"type":"posts","id":"quest_43267","meta":{"index":"posts_1591205157","site":"quest","id":"43267","score":null,"sort":[1346358126000]},"guestAuthors":[],"slug":"outdoor-labs-the-uc-natural-reserve-system","title":"Outdoor Labs: The UC Natural Reserve System","publishDate":1346358126,"format":"standard","headTitle":"QUEST | KQED Science","labelTerm":{"site":"quest"},"content":"\u003cfigure id=\"attachment_43269\" class=\"wp-caption alignleft\" style=\"max-width: 360px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/08/30/outdoor-labs-the-uc-natural-reserve-system/angelo-deer/\" rel=\"attachment wp-att-43269\">\u003cimg class=\"size-full wp-image-43269\" title=\"angelo-deer\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/08/angelo-deer.jpg\" alt=\"\" width=\"360\" height=\"216\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">A young buck, unafraid of visitors, munches under old apple trees at the Angelo Reserve. Photos by Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>When I pulled in at the \u003ca href=\"http://nrs.ucop.edu/reserves/angelo/angelo.htm\">Angelo Coast Range Reserve\u003c/a> nearly five hours' drive to Mendocino County, I knew I was deep in the woods, but what I saw there told me something more about the place—the outside world is really shut out. A family of deer was feasting from old apple trees as two visiting children and their camera-wielding parents looked on at close range.\u003c/p>\n\u003cp>The hills and woods and meadows and streams of Angelo aren't quite like your average piece of back country: the Coast Range hills are drilled with wells and probes, the Douglas-fir and oak-madrone woods are wirelessly networked, the river-terrace meadows are dotted with flags and sensors, and the South Fork Eel River holds experimental nets and cages as well as aquatic life. The Angelo Reserve is a stage for 21st-century research that turns the very outdoors into a scientific laboratory. And it's just one of 38 such stages in the \u003ca href=\"http://nrs.ucop.edu/\">UC Natural Reserve System\u003c/a> that sample nearly all of California's biomes.\u003c/p>\n\u003cp>I was at Angelo with a group of science writers to hear about some of the research projects going on. While the University of California runs it, the Reserve System serves many institutions. At Angelo, for instance, the U.S. Geological Survey has a stream-gauge station on Elder Creek, \u003ca href=\"http://nature.nps.gov/nnl/site.cfm?Site=ELCR-CA\">a National Natural Landmark\u003c/a>.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/08/30/outdoor-labs-the-uc-natural-reserve-system/angelo-usgs/\" rel=\"attachment wp-att-43268\">\u003cimg class=\"aligncenter size-full wp-image-43268\" title=\"angelo-usgs\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/08/angelo-usgs.jpg\" alt=\"\" width=\"600\" height=\"480\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/08/angelo-usgs.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/08/angelo-usgs-400x320.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>The heart of the reserve is the South Fork Eel River, part of the large Eel River watershed. The river not only provides salmon habitat, but also is California's largest sediment provider to the Pacific after the Bay Area. Biologists can tinker with all the ecological variables they can handle, from the members of the food web to the nutrients in the water. They can erect shades to restrict sunlight or screens to keep out predators, and they can add and subtract sediments from the streambed. And the untouched riverbanks minimize pollution and other distortions from human activities. UC Berkeley professor \u003ca href=\"http://ib.berkeley.edu/labs/power/mary_power_history.html\">Mary Power\u003c/a> described some of the intricate trials her group has been carrying out in the Eel River.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/08/30/outdoor-labs-the-uc-natural-reserve-system/angelo-eelriver/\" rel=\"attachment wp-att-43270\">\u003cimg class=\"aligncenter size-full wp-image-43270\" title=\"angelo-eelriver\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/08/angelo-eelriver.jpg\" alt=\"\" width=\"600\" height=\"391\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/08/angelo-eelriver.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/08/angelo-eelriver-400x261.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>I found it charming in a nerdy way to see the river populated with dozens of little experiments as I hiked along the streambed. Of course, I was mostly noticing the rocks. There's underground research at Angelo, too, like the wirelessly networked watershed my group saw during our visit. The power comes from solar panels in the treetops, and the data is beamed live to Berkeley. UC Berkeley professor \u003ca href=\"http://eps.berkeley.edu/development/view_person.php?uid=1164&page=76\">Bill Dietrich\u003c/a> showed us around the installation.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/08/30/outdoor-labs-the-uc-natural-reserve-system/angelo-top/\" rel=\"attachment wp-att-43273\">\u003cimg class=\"aligncenter size-full wp-image-43273\" title=\"angelo-top\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/08/angelo-top.jpg\" alt=\"\" width=\"640\" height=\"360\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/08/angelo-top.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2012/08/angelo-top-400x225.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003c/p>\n\u003cp>The intensive focus on this little watershed promises to pay off on the scale of whole rivers. What intrigued me is that it's shedding light on the zone of undisturbed but decayed rock—saprolite—between sound bedrock and the soil.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/08/30/outdoor-labs-the-uc-natural-reserve-system/angelo-subsoil/\" rel=\"attachment wp-att-43272\">\u003cimg class=\"aligncenter size-full wp-image-43272\" title=\"angelo-subsoil\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/08/angelo-subsoil.jpg\" alt=\"\" width=\"600\" height=\"446\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/08/angelo-subsoil.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/08/angelo-subsoil-400x297.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>This zone is turning out to be important in ways that the trees have always known about, but not us. Some trees seem to rely on the saprolite while others, even in the same biome, ignore it. Saprolite is a new variable that belongs in global climate models, and the data from Angelo is giving us the first outlines of its meaning.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/08/30/outdoor-labs-the-uc-natural-reserve-system/angelo-graph/\" rel=\"attachment wp-att-43271\">\u003cimg class=\"aligncenter size-full wp-image-43271\" title=\"angelo-graph\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/08/angelo-graph.jpg\" alt=\"\" width=\"599\" height=\"400\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/08/angelo-graph.jpg 599w, https://ww2.kqed.org/app/uploads/sites/39/2012/08/angelo-graph-400x267.jpg 400w\" sizes=\"(max-width: 599px) 100vw, 599px\">\u003c/a>\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>\u003ca href=\"http://nrs.ucop.edu/by_name.htm\">The other 37 sites in the UC Natural Reserve System\u003c/a> have their own stories, and having now seen two of them (the other is the White Mountain Research Center, \u003ca href=\"http://ww2.kqed.org/quest/2012/03/22/testing-a-new-drug-for-mountain-sickness/\">where I tested drugs for science\u003c/a>) my appetite is roused to learn more.\u003c/p>\n\n","blocks":[],"excerpt":"The University of California runs a unique set of 38 pristine properties around the state for scientific research.","status":"publish","parent":0,"modified":1366749650,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":15,"wordCount":596},"headData":{"title":"Outdoor Labs: The UC Natural Reserve System | KQED","description":"The University of California runs a unique set of 38 pristine properties around the state for scientific research.","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":"","schema":{"@context":"http://schema.org","@type":"Article","headline":"Outdoor Labs: The UC Natural Reserve System","datePublished":"2012-08-30T20:22:06.000Z","dateModified":"2013-04-23T20:40:50.000Z","image":"https://cdn.kqed.org/wp-content/uploads/2020/02/KQED-OG-Image@1x.png"}},"disqusIdentifier":"43267 http://science.kqed.org/quest/?p=43267","disqusUrl":"https://ww2.kqed.org/quest/2012/08/30/outdoor-labs-the-uc-natural-reserve-system/","disqusTitle":"Outdoor Labs: The UC Natural Reserve System","path":"/quest/43267/outdoor-labs-the-uc-natural-reserve-system","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cfigure id=\"attachment_43269\" class=\"wp-caption alignleft\" style=\"max-width: 360px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/08/30/outdoor-labs-the-uc-natural-reserve-system/angelo-deer/\" rel=\"attachment wp-att-43269\">\u003cimg class=\"size-full wp-image-43269\" title=\"angelo-deer\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/08/angelo-deer.jpg\" alt=\"\" width=\"360\" height=\"216\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">A young buck, unafraid of visitors, munches under old apple trees at the Angelo Reserve. Photos by Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>When I pulled in at the \u003ca href=\"http://nrs.ucop.edu/reserves/angelo/angelo.htm\">Angelo Coast Range Reserve\u003c/a> nearly five hours' drive to Mendocino County, I knew I was deep in the woods, but what I saw there told me something more about the place—the outside world is really shut out. A family of deer was feasting from old apple trees as two visiting children and their camera-wielding parents looked on at close range.\u003c/p>\n\u003cp>The hills and woods and meadows and streams of Angelo aren't quite like your average piece of back country: the Coast Range hills are drilled with wells and probes, the Douglas-fir and oak-madrone woods are wirelessly networked, the river-terrace meadows are dotted with flags and sensors, and the South Fork Eel River holds experimental nets and cages as well as aquatic life. The Angelo Reserve is a stage for 21st-century research that turns the very outdoors into a scientific laboratory. And it's just one of 38 such stages in the \u003ca href=\"http://nrs.ucop.edu/\">UC Natural Reserve System\u003c/a> that sample nearly all of California's biomes.\u003c/p>\n\u003cp>I was at Angelo with a group of science writers to hear about some of the research projects going on. While the University of California runs it, the Reserve System serves many institutions. At Angelo, for instance, the U.S. Geological Survey has a stream-gauge station on Elder Creek, \u003ca href=\"http://nature.nps.gov/nnl/site.cfm?Site=ELCR-CA\">a National Natural Landmark\u003c/a>.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/08/30/outdoor-labs-the-uc-natural-reserve-system/angelo-usgs/\" rel=\"attachment wp-att-43268\">\u003cimg class=\"aligncenter size-full wp-image-43268\" title=\"angelo-usgs\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/08/angelo-usgs.jpg\" alt=\"\" width=\"600\" height=\"480\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/08/angelo-usgs.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/08/angelo-usgs-400x320.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>The heart of the reserve is the South Fork Eel River, part of the large Eel River watershed. The river not only provides salmon habitat, but also is California's largest sediment provider to the Pacific after the Bay Area. Biologists can tinker with all the ecological variables they can handle, from the members of the food web to the nutrients in the water. They can erect shades to restrict sunlight or screens to keep out predators, and they can add and subtract sediments from the streambed. And the untouched riverbanks minimize pollution and other distortions from human activities. UC Berkeley professor \u003ca href=\"http://ib.berkeley.edu/labs/power/mary_power_history.html\">Mary Power\u003c/a> described some of the intricate trials her group has been carrying out in the Eel River.\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/2012/08/30/outdoor-labs-the-uc-natural-reserve-system/angelo-eelriver/\" rel=\"attachment wp-att-43270\">\u003cimg class=\"aligncenter size-full wp-image-43270\" title=\"angelo-eelriver\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/08/angelo-eelriver.jpg\" alt=\"\" width=\"600\" height=\"391\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/08/angelo-eelriver.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/08/angelo-eelriver-400x261.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>I found it charming in a nerdy way to see the river populated with dozens of little experiments as I hiked along the streambed. Of course, I was mostly noticing the rocks. There's underground research at Angelo, too, like the wirelessly networked watershed my group saw during our visit. The power comes from solar panels in the treetops, and the data is beamed live to Berkeley. UC Berkeley professor \u003ca href=\"http://eps.berkeley.edu/development/view_person.php?uid=1164&page=76\">Bill Dietrich\u003c/a> showed us around the installation.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/08/30/outdoor-labs-the-uc-natural-reserve-system/angelo-top/\" rel=\"attachment wp-att-43273\">\u003cimg class=\"aligncenter size-full wp-image-43273\" title=\"angelo-top\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/08/angelo-top.jpg\" alt=\"\" width=\"640\" height=\"360\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/08/angelo-top.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2012/08/angelo-top-400x225.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003c/p>\n\u003cp>The intensive focus on this little watershed promises to pay off on the scale of whole rivers. What intrigued me is that it's shedding light on the zone of undisturbed but decayed rock—saprolite—between sound bedrock and the soil.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/08/30/outdoor-labs-the-uc-natural-reserve-system/angelo-subsoil/\" rel=\"attachment wp-att-43272\">\u003cimg class=\"aligncenter size-full wp-image-43272\" title=\"angelo-subsoil\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/08/angelo-subsoil.jpg\" alt=\"\" width=\"600\" height=\"446\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/08/angelo-subsoil.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/08/angelo-subsoil-400x297.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>This zone is turning out to be important in ways that the trees have always known about, but not us. Some trees seem to rely on the saprolite while others, even in the same biome, ignore it. Saprolite is a new variable that belongs in global climate models, and the data from Angelo is giving us the first outlines of its meaning.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/08/30/outdoor-labs-the-uc-natural-reserve-system/angelo-graph/\" rel=\"attachment wp-att-43271\">\u003cimg class=\"aligncenter size-full wp-image-43271\" title=\"angelo-graph\" src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/08/angelo-graph.jpg\" alt=\"\" width=\"599\" height=\"400\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/08/angelo-graph.jpg 599w, https://ww2.kqed.org/app/uploads/sites/39/2012/08/angelo-graph-400x267.jpg 400w\" sizes=\"(max-width: 599px) 100vw, 599px\">\u003c/a>\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>\u003ca href=\"http://nrs.ucop.edu/by_name.htm\">The other 37 sites in the UC Natural Reserve System\u003c/a> have their own stories, and having now seen two of them (the other is the White Mountain Research Center, \u003ca href=\"http://ww2.kqed.org/quest/2012/03/22/testing-a-new-drug-for-mountain-sickness/\">where I tested drugs for science\u003c/a>) my appetite is roused to learn more.\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/quest/43267/outdoor-labs-the-uc-natural-reserve-system","authors":["6228"],"categories":["quest_4","quest_11","quest_11766"],"tags":["quest_639","quest_921","quest_934","quest_1594","quest_1789","quest_13202","quest_11410","quest_2477","quest_11409","quest_3021"],"featImg":"quest_43273","label":"quest"},"quest_35632":{"type":"posts","id":"quest_35632","meta":{"index":"posts_1591205157","site":"quest","id":"35632","score":null,"sort":[1334847180000]},"guestAuthors":[],"slug":"the-switching-outlets-of-clear-lake","title":"The Switching Outlets of Clear Lake","publishDate":1334847180,"format":"standard","headTitle":"QUEST | KQED Science","labelTerm":{"site":"quest"},"content":"\u003cfigure id=\"attachment_35637\" class=\"wp-caption alignleft\" style=\"max-width: 300px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/04/19/the-switching-outlets-of-clear-lake/cachecreekcut/\" rel=\"attachment wp-att-35637\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/04/cachecreekcut-300x169.jpg\" alt=\"\" title=\"cachecreekcut\" width=\"300\" height=\"169\" class=\"size-thumbnail wp-image-35637\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Recently accelerated erosion in the bed of Cache Creek testifies to a big change upstream: a switch in the drainage of Clear Lake. Photos by Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>The rainy, dynamic terrain of the northern Coast Range features many rivers, but very few natural lakes. Any basins that may form by tectonic activity have short lives. Either they fill up with sediment, or rivers erode into them and they drain dry. \u003c/p>\n\u003cp>Clear Lake, by far the largest lake in the Coast Range, has sediments in it dating back some half a million years. The lake's basin never seems to fill with mud, although Clear Lake has always been shallow. Apparently something builds up the basin's sides whenever the lake outlet threatens to cut downward far enough to drain the lake dry. In recent geologic time, Clear Lake has drained eastward and westward at different times as one exit or the other has been plugged. You can visit both exits and glimpse the geologic evidence yourself.\u003c/p>\n\u003cp>Today Clear Lake drains east to the Central Valley down Cache Creek through a rugged canyon with high, steep walls. But biologists tell us that the fish of Clear Lake come from both the Russian River and the Central Valley. Without that clue, we might not make much of the straight little valley northwest of Clear Lake, just a few meters above the present lake level. Created by slow faulting, the valley holds some bits of water called Blue Lakes. What could have made Clear Lake drain in this direction?\u003c/p>\n\u003cfigure id=\"attachment_35633\" class=\"wp-caption aligncenter\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/04/19/the-switching-outlets-of-clear-lake/clearlakemap/\" rel=\"attachment wp-att-35633\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/04/clearlakemap.jpg\" alt=\"\" title=\"clearlakemap\" width=\"640\" height=\"441\" class=\"size-full wp-image-35633\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/04/clearlakemap.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2012/04/clearlakemap-400x276.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Clear Lake shows signs of having drained northwest, through Blue Lakes, as well as southeast through Cache Creek, its current outlet.\u003c/figcaption>\u003c/figure>\n\u003cp>The east side of Clear Lake is full of young volcanoes ranging in size from Mount Konocti down to a dozen little cones a few tens of thousands of years old. With that in mind it's easy to picture a large lava flow, or the emergence of a small cone, blocking Cache Creek and causing the lake to rise until it spilled through the valley of Blue Lakes to the Russian River.\u003c/p>\n\u003cp>You can drive up state route 20 from the north side of Clear Lake into this valley, and it's easy to picture it holding a river. Then the road hits a large bump, a hill right in the middle of the valley, and that seems to be the end of the line. But geologic mapping has shown that this is an ancient landslide.\u003c/p>\n\u003cfigure id=\"attachment_35635\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/04/19/the-switching-outlets-of-clear-lake/bluelakeslide/\" rel=\"attachment wp-att-35635\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/04/bluelakeslide.jpg\" alt=\"\" title=\"bluelakeslide\" width=\"600\" height=\"377\" class=\"size-full wp-image-35635\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/04/bluelakeslide.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/04/bluelakeslide-400x251.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">The bare-topped hill blocking the valley past Upper Blue Lake is a landslide. The forested land in front is a younger delta fan.\u003c/figcaption>\u003c/figure>\n\u003cp>A look at the topography here is instructive, and Google Maps' \"terrain\" setting is an excellent way to do that. The photo above was taken from the middle \"20\" symbol and the hill is marked with an asterisk.\u003c/p>\n\u003cfigure id=\"attachment_35634\" class=\"wp-caption aligncenter\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/04/19/the-switching-outlets-of-clear-lake/bluelakemap/\" rel=\"attachment wp-att-35634\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/04/bluelakemap.jpg\" alt=\"\" title=\"bluelakemap\" width=\"640\" height=\"460\" class=\"size-full wp-image-35634\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/04/bluelakemap.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2012/04/bluelakemap-400x288.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Annotations: V symbols are delta-forming drainages, S marks landslides or possible landslides.\u003c/figcaption>\u003c/figure>\n\u003cp>Notice how well-organized the stream drainages are leading down to the lakes. Each of the larger streams has built out a delta of sediment. But west of the lakes is an area of poorly organized, hummocky terrain that closely resembles \u003ca href=\"http://ww2.kqed.org/quest/2011/03/31/landslide-season/\">the body of a landslide\u003c/a>. It appears to me that the landslide nearest to Blue Lakes is the smallest and possibly the latest of a whole series.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>The native tribes around Clear Lake have old stories of just such a landslide here. If we take them literally, that would place the event within the last few thousand years. The next thing to happen in this scenario is that Clear Lake would rise still further until it overcame the natural dam on Cache Creek and resumed its interrupted eastward drainage. In fact, there's no reason this should have happened only once.\u003c/p>\n\u003cp>But I mentioned visiting both exits of Clear Lake. Cache Creek goes into roadless country but on the other side, right where it meets state route 16, you can pull over at \u003ca href=\"http://www.yolocounty.org/index.aspx?page=379\">Cache Creek Regional Park\u003c/a> and see this beautiful exposure, about 5 meters high, across the river.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/04/19/the-switching-outlets-of-clear-lake/cachecreekbank/\" rel=\"attachment wp-att-35636\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/04/cachecreekbank.jpg\" alt=\"\" title=\"cachecreekbank\" width=\"600\" height=\"471\" class=\"aligncenter size-full wp-image-35636\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/04/cachecreekbank.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/04/cachecreekbank-400x314.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>From top to bottom its features are plain as day: a nice flat abandoned floodplain, a layer of coarse river rocks and gravel, the rugged profile of a former streambed, and the \u003ca href=\"http://ww2.kqed.org/quest/2012/01/26/geological-outings-around-the-bay-mount-vaca-and-the-monticello-dam/\">tilted bedrock of the Great Valley Sequence\u003c/a>. In the typical river, the streambed is cut downward so slowly, only in the largest \"hundred-year\" storm events, that an exposure like this is never seen. But today's newly invigorated Cache Creek has cut through all this in one clean chop in just a few millennia.\u003c/p>\n\n","blocks":[],"excerpt":"Why has Clear Lake drained two different ways in recent geologic time? Volcanoes and landslides made it happen.","status":"publish","parent":0,"modified":1335901285,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":13,"wordCount":768},"headData":{"title":"The Switching Outlets of Clear Lake | KQED","description":"Why has Clear Lake drained two different ways in recent geologic time? Volcanoes and landslides made it happen.","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":"","schema":{"@context":"http://schema.org","@type":"Article","headline":"The Switching Outlets of Clear Lake","datePublished":"2012-04-19T14:53:00.000Z","dateModified":"2012-05-01T19:41:25.000Z","image":"https://cdn.kqed.org/wp-content/uploads/2020/02/KQED-OG-Image@1x.png"}},"disqusIdentifier":"35632 http://science.kqed.org/quest/?p=35632","disqusUrl":"https://ww2.kqed.org/quest/2012/04/19/the-switching-outlets-of-clear-lake/","disqusTitle":"The Switching Outlets of Clear Lake","path":"/quest/35632/the-switching-outlets-of-clear-lake","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cfigure id=\"attachment_35637\" class=\"wp-caption alignleft\" style=\"max-width: 300px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/04/19/the-switching-outlets-of-clear-lake/cachecreekcut/\" rel=\"attachment wp-att-35637\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/04/cachecreekcut-300x169.jpg\" alt=\"\" title=\"cachecreekcut\" width=\"300\" height=\"169\" class=\"size-thumbnail wp-image-35637\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Recently accelerated erosion in the bed of Cache Creek testifies to a big change upstream: a switch in the drainage of Clear Lake. Photos by Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>The rainy, dynamic terrain of the northern Coast Range features many rivers, but very few natural lakes. Any basins that may form by tectonic activity have short lives. Either they fill up with sediment, or rivers erode into them and they drain dry. \u003c/p>\n\u003cp>Clear Lake, by far the largest lake in the Coast Range, has sediments in it dating back some half a million years. The lake's basin never seems to fill with mud, although Clear Lake has always been shallow. Apparently something builds up the basin's sides whenever the lake outlet threatens to cut downward far enough to drain the lake dry. In recent geologic time, Clear Lake has drained eastward and westward at different times as one exit or the other has been plugged. You can visit both exits and glimpse the geologic evidence yourself.\u003c/p>\n\u003cp>Today Clear Lake drains east to the Central Valley down Cache Creek through a rugged canyon with high, steep walls. But biologists tell us that the fish of Clear Lake come from both the Russian River and the Central Valley. Without that clue, we might not make much of the straight little valley northwest of Clear Lake, just a few meters above the present lake level. Created by slow faulting, the valley holds some bits of water called Blue Lakes. What could have made Clear Lake drain in this direction?\u003c/p>\n\u003cfigure id=\"attachment_35633\" class=\"wp-caption aligncenter\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/04/19/the-switching-outlets-of-clear-lake/clearlakemap/\" rel=\"attachment wp-att-35633\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/04/clearlakemap.jpg\" alt=\"\" title=\"clearlakemap\" width=\"640\" height=\"441\" class=\"size-full wp-image-35633\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/04/clearlakemap.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2012/04/clearlakemap-400x276.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Clear Lake shows signs of having drained northwest, through Blue Lakes, as well as southeast through Cache Creek, its current outlet.\u003c/figcaption>\u003c/figure>\n\u003cp>The east side of Clear Lake is full of young volcanoes ranging in size from Mount Konocti down to a dozen little cones a few tens of thousands of years old. With that in mind it's easy to picture a large lava flow, or the emergence of a small cone, blocking Cache Creek and causing the lake to rise until it spilled through the valley of Blue Lakes to the Russian River.\u003c/p>\n\u003cp>You can drive up state route 20 from the north side of Clear Lake into this valley, and it's easy to picture it holding a river. Then the road hits a large bump, a hill right in the middle of the valley, and that seems to be the end of the line. But geologic mapping has shown that this is an ancient landslide.\u003c/p>\n\u003cfigure id=\"attachment_35635\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/04/19/the-switching-outlets-of-clear-lake/bluelakeslide/\" rel=\"attachment wp-att-35635\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/04/bluelakeslide.jpg\" alt=\"\" title=\"bluelakeslide\" width=\"600\" height=\"377\" class=\"size-full wp-image-35635\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/04/bluelakeslide.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/04/bluelakeslide-400x251.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">The bare-topped hill blocking the valley past Upper Blue Lake is a landslide. The forested land in front is a younger delta fan.\u003c/figcaption>\u003c/figure>\n\u003cp>A look at the topography here is instructive, and Google Maps' \"terrain\" setting is an excellent way to do that. The photo above was taken from the middle \"20\" symbol and the hill is marked with an asterisk.\u003c/p>\n\u003cfigure id=\"attachment_35634\" class=\"wp-caption aligncenter\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/04/19/the-switching-outlets-of-clear-lake/bluelakemap/\" rel=\"attachment wp-att-35634\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/04/bluelakemap.jpg\" alt=\"\" title=\"bluelakemap\" width=\"640\" height=\"460\" class=\"size-full wp-image-35634\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/04/bluelakemap.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2012/04/bluelakemap-400x288.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Annotations: V symbols are delta-forming drainages, S marks landslides or possible landslides.\u003c/figcaption>\u003c/figure>\n\u003cp>Notice how well-organized the stream drainages are leading down to the lakes. Each of the larger streams has built out a delta of sediment. But west of the lakes is an area of poorly organized, hummocky terrain that closely resembles \u003ca href=\"http://ww2.kqed.org/quest/2011/03/31/landslide-season/\">the body of a landslide\u003c/a>. It appears to me that the landslide nearest to Blue Lakes is the smallest and possibly the latest of a whole series.\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 native tribes around Clear Lake have old stories of just such a landslide here. If we take them literally, that would place the event within the last few thousand years. The next thing to happen in this scenario is that Clear Lake would rise still further until it overcame the natural dam on Cache Creek and resumed its interrupted eastward drainage. In fact, there's no reason this should have happened only once.\u003c/p>\n\u003cp>But I mentioned visiting both exits of Clear Lake. Cache Creek goes into roadless country but on the other side, right where it meets state route 16, you can pull over at \u003ca href=\"http://www.yolocounty.org/index.aspx?page=379\">Cache Creek Regional Park\u003c/a> and see this beautiful exposure, about 5 meters high, across the river.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/04/19/the-switching-outlets-of-clear-lake/cachecreekbank/\" rel=\"attachment wp-att-35636\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/04/cachecreekbank.jpg\" alt=\"\" title=\"cachecreekbank\" width=\"600\" height=\"471\" class=\"aligncenter size-full wp-image-35636\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/04/cachecreekbank.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/04/cachecreekbank-400x314.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>From top to bottom its features are plain as day: a nice flat abandoned floodplain, a layer of coarse river rocks and gravel, the rugged profile of a former streambed, and the \u003ca href=\"http://ww2.kqed.org/quest/2012/01/26/geological-outings-around-the-bay-mount-vaca-and-the-monticello-dam/\">tilted bedrock of the Great Valley Sequence\u003c/a>. In the typical river, the streambed is cut downward so slowly, only in the largest \"hundred-year\" storm events, that an exposure like this is never seen. But today's newly invigorated Cache Creek has cut through all this in one clean chop in just a few millennia.\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/quest/35632/the-switching-outlets-of-clear-lake","authors":["6228"],"categories":["quest_11"],"tags":["quest_11002","quest_3516","quest_639","quest_11003","quest_1608","quest_13202","quest_2465"],"featImg":"quest_35637","label":"quest"},"quest_32484":{"type":"posts","id":"quest_32484","meta":{"index":"posts_1591205157","site":"quest","id":"32484","score":null,"sort":[1331237263000]},"guestAuthors":[],"slug":"side-trips-from-interstate-5-panoche-and-tumey-hills","title":"Side Trips from Interstate 5: Panoche and Tumey Hills","publishDate":1331237263,"format":"standard","headTitle":"QUEST | KQED Science","labelTerm":{"site":"quest"},"content":"\u003cfigure id=\"attachment_32499\" class=\"wp-caption alignleft\" style=\"max-width: 300px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/03/08/side-trips-from-interstate-5-panoche-and-tumey-hills/panoche/\" rel=\"attachment wp-att-32499\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/panoche-300x169.jpg\" alt=\"\" title=\"panoche\" width=\"300\" height=\"169\" class=\"size-thumbnail wp-image-32499\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">The Panoche Hills provide a splendid overlook to the Great Valley on good days. Photos by Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>Most people, it's probably fair to say, loathe Interstate 5 between Redding and Bakersfield. If all you want to do is get from point A to point B, I-5 enables that, but the road is so smooth and the route so straight that the typical driver resents the time spent on it, even at 80 mph and faster. Traffic can reach dangerous speeds, eyes get glazed, attention wavers, and tempers grow short.\u003c/p>\n\u003cp>As for me, I love the chance to enjoy I-5. I make it a full day's trip to get from the Bay Area to Southern California or the Shasta region, and that gives me a long enough leash to get off the freeway at least once during the day. So I'd like to share with you some of my favorite side trips, and they don't include Santa Nella.\u003c/p>\n\u003cp>One that I've enjoyed several times goes past the Panoche and Tumey Hills, a big patch of wild land along the east side of the Coast Range managed by the Bureau of Land Management. It's a loop of backroad about halfway to Bakersfield, due west of Fresno. Its north end is Little Panoche Road and its south end is Panoche Road. It includes some dirt road and takes a good hour if you don't stop much. Its two notable landmarks are Mercey Hot Springs and the village of Panoche, in well-hidden Panoche Valley. I've never stopped at either place because it's the countryside that attracts me.\u003c/p>\n\u003cp>Let's have a look at the geologic map of the area, derived from the nice \u003ca href=\"http://www.quake.ca.gov/gmaps/GMC/stategeologicmap.html\">interactive state geologic map\u003c/a>:\u003c/p>\n\u003cfigure id=\"attachment_32500\" class=\"wp-caption aligncenter\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/03/08/side-trips-from-interstate-5-panoche-and-tumey-hills/panochegeomap/\" rel=\"attachment wp-att-32500\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/panochegeomap.jpg\" alt=\"\" title=\"panochegeomap\" width=\"640\" height=\"529\" class=\"size-full wp-image-32500\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/panochegeomap.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/panochegeomap-400x331.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Significant map units: Ku, upper Cretaceous marine rocks; Ep, Paleocene marine rocks; E, Eocene marine rocks; QP, Pliocene-Pleistocene nonmarine rocks; Q, modern and recent sediment; Qoa, Quaternary river terraces; KJf, Franciscan complex; um, ultramafic rocks\u003c/figcaption>\u003c/figure>\n\u003cp>The bulk of the hills consists of late Cretaceous mudstones, laid down in a shallow sea some 80 million years ago when the Sierra Nevada was a great chain of volcanoes like today's Cascade Range. This sea persisted past Cretaceous time into the succeeding Paleocene and Eocene epochs, perhaps 50 or 40 million years ago. There are rare plesiosaur and mosasaur fossils in the older section and lots of fossil wood throughout. But we don't have time to hunt fossils, although collecting for personal purposes is allowed.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>Little Panoche Road runs up the valley of Little Panoche Creek, where at least two levels of stream terraces are visible that testify to different episodes of erosion. They in turn are undoubtedly related to the uplift history of these hills.\u003c/p>\n\u003cfigure id=\"attachment_32498\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/03/08/side-trips-from-interstate-5-panoche-and-tumey-hills/littlepanoche/\" rel=\"attachment wp-att-32498\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/littlepanoche.jpg\" alt=\"\" title=\"littlepanoche\" width=\"600\" height=\"400\" class=\"size-full wp-image-32498\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/littlepanoche.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/littlepanoche-400x267.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Looking across Little Panoche Creek to the north flank of the Panoche Hills.\u003c/figcaption>\u003c/figure>\n\u003cp>The road turns south and runs through Little Panoche Valley, passing the low-key \u003ca href=\"https://merceyhotsprings.com/\">Mercey Hot Springs\u003c/a> resort. The entrance to the BLM's \u003ca href=\"http://www.blm.gov/ca/st/en/fo/hollister/recreation/panoche.html\">Panoche Hills Recreation Area\u003c/a> is here, too. At the head of the valley the road cuts through Glaucophane Ridge, an unexpected exposure of old Franciscan rocks, then goes straight south across the wide and gentle Panoche Valley and ends at Panoche Road. This pocket of farmland is one of Central California's hidden gems. The south side of the valley presents a striking set of terraces. These are mapped as river terraces but might be lake beds; I haven't looked into the literature. In either case they, too, attest to ancient episodes of accelerated erosion.\u003c/p>\n\u003cfigure id=\"attachment_32503\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/03/08/side-trips-from-interstate-5-panoche-and-tumey-hills/panocheterraces/\" rel=\"attachment wp-att-32503\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/panocheterraces.jpg\" alt=\"\" title=\"panocheterraces\" width=\"600\" height=\"387\" class=\"size-full wp-image-32503\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/panocheterraces.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/panocheterraces-400x258.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Buck Peak, in the Griswold Hills, and river terraces of the Panoche Valley.\u003c/figcaption>\u003c/figure>\n\u003cp>Panoche Road west eventually gets you to Paicines, south of Hollister. The road east gets you back to I-5, but all of the crooked part is decent dirt. In wet weather, turn back here, or maybe go a little ways on the paved part and daydream about taking New Idria Road south to the remote ghost town of Idria. The eastern end of the valley has good views of the Panoche Hills from the south, but eventually the road crosses the creek without benefit of a bridge and then turns to dirt.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/03/08/side-trips-from-interstate-5-panoche-and-tumey-hills/panoches/\" rel=\"attachment wp-att-32502\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/panoches.jpg\" alt=\"\" title=\"panoches\" width=\"600\" height=\"438\" class=\"aligncenter size-full wp-image-32502\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/panoches.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/panoches-400x292.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>In fine weather, ford the stream and proceed across some splendid and scenic country.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/03/08/side-trips-from-interstate-5-panoche-and-tumey-hills/panocheroad/\" rel=\"attachment wp-att-32501\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/panocheroad.jpg\" alt=\"\" title=\"panocheroad\" width=\"600\" height=\"414\" class=\"aligncenter size-full wp-image-32501\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/panocheroad.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/panocheroad-400x276.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>At this point, you are in the \u003ca href=\"http://www.blm.gov/ca/st/en/fo/hollister/recreation/tumey.html\">Tumey Hills Recreation Area\u003c/a>. These hills are lower and drier than the Panoches, and the rocks along the road are quite different. They are young sandstones and conglomerates formed as the Coast Range began to rise, just a few million years ago.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/03/08/side-trips-from-interstate-5-panoche-and-tumey-hills/tumeycgl/\" rel=\"attachment wp-att-32504\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/tumeycgl.jpg\" alt=\"\" title=\"tumeycgl\" width=\"500\" height=\"401\" class=\"aligncenter size-full wp-image-32504\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/tumeycgl.jpg 500w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/tumeycgl-400x321.jpg 400w\" sizes=\"(max-width: 500px) 100vw, 500px\">\u003c/a>\u003c/p>\n\u003cp>Watch the road as well as the rocks, but don't miss the landscape. All photos in this post were taken in late March.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/03/08/side-trips-from-interstate-5-panoche-and-tumey-hills/tumeys/\" rel=\"attachment wp-att-32506\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/tumeys.jpg\" alt=\"\" title=\"tumeys\" width=\"600\" height=\"473\" class=\"aligncenter size-full wp-image-32506\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/tumeys.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/tumeys-400x315.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>When you reach I-5, you'll have a choice of eating places to get you ready to roll again. Maybe, like me, you prefer to think of it as the place where the iron dinosaur used to be. It was the creation of the late Carmon Neff of Chowchilla, and I don't know where it went.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/03/08/side-trips-from-interstate-5-panoche-and-tumey-hills/tumeydino/\" rel=\"attachment wp-att-32505\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/tumeydino.jpg\" alt=\"\" title=\"tumeydino\" width=\"600\" height=\"401\" class=\"aligncenter size-full wp-image-32505\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/tumeydino.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/tumeydino-400x267.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\n","blocks":[],"excerpt":"Interstate 5 doesn't have to be a dreary drive. Take a geological side trip on the way, for instance to the hidden Coast Range treasures due west of Fresno.","status":"publish","parent":0,"modified":1332966031,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":19,"wordCount":848},"headData":{"title":"Side Trips from Interstate 5: Panoche and Tumey Hills | KQED","description":"Interstate 5 doesn't have to be a dreary drive. Take a geological side trip on the way, for instance to the hidden Coast Range treasures due west of Fresno.","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":"","schema":{"@context":"http://schema.org","@type":"Article","headline":"Side Trips from Interstate 5: Panoche and Tumey Hills","datePublished":"2012-03-08T20:07:43.000Z","dateModified":"2012-03-28T20:20:31.000Z","image":"https://cdn.kqed.org/wp-content/uploads/2020/02/KQED-OG-Image@1x.png"}},"disqusIdentifier":"32484 http://science.kqed.org/quest/?p=32484","disqusUrl":"https://ww2.kqed.org/quest/2012/03/08/side-trips-from-interstate-5-panoche-and-tumey-hills/","disqusTitle":"Side Trips from Interstate 5: Panoche and Tumey Hills","path":"/quest/32484/side-trips-from-interstate-5-panoche-and-tumey-hills","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cfigure id=\"attachment_32499\" class=\"wp-caption alignleft\" style=\"max-width: 300px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/03/08/side-trips-from-interstate-5-panoche-and-tumey-hills/panoche/\" rel=\"attachment wp-att-32499\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/panoche-300x169.jpg\" alt=\"\" title=\"panoche\" width=\"300\" height=\"169\" class=\"size-thumbnail wp-image-32499\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">The Panoche Hills provide a splendid overlook to the Great Valley on good days. Photos by Andrew Alden\u003c/figcaption>\u003c/figure>\n\u003cp>Most people, it's probably fair to say, loathe Interstate 5 between Redding and Bakersfield. If all you want to do is get from point A to point B, I-5 enables that, but the road is so smooth and the route so straight that the typical driver resents the time spent on it, even at 80 mph and faster. Traffic can reach dangerous speeds, eyes get glazed, attention wavers, and tempers grow short.\u003c/p>\n\u003cp>As for me, I love the chance to enjoy I-5. I make it a full day's trip to get from the Bay Area to Southern California or the Shasta region, and that gives me a long enough leash to get off the freeway at least once during the day. So I'd like to share with you some of my favorite side trips, and they don't include Santa Nella.\u003c/p>\n\u003cp>One that I've enjoyed several times goes past the Panoche and Tumey Hills, a big patch of wild land along the east side of the Coast Range managed by the Bureau of Land Management. It's a loop of backroad about halfway to Bakersfield, due west of Fresno. Its north end is Little Panoche Road and its south end is Panoche Road. It includes some dirt road and takes a good hour if you don't stop much. Its two notable landmarks are Mercey Hot Springs and the village of Panoche, in well-hidden Panoche Valley. I've never stopped at either place because it's the countryside that attracts me.\u003c/p>\n\u003cp>Let's have a look at the geologic map of the area, derived from the nice \u003ca href=\"http://www.quake.ca.gov/gmaps/GMC/stategeologicmap.html\">interactive state geologic map\u003c/a>:\u003c/p>\n\u003cfigure id=\"attachment_32500\" class=\"wp-caption aligncenter\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/03/08/side-trips-from-interstate-5-panoche-and-tumey-hills/panochegeomap/\" rel=\"attachment wp-att-32500\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/panochegeomap.jpg\" alt=\"\" title=\"panochegeomap\" width=\"640\" height=\"529\" class=\"size-full wp-image-32500\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/panochegeomap.jpg 640w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/panochegeomap-400x331.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Significant map units: Ku, upper Cretaceous marine rocks; Ep, Paleocene marine rocks; E, Eocene marine rocks; QP, Pliocene-Pleistocene nonmarine rocks; Q, modern and recent sediment; Qoa, Quaternary river terraces; KJf, Franciscan complex; um, ultramafic rocks\u003c/figcaption>\u003c/figure>\n\u003cp>The bulk of the hills consists of late Cretaceous mudstones, laid down in a shallow sea some 80 million years ago when the Sierra Nevada was a great chain of volcanoes like today's Cascade Range. This sea persisted past Cretaceous time into the succeeding Paleocene and Eocene epochs, perhaps 50 or 40 million years ago. There are rare plesiosaur and mosasaur fossils in the older section and lots of fossil wood throughout. But we don't have time to hunt fossils, although collecting for personal purposes is allowed.\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>Little Panoche Road runs up the valley of Little Panoche Creek, where at least two levels of stream terraces are visible that testify to different episodes of erosion. They in turn are undoubtedly related to the uplift history of these hills.\u003c/p>\n\u003cfigure id=\"attachment_32498\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/03/08/side-trips-from-interstate-5-panoche-and-tumey-hills/littlepanoche/\" rel=\"attachment wp-att-32498\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/littlepanoche.jpg\" alt=\"\" title=\"littlepanoche\" width=\"600\" height=\"400\" class=\"size-full wp-image-32498\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/littlepanoche.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/littlepanoche-400x267.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Looking across Little Panoche Creek to the north flank of the Panoche Hills.\u003c/figcaption>\u003c/figure>\n\u003cp>The road turns south and runs through Little Panoche Valley, passing the low-key \u003ca href=\"https://merceyhotsprings.com/\">Mercey Hot Springs\u003c/a> resort. The entrance to the BLM's \u003ca href=\"http://www.blm.gov/ca/st/en/fo/hollister/recreation/panoche.html\">Panoche Hills Recreation Area\u003c/a> is here, too. At the head of the valley the road cuts through Glaucophane Ridge, an unexpected exposure of old Franciscan rocks, then goes straight south across the wide and gentle Panoche Valley and ends at Panoche Road. This pocket of farmland is one of Central California's hidden gems. The south side of the valley presents a striking set of terraces. These are mapped as river terraces but might be lake beds; I haven't looked into the literature. In either case they, too, attest to ancient episodes of accelerated erosion.\u003c/p>\n\u003cfigure id=\"attachment_32503\" class=\"wp-caption aligncenter\" style=\"max-width: 600px\">\u003ca href=\"http://ww2.kqed.org/quest/2012/03/08/side-trips-from-interstate-5-panoche-and-tumey-hills/panocheterraces/\" rel=\"attachment wp-att-32503\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/panocheterraces.jpg\" alt=\"\" title=\"panocheterraces\" width=\"600\" height=\"387\" class=\"size-full wp-image-32503\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/panocheterraces.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/panocheterraces-400x258.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Buck Peak, in the Griswold Hills, and river terraces of the Panoche Valley.\u003c/figcaption>\u003c/figure>\n\u003cp>Panoche Road west eventually gets you to Paicines, south of Hollister. The road east gets you back to I-5, but all of the crooked part is decent dirt. In wet weather, turn back here, or maybe go a little ways on the paved part and daydream about taking New Idria Road south to the remote ghost town of Idria. The eastern end of the valley has good views of the Panoche Hills from the south, but eventually the road crosses the creek without benefit of a bridge and then turns to dirt.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/03/08/side-trips-from-interstate-5-panoche-and-tumey-hills/panoches/\" rel=\"attachment wp-att-32502\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/panoches.jpg\" alt=\"\" title=\"panoches\" width=\"600\" height=\"438\" class=\"aligncenter size-full wp-image-32502\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/panoches.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/panoches-400x292.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>In fine weather, ford the stream and proceed across some splendid and scenic country.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/03/08/side-trips-from-interstate-5-panoche-and-tumey-hills/panocheroad/\" rel=\"attachment wp-att-32501\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/panocheroad.jpg\" alt=\"\" title=\"panocheroad\" width=\"600\" height=\"414\" class=\"aligncenter size-full wp-image-32501\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/panocheroad.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/panocheroad-400x276.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>At this point, you are in the \u003ca href=\"http://www.blm.gov/ca/st/en/fo/hollister/recreation/tumey.html\">Tumey Hills Recreation Area\u003c/a>. These hills are lower and drier than the Panoches, and the rocks along the road are quite different. They are young sandstones and conglomerates formed as the Coast Range began to rise, just a few million years ago.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/03/08/side-trips-from-interstate-5-panoche-and-tumey-hills/tumeycgl/\" rel=\"attachment wp-att-32504\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/tumeycgl.jpg\" alt=\"\" title=\"tumeycgl\" width=\"500\" height=\"401\" class=\"aligncenter size-full wp-image-32504\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/tumeycgl.jpg 500w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/tumeycgl-400x321.jpg 400w\" sizes=\"(max-width: 500px) 100vw, 500px\">\u003c/a>\u003c/p>\n\u003cp>Watch the road as well as the rocks, but don't miss the landscape. All photos in this post were taken in late March.\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/03/08/side-trips-from-interstate-5-panoche-and-tumey-hills/tumeys/\" rel=\"attachment wp-att-32506\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/tumeys.jpg\" alt=\"\" title=\"tumeys\" width=\"600\" height=\"473\" class=\"aligncenter size-full wp-image-32506\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/tumeys.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/tumeys-400x315.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\u003cp>When you reach I-5, you'll have a choice of eating places to get you ready to roll again. Maybe, like me, you prefer to think of it as the place where the iron dinosaur used to be. It was the creation of the late Carmon Neff of Chowchilla, and I don't know where it went.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>\u003ca href=\"http://ww2.kqed.org/quest/2012/03/08/side-trips-from-interstate-5-panoche-and-tumey-hills/tumeydino/\" rel=\"attachment wp-att-32505\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2012/03/tumeydino.jpg\" alt=\"\" title=\"tumeydino\" width=\"600\" height=\"401\" class=\"aligncenter size-full wp-image-32505\" srcset=\"https://ww2.kqed.org/app/uploads/sites/39/2012/03/tumeydino.jpg 600w, https://ww2.kqed.org/app/uploads/sites/39/2012/03/tumeydino-400x267.jpg 400w\" sizes=\"(max-width: 600px) 100vw, 600px\">\u003c/a>\u003c/p>\n\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/quest/32484/side-trips-from-interstate-5-panoche-and-tumey-hills","authors":["6228"],"categories":["quest_11"],"tags":["quest_533","quest_639","quest_3403","quest_10760","quest_2118","quest_13202"],"featImg":"quest_32499","label":"quest"},"quest_614":{"type":"posts","id":"quest_614","meta":{"index":"posts_1591205157","site":"quest","id":"614","score":null,"sort":[1211590791000]},"guestAuthors":[],"slug":"discuss-the-californias-fire-future-radio-report","title":"Discuss the "California's Fire Future" Radio Report","publishDate":1211590791,"format":"audio","headTitle":"QUEST | KQED Science","labelTerm":{"site":"quest"},"content":"\u003cp>\u003cspan class=\"left\">\u003ca href=\"http://ww2.kqed.org/quest/audio/view/953\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2008/05/radio2-33_sc_fire300.jpg\">\u003c/a>\u003c/span>Scientists predict we’ll be seeing hotter conditions and drier forests in the near future. The Summit Fire that's been burning in the Santa Cruz Mountains is likely a part of that trend. QUEST talks to Malcolm North with the U.S. Forest Service. He says any area that's burned before is vulnerable to burning again, including the Coast Range and Sierra Nevada.\u003c/p>\n\u003cp>\u003cbr clear=\"all\">\u003cbr>\n\u003cspan class=\"left\">\u003ca href=\"http://ww2.kqed.org/quest/audio/view/953\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/images/radio_icon_light.gif\">\u003c/a>\u003c/span>You may \u003ca href=\"http://ww2.kqed.org/quest/audio/view/953\">listen to the \"California's Fire Future\" Radio report\u003c/a> online, as well as find additional links and resources.\u003cbr>\n\u003cbr clear=\"all\">\u003c/p>\n\u003cp> 37.06076 -121.802802\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\u003cp>\u003c/p>\n","blocks":[],"excerpt":null,"status":"publish","parent":0,"modified":1371080000,"stats":{"hasAudio":false,"hasVideo":false,"hasChartOrMap":false,"iframeSrcs":[],"hasGoogleForm":false,"hasGallery":false,"hasHearkenModule":false,"hasPolis":false,"paragraphCount":5,"wordCount":92},"headData":{"title":"Discuss the "California's Fire Future" Radio Report | KQED","description":"Scientists predict we’ll be seeing hotter conditions and drier forests in the near future. The Summit Fire that's been burning in the Santa Cruz Mountains is likely a part of that trend. QUEST talks to Malcolm North with the U.S. Forest Service. He says any area that's burned before is vulnerable to burning again, including","ogTitle":"","ogDescription":"","ogImgId":"","twTitle":"","twDescription":"","twImgId":"","schema":{"@context":"http://schema.org","@type":"Article","headline":"Discuss the "California's Fire Future" Radio Report","datePublished":"2008-05-24T00:59:51.000Z","dateModified":"2013-06-12T23:33:20.000Z","image":"https://cdn.kqed.org/wp-content/uploads/2020/02/KQED-OG-Image@1x.png"}},"disqusIdentifier":"614 http://www.kqed.org/quest/blog/2008/05/23/discuss-the-californias-fire-future-radio-report/","disqusUrl":"https://ww2.kqed.org/quest/2008/05/23/discuss-the-californias-fire-future-radio-report/","disqusTitle":"Discuss the "California's Fire Future" Radio Report","path":"/quest/614/discuss-the-californias-fire-future-radio-report","audioTrackLength":null,"parsedContent":[{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003cp>\u003cspan class=\"left\">\u003ca href=\"http://ww2.kqed.org/quest/audio/view/953\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/2008/05/radio2-33_sc_fire300.jpg\">\u003c/a>\u003c/span>Scientists predict we’ll be seeing hotter conditions and drier forests in the near future. The Summit Fire that's been burning in the Santa Cruz Mountains is likely a part of that trend. QUEST talks to Malcolm North with the U.S. Forest Service. He says any area that's burned before is vulnerable to burning again, including the Coast Range and Sierra Nevada.\u003c/p>\n\u003cp>\u003cbr clear=\"all\">\u003cbr>\n\u003cspan class=\"left\">\u003ca href=\"http://ww2.kqed.org/quest/audio/view/953\">\u003cimg src=\"http://ww2.kqed.org/quest/wp-content/uploads/sites/39/images/radio_icon_light.gif\">\u003c/a>\u003c/span>You may \u003ca href=\"http://ww2.kqed.org/quest/audio/view/953\">listen to the \"California's Fire Future\" Radio report\u003c/a> online, as well as find additional links and resources.\u003cbr>\n\u003cbr clear=\"all\">\u003c/p>\n\u003cp> 37.06076 -121.802802\u003c/p>\n\u003cp>\u003c/p>\u003c/div>","attributes":{"named":{},"numeric":[]}},{"type":"component","content":"","name":"ad","attributes":{"named":{"label":"fullwidth"},"numeric":["fullwidth"]}},{"type":"contentString","content":"\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\u003cp>\u003c/p>\n\u003c/div>\u003c/p>","attributes":{"named":{},"numeric":[]}}],"link":"/quest/614/discuss-the-californias-fire-future-radio-report","authors":["210"],"categories":["quest_6","quest_9"],"tags":["quest_252","quest_639","quest_1095","quest_1130","quest_3351","quest_2141","quest_2349","quest_13206","quest_2507","quest_2826","quest_2993","quest_19"],"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/2024/04/Possible-Podcast-Tile-360x360-1.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/2024/04/All-Things-Considered-Podcast-Tile-360x360-1.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://cdn.kqed.org/wp-content/uploads/2024/04/American-Suburb-Podcast-Tile-703x703-1.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. And you join us on the journey to find the answers.","imageSrc":"https://cdn.kqed.org/wp-content/uploads/2024/04/Bay-Curious-Podcast-Tile-703x703-1.jpg","imageAlt":"\"KQED Bay Curious","officialWebsiteLink":"/news/series/baycurious","meta":{"site":"news","source":"kqed","order":"4"},"link":"/podcasts/baycurious","subscribe":{"apple":"https://podcasts.apple.com/us/podcast/bay-curious/id1172473406","npr":"https://www.npr.org/podcasts/500557090/bay-curious","rss":"https://ww2.kqed.org/news/category/bay-curious-podcast/feed/podcast","google":"https://podcasts.google.com/feed/aHR0cHM6Ly93dzIua3FlZC5vcmcvbmV3cy9jYXRlZ29yeS9iYXktY3VyaW91cy1wb2RjYXN0L2ZlZWQvcG9kY2FzdA","stitcher":"https://www.stitcher.com/podcast/kqed/bay-curious","spotify":"https://open.spotify.com/show/6O76IdmhixfijmhTZLIJ8k"}},"bbc-world-service":{"id":"bbc-world-service","title":"BBC World Service","info":"The day's top stories from BBC News compiled twice daily in the week, once at weekends.","airtime":"MON-FRI 9pm-10pm, TUE-FRI 1am-2am","imageSrc":"https://cdn.kqed.org/wp-content/uploads/2024/04/BBC-World-Service-Podcast-Tile-360x360-1.jpg","officialWebsiteLink":"https://www.bbc.co.uk/sounds/play/live:bbc_world_service","meta":{"site":"news","source":"BBC World Service"},"link":"/radio/program/bbc-world-service","subscribe":{"apple":"https://itunes.apple.com/us/podcast/global-news-podcast/id135067274?mt=2","tuneIn":"https://tunein.com/radio/BBC-World-Service-p455581/","rss":"https://podcasts.files.bbci.co.uk/p02nq0gn.rss"}},"code-switch-life-kit":{"id":"code-switch-life-kit","title":"Code Switch / Life Kit","info":"\u003cem>Code Switch\u003c/em>, which listeners will hear in the first part of the hour, has fearless and much-needed conversations about race. Hosted by journalists of color, the show tackles the subject of race head-on, exploring how it impacts every part of society — from politics and pop culture to history, sports and more.\u003cbr />\u003cbr />\u003cem>Life Kit\u003c/em>, which will be in the second part of the hour, guides you through spaces and feelings no one prepares you for — from finances to mental health, from workplace microaggressions to imposter syndrome, from relationships to parenting. The show features experts with real world experience and shares their knowledge. 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