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- Q12304454 subject Q13302884.
- Q12304454 subject Q8179679.
- Q12304454 subject Q8432369.
- Q12304454 subject Q8524587.
- Q12304454 subject Q8581905.
- Q12304454 subject Q8635025.
- Q12304454 subject Q8826172.
- Q12304454 subject Q8906587.
- Q12304454 subject Q8956795.
- Q12304454 abstract "The Bruneau-Jarbidge caldera (sometimes called a supervolcano) is located in present-day southwest Idaho. The volcano erupted during the Miocene, between ten and twelve million years ago, spreading a thick blanket of ash in the Bruneau-Jarbidge event and forming a caldera. Animals were suffocated and burned in pyroclastic flows within a hundred miles of the event, and died of slow suffocation and starvation much farther away, notably at Ashfall Fossil Beds, located 1000 miles downwind in northeastern Nebraska, where up to two meters of ash was deposited. At the time, the caldera was above the Yellowstone hotspot.The existence of the event was discovered in 1971 by Prof. Mike Voorhies, a paleontologist at the University of Nebraska State Museum. The prehistoric skeletons of camels, lizards, horses, turtles and two hundred fossilized rhinoceros were found in two metres of volcanic ash at a lagerstätte near Royal, Nebraska, the Ashfall Fossil Beds.By its uniquely characteristic chemical "fingerprint" and the distinctive size and shape of its crystals and glass shards, the volcano stood out among dozens of prominent ashfall horizons laid down in the Cretaceous, Paleogene, and Neogene periods of central North America. The event responsible for this fall of volcanic ash was identified at Bruneau-Jarbidge, 1600 kilometers west in Idaho. Prevailing westerlies deposited distal ashfall over a vast area of the Great Plains.The evolving composition of the erupted material indicates that while it is derived in large part from melted material from the middle or upper crust, it also incorporated a young basaltic component.".
- Q12304454 thumbnail HotspotsSRP_update2013.JPG?width=300.
- Q12304454 wikiPageExternalLink supervolcanoes_script.shtml.
- Q12304454 wikiPageExternalLink Nebraska.pdf.
- Q12304454 wikiPageWikiLink Q103924.
- Q12304454 wikiPageWikiLink Q1048423.
- Q12304454 wikiPageWikiLink Q11573.
- Q12304454 wikiPageWikiLink Q1221.
- Q12304454 wikiPageWikiLink Q12707.
- Q12304454 wikiPageWikiLink Q13302884.
- Q12304454 wikiPageWikiLink Q1553.
- Q12304454 wikiPageWikiLink Q159954.
- Q12304454 wikiPageWikiLink Q2122699.
- Q12304454 wikiPageWikiLink Q2195799.
- Q12304454 wikiPageWikiLink Q221616.
- Q12304454 wikiPageWikiLink Q332614.
- Q12304454 wikiPageWikiLink Q34718.
- Q12304454 wikiPageWikiLink Q4121358.
- Q12304454 wikiPageWikiLink Q44626.
- Q12304454 wikiPageWikiLink Q4804942.
- Q12304454 wikiPageWikiLink Q49.
- Q12304454 wikiPageWikiLink Q55810.
- Q12304454 wikiPageWikiLink Q76267.
- Q12304454 wikiPageWikiLink Q8052001.
- Q12304454 wikiPageWikiLink Q8072.
- Q12304454 wikiPageWikiLink Q8179679.
- Q12304454 wikiPageWikiLink Q8432369.
- Q12304454 wikiPageWikiLink Q8524587.
- Q12304454 wikiPageWikiLink Q8581905.
- Q12304454 wikiPageWikiLink Q8635025.
- Q12304454 wikiPageWikiLink Q8826172.
- Q12304454 wikiPageWikiLink Q8906587.
- Q12304454 wikiPageWikiLink Q8956795.
- Q12304454 point "42.3 -115.2".
- Q12304454 type SpatialThing.
- Q12304454 comment "The Bruneau-Jarbidge caldera (sometimes called a supervolcano) is located in present-day southwest Idaho. The volcano erupted during the Miocene, between ten and twelve million years ago, spreading a thick blanket of ash in the Bruneau-Jarbidge event and forming a caldera.".
- Q12304454 label "Bruneau-Jarbidge caldera".
- Q12304454 lat "42.3".
- Q12304454 long "-115.2".
- Q12304454 depiction HotspotsSRP_update2013.JPG.