Accumulation and subsidence of the Pleistocene basaltic lava flows of the eastern Snake River Plain, Idaho

Duane E. Champion; Marvin A. Lanphere; Steven R. Anderson; Mel A. Kuntz

doi:10.1130/0-8137-2353-1.175

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Accumulation and subsidence of the Pleistocene basaltic lava flows of the eastern Snake River Plain, Idaho

Duane E. Champion·Marvin A. Lanphere·Steven R. Anderson·Mel A. Kuntz

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Source-reported bounding extent: 42.26622860486236° to 44.61483553858173° latitude; -114.7260970770847° to -111.15270455443617° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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Duane E. Champion, Marvin A. Lanphere, Steven R. Anderson, Mel A. Kuntz. 2002. Accumulation and subsidence of the Pleistocene basaltic lava flows of the eastern Snake River Plain, Idaho. https://doi.org/10.1130/0-8137-2353-1.175

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