Tension cracks, eruptive fissures, dikes, and faults related to late Pleistocene-Holocene basaltic volcanism and implications for the distribution of hydraulic conductivity in the eastern Snake River Plain, Idaho

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

doi:10.1130/0-8137-2353-1.111

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Tension cracks, eruptive fissures, dikes, and faults related to late Pleistocene-Holocene basaltic volcanism and implications for the distribution of hydraulic conductivity in the eastern Snake River Plain, Idaho

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

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Source-reported bounding extent: 41.95905970222364° to 44.749396677289525° latitude; -113.98207247747594° to -111.09972778490244° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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Mel A. Kuntz, Steven R. Anderson, Duane E. Champion, Marvin A. Lanphere, Daniel J. Grunwald. 2002. Tension cracks, eruptive fissures, dikes, and faults related to late Pleistocene-Holocene basaltic volcanism and implications for the distribution of hydraulic conductivity in the eastern Snake River Plain, Idaho. https://doi.org/10.1130/0-8137-2353-1.111

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