Neogene Normal Faults Related to the Structural Origin of the Eastern Snake River Plain, Idaho

Zenter N. 1989. Neogene Normal Faults Related to the Structural Origin of the Eastern Snake River Plain, Idaho. M.S. Thesis. Idaho State University, Pocatello

Origins of the Eastern Snake River Plain discussed. Surficial basalt believed to cover much thicker rhyolitic deposits. Geographic location: Covers the Snake River Plain area from Twin Falls to Yellowstone.

Type
Academic
Authors
Zenter, N
Date of Issue
1989
Publisher
M.S. Thesis. Idaho State University, Pocatello
Units
CRMO
Keywords
Calderas, Faults (Geologic), Neogene, Physical Sciences, Rhyolites, Snake River Plain, Thesis

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