1970
DOI: 10.3133/wsp1879c
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Ground-water aspects of the lower Henrys Fork region, eastern Idaho

Abstract: The lower Henrys Fork region in eastern Idaho includes the plains and low benches between Ashton and the junction of Henrys Fork and Snake River. The northwestern and western parts of the area are part of the Snake River basalt plain. The central part of the area is occupied by alluvial plains of the Snake, Teton, and Falls Rivers and of Henrys Fork. The alluvial deposits are underlain by basalt. The southeastern part of the area is a bench (Rexburg Bench), chiefly on silicic and ibasaltic volcanic rocks, whic… Show more

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