Ground-Water Hydrology and Projected Effects of Ground-Water Withdrawals in the Sevier Desert, Utah

Authors

United States Geological Survey

Document Type

Report

Publication Date

1983

Abstract

The principal ground-water reservoir in the Sevier Desert is the unconsolidated basin fill. The fill has been divided generally into aquifers and confining beds, although there are no clearcut boundaries between these units--the primary aquifers are the shallow and deep artesian aquifers. Recharge to the ground-water reservoir is by infiltration of precipitation; seepage from streams, canals, reservoirs, and unconsumed irrigation water; and subsurface inflow from consolidated rocks in mountain areas and from adjoining areas. discharge is by wells, springs, seepage to the Sevier River, evapotranspiration, and subsurface outflow to adjoining areas.

Comments

Open-File Report 83-688.

Recommended Citation

United States Geological Survey, "Ground-Water Hydrology and Projected Effects of Ground-Water Withdrawals in the Sevier Desert, Utah" (1983). All U.S. Government Documents (Utah Regional Depository). Paper 151.
https://digitalcommons.usu.edu/govdocs/151