publication . Other literature type . 1983

Ground-water hydrology and projected effects of ground-water withdrawals in the Sevier Desert, Utah

Walter F. Holmes;
Open Access
  • Published: 01 Jan 1983 Journal: Open-File Report (issn: 2331-1258, Copyright policy)
  • Publisher: US Geological Survey
  • Country: United States
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.
Persistent Identifiers
free text keywords: open file report 83-688, ground water, ground-water, ground-water hydrology, projected effects of ground-water, projected effects of ground-water withdrawals, Sevier Desert, Utah, Geology, Hydrology, Groundwater, Environmental science
Related Organizations
Any information missing or wrong?Report an Issue