Studies of geology and hydrology in the Basin and Range Province, Southwestern United States, for isolation of high-level radioactive waste - Characterization of the Bonneville region, Utah and Nevada
Links
- More information: National Geologic Map Database Index Page (html)
- Document: Report (pdf)
- Plates:
- Plate 1 (pdf) Map showing physiographic features of the Bonneville Region, Utah and Nevada
- Plate 2 (pdf) Map showing potential host rocks and areas of thick unsaturated zones, Bonneville Region, Utah and Nevada
- Plate 3 (pdf) Map showing hypothetical altitude of the regional potentiometric surface in the carbonate-rock aquifer and contiguous rocks at depth, Bonneville Region and vicinity, Utah and Nevada
- Plate 4 (pdf) Map showing hydrogeologic units and relative velocities of ground water at the water table, Bonneville Region, Utah and Nevada
- Plate 5 (pdf) Map showing relative ground-water traveltimes and flow paths at the water table and natural discharge areas, Bonneville Region, Utah and Nevada
- Plate 6 (pdf) Hydrogeologic section A-A' showing ground-water flow paths and relative traveltimes, Bonneville Region, Utah and Nevada
- Plate 7 (pdf) Map showing general locations of the principal mining districts, Bonneville Region, Utah and Nevada
- Superseded Publications:
- Download citation as: RIS | Dublin Core
Abstract
The Bonneville region of the Basin and Range province in westcentral Utah and adjacent Nevada includes several basins lying south of the Great Salt Lake Desert. Physiographically, the region consists of linear, north-trending mountain ranges separated by valleys, many of which are closed basins underlain by thick sequences of fill. Surface drainage of open basins and ground-water flow is to the Great Salt Lake Desert. In structure and composition the ranges are faulted Paleozoic rocks, locally intruded by Mesozoic and Tertiary plugs and stocks. In the southern and northeastern parts of the region, volcanic rocks are widespread and form large parts of some mountain ranges. The Paleozoic sedimentary rocks include great thicknesses of carbonate rocks which compose a significant aquifer in the region
Media considered to have potential for isolation of high-level radioactive waste in the region include intrusive rocks, such as granite; ash-flow tuff; and basalt and basaltic andesite lava flows. These rock types, basin fill, and possibly other rock types, may have potential as host media in the unsaturated zone. Quaternary tectonism in the region is evidenced by seismic activity, local areas of above-normal geothermal heat flow, Quaternary faulting, late Cenozoic volcanic activity, and active vertical crustal movement.
The Bonneville region is part of a large ground-water flow system that is integrated partly through basin-fill deposits, but largely through an underlying carbonate-rock sequence. The region includes: (1) several topographically closed basins with virtually no local surface discharge that are drained by the underlying carbonate-rock aquifer; (2) closed basins with local surface discharge by evapotranspiration; and (3) basins open to the Great Salt Lake Desert that discharge by groundwater underflow and evapotranspiration. The carbonate-rock aquifer discharges to large springs in the Desert and in basins tributary to the Desert. The climate is arid to semiarid with the greatest precipitation in the mountain ranges. Most recharge probably occurs by infiltration of runoff as it leaves the mountains, although some recharge probably occurs directly to the carbonate rocks in the mountain areas. The concentration of dissolved solids in ground water is generally less than 500 milligrams per liter. Dissolved-solids concentrations increase in the Great Salt Lake Desert and in major valleys adjoining the Desert. The predominant chemical constituents in ground water are calcium, magnesium, and sodium bicarbonate. Chloride-type water is associated with the higher dissolved-solids content of water in and near the Great Salt Lake Desert.
The majority of the mineral occurrences containing base- and precious-metal deposits in the Bonneville region are of Tertiary age. Fluorspar is the primary industrial mineral. Coal, oil, and gas have not been produced in significant amounts.
| Publication type | Report |
|---|---|
| Publication Subtype | USGS Numbered Series |
| Title | Studies of geology and hydrology in the Basin and Range Province, Southwestern United States, for isolation of high-level radioactive waste - Characterization of the Bonneville region, Utah and Nevada |
| Series title | Professional Paper |
| Series number | 1370 |
| Chapter | G |
| DOI | 10.3133/pp1370G |
| Year Published | 1990 |
| Language | English |
| Publisher | U.S. Government Printing Office |
| Publisher location | Washington, D.C. |
| Contributing office(s) | Utah Water Science Center |
| Description | Report: viii, 38 p; 7 Plates: 31.00 in. x 35.00 in. or smaller |
| First page | G1 |
| Last page | G38 |
| Country | United States |
| State | Nevada, Utah |
| Other Geospatial | Bonneville Region |
| Google Analytic Metrics | Metrics page |