Geology Reports⌕ Search

Geology topics

Research about Nevada, Utah

Source-linked reports with geographic coverage including Nevada, Utah.

60 records · Page 4Linked to original sources

Hydrologic reconnaissance of Deep Creek valley, Tooele and Juab Counties, Utah and Elko and White Pine Counties, Nevada

This report, the fourth in a series by the U. S. Geological Survey in cooperation with the Utah Department of Natural Resources, Division of Water Rights, describes water resources of the western basins of Utah. Its purpose is to present available hydrologic data on Deep Creek valley, to provide an evaluation of the potential water-resource development of the valley, and to identify needed studies that would help provide an understanding of the valley's water supply.

Nevada, Utah↗

Preliminary geologic section from Pahute Mesa, Nevada Test Site, to Enterprise, Utah

The 154-mile long geologic cross section trends nearly perpendicular to the structural grain of the Basin-Range province in Nevada, and in Utah extends eastward into the transition zone between the Basin-Range and Colorado Plateau provinces. The structure is characterized by complex thrust: faults, involving uppermost Precambrian to lower Mesozoic sedimentary rocks, and normal faults which cut: the thick sequence of Tertiary volcanic rocks as well as older rocks. Some of the normal faults are the result of caldera collapse. The principal normal faults trend northerly west: of Delamar, Nev., and form north-trending basins and ranges. Farther east the principal faults trend northwesterly, and form a moderately rugged highland rather than distinct basins and ranges. The uppermost Precambrian-Paleozoic strata thin markedly eastward across the region. The pre-Pennsylvanian sedimentary rocks vary from 32,500 feet: in thickness at the Nevada Test: Site (Harley Barnes, E. N. Hinrichs, F. A. McKeown and P. P. Orkild, written commun., 1963) to 4,500 feet: in the Beaver Dam Mountains in western Utah (Cook, 1960). Thick Mesozoic deposits, similar to those of the Colorado Plateau, are present in western Utah, but are represented in eastern Nevada by only thin patches of Triassic rock.

Nevada, Utah↗

Water-resources appraisal of the Snake Valley area, Utah and Nevada

The Snake Valley area is a north-trending narrow depression that extends about 135 miles along the central Nevada-Utah border. The area covers about 3,480 square miles. Within the area, the principal ground-water reservoir is in the unconsolidated deposits of Quaternary and Tertiary age that underlie about 1.2 million acres. Carbonate rocks of Paleozoic age may form another reservoir system and locally may control the movement of groundwater.

Nevada, Utah↗

Lower Permian stratigraphy of east-central Nevada and adjacent Utah

The Permian section near Ely, Nevada, consists of, in ascending order: Riepe Spring Limestone, a bluff-forming limestone with abundant corals, and Reipetown Sandstone, a buff to red very coarse-grained siltstone with minor carbonates, both formations of Steele (1960); Arcturus Formation, divisible into a Lower Member composed of alternating medium-bedded limestone and buff siltstone, and an Upper Member composed of alternating thin-bedded limestone and buff to red siltstone and gypsum; and Kaibab Limestone, a massive bioclastic limestone. The Wolfcamp-Leonard boundary occurs within the Arcturus Formation. West of Ely the Riepe Spring Limestone and Reipetown Sandstone thin and change into thin-bedded cherty limestone. These beds, plus the basal part of the Arcturus Formation, form the Carbon Ridge Formation at Dry Mountain at Eureka. At Dry Mountain, minor clastic chert occurs in the Arcturus Formation, and beyond to the west clastic chert replaces most of the limestone to form the conglomeratic Garden Valley Formation. The cherty limestone at the base of the Garden Valley is apparently equivalent to the upper part of the Carbon Ridge Formation at Carbon Ridge. Eastward in Utah the Riepe Spring Limestone is recognizable in the Confusion Range, but is almost unrecognizable in the Needle Range. The dolomite content in the Reipetown Sandstone usually increases to 25 percent of the formation in the Confusion and Needle ranges. The Arcturus Formation thins and undergoes moderate lithologic changes. It is equivalent to the rocks above a horizon 300 feet below Bed A of the Arcturus Formation as mapped in the Confusion Range by Hose and Repenning (1959, 1963).

Nevada, Utah↗

Floods of April-June 1952 in Utah and Nevada

The floods of April-June 1952 in the Great Basin and in the Green River basin in Utah came as the result of the heaviest snow cover recorded, a long period of near-record subnormal temperature during March and early April, and an abrupt change to above-normal temperature that induced rapid melting.Rainfall played an insignificant part. Low- and intermediate-elevation snow melted, bringing many streams to record-high level. Large diurnal fluctuations of discharge were evident on smaller streams. The temperature remained high until mid-May. As high-elevation snow became primed for runoff, the temperature dropped enough to refreeze and alter the structure of snow cover, thus reducing the effectiveness of the subsequent melting temperature. Had there been no respite from melting temperatures much greater peak discharges would have occurred, with damage greatly exceeding that experienced. Streams remained at high levels for several weeks. Record peaks were reached on Strawberry River, lower Weber River, Ogden River, Spanish Fork, lower Provo River, and Jordan River in Utah; Humboldt River and its tributaries draining the north area of the basin in Nevada; and the central Bear River in Idaho and Wyoming. Record volumes for the water year were measured on many streams in the northcentral part of Utah, the northeastern part of Nevada, and the central part of the Bear River basin in Idaho and Wyoming. Damage in the Great Basin reached \$10 million and in the Green River basin, more than$300,000. Two lives were lost on Ogden River. The greatest urban damage, in Salt Lake City, totaled \$1.9 million; the greatest single damage, to Denver and Rio Grande Western Railroad, was \$510,000.

Nevada, Utah↗