Open Access. Powered by Scholars. Published by Universities.®

Digital Commons Network™

Open Access. Powered by Scholars. Published by Universities.®

Utah State University

Discipline
Keyword
Publication Year
Publication
Publication Type
File Type

Articles 10771 - 10800 of 13050

Full-Text Articles in Entire DC Network

Geologic Map And Coal Sections Of The Red Point Quadrangle, Emery County, Utah, United States Geological Survey Jan 1981

Geologic Map And Coal Sections Of The Red Point Quadrangle, Emery County, Utah, United States Geological Survey

All U.S. Government Documents (Utah Regional Depository)

Red Point quadrangle, in Emery County in central Utah, was mapped in 1979 as part of the U.S. Geological Survey's program to evaluate land in the public domain for potential coal leasing.


Geologic Map And Coal Sections Of The Cap Quadrangle, Emery County, Utah, United States Geological Survey Jan 1981

Geologic Map And Coal Sections Of The Cap Quadrangle, Emery County, Utah, United States Geological Survey

All U.S. Government Documents (Utah Regional Depository)

The Cap quadrangle, in Emery County in central Utah, was mapped in 1977-79 as part of the U.S. Geological Survey's program to evaluate lands in the public domain for potential coal leasing.


Geological Map And Coal Sections Of The Mahogany Point Quadrangle, Emery County, Utah, United States Geological Survey Jan 1981

Geological Map And Coal Sections Of The Mahogany Point Quadrangle, Emery County, Utah, United States Geological Survey

All U.S. Government Documents (Utah Regional Depository)

The Mahogany Point quadrangle, in Emery County in central Utah, was mapped in 1978-79 as part of the U.S. Geological Survey's program to evaluate land in the public domain for potential coal leasing. Mapping was done using U.S. Forest Service color aerial photographs at a scale of 1:15, 840 on U.S. Geological Survey topographic maps at a scale of 1:24,000. The quadrangle was mapped previously by Spieker (1931) at a scale fo 1:62,500.


Newly Identified Intertonguing Between The Star Point Sandstone And The Blackhawk Formation And The Correlation Of Coal Beds In The Northern Part Of The Wasatch Plateau, United States Geological Survey Jan 1981

Newly Identified Intertonguing Between The Star Point Sandstone And The Blackhawk Formation And The Correlation Of Coal Beds In The Northern Part Of The Wasatch Plateau, United States Geological Survey

All U.S. Government Documents (Utah Regional Depository)

On the basis of fieldwork and drilling completed in the Fall of 1980, several zones of intertonguing between the Star Point Sandstone and the overlying Blackhawk Formation have been identified in the northern part of the Wasatch Plateau, Carbon County, Utah (sheet 1). As a result of this work, correlations of important coal beds have been revised. The U.S. Geological Survey drilled a total of 12 holes in the area, from the west side of Pleasant Valley, near Slaughterhouse Canyon, to the eastern part of the Beaver Creek drainage (sheet 1) (Blanchard and others, 1976; U.S. Geological Survey, 1980). In …


Seepage Study Of The Sevier River And The Central Utah, Mcintyre, And Leamington Canals, Juab And Millard Counties, Utah, United States Geological Survey Jan 1981

Seepage Study Of The Sevier River And The Central Utah, Mcintyre, And Leamington Canals, Juab And Millard Counties, Utah, United States Geological Survey

All U.S. Government Documents (Utah Regional Depository)

A study of the gains or losses of the Sevier River and the Central Utah, McIntyre, and Leamington Canals in the Leamington area, in Juab and Millard Counties, Utah, was made to determine changes in those reaches. Three to seven sets of seepage measurements made during 1980 were used in the analysis. Adjustments for fluctuations in flow were made from information obtained from water-stage recorders operated at selected locations during the time of each seepage run.


Water-Resources Studies In Utah July 1, 1980 To June 30, 1981, United States Geological Survey Jan 1981

Water-Resources Studies In Utah July 1, 1980 To June 30, 1981, United States Geological Survey

All U.S. Government Documents (Utah Regional Depository)

This report summarizes the progress on water-resources studies in Utah by the U.S. Geological Survey during the period July 1, 1980, to June 30, 1981. Much of the work was done in cooperation with the State of Utah or local agencies. Additional supporting funds were transferred from other Federal agencies or appropriated directly to the Geological Survey.


Summary Utah/Western Colo, 1992 System Study, United States Department Of Energy Western Area Power Administration Jan 1981

Summary Utah/Western Colo, 1992 System Study, United States Department Of Energy Western Area Power Administration

All U.S. Government Documents (Utah Regional Depository)

The Utah/western Colorado area of the Rocky Mountain Region has adequate coal and water resources to support additional thermal generation plants beyond those already in service. Also within the region are several sites suitable for large-sized hydroelectric pumped-storage projects for purposes of supplying peaking power. The close proximity of these types of electric generating facilities is desirable in providing offpeak energy during the pumping cycle for the pumped-storage units. Considering that the potential capacity of each type of generation is in the 500 to 1,000 (two units) MW range per site and would require major extra-high-voltage (EHV) transmission developments, it …


Wild Ungulate Forage Requirements -- A Review, United States Bureau Of Land Management Jan 1981

Wild Ungulate Forage Requirements -- A Review, United States Bureau Of Land Management

All U.S. Government Documents (Utah Regional Depository)

This report discusses the nutritional and intake requirements of the major big game ungulates of North America. Forage intake rates for the various species are detailed, and major factors governing intake rates are discussed. The importance of forage nutritional value as much as quantity is emphasized, and both biotic and abiotic factors influencing forage quality are presented. Methods of forage protection and improvement are briefly defined.


A Feasibility Study Of The Biological Effects Of Fallout On People In Utah, Nevada, And Arizona, United States Department Of Health And Human Services, Bureau Of Radiological Health Jan 1981

A Feasibility Study Of The Biological Effects Of Fallout On People In Utah, Nevada, And Arizona, United States Department Of Health And Human Services, Bureau Of Radiological Health

All U.S. Government Documents (Utah Regional Depository)

This is the final report of the analysis of the Utah, Nevada, and Arizona Thyroid Feasibility Study. The report is divided into four sections: (1) Introduction and background; (2) Analysis of Linkage Study with the Utah Cancer Registry and Rocky Mountain Cancer Data System; (3) Evaluation of Tracing a Sample of the Original Utah, Nevada, and Arizona Study Groups; and (4) Options for Future Studies.


Application Of Mineral-Solution Equilibria To The Search For Sanstone-Type Uranium Deposits In The Beaver Basin, Utah, W. R. Miller, J. B. Mchugh, U.S. Geological Survey Jan 1981

Application Of Mineral-Solution Equilibria To The Search For Sanstone-Type Uranium Deposits In The Beaver Basin, Utah, W. R. Miller, J. B. Mchugh, U.S. Geological Survey

All U.S. Government Documents (Utah Regional Depository)

An improved computer modeling program was used to calculate the saturation indexes of 50 waters from the Beaver basin in west-central Utah with respect to uraninite and coffinite. The mineral-solution study showed that the chemical environment of parts of the Beaver basin is favorable for the occurrence of sandstone-type uranium deposits. The ground waters from several areas are supersaturated with respect to uraninite and coffinite. Two areas, in particular, an area west of the town of Beaver and an area near the settlement of Manderfield, have been identified as most favorable for exploration. The methods described in this study can …


Geologic Map Of The Steamboat Mountain And Bible Spring Quadrangles, Western Iron County, Utah, Myron G. Best, Robert L. Davis, U.S. Geological Survey Jan 1981

Geologic Map Of The Steamboat Mountain And Bible Spring Quadrangles, Western Iron County, Utah, Myron G. Best, Robert L. Davis, U.S. Geological Survey

All U.S. Government Documents (Utah Regional Depository)

Geology mapped in 1980 with the assistance of Lehi F. Hintze and students in the Brigham Young University summer geology field course. This report includes geological maps along with a detailed key.


Shallow Electromagnetic Data From Three Known Fault Zones In The Paradox Basin, Utah, Raymond D. Watts, U.S. Geological Survey Jan 1981

Shallow Electromagnetic Data From Three Known Fault Zones In The Paradox Basin, Utah, Raymond D. Watts, U.S. Geological Survey

All U.S. Government Documents (Utah Regional Depository)

This report describes a preliminary investigation of the effectiveness of two electromagnetic exploration methods as means of finding unmapped faults in the Paradox Basin environment. Results indicate that the Very Low Frequency (VLF method is useful. VLF profiles were measured across three known fault traces near Gibson Dome, San Juan County, Utah. Each fault or set of faults generated a significant anomaly. In some cases, the anomaly due to the fault was superimposed on a larger scale anomaly caused by the transition from unaltered rocks away from the fault to altered rocks in or on one side of the fault …


Geochemical Results From A Rock Geochemical Survey In The Mount Belknap Caldera Vicinity, Utah, Robert E. Tucker, William R. Miller, J. N. Motooka, U.S. Geological Survey Jan 1981

Geochemical Results From A Rock Geochemical Survey In The Mount Belknap Caldera Vicinity, Utah, Robert E. Tucker, William R. Miller, J. N. Motooka, U.S. Geological Survey

All U.S. Government Documents (Utah Regional Depository)

Rock, stream-sediment, and hydrogeochemical surveys were conducted in the Mount Belknap caldera area, south-central Utah, during the summer of 1979. The presence of leucocratic rocks and relatively high concentrations of the elements Nb, Be, Ga, Y, Pb, Sn, Mo, and F with corresponding low concentrations of the elements Ba, Mg, Ca, Fe, Sr, and Cu suggests that late phase highly differentiated felsic magmas were intruded and (or) erupted in the caldera vicinity. The presence of Mo and Sn in the rocks and F in the water samples suggest that the ore elements were concentrated, first in residual fluids in the …


Mineral Resources Of The Phipps-Death Hollow Instant Study Area, Garfield County, Utah, G. W. Weir, M. E. Lane, U.S. Geological Survey Jan 1981

Mineral Resources Of The Phipps-Death Hollow Instant Study Area, Garfield County, Utah, G. W. Weir, M. E. Lane, U.S. Geological Survey

All U.S. Government Documents (Utah Regional Depository)

During 1979 and 1980 the U.S. Geological Survey and the U.S. Bureau of Mines conducted field studies to evaluate the mineral-resource potential of the Phipps-Death Hollow Instant Study Area, Garfield County, Utah. Field studies included geological mapping (Weir and Beard, 1981), geochemical sampling, and a search for mines, prospects and mineralized areas.


Mineral Resources Of The Escalante Canyon Instant Study Area, Garfield County, Utah, Gordon W. Weir, Michael E. Lane, U.S. Geological Survey, U.S. Bureau Of Mines Jan 1981

Mineral Resources Of The Escalante Canyon Instant Study Area, Garfield County, Utah, Gordon W. Weir, Michael E. Lane, U.S. Geological Survey, U.S. Bureau Of Mines

All U.S. Government Documents (Utah Regional Depository)

During 1979 and 1980 the U.S. Geological Survey and the Bureau of Mines conducted field investigations to evaluate the mineral resources potential of the Escalante Canyon Instant Study Area, Garfield County, Utah. Field studies included geological mapping and reconnaissance (Weir and Beard, 1981), geochemical sampling, and a survey of known mines, prospects, and mineralized areas (Lane, 1981).


Hydrology Of The Ferron Sandstone Aquifer And Effects Of Proposed Surface-Coal Mining In Castle Valley, Utah, Gregory C. Lines, Daniel J. Morrissey, Thomas A. Ryer, Richard H. Fuller, U.S. Geological Survey Jan 1981

Hydrology Of The Ferron Sandstone Aquifer And Effects Of Proposed Surface-Coal Mining In Castle Valley, Utah, Gregory C. Lines, Daniel J. Morrissey, Thomas A. Ryer, Richard H. Fuller, U.S. Geological Survey

All U.S. Government Documents (Utah Regional Depository)

Coal in the Ferron Sandstone Member of the Mancos Shale of Cretaceous age has traditionally been mined by underground techniques in the Emery Coal Field in the southern end of Castle Valley in east-central Utah. However, approximately 99 million tons are recoverable by surface mining. Ground water in the Ferron is the sole source of supply for the town of Emery, but the aquifer is essentially untapped outside the Emery area. The Ferron Sandstone Member crops out along the eastern edge of Castle Valley and generally dips 2" to 10" to the northwest beneath the surface. Sandstones in the Ferron …


Off-Road Vehicular Destabilization Of Hillslopes: The Major Contributing Factor To Destructive Debris Flows In Ogden, Utah, 1979, John K. Nakata Jan 1981

Off-Road Vehicular Destabilization Of Hillslopes: The Major Contributing Factor To Destructive Debris Flows In Ogden, Utah, 1979, John K. Nakata

All U.S. Government Documents (Utah Regional Depository)

A severe rain storm on August 11 and 18, 1979, caused major flood damage in urban areas of east Ogden, Utah. At least 3.85 cm of rain fell in a 7 hour-period. The severity of damage was dramatically increased by water diverted from the Brigham-Ogden Canal, when it was clogged by a debris flow in the vicinity or Third, Taylor, and Polk Streets (Fig. 1). The purpose or this investigation is to ascertain the sequence of events that followed the storm, and to quantify the processes insofar as possible. An inspection of the area on September 21-25, 1979 , and …


Analyses Of Rock, Stream-Sediment, And Water Samples From The Vermilion Cliffs-Paria Canyon Instant Study Area, Coconino County, Arizona, And Kane County, Utah, Alfred L. Bush, Michael E. Lane, U.S. Geological Survey Jan 1981

Analyses Of Rock, Stream-Sediment, And Water Samples From The Vermilion Cliffs-Paria Canyon Instant Study Area, Coconino County, Arizona, And Kane County, Utah, Alfred L. Bush, Michael E. Lane, U.S. Geological Survey

All U.S. Government Documents (Utah Regional Depository)

This open-file report contains the complete analyses of all rock, stream-sediment, and water samples collected and used by the U.S. Geological Survey and the U.S. Bureau of Mines in the preparation of Open-File Report 80-1056 (Bush and Lane, 1980). In the tables that follow, Qls indicates a landslipped mass of any form or origin, and only the abbreviated name of rock units is used.


Geophysical Measurements In The Beaver Basin, West-Central Utah; Part 1--Slingram, Magnetic, And Self-Potential Profiles, Vincent J. Flanigan, David L. Campbell, U.S. Geological Survey Jan 1981

Geophysical Measurements In The Beaver Basin, West-Central Utah; Part 1--Slingram, Magnetic, And Self-Potential Profiles, Vincent J. Flanigan, David L. Campbell, U.S. Geological Survey

All U.S. Government Documents (Utah Regional Depository)

This report consists of figures showing profile locations (fig. 1, table 1) in the Beaver Basin, west-central Utah, and ground geophysical data collected in September 1980 along these traverses (figs. 2-11). These data consist of slingram electromagnetic (real and imaginary components at 222, 444, 888, 1777, and 3555 Hz), ground magnetic and self-potential measurements collected at 200-foot (61-m) intervals along about 8.8 miles (14.2 km) of survey line. Table 2 lists equipment used. The report contains data only, and no interpretations of the data are included.


Preliminary Hydrologic Evaluation Of The North Horn Mountain Coal-Resource Area, Utah, M. J. Graham, John E. Tooley, Don Price, U.S. Geological Survey Jan 1981

Preliminary Hydrologic Evaluation Of The North Horn Mountain Coal-Resource Area, Utah, M. J. Graham, John E. Tooley, Don Price, U.S. Geological Survey

All U.S. Government Documents (Utah Regional Depository)

North Horn Mountain is part of a deeply dissected plateau in central Utah which is characterized by deep, arrow, steep-walled canyons with local relief of more that 1,000 feet. Geologic units exposed in the North Hort Mountain area range in age from Late Cretaceous to Holocene and contain two mineable seams of Cretaceous coal. The area is in the drainage basin of the San Rafael River, in the Colorado River Basin. Runoff from the mountain is ephemeral. This runoff to the San Rafael River sis by way of Cottonwood and Ferron Creeks and represents less than 10 percent of their …


Geologic Map And Coal Sections Of The Red Point Quadrangle, Eugene G. Elllis, U.S. Forest Service, U.S. Geological Survey, Joseph R. Frank Jan 1981

Geologic Map And Coal Sections Of The Red Point Quadrangle, Eugene G. Elllis, U.S. Forest Service, U.S. Geological Survey, Joseph R. Frank

All U.S. Government Documents (Utah Regional Depository)

Red Point quadrangle, in Emery County in central Utah, was mapped in 1979 as a part of the U.S. Geological Survey's progress to evaluate lands in the public domain for potential coal leasing. Mapping was done using U.S. Forest Service color aerial photographs at a scale of 1:15,640 and U.S. Geological Survey black-and-white aerial photographs at a scale of 1:30,000. The quadrangle was mapped previously by Spicker (1931) at a scale of 1:62,500.


Why Windspeeds Increase On High Mountain Slopes At Night, United States Department Of Agriculture, Forest Service Jan 1981

Why Windspeeds Increase On High Mountain Slopes At Night, United States Department Of Agriculture, Forest Service

Forestry

The purpose of this report is to explain the windspeed increase on mountain slopes at night. Additional work is required to determine such things as the frequency of the winds, the area affected, seasonal variation, and the effect on fire behavior. Also, additional studies are needed to develop the type of procedures required to forecast these nocturnal mountain winds.


Visual Impacts Of Forest Management Activities: Findings On Public Preferences, United States Department Of Agriculture, Forest Service Jan 1981

Visual Impacts Of Forest Management Activities: Findings On Public Preferences, United States Department Of Agriculture, Forest Service

Forestry

A major concern of forest land managers is the visual impact that activities such as timber harvest, road building, and mining have on the forest landscape. Management of the visual resource is a regular part of planning on National Forests, and many other public and private forest land managers are increasing their efforts to protect and enhance this resource. The Forest Residue and Harvesting Research Program at the Intermountain Station includes studies of the impact of harvest and roading activities on visual quality. Preliminary results were reported earlier (Schweitzer, Ullrich, and Benson 1976). This report updates earlier findings and presents …


Interior West Watershed Management, United States Department Of Agriculture, Forest Service Jan 1981

Interior West Watershed Management, United States Department Of Agriculture, Forest Service

Water

Habitat type classification systems are reviewed for potential use in watershed management. Information on climate, soils, and vegetation related to the classifications are discussed. Possible cooperative applications of vegetation and habitat type classifications to watershed management are explored.


Theoretical Predictions For Ion Composition In The High-Latitude Winter F-Region For Solar Minimum And Low Magnetic Activity, Jan Josef Sojka, W. John Raitt, Robert W. Schunk Jan 1981

Theoretical Predictions For Ion Composition In The High-Latitude Winter F-Region For Solar Minimum And Low Magnetic Activity, Jan Josef Sojka, W. John Raitt, Robert W. Schunk

All Physics Faculty Publications

We combined a simple plasma convection model with an ionospheric-atmospheric density model in order to study the ion composition in the high-latitude winter F-region at solar minimum for low geomagnetic activity. Our numerical study produced time-dependent, 3-dimensional, ion density distributions for the ions NO+, O2 +, N2 +, O+, N+, and He+. We covered the high-latitude ionosphere above 54°N magnetic latitude and at altitudes between 160 and 800 km for a time period of 1 complete day. From our study we found the following (1) The ion composition exhibits a significant variation with latitude, local time, altitude, and universal time. …


A Theoretical Study Of The High-Latitude Winter F Region At Solar Minimum For Low Magnetic Activity, Jan Josef Sojka, W. J. Raitt, Robert W. Schunk Jan 1981

A Theoretical Study Of The High-Latitude Winter F Region At Solar Minimum For Low Magnetic Activity, Jan Josef Sojka, W. J. Raitt, Robert W. Schunk

All Physics Faculty Publications

We combined a simple plasma convection model with an ionospheric-atmospheric composition model in order to study the high-latitude winter F region at solar minimum for low magnetic activity. Our numerical study produced time dependent, three-dimensional ion density distributions for the ions NO+, O2 +, N2 +, O+, N+, and He+. We covered the high-latitude ionosphere above 54°N magnetic latitude and at altitudes between 160 and 800 km for a time period of one complete day. The main result we obtained was that high-latitude ionospheric features, such as the ‘main trough,’ the ‘ionization hole,’ the ‘tongue of ionization,’ the ‘aurorally produced …


Final Environmental Impact Statement, U.S. Department Of Housing And Urban Development Jan 1981

Final Environmental Impact Statement, U.S. Department Of Housing And Urban Development

Elusive Documents

No abstract provided.


Radar Measurements Of High-Latitude Ion Composition Between 140 And 300 Km Altitude, J. D. Kelly, Vincent B. Wickwar Jan 1981

Radar Measurements Of High-Latitude Ion Composition Between 140 And 300 Km Altitude, J. D. Kelly, Vincent B. Wickwar

All Physics Faculty Publications

The Chatanika radar has been used to measure the ratio of atomic (O+) ions to molecular (O2 +, NO+) ions in the high-latitude ionosphere. The radar results agreed well with simultaneous in situ rocket data, giving confidence in the radar method of deducing ion composition. Measurements made over long periods of time show seasonal variations, diurnal variations, and variations due to auroral processes. The transition altitude, where the number densities of atomic and molecular ions are equal, is a convenient parameter for describing the composition variation with altitude or ‘composition altitude profile.’ The transition …


An Intense Wave/Particle Event In The Auroral Ionosphere, A. D. Johnstone, Jan Josef Sojka, W. Gibbons, B. K. Madahar, L.J. C. Woolliscroft Jan 1981

An Intense Wave/Particle Event In The Auroral Ionosphere, A. D. Johnstone, Jan Josef Sojka, W. Gibbons, B. K. Madahar, L.J. C. Woolliscroft

All Physics Faculty Publications

An intense burst of VLF waves, at frequencies just above the local proton gyrofrequency, was observed shortly after each of two intense bursts of field‐aligned suprathermal electrons (E < 250eV) by instruments carried on a sounding rocket flown in diffuse aurora. If the two phenomena are associated with each other, the implication is that the electron acceleration occurred nearby, in a relatively small volume.


Auroral Plasma Lines: A First Comparison Of Theory And Experiment, E. S. Oran, Vincent B. Wickwar, W. Kofman, A. Newman Jan 1981

Auroral Plasma Lines: A First Comparison Of Theory And Experiment, E. S. Oran, Vincent B. Wickwar, W. Kofman, A. Newman

All Physics Faculty Publications

In this preliminary report on low-energy (0.3 to 3 eV) secondary electrons in the auroral E layer (90 to 150 km), we compare intensities of plasma lines observed with the Chatanika radar to theoretical predictions obtained from a detailed numerical model. The model calculations are initiated with a flux of energetic auroral primary electrons which enter the atmosphere and lose energy to electrons, ions, and neutrals through a combination of elastic and inelastic collisions. This flux is chosen in order that the total calculated ionization rate matches one that is deduced from the radar measurements. From these same calculations the …