2 edition of Characteristics of aquifers in the northern Uinta Basin area, Utah and Colorado found in the catalog.
Characteristics of aquifers in the northern Uinta Basin area, Utah and Colorado
Hood, J. W.
Bibliography: p. 39-42.
|Statement||by James W. Hood ; prepared by the United States Geological Survey in cooperation with the Utah Department of Natural Resources, Division of Water Rights.|
|Series||Technical publication - State of Utah, Department of Natural Resources ; no. 53, Technical publication (Utah. Dept. of Natural Resources) ;, no. 53.|
|Contributions||Geological Survey (U.S.), Utah. Division of Water Rights.|
|LC Classifications||TA7 .U77 no. 53, GB1199.3.U36 .U77 no. 53|
|The Physical Object|
|Pagination||vi, 71 p. (p. 64-71 advertisements):|
|Number of Pages||71|
|LC Control Number||77623637|
The Uinta-Animas Aquifer is located in three basins, primarily located in the Uinta Basin in Utah, the Piceance Basin in northwestern Colorado. and the San Juan Basin of New Mexico. Water bearing units are comprised of sandstone, conglomerate, and siltstone. The average thickness of each basin can be anywhere from to feet. SELECTED REFERENCES FOR THE UINTA BASIN, UTAH Listed by Author Craig D. Morgan Utah Geological Survey The following selected reference on the geology of the Uinta Basin is not intended to be a complete bibliography. Craig Morgan who compiled the File Size: KB.
special study utah geological survey a division of utah department of natural resources moderately saline groundwater in the uinta basin, utah. Utah geologic units; Geologic units in Uintah county, Utah. Eastern Uinta Basin Members of the Green River Formation (Eocene) at surface, covers 27 % of this area. Eastern Uinta Basin Members of the Green River Formation (Evacuation Creek Mbr, Parachute Creek Mbr (oil shale), Garden Gulch Mbr, and Douglas Creek Mbr.).
Uinta is applied to natural features and to the Uinta Utes -- Uinta Basin, Uinta River, Uinta Mountains, Uinta National Forest, etc. Uintah (a variant of Uinta) is applied to political entities -- Uintah County, Uintah School District, Uintah & Ouray Reservation, etc. The U.S. Board on Geographic Names lists the official spelling for Uinta Basin as Uinta -- not Uintah -- as it is a natural. The USGS (U.S. Geological Survey) publishes a set of the most commonly used topographic maps of the U.S. called US Topo that are separated into rectangular quadrants that are printed at "x29" or larger. Uinta Basin is covered by the Brennan Basin, UT US Topo Map quadrantFruita, CO: 85 mi.
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Characteristics of aquifers in the northern Uinta Basin area, Utah and Colorado () The Publications Warehouse does not have links to digital versions of this publication at this time.
Technical Publication No. 53, Characteristics of Aquifers in the Northern Uinta Basin Area, Utah and Colorado; Utah Department of Natural Resources; Technical Publication No. 54, Hydrologic Evaluation of Ashley Valley, Northern Uinta Basin Area, Utah; Utah Department of Natural Resources; By USGS Uinta-Piceance Assessment Team.
Chapter 3. Petroleum Systems of the Uinta and Piceance Basins—Geochemical Characteristics of Oil Types By Paul G. Lillis, Augusta Warden, and J. David King. Chapter 4. Thermal Maturity and Oil and Gas Generation History of Petroleum Systems in the Uinta-Piceance Province, Utah and Colorado.
The Uinta Basin (also known as the Uintah Basin) is a physiographic section of the larger Colorado Plateaus province, which in turn is part of the larger Intermontane Plateaus physiographic division.
It is also a geologic structural basin in eastern Utah, east of the Wasatch Mountains and south of the Uinta Uinta Basin is fed by creeks and rivers flowing south from the Uinta. Technical Publication No.
53, Characteristics of Aquifer in the Northern Uinta Basin Area, Utah and Colorado; Utah Department of Natural Resources; Technical Publication No. 55, Reconnaissance of Water Quality in the Duchesne River Basin and Some Adjacent Drainage Areas, Utah; Utah Department of Natural Resources; Year Published: Controls on organic matter distributions in Eocene Lake Uinta, Utah and Colorado.
The Green River Formation deposited in Eocene Lake Uinta in the Uinta and Piceance Basins, Utah and Colorado, contains the largest oil shale resource in the world with an estimated trillion barrels of oil in-place in the Piceance Basin and trillion barrels in the Uinta Basin.
This page Bulletin covers research and results of the Utah Geological Survey’s study of the geology, chemistry, and best practices related to produced water in the Uinta Basin. It includes (1) descriptions and maps of Uinta Basin reservoirs and aquifers, (2) statistical trends of the basin’s water quality, and (3) overviews of produced.
The northern Uinta Basin area covers about 5, square miles (13, square kilometers) in northeastern Utah and northwestern Colorado. Much of the lowlands are arid to semiarid, but the highest parts of the Uinta Mountains have a humid climate. Duringthe average annual precipitation ranged from less than 8 inches ( millimeters) in the lowest part of the area at the Green River.
Hood, J.W.,Characteristics of aquifers in the northern Uinta Basin area, Utah and Colorado: U.S. Geological Survey Open-File Report87 p. Howells, Lewis,Base of moderately saline ground water in San Juan County, Utah: Utah Department of Natural Resources Technical Publicat 35 p.
The area of this report is the SE. part of the Uinta Basin and constitutes about 2, sq miles in NE. Utah and NW. Colorado. The oldest rocks exposed are the massive sandstone and variegated shale of the Wasatch Formation of Eocene age.
The Wasatch Formation is divided into the main body and the Renegade Tongue (new name). Formation in Colorado to time-equivalent strata within the Mancos Shale of the eastern Uinta Basin, Utah. A structure map shows the top of the Niobrara equivalent (NE) deepens from near sea level at the Utah-Colorado line to more t feet below sea level at the.
A FIELD GUIDE TO THE MIDDLE TO UPPER TURONIAN FRONTIER FORMATION, “VERNAL DELTA COMPLEX,” NORTHERN UINTA BASIN, UTAH AND COLORADO Andrew J. Hutsky and Christopher R.
Fielding DEPOSITIONAL HISTORY AND LATERAL VARIABILITY OF A MICROBIAL CARBONATE IN THE MIDDLE GREEN RIVER FORMATION, THREE MILE CANYON, EASTERN UINTA BASIN. As petroleum production increases in the Uinta Basin, Utah, operators are pressed to establish suitable saline water disposal plans.
Several natural gas operators have identified the Birds Nest aquifer in central Uintah County as a possible large-scale, saline water disposal zone; however, disposal into this aquifer poses unique challenges and.
Why is it important to protect an aquifer's recharge area. Wiki User Mom kimmo. I'm. Related Questions. Asked in Earth Sciences Why do artesian aquifers contain water under.
in the southeastern uinta basin, utah and colorado u.s. geological survey water-resources investigations open-file report 81 ""': gi n/\l.
united states department of the interior geological survey selected biological characteristics of streams in the south eastern uinta basin, utah and colorado. What and Where Are Designated Groundwater Basins and What and Where Are the Denver Basin Groundwater Aquifers Presented by Robert Longenbaugh Colorado Legislature September 4, Designated Ground Water Basins Created by the Ground Water Management Act: through Size: 2MB.
The potential for developing oil-shale resources in the southeastern Uinta Basin of Utah and Colorado has created the need for information on the quantity and quality of water available in the area. This report describes the availability and chemical quality of ground water, which might provide a source or supplement of water supply for an oil-shale industry.
The Colorado plateau aquifer system is comprised of four major aquifers. These aquifers include the Uinta-Animas, the Mesaverde, Dakota-Glen Canyon, and Coconino-De Chelly aquifers are a crucial groundwater supply to the four corner states of the Southwest region of the U.S.
The Great Basin is the largest area of contiguous endorheic watersheds in North spans nearly all of Nevada, much of Oregon and Utah, and portions of California, Idaho, and is noted for both its arid climate and the basin and range topography that varies from the North American low point at Badwater Basin in Death Valley to the highest point of the contiguous United States Coordinates: 40°40′N °40′W /.
Title. Hydrologic and climatologic data, southeastern Uinta basin, Utah and Colorado: water year / Related Titles.
Series: Open-file report / U.S. Geological Survey, By. Conroy, Loretta S. Hike, hike, hike. Damn my pack is heavy. Hike, hike, hike. Take a picture. Hike some more. That about describes a backpacking trip to Naturalist Basin in Utah’s Uinta Mountains.
Oh, and the scenery is ‘effin’ spectacular. So much so, that Naturalist Basin is one of the most popular backpacking areas in the entire range. Location 1: Ut St. 1 - 9S 21E sec. 26 Near basin center ft ft ft Possible basinward Shortite fracture fill .Due to the recent increase in crude oil prices and concerns over diminishing conventional reserves, the Utah Geological Survey has reexamined the Uinta Basin's oil-shale resource, primarily in the Mahogany zone of the Green River Formation.
Past assessments, the first conducted in and subsequent studies continuing through the early s, concentrated on the Eocene Green River Formation's.