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Author: Bern S. Hinckley
Publisher:
ISBN:
Category : Geothermal resources
Languages : en
Pages : 48
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Book Description
Author: Bern S. Hinckley
Publisher:
ISBN:
Category : Geothermal resources
Languages : en
Pages : 48
Get Book Here
Book Description
Author: Bern S. Hinckley
Publisher:
ISBN:
Category : Geothermal resources
Languages : en
Pages :
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Book Description
Author:
Publisher:
ISBN:
Category :
Languages : en
Pages :
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The geothermal resources of the Wind River Basin were investigated. Oil-well bottom-hole temperatures, thermal logs of wells, and heat flow data have been interpreted within a framework of geologic and hydrologic constraints. Basic thermal data, which includes the background thermal gradient and the highest recorded temperature and corresponding depth for each basin, is tabulated. Background heat flow in the Wind River Basin is generally insufficient to produce high conductive gradients. Only where hydrologic systems re-distribute heat through mass movement of water will high temperatures occur at shallow depths. Aquifers which may have the confinement and structural characteristics necessary to create such geothermal systems are the Lance/Fort Union, Mesa Verde, Frontier, Muddy, Cloverly, Sundance, Nugget, Park City, Tensleep, Amsden, Madison, Bighorn, and Flathead Formations. Of these the Tensleep Sandstone and Madison Limestone are the most attractive in terms of both productivity and water quality. Most of the identified geothermal anomalies in the Wind River Basin occur along complex structures in the southwest and south. The most attractive geothermal prospects identified are anomalous Areas 2 and 3 north of Lander, Sweetwater Station Springs west of Jeffrey City, and the thermal springs southwest of Dubois. Even in these areas, it is unlikely temperatures in excess of 130 to 150°F can be developed. 16 refs., 7 figs., 7 tabs. (ACR).
Author:
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ISBN:
Category : Geothermal resources
Languages : en
Pages :
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Author: Edward R. Decker
Publisher:
ISBN:
Category : Electric power
Languages : en
Pages : 34
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Author:
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Category :
Languages : en
Pages :
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The Wind River Valley, on the west slope of the Cascade Range, is a northwest-trending drainage that joins the Columbia River near Carson, Washington. The region has been heavily dissected by fluvial and glacial erosion. Ridges have sharp crests and deep subsidiary valleys typical of a mature topography, with a total relief of as much as 900 m. The region is vegetated by fir and hemlock, as well as dense, brushy ground-cover and undergrowth. The lower 8 km of the valley is privately owned and moderately populated. The upper reaches lies within the Gifford Pinchot National Forest, and include several campgrounds and day parks, the Carson National Fish Hatchery, and the Wind River Ranger Station and Wind River Nursery of the US Forest Service. Logging activity is light due to the rugged terrain, and consequently, most valley slopes are not accessible by vehicle. The realization that a potential for significant geothermal resources exists in the Wind River area was brought about by earlier exploration activities. Geologic mapping and interpretation was needed to facilitate further exploration of the resource by providing a knowledge of possible geologic controls on the geothermal system. This report presents the detailed geology of the lower Wind River valley with emphasis on those factors that bear significantly on development of a geothermal resource.
Author:
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 138
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Author:
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Category :
Languages : en
Pages :
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Separate abstracts were prepared for two papers. (MHR).
Author: Geological Survey of Wyoming
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 50
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Author:
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ISBN:
Category : Aeronautics
Languages : en
Pages : 1160
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