Author: Michael A. Korosec
Publisher:
ISBN:
Category : Geothermal resources
Languages : en
Pages : 20
Book Description
The Low Temperature Geothermal Resources of Eastern Washington
Author: Michael A. Korosec
Publisher:
ISBN:
Category : Geothermal resources
Languages : en
Pages : 20
Book Description
Publisher:
ISBN:
Category : Geothermal resources
Languages : en
Pages : 20
Book Description
Low Temperature Geothermal Resource Evaluation of the Moses Lake-Ritzville-Connell Area, Washington
Author: Scott Widness
Publisher:
ISBN:
Category : Connell (Wash.)
Languages : en
Pages : 27
Book Description
Publisher:
ISBN:
Category : Connell (Wash.)
Languages : en
Pages : 27
Book Description
Low-temperature Geothermal Resources of Washington
Author: J. Eric Schuster
Publisher:
ISBN:
Category : Geothermal resources
Languages : en
Pages : 53
Book Description
Publisher:
ISBN:
Category : Geothermal resources
Languages : en
Pages : 53
Book Description
The Low-temperature Geothermal Resource of the Moses Lake-Ritzville-Connell Area, East-central Washington
Author: Scott Edward Widness
Publisher:
ISBN:
Category : Geothermal resources
Languages : en
Pages : 714
Book Description
Publisher:
ISBN:
Category : Geothermal resources
Languages : en
Pages : 714
Book Description
Fluid-temperature Logs for Selected Wells in Eastern Washington
Author: Washington State University
Publisher:
ISBN:
Category : Geothermal resources
Languages : en
Pages : 351
Book Description
Publisher:
ISBN:
Category : Geothermal resources
Languages : en
Pages : 351
Book Description
Low Temperature Geothermal Resource Evaluation of the Moses Lake-Ritzville-Connell Area, Washington
Author:
Publisher:
ISBN:
Category :
Languages : en
Pages :
Book Description
The study area is located in portions of Adams, Grant, Lincoln, and Franklin counties of eastern Washington. The area is representative of a complex stratigraphic and geohydrologic system within the basalt flows of the Columbia River Basalt Group. Fluid temperature data were collected by three different agencies. The Geological Engineering Section (WSU) at Washington State University, runs a continuous fluid temperature (FT) log as part of a complete suite of geophysical logs. The US Geological Survey (USGS) runs a continuous fluid FT log in conjunction with caliper and natural-gamma logs. Southern Methodist University (SMU) and the Washington State Department of Natural Resources, Division of Geology and Earth Resources (DNR), have cooperated in gathering FT data. The DNR-SMU data were collected by taking temperature measurements at 5 m intervals. Bottom-hole temperatures (BHT) and bottom-hole depths (BHD) of selected wells in the study area are given. A technique developed by Biggane (1982) was used to determine the geothermal gradients within the area. A least squares linear regression analysis of the relationship between the BHT and BHD was used to determine the geothermal gradient of a given well data group (WDG).
Publisher:
ISBN:
Category :
Languages : en
Pages :
Book Description
The study area is located in portions of Adams, Grant, Lincoln, and Franklin counties of eastern Washington. The area is representative of a complex stratigraphic and geohydrologic system within the basalt flows of the Columbia River Basalt Group. Fluid temperature data were collected by three different agencies. The Geological Engineering Section (WSU) at Washington State University, runs a continuous fluid temperature (FT) log as part of a complete suite of geophysical logs. The US Geological Survey (USGS) runs a continuous fluid FT log in conjunction with caliper and natural-gamma logs. Southern Methodist University (SMU) and the Washington State Department of Natural Resources, Division of Geology and Earth Resources (DNR), have cooperated in gathering FT data. The DNR-SMU data were collected by taking temperature measurements at 5 m intervals. Bottom-hole temperatures (BHT) and bottom-hole depths (BHD) of selected wells in the study area are given. A technique developed by Biggane (1982) was used to determine the geothermal gradients within the area. A least squares linear regression analysis of the relationship between the BHT and BHD was used to determine the geothermal gradient of a given well data group (WDG).
Low-temperature Geothermal Resources of Washington
Geophysical Logs of Selected Wells in Eastern Washington
Author:
Publisher:
ISBN:
Category :
Languages : en
Pages :
Book Description
This report consists of geophysical well logs compiled during studies of the geohydrology and low temperature geothermal resources of eastern Washington. The geophysical logs are divided into two groups. Part A consists of wells concentrated in the Moses Lake-Ritzville-Connell area. Results of the geohydrologic study are discussed in Widness (1983, 1984). Part B consists of wells outside of the Moses Lake-Ritzville-Connell study area.
Publisher:
ISBN:
Category :
Languages : en
Pages :
Book Description
This report consists of geophysical well logs compiled during studies of the geohydrology and low temperature geothermal resources of eastern Washington. The geophysical logs are divided into two groups. Part A consists of wells concentrated in the Moses Lake-Ritzville-Connell area. Results of the geohydrologic study are discussed in Widness (1983, 1984). Part B consists of wells outside of the Moses Lake-Ritzville-Connell study area.
The Low Temperature Geothermal Resource of the Yakima Region
Author: Washington (State). Division of Geology & Earth Resources
Publisher:
ISBN:
Category : Geothermal resources
Languages : en
Pages : 37
Book Description
Publisher:
ISBN:
Category : Geothermal resources
Languages : en
Pages : 37
Book Description
The Low-temperature Geothermal Resource and Stratigraphy of Portions of Yakima County, Washington
Author: John Biggane
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 128
Book Description
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 128
Book Description