Geochemical Characterization of the Mountain Home Geothermal System
The Mountain Home (MH) geothermal system of the western Snake River Plain (SRP) magmatic province was discovered in 2012 by the Snake River Geothermal Drilling Project. Artesian flowing water with a temperature of 150°C was encountered at a depth of 1745 m below ground surface (mbgs) and extensive m...
Main Author: | Atkinson, Trevor Alex |
---|---|
Format: | Others |
Published: |
DigitalCommons@USU
2015
|
Subjects: | |
Online Access: | https://digitalcommons.usu.edu/etd/4599 https://digitalcommons.usu.edu/cgi/viewcontent.cgi?article=5628&context=etd |
Similar Items
-
In Situ Stress and Geology from the MH-2 Borehole, Mountain Home, Idaho: Implications for Geothermal Exploration from Fractures, Rock Properties, and Geomechanics
by: Kessler, James Andrew
Published: (2014) -
Hydrogeochemical Characteristics of the Ngatamariki Geothermal Field and a Comparison with the Orakei Korako Thermal Area, Taupo Volcanic Zone, New Zealand.
by: O'Brien, Jeremy Mark
Published: (2010) -
A HYDROLOGIC CHARACTERIZATION OF THREE HEADWATER MOUNTAIN WETLANDS IN EASTERN KENTUCKY, USA
by: Hoy, Catherine
Published: (2012) -
Anaerobic carboxydotrophic bacteria in geothermal springs identified using stable isotope probing
by: Allyson Lee Brady, et al.
Published: (2015-09-01) -
Sequential Thrusting Beneath the Willard Thrust Fault, Wasatch Mountains, Ogden, Utah
by: Schirmer, Tad William
Published: (1985)