Wednesday, April 5, 2017

USA, Idaho: Project HOTSPOT Encounters 150°C Flowing Artesian Hydrothermal Fluids at 1,745 m Depth

Geology and in situ stress of the MH-2 borehole, Idaho, USA: Insights into western Snake River Plain structure from geothermal exploration drilling (Lithosphere)

Project HOTSPOT, the Snake River Scientific Drilling Project (International Continental Scientific Drilling Program), tested for deep geothermal resources and examined the petrology of volcanic rocks with three drill-holes in the central and western Snake River Plain (western USA). The MH-2 drillhole targeted fractured crystalline and hydrothermally altered basalt in the area of the Mountain Home Air Force Base (Idaho) to a total depth of 1,821 m. 

At 1,745 m depth the drill-hole encountered flowing artesian hydrothermal fluids of at least 150°C.

These data indicate that the transition from the central to western Snake River Plain is characterized by complex structures developed in response to a transitional stress state related to Snake River Plain and western Basin and Range stress regimes. The western Basin and Range stress and tectonic regime may extend from northern Nevada into western Idaho and may enhance the potential for geothermal resources by creating interconnected fracture and fault-related permeability at depth.

Lithosphere, L609.1, first published on April 4, 2017