References
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Velinskij VV Geotermicheskie issledovanija na Teleckom ozere (Geothermal studies on Lake Teletskoye )
Report of Heat Flow Measurements in Peru and Ecuador
Preliminary Geology and Geothermal Resource Potential of the Western Snake River Plain, Oregon
Temperatures, heat flow, and water chemistry from drill holes in the Raft River geothermal system, Cassia County, Idaho
Evaluation of the Susanville, California Geothermal Resource
The Susanville geothermal anomaly, located in northeast California, has been identified as a resource with potential for the development of geothermal energy for direct use applications. As a result of the City of Susanville's interest in developing the resource for a cityride space heating program, the Water and Power Resources Service (formerly the Bureau of Reclamation) and the Earth Sciences Division of Lawrence Berkeley Laboratory (LBL) have collaborated since 1978 on a geothermal resource evaluation project. As part of this project, twelve exploratory temperature gradient holes have been drilled (bringing the total number of old and new holes and wells …
Near-surface hydrothermal regime of the Lassen Known Geothermal Resource Area, California
The Terrain Effect on Terrestrial Heat Flow
Geothermal records of climatic change in New South Wales
Heat flow in the Coso Geothermal Area, Inyo County, California
Detailed heat flow measurements over the Juan de Fuca Ridge System
Geothermal processes at the Galapagos Spreading Center
Geophysical measurements at candidate drill sites along an east-west flow line in the Central Atlantic Ocean
The result of detailed geophysical surveys at IPOD candidate drill sites along a flowline transect in the Central Atlantic Ocean, is discussed with particular emphasis given to sites AT-3 and AT-7. The oceanic crustal sections at these sites, which were formed on opposite sides of a spreading center at the time of formation of magnetic anomalies 33 and 34 (∼ 76 to 80 my BP), have similar geophysical characteristics. The seismicvelocity structure, as determined through use of ocean-bottom seismometers and sonobuoys, shows typical oceanic-crust seismic structure for 80 my BP crust — 0.6 km thick layer 2B with velocity 4.70 …
Report of Heat Flow Measurements in Boivia
The Creep of Ice, Geothermal Heat Flow, and Roosevelt Island, Antarctica
Measurements of ice velocity, thickness, and surface topography on the large ice rise known as Roosevelt Island are consistent with Glen’s flow law, , for values of τ between 5 × 104 N m–2 and 1.4 × 105 N m–2, and there is no indication of a reduction in n at low stresses. If n = 3 there must be progressive softening of the ice towards the edge of the ice rise, and this probably represents the combined effects of warming and recrystallization leading to a fabric favoring shear. Assuming that near the centre of the ice rise, where the …