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dc.contributor.author Zablocki, CJ. en_US
dc.contributor.author Tilling, RI. en_US
dc.contributor.author Peterson, DW. en_US
dc.contributor.author Christiansen, RL. en_US
dc.contributor.author Keller, GV en_US
dc.date.accessioned 2012-01-27T20:19:13Z en_US
dc.date.available 2012-01-27T20:19:13Z en_US
dc.date.issued 1976-01-01 en_US
dc.identifier.citation Zablocki CJ, Tilling RI, Peterson DW, Christiansen RL, Keller GV. Deep research drill hole at Kilauea Volcano, Hawaii. [1,262 m] Denver (CO): Geological Survey. en_US
dc.identifier.uri http://hdl.handle.net/10524/19370 en_US
dc.description Report Number: USGS-OFR-76-538; OSTI ID: 7329255 en_US
dc.description.abstract A 1262-m-deep bore hole was drilled at the summit of Kilauea Volcano, Hawaii, to test predictions based on surface geophysical surveys and to obtain information on the hydrothermal regime above a postulated magma reservoir. Data from the drilling and geophysical borehole logs tend to confirm earlier predictions that a mound of brackish or saline water is present above the inferred magma body. Temperatures within the hydrothermal system are not sufficiently high to indicate deposits of economic interest, but the gradient toward the bottom of the hole (approximately 160 m below sea level) is high, about 370/sup 0/C per kilometer. The maximum temperature, 137/sup 0/C, is at the hole bottom. en_US
dc.description.sponsorship Report Number USGS-OFR-76-538 en_US
dc.format.extent 38 pages en_US
dc.language.iso en-US en_US
dc.publisher Geological Survey en_US
dc.subject hydrothermal en_US
dc.subject magma en_US
dc.subject volcanic en_US
dc.subject groundwater en_US
dc.subject Hawaii en_US
dc.subject Kilauea en_US
dc.title Deep research drill hole at Kilauea Volcano, Hawaii. [1,262 m] en_US
dc.type Report en_US
dc.type.dcmi Text en_US

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