| Abstract: | Transient electromagnetic soundings were used to map the geoelectrical structure of Newberry Volcano in central Oregon. An extensive conductor was found to underlie the volcano and to have resistivities from 20 OMEGA m to 72 OMEGA m. The depth to the conductor ranges from 410 m to 870 m. Inside the caldera, low basement resistivities are the result of hot fluids. The cause of the conductor outside the caldera is not known; however, we speculate that it is due to the water table. |
| Genre: | Conference Paper |
| ProdID: | 70013216 |
| Citation Author: | Fitterman, David, V.; Neev, Deborah, K. |
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| Citation End Page: | 410 |
| Citation Issue: | pt 2 |
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| Citation Language: | English |
| Citation Larger Work Title: | Transactions - Geothermal Resources Council |
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| Citation Number Of Pages: | 4 |
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| Citation Publisher: | Geothermal Resources Council |
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| Citation Search Results Text: | TRANSIENT SOUNDING INVESTIGATION OF NEWBERRY VOLCANO, OREGON.; 1985; Conference Paper; Transactions - Geothermal Resources Council; Fitterman, David, V.; Neev, Deborah, K. |
| Citation Start Page: | 407 |
| Citation Volume: | 9 |
| Citation Year: | 1985 |
| Type: | citation/reference |
| Text: | TRANSIENT SOUNDING INVESTIGATION OF NEWBERRY VOLCANO, OREGON.; 1985; Conference Paper; Transactions - Geothermal Resources Council; Fitterman, David, V.; Neev, Deborah, K. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Tue, 1 Jan 1985 00:00 -0600 |
| Publisher: | Geothermal Resources Council |
