Clackamas 4800-foot thermal gradient hole: Cascade geothermal drilling: Final technical report
Thermal Power Company (Thermal) completed a thermal gradient hole to about 5000 feet (1524 m) total depth in Section 28, Township 8 South, Range 8 East, Willamette Meridian, Marion County, Oregon. The objective was to obtain data for the characterization of the deep hydrothermal regime in the Cascad...
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| Médium: | Report |
| Jazyk: | angličtina |
| Vydáno: |
1987
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| Témata: | |
| On-line přístup: | https://www.osti.gov/biblio/5435503 https://doi.org/10.2172/5435503 |
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| _version_ | 1878907257660375042 |
|---|---|
| author | Joe Iovenitti |
| author2 | William L. D'Olier |
| author_browse | Joe Iovenitti William L. D'Olier |
| author_facet | Joe Iovenitti William L. D'Olier |
| author_sort | joe iovenitti |
| collection | OpenAlex (Petróleo y Energía) |
| description | Thermal Power Company (Thermal) completed a thermal gradient hole to about 5000 feet (1524 m) total depth in Section 28, Township 8 South, Range 8 East, Willamette Meridian, Marion County, Oregon. The objective was to obtain data for the characterization of the deep hydrothermal regime in the Cascades volcanic region in order to better define its geothermal resource potential. The depth and location of the thermal gradient hole were designed by Thermal to test the basis of the Clackamas geothermal system exploration model developed by Chevron Resources Company. |
| doi_str_mv | 10.2172/5435503 |
| first_indexed | 2026-10-13T04:26:34Z |
| format | Report |
| id | openalex-W100245368 |
| language | English |
| last_indexed | 2026-10-13T04:26:34Z |
| publishDate | 1987 |
| publishDateSort | 1987 |
| record_format | oai_dc |
| spelling | Clackamas 4800-foot thermal gradient hole: Cascade geothermal drilling: Final technical report Joe Iovenitti William L. D'Olier Geothermal Energy Systems and Applications Geological Studies and Exploration Geophysical and Geoelectrical Methods geothermal potential geothermal exploration Clackamas County, Oregon Thermal Power Company (Thermal) completed a thermal gradient hole to about 5000 feet (1524 m) total depth in Section 28, Township 8 South, Range 8 East, Willamette Meridian, Marion County, Oregon. The objective was to obtain data for the characterization of the deep hydrothermal regime in the Cascades volcanic region in order to better define its geothermal resource potential. The depth and location of the thermal gradient hole were designed by Thermal to test the basis of the Clackamas geothermal system exploration model developed by Chevron Resources Company. 10.2172/5435503 OpenAlex (Petróleo y Energía) |
| spellingShingle | Clackamas 4800-foot thermal gradient hole: Cascade geothermal drilling: Final technical report Joe Iovenitti Geothermal Energy Systems and Applications Geological Studies and Exploration Geophysical and Geoelectrical Methods geothermal potential geothermal exploration Clackamas County, Oregon |
| title | Clackamas 4800-foot thermal gradient hole: Cascade geothermal drilling: Final technical report |
| title_full | Clackamas 4800-foot thermal gradient hole: Cascade geothermal drilling: Final technical report |
| title_fullStr | Clackamas 4800-foot thermal gradient hole: Cascade geothermal drilling: Final technical report |
| title_full_unstemmed | Clackamas 4800-foot thermal gradient hole: Cascade geothermal drilling: Final technical report |
| title_short | Clackamas 4800-foot thermal gradient hole: Cascade geothermal drilling: Final technical report |
| title_sort | clackamas 4800-foot thermal gradient hole: cascade geothermal drilling: final technical report |
| topic | Geothermal Energy Systems and Applications Geological Studies and Exploration Geophysical and Geoelectrical Methods geothermal potential geothermal exploration Clackamas County, Oregon |
| topic_facet | Geothermal Energy Systems and Applications Geological Studies and Exploration Geophysical and Geoelectrical Methods geothermal potential geothermal exploration Clackamas County, Oregon |
| url | https://www.osti.gov/biblio/5435503 https://doi.org/10.2172/5435503 |