Hydrogeologic appraisal of the Klamath Falls geothermal area, Oregon.
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Hydrogeologic appraisal of the Klamath Falls geothermal area, Oregon.

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Published by U.S. Dept. of the Interior in Washington .
Written in English

Subjects:

  • Geothermal Resources - Oregon

Book details:

Edition Notes

11

The Physical Object
Pagination45 p.
Number of Pages45
ID Numbers
Open LibraryOL22016533M

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Book: Hydrogeologic appraisal of the Klamath Falls geothermal area, Oregon Title: Hydrogeologic appraisal of the Klamath Falls geothermal area, Oregon Full Record. Hydrogeologic appraisal of the Klamath Falls geothermal area, Oregon (OCoLC) Material Type: Internet resource: Document Type: Book, Internet Resource: All Authors / Contributors: Edward A Sammel. Hydrogeologic appraisal of the Klamath Falls geothermal area, Oregon / by Edward A. Sammel. Hydrogeologic Appraisal of the Klamath Falls Geothermal Area, Oregon: Sammel EA: Books - or: Sammel EA.

Buy Hydrogeologic Appraisal of the Klamath Falls Geothermal Area, Oregon by Sammel EA (ISBN:) from Amazon's Book Store. Everyday low prices and free delivery on eligible : Sammel EA. Buy Hydrogeologic appraisal of the Klamath Falls geothermal area, Oregon (Geohydrology of geothermal systems) by Sammel, Edward A (ISBN:) from Amazon's Book Store. Everyday low prices and free delivery on eligible : Edward A Sammel. The City of Klamath Falls, Oregon, is located in a Known Geothermal Resource Area (KGRA) that has been directly used to heat homes, businesses, schools, and institutions since the early s. In , Klamath Falls and Klamath County became interested in establishing a geothermal dis-trict heating system to extend the benefits of the geothermal. Despite his well-used passport and variety of travels, Lund still sees Klamath Falls as a unique location, especially for its geothermal, coupled with the proximity of Oregon Tech.

Hydrogeologic Appraisal of the Klamath Falls Geothermal Area, Oregon (eBook): Sammel, Edward A. HYDROGEOLOGIC APPRAISAL OF KLAMATH FALLS GEOTHERMAL AREA, OREGONG5 Massive diatomites of the Yonna Formation have counterparts in Butte Valley, California, about 20 miles southwest of Klamath Falls, where they underlie Pliocene volcanic rocks of the High Cascades (Moore, ; Wood, ). The first area chosen for study is the Klamath Falls area in southern Klamath County {plate 1 L where surface indications appear favorable and where natural hot water has been used for space heating since the early 's. Another slightly smaller geothermal zone on the southwest side of the Klamath Hills 10 miles south of Klamath Falls occurs. Geothermal phenomena observed in the vicinity of Klamath Falls include hot springs with temperatures that approach °F (96 o C) (the approximate boiling temperature for the altitude), steam and water wells with temperatures that exceed °F (°C), and hundreds of warm-water wells with temperatures mostly ranging from 68° to 95°F (20° to 35°C).