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Abstract
Data sets for spring and stream chemistry are combined to estimate convective heat discharge and discharge anomalous amounts of sodium and chloride for the Wood River group of springs south of Crater Lake. The best estimate of heat discharge is 87 MWt based on chloride inventory; this value is 3-5 times the heat input to Crater Lake itself. Anomalous discharges of sodium and chloride are also larger that into Crater Lake. Difference between the chemical and thermal characteristics of the discharge into Crater Lake and those from the Wood River group of springs suggest that the heat sources for the two systems may be different, although both ultimately related to the volcanic system.
Study Area
| Publication type | Book chapter |
|---|---|
| Publication Subtype | Book Chapter |
| Title | Convective heat discharge of Wood River group of springs in the vicinity of Crater Lake, Oregon |
| Volume | 18 |
| Year Published | 1994 |
| Language | English |
| Publisher | Geothermal Resources Council |
| Publisher location | Davis, CA |
| Contributing office(s) | Cascades Volcano Observatory, Volcano Hazards Program |
| Description | 8 p. |
| Larger Work Type | Book |
| Larger Work Subtype | Monograph |
| Larger Work Title | Restructuring the geothermal industry |
| First page | 229 |
| Last page | 236 |
| Country | United States |
| State | Oregon |
| Other Geospatial | Crater Lake, Wood River |
| Online Only (Y/N) | N |
| Additional Online Files (Y/N) | N |
| Google Analytic Metrics | Metrics page |