Core OL-92 from Owens Lake: Project rationale, geologic setting, drilling procedures, and summary
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- Larger Work: An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California
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Abstract
Several lines of evidence indicated that Owens Lake, a now-dry lake in southeast California, would probably yield a continuous and climatically informative sedimentary record. Also, the details of modern climate and runoff in the area are exceptionally well known, providing a firm basis for interpreting various types of evidence from a core in terms of past climates. Drilling was carried out in early 1992 to retrieve this record.
The resulting core, OL-92, was taken from the south-central part of the lake (lat 36°22.85′ N, long 117°57.95′ W). Lake surface elevation at the drill site is 1,085 m. The core’s length is 322.86 m, recovery was ~80%, and the age of its basal sediments is ~800 ka.
Study of the core has revealed lithologic, chemical, mineralogic, geophysical, and paleontologic evidence that reflects alternating periods of high- and low-volume runoff into Owens Lake. This volume presents these studies and summarizes their paleoclimatic significance.
Study Area
Publication type | Book chapter |
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Publication Subtype | Book Chapter |
Title | Core OL-92 from Owens Lake: Project rationale, geologic setting, drilling procedures, and summary |
DOI | 10.1130/0-8137-2317-5.1 |
Volume | 317 |
Year Published | 1997 |
Language | English |
Publisher | Geological Society of America |
Description | 8 p. |
Larger Work Type | Book |
Larger Work Subtype | Monograph |
Larger Work Title | An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California |
First page | 1 |
Last page | 8 |
Country | United States |
State | California |
Other Geospatial | Owens Lake |
Google Analytic Metrics | Metrics page |