Paleomagnetism and potassium-argon ages of the Sonoma Volcanics, California
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Abstract
Paleomagnetic data and potassium-argon ages indicate that the Sonoma Volcanics was erupted during the Pliocene Gilbert reversed and Gauss normal polarity epochs. The Gilbert reversed epoch is represented in the Howell Mountains east of Napa and east of St. Helena, in the mountains immediately east of the Valley of the Moon, and on the hill just north of Santa Rosa. The Gauss normal epoch is represented by the rocks from Mount St. Helena and possibly by the flows from the upper part of Sonoma Mountain and the rhyolite flows north of Sonoma. The age of the volcanic rocks ranges from 5.3 m.y. to about 2.9 m.y. Volcanic rocks approximately 11.8 m.y. old occur at Burdell Mountain northwest of Novato. This volcanic sequence is probably part of the Tolay Volcanics of the Petaluma area.
Study Area
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Paleomagnetism and potassium-argon ages of the Sonoma Volcanics, California |
| Series title | GSA Bulletin |
| DOI | 10.1130/0016-7606(1972)83[2063:PAPAOT]2.0.CO;2 |
| Volume | 83 |
| Issue | 7 |
| Year Published | 1972 |
| Language | English |
| Publisher | Geological Society of America |
| Contributing office(s) | Geology, Minerals, Energy, and Geophysics Science Center |
| Description | 10 p. |
| First page | 2063 |
| Last page | 2072 |
| Country | United States |
| State | California |
| Other Geospatial | Sonoma Volcanics |
| Google Analytic Metrics | Metrics page |