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- W2258536432 abstract "The sedimentary serpentinites we will visit are exposed in the southeast plunging Wilbur Springs anticline, where they interfinger with lower Cretaceous turbidites of the Great Valley Sequence. The Wilbur Springs area (Fig. 65) lies astride this anticlinal structure on the western edge of the Sacramento Valley approximately 175 km north of San Francisco (Fig. 61). The area is named for a hot springs resort on Sulfur Creek, which is located upstream from the Lodoga Road connecting Bear Valley with Highway 20. Barren, block-strewn, grass-free slopes or dense brush characterize areas underlain by serpentinite. Outcrops are sparse, and mainly confined to road and stream cuts. However, even in areas of poor exposure, contacts are easily traced in soils and subcrop. Because of the serpentinite, the area is highly suceptible to landslides and soil creep which locally bury or displace contacts." @default.
- W2258536432 created "2016-06-24" @default.
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- W2258536432 date "2015-04-05" @default.
- W2258536432 modified "2023-10-03" @default.
- W2258536432 title "Descriptions of Field Trip Stops 7, 8, and 9" @default.
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- W2258536432 doi "https://doi.org/10.2110/sepmfg.03.117" @default.
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