Geology of the Teakettle Creek watershedsAuthor(s): Robert S. LaMotte
Source: Form 406. Berkeley, CA: U.S. Department of Agriculture, Forest Service, California Forest and Range Experiment Station. 35 p.
Publication Series: Miscellaneous
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The Teakettle Creek Experimental Watersheds lie for the most part on quartzites of probable Triassic age. However one of the triplicate drainages has a considerable acreage developed on weathered granodiorite. Topography is relatively uniform and lends itself to triplicate watershed studies. Locations for dams are suitable if certain engineering precautions are taken. So far as observed botanic and soil conditions also lend themselves to experimental watershed studies.
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CitationLaMotte, Robert S. 1937. Geology of the Teakettle Creek watersheds. Form 406. Berkeley, CA: U.S. Department of Agriculture, Forest Service, California Forest and Range Experiment Station. 35 p.
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