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Geology of the Teakettle Creek watersheds
Author(s): Robert S. LaMotte
Date: 1937
Source: Form 406. Berkeley, CA: U.S. Department of Agriculture, Forest Service, California Forest and Range Experiment Station. 35 p.
Publication Series: Miscellaneous
PDF: Download Publication (18.0 MB)Description
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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Citation
LaMotte, 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.Related Search
- Current status of experimental paired-watershed research in the USDA Forest Service
- Impacts of forest management on runoff and erosion
- Hydrological responses to changes in forest cover on uplands and peatlands. Chapter 13.
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