Abstract
GEOMORPHIC SETTING: Buckhorn Mountain is an exposed decomposed granite batholith which separates Shasta and Trinity Counties in NW California. Highway 299 W traverses Buckhorn Mountain for almost 15 miles over steep mountainous terrain. The Shasta Bally Batholith granitics have a high percentage of biotite and mica-type minerals that weather easily. Weathering is extensive because the batholith is deeply fractured, thus allowing the intrusion of water.
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Ghiassian, H., Gray, D.H., and Hryciw, R. (1998). “Stabilization of Coastal Slopes by Anchored Geosynthetic Systems.” J. of Geotechnical Engr. (ASCE), Vol. 123, No. GT8, pp. 736-743.
Gray, D.H. (2002). “Optimizing Soil Compaction and Other Strategies,” Erosion Control 9(6):27-34 (Sept/Oct 2002)
McCullah, J. A. (2006). Biotechnical Soil Stabilization of Decomposed Granite Soils – 20 Years of Lessons Learned on Buckhorn Mountain, Land and Water Magazine, Vol.??, pp
McCullah, J. et.al., (2005), Effective Compost and Bioengineering Techniques for Adverse Soil Conditions, Proceedings,International Erosion Control Association Conference, Dallas 2005.
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Goldsmith, W., Gray, D., McCullah, J. (2014). Project #13: Buckhorn Mountain. In: Bioengineering Case Studies. Springer, New York, NY. https://doi.org/10.1007/978-1-4614-7996-3_14
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DOI: https://doi.org/10.1007/978-1-4614-7996-3_14
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