Latitude & Longitude (WGS84):
38° 31' 22'' North , 120° 55' 17'' West
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mindat:1:2:77730:9
A former Cr-Fe occurrence/mine located in the W½ (NW¼ ?) sec. 30, T8N, R10E, MDM, about 7 km SE of Latrobe, just N of the Cosumnes River, on private land. Owned by Robert Haddock and R. H. Chaix, California (1976). Operated by the Trio Chrome Co. under lease from Haddock and Chaix, California (1976). Operated by Theresa Garibaldi (timeframe unstated). MRDS database stated accuracy for this location is 500 meters.
The ore body strikes N60W and dips 70N at a thickness of 3 meters and a length of 19 meters. The ore body is disseminated and lenticular in form. The primary mode of origin is magmatic differentiation. The wallrock alteration is intense (carbonitization). The ore is coarse-grained and ranges from a medium-grade disseminated ore to nearly pure chromite. Local rocks include ultramafic rocks, chiefly Mesozoic, unit 2 (Western Sierra Nevada and Klamath Mountains) and/or Mesozoic volcanic rocks, unit 2 (Western Sierra Foothills and Western Klamath Mountains).
Workings include surface openings comprised of an open cut.
According to Taliaferro and Bradley, about 200 long tons were produced during WWI, but federal records list only 107 long tons. The average minable grade of chromite is 28 to 33%. About 20 long tons of ore remain on the dump and unmined reserves are nearly exhausted.
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2 valid minerals.
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References
Bradley, W.W., Huguenin, Emile, Logan, C.A., Tucker, W.B., and Waring, C.A. (1918), Manganese and chromium in California: California Mining Bureau. Bulletin 76, 248 pp.: 135.
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To cite: Ralph, J., Von Bargen, D., Martynov, P., Zhang, J., Que, X., Prabhu, A., Morrison, S. M., Li, W., Chen, W., & Ma, X. (2025). Mindat.org: The open access mineralogy database to accelerate data-intensive geoscience research. American Mineralogist, 110(6), 833–844.
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