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(1976) Hot springs mercury deposition at Mc Dermitt mine, Humboldt County, Nevada.
It also includes various stream deposits, gravel, fanglomerates, and older gravels.
It is not very consistent in description from county to county.
Hydrothermal fluids then deposited the antimony and mercury mineralization and silicified the parent tuff. This geological map and associated information on rock units at or nearby to the coordinates given for this locality is based on relatively small scale geological maps provided by various national Geological Surveys.
This occurred at about 15.7±0.4 Ma based on Noble et al. Sometimes the silica and ore replacement is so thorough the parent rock textures and grains can no longer be recognized, even in thin sections under the microscope. This does not necessarily represent the complete geology at this locality but it gives a background for the region in which it is found.
(1967) The growth of Hg S and Hg3S2Cl2 single crystals by a vapor phase method.
Ridge, Ed., Ore Deposits of the United States, 1933-1967, vol. Oregon Department of Geology and Mineral Industries Bulletin B-055. Bureau of Mines Staff (1965) Mercury potential of the United States. (1974) Corderoite, first natural occurrence of α-Hg3S2Cl2, from the Cordero mercury deposit, Humboldt County, Nevada. (1975) Chronology of volcanism, tectonism, and mineralization of the Mc Dermitt caldera, Nevada-Oregon (abs.) Geol. (1976) Volcanic rocks of the Mc Dermitt caldera, Nevada-Oregon: U.