Trace of mineralized Mosquito fault near the south head of Evans Amphitheater, looking southwest. Lake County, Colorado. 1929.
Dates
Date Taken
1929
Summary
Trace of mineralized Mosquito fault near the south head of Evans Amphitheater, looking southwest. Barren Weber (?) formation and Tertiary porphyry exposed on Little Ellen Hill over the potentially productive Leadville dolomite, which passes beneath the valley to the right. Rocks exposed on slopes of West Dyer Mountain include the Leadville dolomite, early Paleozoic formations and pre-Cambrian rocks. Lake County, Colorado. 1929. Figure 79, with graphics, in U.S.Geological Survey Professional paper 235. 1953.
Summary
Trace of mineralized Mosquito fault near the south head of Evans Amphitheater, looking southwest. Barren Weber (?) formation and Tertiary porphyry exposed on Little Ellen Hill over the potentially productive Leadville dolomite, which passes beneath the valley to the right. Rocks exposed on slopes of West Dyer Mountain include the Leadville dolomite, early Paleozoic formations and pre-Cambrian rocks. Lake County, Colorado. 1929. Figure 79, with graphics, in U.S.Geological Survey Professional paper 235. 1953.
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