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Calcite from
Mi Vida Mine, Lisbon Valley Mining District, San Juan County, Utah, USA


Locality type:Mine
Classification
Species:Calcite
Formula:CaCO3
Confirmation
Validity:Believed Valid
Associated Minerals Based on Photo Data:
Tyuyamunite4
Liebigite1
Data
Mineral Data:Click here to view Calcite data
Locality Data:Click here to view Mi Vida Mine, Lisbon Valley Mining District, San Juan County, Utah, USA
Data Identifiers
Mindat Occurrence Record ID:791874
Long-form Identifier:1:3:791874:2
GUID (UUID V4):0
Nearest other occurrences of Calcite
5.7km (3.5 miles) ⓘBlue Crystal Mine, Lisbon Valley Mining District, San Juan County, Utah, USA
6.9km (4.3 miles) ⓘRadon Mine, Lisbon Valley Mining District, San Juan County, Utah, USA
8.7km (5.4 miles) ⓘLisbon Mine & Mill (Lisbon; Lisbon Mine-Rio Algom), Lisbon Valley Mining District, San Juan County, Utah, USA
11.7km (7.3 miles) ⓘLisbon Valley Copper Mine, Lisbon Valley Mining District, San Juan County, Utah, USA
12.0km (7.4 miles) ⓘBlackbird Mine, Lisbon Valley Mining District, San Juan County, Utah, USA
13.2km (8.2 miles) ⓘWood Mine, San Juan County, Utah, USA
21.1km (13.1 miles) ⓘFirefly–Pigmay Mine, La Sal Creek Mining District, San Juan County, Utah, USA
21.7km (13.5 miles) ⓘLittle Don Mine, La Sal Creek Mining District, San Juan County, Utah, USA
22.4km (13.9 miles) ⓘVanadium Queen Mine, La Sal Creek Mining District, San Juan County, Utah, USA
23.8km (14.8 miles) ⓘBlue Cap Mine, La Sal Creek Mining District, San Juan County, Utah, USA
References
Page, Lincoln R., Stocking, Hobart E., Smith, Harriet B. (1956) Contributions to the geology of uranium and thorium by the United States Geological Survey and Atomic Energy Commission for the United Nations International Conference on Peaceful Uses of Atomic Energy, Geneva, Switzerland, 1955. Professional Paper 300. US Geological Survey doi:10.3133/pp300
Gross, Eugene Bischoff (1956) Mineralogy and paragensis of the uranium ore, Mi Vida Mine, San Juan County, Utah. Economic Geology, 51 (7) 632-648 doi:10.2113/gsecongeo.51.7.632
 
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