The Mount Aetna Molybdenum Prospect is a molybdenum mine located in Chaffee county, Colorado at an elevation of 12,008 feet.
About the MRDS Data:
All mine locations were obtained from the USGS Mineral Resources Data System. The locations and other information in this database have not been verified for accuracy. It should be assumed that all mines are on private property.
Elevation: 12,008 Feet (3,660 Meters)
Primary Mineral: Molybdenum
Lat, Long: 38.5775, -106.31440
Map: View on Google Maps
MRDS mine locations are often very general, and in some cases are incorrect. Some mine remains have been covered or removed by modern industrial activity or by development of things like housing. The satellite view offers a quick glimpse as to whether the MRDS location corresponds to visible mine remains.
Mount Aetna Molybdenum Prospect MRDS details
Primary: Mount Aetna Molybdenum Prospect
Secondary: Monarch Molybdenum Property
Secondary: D & G Mining Property
Land ownership: National Forest
Note: the land ownership field only identifies whether the area the mine is in is generally on public lands like Forest Service or BLM land, or if it is in an area that is generally private property. It does not definitively identify property status, nor does it indicate claim status or whether an area is open to prospecting. Always respect private property.
Type: Located Claim
Owner Name: D. And G Mining Co.
Info Year: 1980
Owner Name: Monarch Molybdenum And Resources, 62 W. 4th So, Slc, Utah
Home Office: Utah
Info Year: 1980
Record Type: Site
Operation Category: Prospect
Operation Type: Unknown
Mining Method: Unknown
Discovery Year: 1962
Years of Production:
General Physiographic Area: Rocky Mountain System
Physiographic Province: Southern Rocky Mountains
Mineral Deposit Model
Comment (Geology): INITIAL INTEREST WAS CREATED IN AREA BY OUTCROP OF MOLY- BEARING, QTZ-PYRITE VEINS EXPOSED ON THE WEST FRINGE OF HOFFMAN PARK (SEE MAP ON FILE). THESE RANGE UP TO SEVERAL FEET IN WIDTH AND EXTEND AS FAULT-VEINS ALONG A NE-SW TREND FOR SEVERAL TENS TO SEVERAL HUNDRED OF FEET. LEAD, ZINC AND FLUORITE OFTEN ACCOMPANY THE MOLYBDENITE. IN OTHER INSTANCES MOLYBENITE OCCURS IN QTZ-PYRITE STRINGERS AND VEINLETS. PROPYLITIC ALTERATION IS RATHER GENERAL WITH LOCAT INTER- VALS OF MODERATE TO STRONG ARGILLIC AND SERICITIC ALTERATION PARTICULARLY ALONG CRUSHED & MINERALIZED FAULTS AND JOINT SYSTEMS IT IS POSSIBLE THAT PREVAILING, WEAKER PROPYLITIC ALTERA- TION INTERSECTED IN THESE HOLES REPRESENTS THE UPPER FRINGE OF DEEPER SERICITIC AND POTASSIC ALTERATION.
Reference (Geology): 1957. 110 PP.
Reference (Geology): CARPENTER, ROBERT H. SUMMARY REPORT ON MONARCH MOLYBDENUM
Reference (Geology): TARGET AREA, CHAFFEE COUNTY, COLORADO. CONFIDENTIAL REPT.
Reference (Geology): ON FILE AT IFOC. JUN 3, 1978. 6 PP.
Reference (Geology): DINGS, MC CLELLAND G., AND C. S. ROBINSON. GEOLOGY AND ORE
Reference (Geology): DEPOSITS OF THE GARFIELD QUAD., COLORADO. USGS PP 289.