The Wager Gulch Limonite Deposit is a iron mine located in Hinsdale county, Colorado at an elevation of 10,699 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.
Mine Info
Elevation: 10,699 Feet (3,261 Meters)
Commodity: Iron
Lat, Long: 37.88861, -107.36111
Map: View on Google Maps
Wager Gulch Limonite Deposit MRDS details
Site Name
Primary: Wager Gulch Limonite Deposit
Commodity
Primary: Iron
Location
State: Colorado
County: Hinsdale
District: Carson District
Land Status
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.
Holdings
Not available
Workings
Not available
Ownership
Not available
Production
Not available
Deposit
Record Type: Site
Operation Category: Past Producer
Operation Type: Unknown
Year First Production: 1875
Year Last Production: 1875
Discovery Method: Ore-Mineral In Place
Years of Production:
Organization:
Significant: N
Deposit Size: S
Physiography
General Physiographic Area: Rocky Mountain System
Physiographic Province: Southern Rocky Mountains
Mineral Deposit Model
Not available
Orebody
Not available
Structure
Type: R
Description: San Juan Volcanic Field, San Juan Depression
Type: L
Description: San Juan-Uncompahgre Calderas, Lake City Caldera, Carson Volcano
Alterations
Alteration Type: L
Alteration Text: Oxidation Of Fe Sulfide To Limonite
Rocks
Name: Alluvium
Role: Host
Age Type: Host Rock
Age Young: Holocene
Analytical Data
Not available
Materials
Ore: Limonite
Comments
Comment (Deposit): LIMONITE OCCURS AS VARIETY OF YELLOW, RED, AND BROWN HYDROUS FE OXIDES IN BOG DEPOSIT STILL BEING FORMED. DEPOSIT VARIES IN COMPOSITION, TEXTURE, AND FE CONTENT. FE APPARENTLY TAKEN INTO SOLUTION BY METEORIC WATERS THAT PASS THROUGH OXIDIZING FE-SULFIDE-BEARING ROCKS AND VEINS. WATER ISSUES FROM BASE OF CLIFFS AS FERRUGINOUS SPRINGS FROM WHICH FE IS PRECIPITATED AS LIMONITE BOG IRON IN SWAMPY GULCH BOTTOM.
Comment (Workings): SURFACE CUT
Comment (Location): DEPOSIT REPORTEDLY LIES ABOVE FORKS OF WAGER GULCH ABOUT ONE MILE BELOW CARSON. ELEV AND LAT-LONG GIVEN ARE FOR CONFLUENCE OF WAGER GULCH AND WEST FORK IN NE NE SEC. 24. ; INFO FROM LAND.ST :1977
Comment (Development): SMALL AMOUNT OF BOG IRON ORE WAS MINED IN LATE 1800S FOR USE AS NONFERROUS SMELTER FLUX IN LAKE CITY.
References
Reference (Deposit): HARRER, C.M., AND TESCH, W.J., JR., 1959, RECONNAISSANCE OF IRON OCCURRENCES IN COLORADO: USBM IC-7918, P. 44.
Reference (Deposit): LIPMAN, P.W., 1976, GEOLOGIC MAP OF THE LAKE CITY CALDERA AREA, WESTERN SAN JUAN MOUNTAINS, SOUTHWESTERN COLORADO: USGS MAP I-962.
Reference (Deposit): LARSEN, E.S., 1911, THE ECONOMIC GEOLOGY OF CARSON CAMP, HINSDALE COUNTY, COLORADO: USGS BULL. 470, P. 30-38.
Colorado Mining Photos
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