Sunrise Mine

Past Producer in Montrose county in Colorado, United States with commodities Copper, Silver, Manganese
Sections on this page
  1. Identification information
  2. Geographic coordinates
  3. Site location context
  4. Geographic areas
  5. Public Land Survey System information
  6. Commodities
  7. Materials information
  8. Alteration
  9. Host and associated rocks
  10. Nearby scientific data
  11. Geologic structures
  12. Controls for ore emplacement
  13. Economic information about the deposit and operations
  14. Mining district
  15. Land status
  16. Links to other databases
  17. Bibliographic references
  18. General comments
  19. Reporter information

Geologic information

Identification information

Deposit ID 10087937
MRDS ID D010957
Record type Site
Current site name Sunrise Mine
Alternate or previous names Patented Claim: Sunrise, Ms 16001
Related records 10265087

Geographic coordinates

Geographic coordinates: -108.92568, 38.40193 (WGS84)
Elevation 1920
Relative position 10.4 MILES N 77 W FROM URAVAN

Site location context

Political divisions (FIPS codes)

Montrose(county)

Colorado(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Roc Creek(quadrangle 1:24,000 scale)

Nucla(quadrangle 1:100,000 scale)

Moab(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Upper Dolores(hydrologic unit)

Upper Colorado-Dolores(hydrologic accounting unit)

Upper Colorado-Dolores(hydrologic subregion)

Upper Colorado(hydrologic region)

Geographic areas

Country State County
United States Colorado Montrose

Public Land Survey System information

Meridian Township Range Section Fraction State
New Mexico 048N 019W 23,24 E2 OF SE OF NE (23) Colorado

Comments on the location information

  • MINE LIES ON NE SIDE OF PARADOX VALLEY AND BELOW RIM OF CARPENTER RIDGE ; INFO FROM LAND.ST :1975

Commodities

Commodity Importance
Copper Primary
Silver Primary
Manganese Critical Tertiary

Comments on the commodity information

  • COPPER PITCH DEFINED AS MIXTURE OF TENORITE, MALACHITE, CHRYSOCOLLA, LIMONITE, AND MN OXIDE

Materials information

Materials Type of material
Bornite Ore
Chrysocolla Ore
Covellite Ore
Malachite Ore
Barite Gangue
Calcite Gangue
Limonite Gangue

Alteration

  • (Local) Oxidation Of Sulfides To Carbonates And Oxides

Host and associated rocks

  • Host or associated Host
    Rock type Sedimentary Rock > Clastic Sedimentary Rock > Sandstone
    Rock unit name Wingate Sandstone
    Rock description Wingate Sandstone

Nearby scientific data

(1) -108.92568, 38.40193

Economic information

Geologic structures

Type of structure Regional
Structure description Paradox Basin Fold And Fault Belt
Type of structure Local
Structure description Paradox Anticline, Paradox Valley Graben, Unnamed Fault

Controls for ore emplacement

  • Fault Cutting Poorly Cemented, Friable Sandstone

Economic information about the deposit and operations

Development status Past Producer
Commodity type Metallic
Deposit size Small
Significant No
Discovery year 1902
Discoverer John R. Galloway And A.C. Hamilton (Claimants)

Mining district

District name La Sal (Paradox Valley) District

Land status

Ownership category Private

Comments on the workings information

  • MINE DEVELOPED BY TWO TUNNELS: LOWER TUNNEL DRIVEN ALONG VEIN FOR AT LEAST 300 FT TO CAVED AREA; UPPER TUNNEL LIES 80 FT HIGHER THAN LOWER, DRIVEN ON VEIN FOR AT LEAST 50 FT TO CAVED AREA.

Reference information

Bibliographic references

General comments

Subject category Comment text
Deposit DEPOSITED ON NE RIM OF PARADOX VALLEY ALONG NORMAL FAULT TRENDING GENERALLY N 35 E, 80 SE AND CUTTING POORLY CEMENTED, FRIABLE VINGATE SANDSTONE. FAULT EXTENDS NE FROM BULGE IN INTRUSIVE CORE OF PARADOX VALLEY SALT ANTICLINE. IN UPPER LEVEL, ORE IS PRIMARILY MASSIVE CHALCOPYRITE WITH LESSER AMOUNTS OF INTERGGROWN CHALCOPYRITE-BORNITE-LUZONITE. ORE FROM LOWER LEVEL COMPOSED OF MASSIVE CHALCOCITE WHICH FILLS VEINS AND OPEN FRACTURES, WITH OR WITHOUT CALCITE-BARITE GANGUE. BOTH ORES OXIDIZED: CHALCOPYRITE ALTERED TO CU PITCH, MALACHITE, AND LIMONITE; CHALCOCITE ALTERED TO MALACHITE AND CU PITCH. MASSIVE CHALCOPYRITE APPEARS TO HAVE REPLACED SANSTONE NEAR FAULT; BRECCIATED AND REPLACED BY LATER CHALCOCITE AND THEN BY CU PITCH. ORE CHARACTERIZED BY NODULAR OR BOTRYOIDAL MASSES OF BORNITE WITH CONCENTRIC BANDS OF CHALCOPYRITE AND COLLOFORM INTERGROWTHS OF CHALCOPYRITE AND LUZONITE. CU PITCH SELECTIVELY REPLACES LUZONITE IN CENTERS OF COLLOFORM MASSES. BLUE AND WHITE MASSIVE CHALCOCITE ORE
Deposit FILLS VEIN AND REPLACES GANGUE (CALCITE), WITH SOME SMALL REPLACEMENT BY CHALCOPYRITE, COVELLITE, MALACHITE, AND CU PITCH.

Reporter information

Type Date Name Affiliation Comment
Reporter 01-NOV-1983 Schwochow, Stephen D. Colorado Geological Survey

Beyond USGS

Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.

External references

Authoritative Colorado resources

These are landing pages for further research — the state agencies don't currently expose per-mine deep links.