Rio Grande Claims

Occurrence in Hinsdale county in Colorado, United States with commodity Uranium
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. Host and associated rocks
  8. Nearby scientific data
  9. Geologic structures
  10. Economic information about the deposit and operations
  11. Mining district
  12. Land status
  13. Ownership information
  14. Links to other databases
  15. Bibliographic references
  16. General comments
  17. Reporter information

Geologic information

Identification information

Deposit ID 10014105
MRDS ID D010742
Record type Site
Current site name Rio Grande Claims
Alternate or previous names Unpatented Claims: Rio Grande 1-10

Geographic coordinates

Geographic coordinates: -107.38896, 37.76445 (WGS84)
Elevation 3011
Relative position 18.5 MILES S 13 W FROM LAKE CITY

Site location context

Political divisions (FIPS codes)

Hinsdale(county)

Colorado(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Pole Creek Mountain(quadrangle 1:24,000 scale)

Silverton(quadrangle 1:100,000 scale)

Durango(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Rio Grande Headwaters(hydrologic unit)

Rio Grande Headwaters(hydrologic accounting unit)

Rio Grande Headwaters(hydrologic subregion)

Rio Grande(hydrologic region)

Federal lands

Rio Grande National Forest(National Forest)

National Forest FS(Type of land area)

FS(Federal land areas administered by FS)

Geographic areas

Country State County
United States Colorado Hinsdale

Public Land Survey System information

Meridian Township Range Section Fraction State
New Mexico 041N 005W 35 S2 Colorado

Comments on the location information

  • ON SOUTH SIDE OF ROAD 2.1 MILES WEST OF RIO GRANDE RESERVOIR. ; INFO FROM LAND.ST :1977

Commodities

Commodity Importance
Uranium Primary

Analytical data

Result BACKGROUND RADIATION 0.05 MR/HR, RANGE 0.2 TO 0.3 MR/HR
Result STEVEN AND OTHERS' SAMPLE CONTAINED 0.13% U308

Host and associated rocks

  • Host or associated Associated
    Rock type Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite
    Rock unit name Eolus Granite;Ute Ridge Tuff
    Rock description Eolus Granite;Ute Ridge Tuff
    Stratigraphic age (youngest) Neoproterozoic
    Stratigraphic age (youngest) Mesoproterozoic
  • Host or associated Host
    Rock type Plutonic Rock > Granitoid > Granite
    Rock unit name Eolus Granite;Ute Ridge Tuff
    Rock description Eolus Granite;Ute Ridge Tuff
    Stratigraphic age (youngest) Precambrian
    Chronological age 1460
    Dating method U-Pb (zircon)
    Type of media Zircon
    Stratigraphic age (youngest) Precambrian
    Chronological age 1460
    Dating method K-Ar
    Stratigraphic age (youngest) Precambrian
    Chronological age 1466
    Dating method Rb-Sr

Nearby scientific data

(1) -107.38896, 37.76445

Economic information

Geologic structures

Type of structure Regional
Structure description San Juan Volcanic Field
Type of structure Local
Structure description Ute Creek Caldera, Lost Lake Caldera; Unnamed Fault

Economic information about the deposit and operations

Development status Occurrence
Commodity type Metallic
Deposit size Small
Significant No

Mining district

District name Rio Grande Reservoir Area

Land status

Ownership category National Forest

Ownership information

  • Type Owner
    Owner C. C. Wetherill

Comments on the workings information

  • BULLDOZER TRENCHING

Comments on development

  • LOCAL RANCHERS DISCOVERED RADIOACTIVE ANOMALY, BUT CONSIDERABLE TRENCHING FAILED TO SHOW ORE-GRADE MATERIAL, AND CLAIMS WERE ABANDONED.

Reference information

Bibliographic references

General comments

Subject category Comment text
Deposit ANOMALY WAS ABOVE-BACKGROUND RADIOACTIVITY IN FRACTURES(?) IN SMALL OUTCROP OF PRECAMBRIAN EOLUS GRANITE BENEATH THICK, INTRACALDERA UTE RIDGE TUFF IN UTE CREEK CALDERA. THICK INTRACALDERA SECTION OF TUFF AND THIN OUTFLOW SHEET SUGGEST SUBSIDENCE OF CALDERA CONCURRENT WITH ERUPTION. SUBSIDENCE RIM ON EAST NOTED BY STEVEN AND LIPMAN (1976), BUT LACK OF RING FRACTURE ON WEST SUGGESTS TRAP-DOOR COLLAPSE. LATER INTRUSIVES ALONG SOUTH RIM ON UTE CREEK AND ALONG WNW-TRENDING FAULT ACROSS RIVER VALLEY SW OF DEPOSIT. CALDERA IS TANGENTIAL ON EAST WITH LATER, BURIED LOST LAKE CALDERA.

Reporter information

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

Beyond USGS

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

Authoritative Colorado resources

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