Unnamed

Occurrence in Alaska, United States with commodity Copper
Sections on this page
  1. Identification information
  2. Geographic coordinates
  3. Site location context
  4. Geographic areas
  5. Commodities
  6. Materials information
  7. Host and associated rocks
  8. Nearby scientific data
  9. Economic information about the deposit and operations
  10. Mining district
  11. Links to other databases
  12. Bibliographic references
  13. General comments
  14. Reporter information

Geologic information

Identification information

Deposit ID 10003111
MRDS ID A015643
Record type Site
Current site name Unnamed

Geographic coordinates

Geographic coordinates: -142.82338, 69.46991 (WGS84)
Relative position Accurate to within 1,524 meters (5,000 ft). Brosge' and Reiser, 1976, Locality 17 and Grybeck, 1977, p. 42, Locality 9.

Site location context

Political divisions (FIPS codes)

North Slope(Borough)

Alaska(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Demarcation Point B-4(quadrangle 1:63,360 scale)

Demarcation Point SW(quadrangle 1:100,000 scale)

Demarcation Point C(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Eastern Arctic(hydrologic accounting unit)

Arctic Alaska(hydrologic subregion)

Alaska(hydrologic region)

Federal lands

Arctic National Wildlife Refuge(National Wildlife Refuge)

National Wildlife Refuge FWS(Type of land area)

FWS(Federal land areas administered by FWS)

Geographic areas

Country State
United States Alaska

Commodities

Commodity Importance
Copper Primary

Materials information

Materials Type of material
Chalcopyrite Ore
Quartz Gangue

Host and associated rocks

  • Host or associated Host
    Rock type Volcanic Rock (Aphanitic) > Mafic Volcanic Rock

Nearby scientific data

(1) CPxwn

Economic information

Comments on the geologic information

  • Geologic Description = Chalcopyrite is present in quartz veins in mafic volcanic rocks.??These observations where likely made in rocks mapped as Precambrian volcaniclastic rocks of Redwacke Creek (Reiser and others, 1980). Potassium-argon dating of these rocks indicates Early Jurassic to Late Triassic ages which are not consistent with mapped field relations (Reiser and others, 1980).??Marker beds used in detailed mapping along the U.S.-Canada border consist of volcanicastic rocks that are Ordovician or Cambrian in age and likely stratigraphically equivalent to the Whale Mountain volcanics that contain a Late Cambrian fauna in their basal part (Kelley and others, 1992). Although the age of the volcaniclastic rocks of Redwacke Creek is uncertain and presumed to be Precambrian by Reiser and others (1980), work by Lane and others (1995) and Kelley and others (1992) raises the possibility that the volcaniclastic rocks that have reported to be mineralized are Cambrian to Ordovician in age: if so, the mineralization in them is not akin to mineralization in Precambrain volcanics in the Sadlerochit and Shublik Mountains.
  • Age = Unkown

Economic information about the deposit and operations

Development status Occurrence
Commodity type Metallic

Comments on exploration

  • Status = Inactive

Mining district

District name Canning

Reference information

Bibliographic references

Comments on the references

  • Primary Reference = Brosge' and Reiser, 1976.

General comments

Subject category Comment text
Deposit Model Name = Mafic-hosted Cu

Reporter information

Type Date Name Affiliation Comment
Reporter 13-SEP-1996 Powers, M.T. U.S. Geological Survey
Reporter 13-SEP-1996 Huber, D.F. U.S. Geological Survey
Reporter 13-SEP-1996 Kelley, J.S. U.S. Geological Survey

Beyond USGS

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

Authoritative Alaska resources

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