Unnamed Near Kushneahin Lake

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

Geologic information

Identification information

Deposit ID 10003643
MRDS ID A106407
Record type Site
Current site name Unnamed Near Kushneahin Lake

Geographic coordinates

Geographic coordinates: -133.50382, 56.52667 (WGS84)
Relative position SEE LOCATION COMMENTS

Site location context

Political divisions (FIPS codes)

Wade Hampton(Census area)

Alaska(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Petersburg C-5(quadrangle 1:63,360 scale)

Port Alexander NE(quadrangle 1:100,000 scale)

Petersburg(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Central Southeast Alaska(hydrologic accounting unit)

Southeast Alaska(hydrologic subregion)

Alaska(hydrologic region)

Federal lands

Tongass National Forest(National Forest)

National Forest FS(Type of land area)

FS(Federal land areas administered by FS)

Geographic areas

Country State
United States Alaska

Comments on the location information

  • LOCATION GIVEN ABOVE IS APPROXIMATELY THE CENTER OF A VIVID YELLOW-ORANGE ALTERED ZONE ON SOUTHERN KUPREANOF ISLAND THAT EXTENDS FOR AT LEAST 1 KM ALONG AN UNNAMED CREEK IN SECTION 2, T. 62 S., R. 76 E., AND SECTION 35, T. 61 S., R. 76 E.. SEE ALSO PE018 FOR A CLAIM BLOCK CENTERED ON THIS ALTERED ZONE. LOCALITY 24 OF GRYBECK, BERG, AND KARL (1984).

Commodities

Commodity Importance
Copper Primary
Molybdenum Primary

Nearby scientific data

(1) -133.50382, 56.52667

Economic information

Ore body information

  • General form SEE DEPOSIT DESCRIPTION COMMENTS

Economic information about the deposit and operations

Development status Occurrence
Commodity type Metallic
Significant No

Comments on exploration

  • Status = Inactive

Mining district

District name Kupreanof

Comments on the production information

  • NONE

Comments on the workings information

  • NONE OTHER THAN PROBABLE EXAMINATION BY VARIOUS INDUSTRY GEOLOGISTS WHO HAVE WORKED IN THE AREA.

Reference information

Bibliographic references

  • Deposit

    Grybeck, D. J., Berg, H. C., and Karl, S. M., 1984, Map and description of the mineral deposits in the Petersburg and eastern Port Alexander quadrangles: U.S. Geological Survey Open-File Report 84-837, 86 p., 1 sheet, scale 1:250,000.

  • Deposit

    Brew, D. A., Ovenshine, A. T., Karl, S. M., and Hunt, S. J., 1984, Preliminary reconnaissance geologic map of the Petersburg and parts of the Port Alexander and Sumdum 1:250,000 quadrangles, southeastern Alaska: U. S. Geological Survey Open-File Report 84-405, 43 p., 2 sheets, scale 1:250,000.

  • Deposit

    Brew, D.A., 1997, Reconnaissance geologic map of the Petersburg C-5 quadrangle, southeastern Alaska: U. S. Geological Survey Open-File Report 97-156-K, scale 63,360, one sheet, 18 p. pamphlet.

General comments

Subject category Comment text
Deposit EXTENSIVE VIVID EXPOSURES OF YELLOW-ORANGE ALTERED RHYOLITE, RHYOLITE TUFF, AND RHYOLITIC GLASS OF QUATERNARY OR TERTIARY AGE OUTCROP IN CREEK BED AND BLUFFS FOR AT LEAST ONE-HALF MILE (BREW AND OTHERS, 1984; BREW, 1997 [OF 97-156-K]). BRIEFLY EXAMINED BY THE USGS IN 1982 AND 1996. DISSEMINATED PYRITE IS PRESENT LOCALLY BUT NO OBVIOUS SIGNS OF CU, MO, OR OTHER ORE MINERALS. SEVERAL GRAB SAMPLES OF THE MOST-ALTERED RHYOLITE AND ASSOCIATED ROCKS SHOW 5 PPM OR LESS CU AND MO. THE PYRITE AND HOST ROCKS ARE PART OF A LARGE FELSIC IGNEOUS SYSTEM. THE SURROUNDING AREA IS HEAVILY WOODED BUT AERIAL RECONNAISSANCE SHOWS WIDESPREAD EVIDENCE OF SIMILAR IRON-STAINED ZONES OVER AN AREA AT LEAST SEVERAL MILES IN DIAMETER. ALTHOUGH NO OBVIOUS MINERALIZATION HAS BEEN FOUND TO DATE, THE SITE IS INCLUDED BECAUSE THIS ALTERED ZONE IS SO LARGE AND SO PROMINENT AND IT INDICATES THE PRESENCE OF A VERY LARGE FELSIC HYDROTHERMAL SYSTEM.

Reporter information

Type Date Name Affiliation Comment
Reporter 01-NOV-1998 Berg, H. C. (Grybeck, D. J.) 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.