Venus

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

Geologic information

Identification information

Deposit ID 10094023
MRDS ID A012153
Record type Site
Current site name Venus

Geographic coordinates

Geographic coordinates: -149.32333, 67.62972 (WGS84)
Relative position The Venus prospect is centered about 3 1/4 miles north-northwest along Big Spruce Creek from its confluence with the Bettles River (NW1/4 sec. 3 and NE1/4 sec. 4, T. 32 N., R. 8 W. and sec. 34, T. 33 N., R. 8 W., of the Fairbanks Meridian) and 11 miles east-northeast of Sukakpak Mountain. The Venus prospect is part of a large claim group (now inactive?) that also encompasses the Victor (CH064) and Eva (CH063) prospects. The location of the reference point is accurate within a 1/2-mile radius.

Site location context

Political divisions (FIPS codes)

Yukon-Koyukuk(Census area)

Alaska(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

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

Chandalar N(quadrangle 1:100,000 scale)

Chandalar(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Alaska(hydrologic region)

Federal lands

Doyon, Limited(ANCSA Region)

ANCSA Region NTVPIC(Type of land area)

NTVPIC(Federal land areas administered by NTVPIC)

Geographic areas

Country State
United States Alaska

Commodities

Commodity Importance
Silver Primary
Gold Primary
Copper Primary
Molybdenum Secondary

Materials information

Materials Type of material
Bornite Ore
Chalcopyrite Ore
Magnetite Ore
Molybdenite Ore
Pyrite Ore
Epidote Gangue

Alteration

  • (Local) Extensive propylitic alteration, along with restricted areas of sericitic to potassic alteration in meta-intrusives, and hornfels and skarn in adjacent calcareous rocks.

Mineral occurrence model information

Model code 53
USGS model code 17
Deposit model name Porphyry Cu
Mark3 model number 4
Model code 58
USGS model code 18a
Deposit model name Porphyry Cu, skarn-related
Mark3 model number 9

Host and associated rocks

  • Host or associated Associated
    Rock type Plutonic Rock > Mafic Intrusive Rock > Diorite
  • Host or associated Host
    Rock type Plutonic Rock > Mafic Intrusive Rock > Diorite

Nearby scientific data

(1) -149.32333, 67.62972

Economic information

Comments on the geologic information

  • Geologic Description = The Venus prospect is generally described as a porphyry copper deposit associated with Cu-Au-Ag skarns (Cobb and Cruz, 1983, Nokleberg and others, 1987). The skarn occurrences at Venus, along with a number of other skarn prospects in the Chandalar district, were described in general by Newberry and others (1986), who noted that many of them exhibit both prograde and retrograde mineral assemblages and that their mineralogy, mineralization, and alteration classify them as continental-margin, porphyry-related copper skarns. Nicholson (1990) noted that some workers have suggested that some of the prospects in the area may have volcanogenic affinities. The local geology at Venus is described by Ventures Resource Corporation (1998) as an elongated, altered and foliated granodiorite pluton bounded on the east by overthrust Skajit Limestone and on the west by Skajit Limestone and gray phyllite, felsic calc-schist, and chloritic schist.? the porphyry mineralization at Venus consists of disseminations and fracture fillings of pyrite, chalcopyrite, and minor molybdenite in schistose Devonian meta-granodiorite porphyry. The meta-granodiorite porphyry is extensively propylitically altered and pyritized (2 percent to 3 percent pyrite), along with restricted zones of sericitic to potassic alteration. The intrusive hosted mineralization grades approximately 0.1 percent to 0.2 percent Cu and generally less than 0.01 ounce of gold per ton (Ventures Resource Corporation, 1998). A hand specimen described by Newberry and others (1986) as porphyry contains quartz, sericite, pyrite, chalcopyrite, chlorite, and molybdenite. An analysis of the hand specimen returned 0.38 percent Cu, 1 ppm Ag, less than 0.1 ppm Au, 0.002 percent Zn, and 0.001 percent Pb.? the skarn mineralization is massive pyrite-chalcopyrite. The skarns are in Devonian Skajit Limestone and calc-schists adjacent to, and as xenoliths within, the meta-intrusives. The skarns are principally garnet-magnetite-diopside bodies displaying retrograde vein and replacement epidote-amphibole-chlorite-calcite-quartz. Mineralization in the skarns is variable but generally runs 1.5 percent to 6 percent Cu, less than 0.01 ounce of gold per ton, and as much as about 1 ounce of silver per ton (Newberry and others, 1986; Nicholson, 1990; Ventures Resource Corporation, 1998). The mineralogy of a skarn hand specimen described by Newberry and others (1986) includes garnet, magnetite, chalcopyrite, pyrite, epidote, actinolite, serpentine and talc. An analysis of this hand specimen returned 2.0 percent Cu, 14.5 ppm Ag, 0.14 ppm Au, 0.014 percent Zn, and 0.002 percent Pb.
  • Age = Devonian based on reported Early Devonian Pb/Pb zircon ages from the associated Baby Creek batholith and Horace Mountain plutons (Dillon and others, 1996).

Economic information about the deposit and operations

Development status Prospect
Commodity type Metallic

Comments on exploration

  • Status = Active

Mining district

District name Koyukuk

Comments on the reserve resource information

  • Reserves = Reserve estimates made on very limited data for the porphyry mineralization range from 300,000 tons of 0.3 percent Cu (Nicholson, 1990) to a potential resource of 495 million pounds of Cu (Ventures Resource Corporation, 1998). In general, the Cu deposits discovered to date in the Chandalar quadrangle have been characterized by relatively small tonnages in high-grade deposits and low grades in disseminated deposits.

Comments on the workings information

  • Workings / Exploration = Initial claim block was staked from 1967 to 1970 by Bear Creek Mining (Kennecott). Their exploration programs from 1970 to 1974, directed toward evaluating the porphyry copper potential, included 2,465 feet of diamond drilling in five diamond drill holes (all in meta-intrusives) in 1973-1974. Information posted on the Ventures Resource Corporation website (URL http://www.venturesresource.com/) in 1998 describes a 2,000-foot x 7,000-foot geochemical soil survey grid on the property with Cu values greater than 100 ppm and maximum values greater than 2,000 ppm, extending over several thousand feet (Ventures Resource Corporation, 1998). Reconnaissance exploration was reported in 1983, 1990-1991, and 1996.

Reference information

Bibliographic references

Comments on the references

  • Primary Reference = Ventures Resource Corporation, 1998

General comments

Subject category Comment text
Deposit Model Name = Porphyry Cu and Cu porphyry skarn-related deposits (Cox and Singer, 1986; models 17 and 18a)
Deposit Other Comments = See also: Victor (CH064), Evelyn Lee (CH059), Eva (CH063), and Geroe Creek (CH053). Most of the publications describing this area provide a combined description of the Venus-Victor-Eva prospects. The land (and presumably the original claims) have been acquired by Doyon, Limited via its Alaska Native Claims Settlement Act selections. Alaska Kardex No. 031-53D (Kardex is a card file mining claim information system located at the State of Alaska DNR Public Information Center in Fairbanks).

Reporter information

Type Date Name Affiliation Comment
Reporter 17-NOV-1999 J.M. Britton 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.