Little Squaw (Cosine

Past Producer in Alaska, United States with commodities Gold, Silver, Lead, Zinc
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 10001767
MRDS ID A012556
Record type Site
Current site name Little Squaw (Cosine
Alternate or previous names Sine, Crystal, Big Squaw Quartz, Parabola, Engineers Exploration Syndicate, Idaho-Alaska Corp.)

Geographic coordinates

Geographic coordinates: -148.19329, 67.55974 (WGS84)
Relative position The Little Squaw mine is approximately 3 miles south of the southeast end of Squaw Lake on the ridge between Little Squaw and Squaw Creeks; it is approximately 3 miles above Little Squaw Lake (sec. 34, T. 32 N., R. 3 W., of the Fairbanks Meridian). The mine location is shown by a mine symbol on the current topographic map, and the location is also shown on fig. 2 in Chipp (1970); the location is accurate within a 1/4-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-3(quadrangle 1:63,360 scale)

Chandalar N(quadrangle 1:100,000 scale)

Chandalar C(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Alaska(hydrologic region)

Geographic areas

Country State
United States Alaska

Commodities

Commodity Importance
Gold Primary
Silver Secondary
Lead Secondary
Zinc Critical Secondary

Materials information

Materials Type of material
Arsenopyrite Ore
Galena Ore
Gold Ore
Pyrite Ore
Sphalerite Ore
Scorodite Ore
Quartz Gangue

Alteration

  • (Local) Veins are oxidized generally to about 75 ft depth; the principal oxidation products include scorodite and limonite.

Mineral occurrence model information

Model code 273
USGS model code 36a
Deposit model name Low-sulfide Au-quartz vein
Mark3 model number 27

Host and associated rocks

  • Host or associated Host
    Rock type
    Stratigraphic age (youngest) Devonian

Nearby scientific data

(1) -148.19329, 67.55974

Economic information

Comments on the geologic information

  • Geologic Description = The vein on the Little Squaw property is one of several auriferous quartz veins in an area trending northeast from the heads of Tobin and Big creeks to Squaw and Little Squaw creeks. In general, most of the gold-bearing quartz veins in this area are in or near steeply-dipping, northwest-trending normal faults in Devonian quartz-muscovite schist, phyllite, and quartzite intruded by Devonian mafic sills and dikes (Chipp, 1970). The mafic intrusions have been metamorphosed to greenstone or greenschist. Major structural features include large-scale northeast-trending anticlines and synclines, northeast-trending thrusts, and the northwest-trending, high-angle cross faults. Most of the veins are less than 10 feet thick and are discontinuous, pinching out within a few hundred feet or less. The veins are composed principally of white crystalline to microcrystalline quartz, and their sulfide content is generally less than 5 percent. The principal sulfides (in relative order of abundance) are arsenopyrite, galena, sphalerite, and pyrite. Scorodite and limonite are commonly oxidation products. The quartz veins exhibit evidence of post-depositional shearing, indicating that the veins were emplaced before or during fault movement. The genesis of these gold deposits is still in question; various authors have hypothesized genetic links to a variety of felsic and mafic igneous rocks from which the gold was remobilized during metamorphism (Mertie, 1925; Boadway, 1933; Chipp, 1970; Dillon, 1982).? the Little Squaw vein is generally described as brecciated and recrystallized quartz containing free gold, pyrite, arsenopyrite, galena, and sphalerite. Ashworth (1983) described two generations of quartz: (1) 'barren' massive, white, coarsely crystalline quartz on the hanging wall that is generally devoid of sulfides; and (2) 'main stage' quartz in the footwall that contains smeared arsenopyrite and scorodite, and gold that forms blebs in the quartz and wires in the vugs. At the surface, the vein is 4 feet wide and dips approximately 80 degrees south. At the bottom of a 60-foot winze the dip flattens to 60 degrees south, and the vein reportedly consists of several quartz stringers with abundant arsenopyrite. The vein averages 67 inches wide and consists mostly of barren quartz except for an 8- to 12-inch-wide footwall zone which appears streaked and ribbony due to abundant pyrite and arsenopyrite. Native gold, as flakes or wires, is common at the Little Squaw. In 1933, the vein was described as having a proven length of 200 feet and a depth of 130 feet with a grade of $38.50 per ton over a 4-foot width ($20 per ounce of gold) (Boadway, 1933). In 1934, a weighted average value of 0.505 ounce of gold per ton was determined by using the lower of duplicate assays.
  • Age = Middle Cretaceous based on arguments by Dillon (1982) that the age of emplacement of the gold-bearing quartz veins of the Koyukuk and Chandalar districts was between the Neocomian metamorphism of the Devonian host rocks and their erosional unroofing and cooling in Albian time.
  • Age = Host rock is Devonian.

Economic information about the deposit and operations

Development status Past Producer
Commodity type Metallic

Comments on exploration

  • Status = Inactive

Mining district

District name Chandalar

Comments on the production information

  • Production Notes = Early production figures probably combined placer and lode production and indicate that approximately 65,000 oz were produced from lode and placer through 1995. Goldfarb and others (1997) reported that lode production was 17,000 oz and associated placer production was 46,000 oz.

Comments on the reserve resource information

  • Reserves = Various reserve figures have been published for the Chandalar area lode properties; these typically do not differentiate reserves for specific properties. Some of these figures are as follows: 12,000 tonnes grading 75 grams of gold per ton at the Mikado and Little Squaw (Nokleberg and others, 1996); an inferred lode reserve for the Chandalar district lodes of 45,000 tons with a grade of 2 ounces of gold per ton was reported as late as 1997 (Swainbank and others, 1998). Baggs and others (1988) reported measured reserves of 9,100 metric tons grading 58.70 grams of gold per metric ton as of 1980.

Comments on the workings information

  • Workings / Exploration = A 185-foot adit with a raise to the surface at 160 feet and a 60-foot winze at 135 feet were reported completed between 1910 and 1933 (Cobb, 1983, OFR 83-278; Stanford, 1931). A road from the Little Squaw to a mill site on Spring Creek was built in 1909-10. Milling 27 tons of ore from the Little Squaw mine at this mill produced an average recovery of $22 per ton at $20 per ounce of gold; the recovery probably was only the free gold. In 1912, a 3-stamp mill was brought to Big Creek to test the Little Squaw ore and used until 1915. Considerable development work has been conducted in the area beginning in 1960 and has been reported to include 1,500 feet of underground workings, surface trenching, and installation of a 100-ton-per-day mill. While most of this work probably focused on the nearby Mikado property, some of the work was probably performed on the Little Squaw property as well.

Reference information

Bibliographic references

Comments on the references

  • Primary Reference = Chipp, 1970

General comments

Subject category Comment text
Deposit Model Name = Low-sulfide Au-quartz veins (Cox and Singer, 1986; model 36a)
Deposit Other Comments = See also: Mikado Mine (CH045); there may be some confusion in the literature between Little Squaw and Mikado veins. The names Idaho-Alaska Corp. and Engineers Exploration Syndicate associated with this property refer to the transaction in 1932 in which the Idaho-Alaska Corp. took over the leases and options on various properties in the Chandalar district formerly held by the Engineers Exploration Syndicate. Other site names are names of claims on or near the mine.

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.