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Clipper

Past Producer in Alaska, United States with commodities Gold, Antimony
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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. Host and associated rocks
  9. Nearby scientific data
  10. Economic information about the deposit and operations
  11. Mining district
  12. Links to other databases
  13. Bibliographic references
  14. General comments
  15. Reporter information

Geologic information

Identification information

Deposit ID 10107550
MRDS ID A015267
Record type Site
Current site name Clipper
Alternate or previous names Lounsbury
Related records 10257487

Geographic coordinates

Geographic coordinates: -148.00684, 64.8666 (WGS84)
Relative position The Clipper mine is located in the SE1/4SW1/4 sec. 32, T. 1 N., R. 2 W., Fairbanks Meridian, near the head of Eva Creek. It is approximately 1.4 miles north-northeast of the town of Ester at an elevation of about 1,100 feet. It is included in locality 14 of Cobb (1972 [MF 410]).

Site location context

Political divisions (FIPS codes)

Fairbanks North Star(Borough)

Alaska(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Fairbanks D-3(quadrangle 1:63,360 scale)

Fairbanks N(quadrangle 1:100,000 scale)

Fairbanks C(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Alaska(hydrologic region)

Geographic areas

Country State
United States Alaska

Commodities

Commodity Importance
Gold Primary
Antimony Critical Secondary

Materials information

Materials Type of material
Arsenopyrite Ore
Gold Ore
Stibnite Ore

Alteration

  • (Local) Wall-rock silicification extends at least 10 inches into both the footwall and hanging wall of the vein (Bundtzen and others, 1982 [OFR 157]). Later hydrothermal silica vein injection was accompanied by the emplacement of free gold with arsenopyrite, stibnite, and boulangerite.

Host and associated rocks

  • Host or associated Host
    Rock type Metamorphic Rock > Schist > Mica Schist
    Rock unit name Fairbanks-Birch Creek Schist;Fairbanks-Birch Creek Schist;Fairbanks-Birch Creek Schist;Fairbanks-Birch Creek Schist
    Rock description Fairbanks-Birch Creek Schist;Fairbanks-Birch Creek Schist;Fairbanks-Birch Creek Schist;Fairbanks-Birch Creek Schist

Nearby scientific data

(1) -148.00684, 64.8666
ListMap

Economic information

Comments on the geologic information

  • Geologic Description = The Clipper mine consists of gold-bearing quartz-sulfide zones along a north-northwest-trending, nearly vertical fracture that cuts foliation and compositional banding in polymetamorphic schist and quartzite (Bundtzen and others, 1982 [OFR 157]). The 1- to 2-inch wide vein is laterally displaced 2 to 11 feet by seven cross-cutting faults that strike N. 50-85 E. and dip 35-65 N.? In 1982, Bundtzen and others (1982 [OFR 157]) spent seven days mapping approximately 800 feet of underground workings at the Clipper gold mine, and the following is a summary of their findings. Bedrock in the area is Fairbanks Schist that consists of four lithologic units: chlorite-muscovite schist, quartz-mica schist with quartzite bands, a porphyroblastic felsdpathic schist, and a bleached, garnetiferous biotite-muscovite schist. The more quartzose rocks form blocky, resistant walls in mine workings, whereas the more micaceous rocks form irregular walls, cavities, and open spaces. In thin section, the schist is composed of as much as 50 percent white mica, 30 to 65 percent interlocking quartz grains, minor albitized plagioclase, chlorite and very minor garnet. tourmaline, sphene and zoisite inclusions. The mineral assemblages suggest that a prograde, upper greenschist facies metamophic event (garnet plus plagioclase plus biotite plus white mica) has been overprinted by a lower grade metamorphic event (chlorite plus albite plus zoisite).? Structurally, an early crenulation-kink-band deformation (F1) consistently records a northwest-southeast stress field that plunges to the northeast. During a later F2 event, the rocks were gently folded into synclines and anticlines with amplitudes ranging from 6 to 50 feet. A major, north-northwest-trending, steeply dipping, joint set cuts the layered rocks underground. These structural features apparently served as primary channels for ore fluids; the majority of veins in the drift and stopes are parallel to these joint sets. A few prominent, but unmineralized, steeply dipping joints and fractures strike N. 25-35 W.? the fault above the Clipper vein varies from N. 5 E. to N. 25 W. and generally trends N. 5-10 W., almost normal to regional structure. The mineralized shears dip from 65 SW. to vertical, and only rarely does the fault system associated with the veins dip steeply to the northeast. The vein system south of an old seismograph station consists of thin, gold-bearing veinlets, 1 to 3 inches wide in 2- to 4-foot-wide, horse-like stockwork zones. Within these zones, handsorting produced very high grade ore; one 3-inch channel sampled from the Bonanza winze assayed 26.09 ounces of gold per ton. North of the seismograph station, the vein occupies a significantly wider (4 to 24 inches) zone in single or multiple splays. Assays from eight channel samples along two major sections of ore averaged 0.87 ounce of gold per ton over an average width of 12 inches. The last structural event in the Clipper mine
  • Geologic Description = is represented by a series of faults that trend N. 50-85 E. and dip 35-55 N.; they offset the Clipper vein system laterally from 2 to 11 feet.? This deposit is a hydrothermal vein; massive, fractured to euhedral, crystalline quartz constitutes greater than 95 percent of the vein material. Wall-rock silicification was followed by at least two stages of silica vein injection; the last was accompanied by free gold and disseminated to rare massive arsenopyrite, stibnite, and boulangerite. In one specimen, free gold is intimately associated with fine needles of boulangerite that apparently intrude arsenopyrite. Free gold observed in hand specimens occurs as small angular segregations or thin plates averaging about 0.5 mm in length. Select samples showed masses of free gold as much as a quarter of an inch in diameter. One sample of gold was 768 fine and had silver as the major impurity. Other samples analyzed ranged from 682.9 to790.4 fine (Glover, 1950).? According to G.P. Lounsbury, the mine owner at the time of Bundtzen's visit in 1982, the most productive years were 1937-42 when approximately 1,400 ounces of gold worth about $50,000 were recovered from an unknown amount of high-grade, hand-sorted ore (Bundtzen and others, 1982 [OFR 157, p. 3]). Investigations by Hill (1933) and Pilgrim (1931, 1932, 1933) indicated that by 1932, a 235- to 250-foot drift had been driven to explore a 1- to 8-inch-thick, steeply dipping vein trending N. 10-15 E. Most of these workings were mined by hand by the owner, Lloyd Lounsbury (D. Wietchy, oral commun., 2000). By 1982, there was at least 800 feet of underground workings but there is no record of recent production (Bundtzen and others, 1982 [OFR 157]).
  • Age = Auriferous quartz veins cut Fairbanks Schist; these are considered to be pre-Devonian and probably Proterozoic in age (Newberry and others, 1996).

Economic information about the deposit and operations

Development status Past Producer
Commodity type Metallic

Comments on exploration

  • Status = Inactive

Mining district

District name Fairbanks

Comments on the production information

  • Production Notes = There is no record of production prior to 1932. In 1937, nineteen tons of ore averaging 0.8 ounce of gold per ton was milled, and in 1938, twenty-five tons of ore of the same grade was milled (Reed, 1938). According to G.P. Lounsbury, the mine owner at the time of Bundtzen's visit in 1982, the most productive years were 1937-42, when approximately 1,400 ounces of gold worth $50,000 were recovered from an unknown amount of high-grade, hand-sorted ore (Bundtzen and others, 1982 [OFR 157, p. 3]).

Comments on the workings information

  • Workings / Exploration = Investigations by Hill (1933) and Pilgrim (1930, 1931, 1932 indicate that by 1932, a 235- to 250-foot drift had been driven to explore a 1- to 8-inch thick, steeply dipping vein trending N. 10-15 E. Most of these workings were mined by hand by the owner at that time, Lloyd Lounsbury (D. Wietchy, oral commun., 2000). In 1982, Bundtzen and others (1982 [OFR 157]) spent seven days mapping approximately 800 feet of underground workings at the mine. It was unclear to Bundtzen and his colleagues if the early work reported by Hill and Pilgrim were part of the workings accessible to them or were part of older, caved workings on the hillside about 60 vertical feet above the portal open to them.

Reference information

Bibliographic references

Comments on the references

  • Primary Reference = Bundtzen and others, 1982 (OFR 157)

General comments

Subject category Comment text
Deposit Model Name = Schist-hosted gold-quartz vein

Reporter information

Type Date Name Affiliation Comment
Reporter 31-JUL-2001 J.R. Guidetti Schaefer Avalon Development Corporation
Reporter 31-JUL-2001 C.J. Freeman Avalon Development Corporation

Beyond USGS

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

Maps centered on this site

Authoritative Alaska resources

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