Quadrangle map, 1:250,000-scale | AN |
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Quadrangle map, 1:63,360-scale | D-6 |
Latitude | 61.825 |
Longitude | -149.241 |
Nearby scientific data | Find additional scientific data near this location |
Location and accuracy | Marked with adit symbol and labeled 'Fern Mine' on the Anchorage D-6 1:63,360-scale topographic map, at headwaters of Archangel Creek. Accurate within 400 ft. This is locality 19 of Cobb (1972) and locality 16 of MacKevett and Holloway (1977). |
Geologic descriptionQuartz veins and stringers in shear zone cutting comminuted and kaolinized tonalite of the Late Cretaceous Willow Creek Pluton, a zoned pluton: the outer part consists of hornblende quartz diorite and lesser hornblende tonalite; the core consists of hornblende-biotite granodiorite, and lesser hornblende-biotite quartz monzodiorite and biotite quartz monzonite. The main vein is as wide as 18 ft and is made up of quartz, gouge, and altered tonalite (Ray, 1954). Ore concentrated at intersections of main vein and smaller cross veins. The stringer veins are displaced and broken up into distinct blocks by major post-mineralization faults. Wall-rock alteration within a few inches of the veins is intense, but seldom extends more than 10 to 12 inches beyond the quartz filling (Ray, 1954). The wall rock has been intensely altered with ankerite, kaolinite, and secondary quartz (Ray, 1933). Metallic minerals include pyrite, arsenopyrite, tetrahedrite, galena, nagyagite, gold, and sparse scheelite (Ray, 1933). Assay of channel samples indicate a 12 ft sample of quartz stringers in altered country rock has 1.0 oz/ton Au, 8 to 12 inches of massive quartz yielded 0.45 oz/ton Au, and 2.5 ft zone of quartz and altered country rock show 2.3 oz/ton Au (Ray, 1933). | |
Geologic map unit | (-149.243209478125, 61.8244724617165) |
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Mineral deposit model | Low-sulfide Au-quartz veins (Cox and Singer, 1986; model 36a) |
Mineral deposit model number | 36a |
Age of mineralization | Late Cretaceous or younger; veins cut the Late Cretaceous Willow Creek Pluton. |
Alteration of deposit | Wall rock has been intensely altered with ankerite, kaolinite, and secondary quartz (Ray, 1933). Wall-rock alteration within a few inches of the veins is intense, but seldom extends more than 10 to 12 inches beyond the quartz filling (Ray, 1954). |
Workings or exploration |
An adit was driven 40 ft to vein and then 56 ft along vein in attempt to find the ore shoot exposed at surface (Capps, 1919). By 1920, the adit was driven 300 ft (Chapin, 1920). A mill was installed, and both mine and mill operated in 1922 (Brooks and Capps, 1924). The first gold from the mine was produced in 1922. The Fern Gold Mining Company milled its last ore in 1928. Explored by more than 4,000 ft of underground workings plus stopes on 2 levels by 1931 (Ray, 1933). Workings extended beneath a tunnel of the adjoining Talkeetna mine (ARDF number AN025), but do not connect. In 1931, Thomas McDougal leased the property and worked the mine as the Fern Gold Leasing Company (Stoll, 1997). Mining stopped in 1941 and McDougal gave up the lease in 1945. During the time from 1931 to 1941, two new levels of adits were driven with over 3,000 ft aggregate length. In 1945, A.G. Dodson obtained a lease for the property and operated the mine until his death in late 1950. A mill and cyanide plant were present on the property, however the mill was destroyed by fire in 1946. A new mill was completed in 1948. Assay of channel samples indicate a 12 ft sample of quartz stringers in altered country rock has 1.0 oz/ton Au, 8 to 12 inches of massive quartz yielded 0.45 oz/ton Au, and 2.5 ft zone of quartz and altered country rock show 2.3 oz/ton Au (Ray, 1933). |
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Indication of production | Yes; medium |
Production notes | The Fern mine, under McDougal (1931-1941), had an estimated production worth over $1,000,000 (Ray, 1954). Stoll (1997) estimates that from the Fern Gold Mining Company's first gold shipments, in 1922, into 1950 under Dodson, the Fern vein yielded roughly 44,000 ounces of gold. In aggregate gold recovery, the Fern lode is the district's fourth most important, after Lucky Shot-War Baby (ARDF numbers AN002 and AN003), Independence (ARDF number AN001), and Gold Bullion (ARDF number AN004). |
Additional commentsMarmot and Bartholf-Isaacs prospects probably all became part of Fern property. Capps (1915) reports assessment work at Bartholf-Issacs prospect in 1914 and Chapin (1921) reports work during the winter of 1919-1920 at Marmot prospect. This is the last references to these two prospects in the literature. |