Haida Mine (Hyda Mine; Mammoth Mine), Kasaan Peninsula, Prince of Wales Island, Ketchikan Mining District, Prince of Wales-Hyder Census Area, Alaska, USAi

Regional Level Types
Haida Mine (Hyda Mine; Mammoth Mine)	Mine
Kasaan Peninsula	Peninsula
Prince of Wales Island	Island
Ketchikan Mining District	Mining District
Prince of Wales-Hyder Census Area	Census Area
Alaska	State
USA	Country

Location: The Haida Mine is shown on the USGS 1:63,360-scale topographic map by name. It is about 0.5 mile north of the center of section 26, T. 72 S., R. 84 E. The geology and workings of the Haida Mine are shown on Plate 21 of Warner and others (1961).

Geology: Much of the area surrounding the Haida Mine is covered by glacial drift, alluvium, and dense vegetation. The rocks that are exposed consist mainly of fine-grained greenstone; very little intrusive igneous rock is known although there is a diorite dike about 500 feet southwest of the mine (Warner and others, 1961).

The deposit consists mostly of magnetite replacing greenstone. Locally the greenstone contains lenses of calcareous sedimentary rocks and is replaced by garnet and epidote. Pyrite and chalcopyrite are disseminated in the magnetite as tiny veinlets. Three small masses of copper-bearing magnetite are known. Samples of this material contain an average of about 33 percent iron, 0.88 percent copper, 0.03 ounce of gold per ton, and 0.2 ounce of silver per ton.

Development of the property began in 1905 and there was a small shipment of ore in 1907. Apparently, there has been no work on the property since 1908 (Roppel, 1991). The workings consist of several open cuts, pits, and trenches, a short adit, and two shafts. The workings and the geology of the deposit are shown on plate 21 of Warner and others (1961). The Haida Mine is one of many copper-iron deposits on the Kasaan Peninsula having similar geology and origin (Warner and others, 1961; Eberlein and others, 1983; Brew, 1996).

The rocks on the peninsula consist mainly of andesite ('greenstone' in much of the older literature) interbedded with about 25 percent sedimentary rocks comprising approximately equal amounts of limestone or marble, calcareous mudstone and sandstone, and graywacke and conglomerate. These units are part of the Luck Creek Breccia of Silurian and Devonian age, but many of the sedimentary units are similar to and probably grade into rocks of the Silurian and Ordovician, Descon Formation.

The bedded rocks are intruded by a profusion of Silurian or Ordovician dikes, sills, and irregular masses of porphyritic gabbro, basalt, andesite, diorite, dacite, and granodiorite. Near some of the deposits, these intrusions may make up 20 percent or more of the outcrop and usually are associated with the development of tactite and alteration of the greenstone. The area subsequently was intruded by several large Silurian or Ordovician plutons; they are mainly granodiorite but locally are diorite and gabbro.

The ore deposits are typically small and of irregular shape; often the ore bodies form lenses or mantos. Some of the deposits conform to the layering in the greenstone and sedimentary rocks.

The principal ore minerals are chalcopyrite, pyrite, and magnetite; hematite is often present and a little molybdenite occurs in some deposits. Most of the deposits are associated with tactite or skarn with varying amounts of actinolite, calcite, chlorite, garnet, diopside, epidote, and hornblende.
There was significant by-product silver and gold in the ore that was mined in the past, and the gold values in some deposits are high enough to have encouraged exploration in recent years.

Marble is more common in the deposits in the western part of the peninsula, where the gold values are generally higher as well (Wright and Wright, 1908; Wright, 1915; Warner and others, 1961; Myers, 1985; Bond, 1993; Maas and others, 1995).

Early interpretations of the ore deposits on the Kasaan Peninsula emphasize their contact metamorphic origin and their probable Mesozoic age (for example, Warner and others, 1961). However, recent radiometric dating and mapping indicate that the deposits formed in a Silurian or Ordovician, arc-related environment characterized by deposition of andesite and submarine sedimentary rocks that were intruded by swarms of dikes of varying composition, mineralized, and then intruded by large granodiorite plutons (Hedderly-Smith, 1999 [Inventory]).

The copper deposits of the Kasaan Peninsula were known to the Russians and the first claim was staked in 1867. Most of the production and development occurred from about 1900 to 1918, especially from 1905 to 1907, when copper prices soared and a smelter was built at Hadley on the north side of the Kasaan Peninsula. After World War I, copper supply exceeded demand, prices fell, and there has been no further copper production since 1918 (Wright, 1915; Warner and others, 1961; Roppel, 1991; Maas and others, 1995).

However, because of the intense and widespread mineralization on the peninsula, the area has repeatedly been re-examined for copper, iron, and gold, notably during WW II (Warner and others, 1961) and in the last several decades.

Workings: The workings consist of several open cuts, pits, and trenches, a short adit, and two shafts. The workings and the geology of the deposit are shown on plate 21 of Warner and others (1961).

Age: The deposit formed in a Silurian or Ordovician, submarine arc-related environment characterized by the deposition of volcanic and sedimentary rocks, the intrusion of swarms of dikes of diverse composition, and the emplacement of several large plutons.

Alteration: Greenstone and marble are replaced by magnetite, garnet, and epidote.

Production: Development of the property began in 1905 and there was a small shipment of ore in 1907. Apparently, there has been no work on the property since 1908.

Reserves: None.

Commodities (Major) - Ag, Au, Cu, Fe

Development Status: Yes; small

Deposit Model: Cu-Fe skarn (Cox and Singer, 1986; model 18d).

Other Databases

Link to USGS - Alaska:	CR052

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References