Mamie Mine, Kasaan Peninsula, Prince of Wales Island, Ketchikan Mining District, Prince of Wales-Hyder Census Area, Alaska, USAi

Regional Level Types
Mamie 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

In 1998, Sealaska Corporation purchased the patented ground that covers the Mamie and Stevenstown mines and they hold the subsurface rights to the land around them.
Location: The location of the Mamie Mine is shown on the USGS 1:63,360-scale topographic map. It is near the southwest corner of section 24, T. 73 S., R. 86 E. The extensive surface and underground workings and the geology of the mine area are shown on plate 6 of Warner and others (1961).
Geology: The Mamie Mine is on the west flank of a syncline (Warner and others, 1961). The tactite and greenstone host rocks are complexly faulted and folded. The rocks are cut by numerous large, irregular masses and dikes of diorite, andesite, diorite porphyry, and dacite. The ore bodies are mainly in a contorted layer of magnetite 15 to 50 feet thick that is at least 500 feet long. Pyrite and chalcopyrite are disseminated through the magnetite and tactite. The ore bodies consisted of several irregular, copper-rich masses near the periphery of the magnetite bodies. The ore contained about 1.8 percent copper, 0.0204 ounce of gold per ton, and 0.126 ounce of silver per ton. The Mamie Mine consists of 3 glory holes, 3 adits, a shaft, and many drifts and crosscuts. There are about 5,000 feet of workings to a depth of about 200 feet. Details of the geology and the workings are shown on plate 6 of Warner and others (1961). The early history of the Mamie Mine is intimately tied to the 350-ton smelter at Hadley on the north side of Kasaan Peninsula (Wright, 1915; Warner and others, 1961; Roppel, 1991). The smelter, which operated intermittently from late 1905 to 1908, was built to process ore from the Mamie Mine that was delivered to it by an aerial tramway. In 1908, however, the smelter closed due to low copper prices and to the generally marginal economics of small copper smelters. In 1913, Granby Consolidated Mining Company acquired the Mamie and Stevenstown mines and shipped ore until 1918. There has been no production since. The Mamie Mine produced over $1,000,000 in copper ore from 1905 to 1918. Warner and others (1961) and Wright and Tolonen (1947) estimate that the Mount Andrew (CR071), Stevenstown, and Mamie (CR073) mines have a combined resource of 2,684,000 long tons of ore, but indicate that about 80 percent of that is at the Mount Andrew Mine and most of the rest is at the Mamie Mine. This material has an average grade of 47.8 percent iron, 0.32 percent copper, and 0.011 ounce of gold and 0.55 ounce of silver per ton (Wright and Tononen, 1947). The Mamie 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 Mamie Mine consists of 3 glory holes, 3 adits, a shaft, and many drifts and crosscuts. There are about 5,000 feet of workings to a depth of about 200 feet. Details of the geology and the workings are shown on plate 6 of Warner and others (1961). The early history of the Mamie Mine is intimately tied to the 350-ton smelter at Hadley on the north side of the Kasaan Peninsula (Wright, 1915; Warner and others, 1961; Roppel, 1991). The smelter, which operated intermittently from late 1905 to 1908, was built to process ore from the Mamie Mine that was delivered to it by an aerial tramway. In 1908, however, the smelter closed due to low copper prices and to the generally marginal economics of small copper smelters. In 1913, Granby Consolidated Mining Company acquired the Mamie and Stevenstown mines and shipped ore until 1918. There has been no production since. The Mamie Mine produced over $1,000,000 in copper ore from 1905 to 1918.
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: Pervasive development of tactite.
Production: The Mamie Mine produced over $1,000,000 in copper ore from 1905 to 1918.
Reserves: Warner and others (1961) and Wright and Tolonen (1947) estimate that the Mount Andrew (CR071), Stevenstown, and Mamie (CR073) mines have a combined resource of 2,684,000 long tons of ore, but indicate that about 80 percent of that is at the Mount Andrew Mine and most of the rest is at the Mamie Mine. This material has an average grade of 47.8 percent iron, 0.32 percent copper, and 0.011 ounce of gold and 0.55 ounce of silver per ton (Wright and Tononen, 1947).

Commodities (Major) - Cu, Fe; (Minor) - Ag, Au
Development Status: Yes; medium
Deposit Model: Cu-Fe skarn (Cox and Singer, 1986; model 18d).

Other Databases

Link to USGS - Alaska:	CR073

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References