Unnamed (in headwaters of Grubstake Creek)

The Unnamed (in headwaters of Grubstake Creek) is a copper and gold mine located in Alaska.

About the MRDS Data:

All mine locations were obtained from the USGS Mineral Resources Data System. The locations and other information in this database have not been verified for accuracy. It should be assumed that all mines are on private property.

Mine Info

Satelite View

MRDS mine locations are often very general, and in some cases are incorrect. Some mine remains have been covered or removed by modern industrial activity or by development of things like housing. The satellite view offers a quick glimpse as to whether the MRDS location corresponds to visible mine remains.

Site Name

Primary: Unnamed (in headwaters of Grubstake Creek)

Commodity

Primary: Copper
Primary: Gold
Secondary: Zinc
Secondary: Lead
Secondary: Iron

Location

State: Alaska
District: Chistochina

Land Status

Not available

Holdings

Not available

Workings

Not available

Ownership

Not available

Production

Not available

Deposit

Record Type: Site
Operation Category: Prospect
Operation Type: Unknown
Years of Production:
Organization:
Significant:

Physiography

Not available

Mineral Deposit Model

Model Name: Porphyry Cu-Au

Orebody

Not available

Structure

Not available

Alterations

Alteration Type: L
Alteration Text: Potassic alteration with the introduction of K-feldspar and biotite occurs in the core of the system. Locally the rocks are sericitized and phyllically altered. Higher in the system, the rocks are silicified, altered to clay, and carbonatized. Bull and her co-authors (1997 and 1999) indicate that galena is more abundant distally.

Rocks

Not available

Analytical Data

Not available

Materials

Ore: Galena
Ore: Chalcopyrite
Ore: Arsenopyrite
Ore: Sphalerite
Ore: Malachite
Ore: Magnetite
Gangue: Quartz

Comments

Comment (Deposit): Other Comments = Upper Grubstake Gulch contains part of a copper-gold porphyry that only has been examined in reconnaissance. Additional information can be obtained from Ahtna Minerals in Anchorage, Alaska.

Comment (Exploration): Status = Inactive

Comment (Reference): Primary Reference = Bull, Freeman, and Schneider, 1999

Comment (Geology): Geologic Description = The upper part of Grubstake Creek consists mainly of highly altered, border phase rocks of the Pennsylvanian to Permian, Ahtell Creek quartz monzonite. The Ahtell Creek rocks are intruded into the Pennsylvanian to Permian,Tetelna Formation which is mainly volcanic rocks. Both the Ahtell pluton and the Tetelna Formation are cut by composite dikes and irregular bodies of a mid-Jurassic complex that varies from diorite to quartz diorite (Richter and Matson, 1968; Bull, Schneider, and Freeman, 1997; Bull, Freeman, and Schneider, 1999). Where the Tetelna rocks have been intruded by the diorite complex they have been converted to multicolored, biotite and hornblende hornfels. Porphyry-type mineralization occurs mainly in the diorite complex and adjacent hornfels. Various subtypes occur: 1) propylitic altered zones with as much as 10 % pyrite are cut by quartz-carbonate veins that contain pyrite, chalcopyrite, and galena; 2) potassic altered zones containing secondary biotite and K-feldspar are cut by quartz-K feldspar veins, veinlets, and disseminated concentrations of as much as 15% pyrite, chalcopyrite, arsenopyrite, and magnetite; and 3) sericite/phyllic altered zones locally stained with malachite contain 5-30 % sulfides. There are widespread localized zones of argillic and iron-carbonate alteration. The hornfelsed Tetelna Formation within about 100 feet of diorite also has several subtypes of porphyry mineralization including: 1) silicified zones containing as much as 15% pyrite; 2) quartz-carbonate veins with pyrite, chalcopyrite, arsenopyrite, and galena; and 3) chloritic-magnetite or chloritic-pyrite breccia cut by quartz-pyrite-chalcopyrite veinlets. The hornfels adjacent to chloritic zones is typically bleached. Based on reconnaissance mapping by Homestake Mining Company geologists (Bull, Scheider, and Freeman, 1997; Bull, Freeman, and Schneider, 1999) the porphyry alteration and mineralization is crudely zoned, with potassic alteration occurring at lower elevations and in upper Grubstake Creek. Discrete veins in the Grubstake area such as the J. D. Lyons prospect (GU018) appear to be related to the hornfels phase of this porphyry deposit. The rocks in the area are deformed and so extensively altered that much more detailed work will be needed to accurately map the complex. The porphyry in upper Grubstake has not been tested by drilling, but it has been mapped and sampled by Cominco geologists (St.George, 1992) as well as the geologists affiliated with Homestake Mining Company. St. George found soils that are highly anomalous in gold along reconnaissance lines through upper Grubstake Creek. Soils collected by Homestake Mining Company indicate that a broad area that covers much of upper Grubstake and upper Slope Creeks contains more than 200 ppb gold. Eighty-four rock samples collected mostly in the Grubstake area contained a mean gold concentration of about 240 ppb gold; copper in these samples averaged about 350 ppm, and locally exceeded 1%.

Comment (Deposit): Model Name = Porphyry Cu-Au (Cox and Singer, 1986; model 20c)

Comment (Commodity): Gangue = Carbonate

Comment (Commodity): Gangue = iron-carbonate

Comment (Geology): Age = the porphyry deposit is probably related to the emplacement of a Jurassic diorite complex.

Comment (Workings): Workings / Exploration = Grubstake Creek has been explored extensively since the discovery of viable placer deposits in 1934 (GU017). Work by Richter and his associates appears to have triggered exploration in the 1960's and 1970's (Richter, 1964 and 1966; Richter and Matson, 1968). Kirk Stanley was active at this time. In more recent years the area has been studied by Cominco Exploration (St. George, 1992), and Homestake Mining Company (Bull, Schneider and Freeman, 1997; and Bull, Freeman, and Schneider, 1999). Ahtna Minerals Company has recently consolidated the geologic data as much of the prospect area lies on Ahtna regional Native corporation land.

References

Reference (Deposit): Bull, Katharine, Freeman, Larry, and Schneider, Craig, 1999, Slana property summary report for Homestake Mining Company: 11 p. and analytical appendices. (Report available, Ahtna Minerals Co., Anchorage, Alaska).

Reference (Deposit): Bull, Katharine, Schneider, Craig, and Freeman, Larry, 1997, Summary report for Ahtna Corporation: 12 p., appendices and maps. (Report available, Ahtna Minerals Co., Anchorage, Alaska).

Reference (Deposit): St. George, Phil, 1992, 1992 Ahtna Lands. Gulkana Quad Reconnaissance: Cominco Alaska Exploration, 1 p., maps, scale 1:63,360. (Report held by Ahtna Minerals Co., Anchorage, Alaska).

Reference (Deposit): Richter, D.H., and Matson, N.A., 1968, Distribution of gold and some base metals in the Slana area, eastern Alaska Range, Alaska: U.S. Geological Survey Circular 593, 20 p.

Reference (Deposit): Richter, D.H., 1966, Geology of the Slana district on south-central Alaska: Alaska Division of Geological and Geophysical Surveys Geological Report 2l, 36b p., 3 sheets, scale 1:63,360.

Reference (Deposit): Richter, D.H., 1964, Geology and mineral deposits of the Ahtell Creek area, Slana District, south-central Alaska: Alaska Division of Geological and Geophysical Surveys Geologic Report 6, 17 p., 1 sheet, scale 1:31,680.

The Top Ten Gold Producing States

These ten states contributed the most to the gold production that built the West from 1848 through the 1930s. The Top Ten Gold Producing States.