Mount Casca

The Mount Casca is a uranium and phosphorus-phosphates 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

Name: Mount Casca

State:  Alaska

County:  na

Elevation:

Commodity: Uranium, Phosphorus-Phosphates

Lat, Long: 65.348, -141.05400

Map: View on Google Maps

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.


Satelite image of the Mount Casca

Mount Casca MRDS details

Site Name

Primary: Mount Casca
Secondary: VABM Casca


Commodity

Primary: Uranium
Primary: Phosphorus-Phosphates


Location

State: Alaska
District: Black


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: Phosphate, upwelling type


Orebody

Not available


Structure

Not available


Alterations

Alteration Type: L
Alteration Text: Alteration at Mount Casca prospect consists of pervasive silicification with chalcedony-lined vugs and irregular quartz veining. Iron and manganese oxides are present within breccia zones (DiMarchi and others, 1993).


Rocks

Not available


Analytical Data

Not available


Materials

Ore: Collophane
Ore: Apatite


Comments

Comment (Exploration): Status = Active

Comment (Workings): Workings / Exploration = The Mount Casca prospects were explored by WGM Inc. in 1975 and 1976, by Union Carbide in 1977, and by ASA Inc. in 1993. WGM Inc. conducted a soil sampling and trenching program, and Union Carbide took soil and rock samples and also did some petrographic analysis. ASA Inc.'s program consisted of selective rock sampling and mapping of the prospect (DiMarchi and others, 1993).

Comment (Deposit): Model Name = Upwelling-type phosphate deposit? (Cox and Singer, 1986; model 34c)

Comment (Deposit): Other Comments = This prospect lies on Doyon, Limited selected or conveyed land. For more information, contact Doyon, Limited. This site is within the Yukon-Charley Rivers National Preserve.

Comment (Geology): Age = Cambrian or younger, based on the age of the host rocks.

Comment (Reference): Primary Reference = DiMarchi and others, 1993

Comment (Geology): Geologic Description = The main geologic unit in the Mount Casca area is a massive boulder-conglomerate of the Ordovician to Devonian Road River Formation (Dover and Miyaoka, 1988). The massive conglomerate is overlain by thin wedges of algal limestone of the Devonian Ogilvie Formation and underlain by the Cambrian Funnel Creek Limestone. The massive conglomerate is clast supported with an unsorted matrix. Clasts are mostly silicified oolitic limestone, chert pebbles, granular apatite, and fossil fragments. In some places, phosphate nodules as much as 5 inches in diameter were reported (DiMarchi and others, 1993). The conglomerate also contains limestone breccias. The conglomerate contains anomalous phosphorous and uranium geochemical values. The phosphorous is located in phosphate nodules and apatite, and the uranium is in collophane and uranium-bearing apatite (DiMarchi and others, 1993). The limestone breccias contain 400 parts per million uranium, and 16.5 percent P2O5 (Doyon, Limited, 1986). Alteration in the conglomerate appears as pervasive silicification with chalcedony-lined vugs and irregular quartz veining. Within breccia zones, many iron and manganese oxides are present (DiMarchi and others, 1993). The Mount Casca prospect was explored by WGM Inc. in 1975 and 1976, by Union Carbide in 1977, and by ASA Inc. in 1993. WGM Inc. conducted a soil sampling and trenching program, and Union Carbide took soil and rock samples, and also did some petrographic analysis. ASA Inc.'s program consisted of selective rock sampling and mapping of the prospect (DiMarchi and others, 1993).


References

Reference (Deposit): DiMarchi, J.J., Weglarz, T.B., Adams, D.D., Hubert, J.A., and West, A.W., 1993, 1993 annual report reconnaissance program, Doyon option lands: ASA Inc., 120 p. (Report held by Doyon Ltd., Fairbanks, Alaska.)

Reference (Deposit): Doyon, Limited, 1986, Mines, prospects, and geochemical anomalies on Doyon, Limited, regional overselection lands, Alaska: Fairbanks, Alaska, Doyon, Limited, Report 86-01A, v. 1, 150 p. (Report held by Doyon, Limited, Fairbanks, Alaska.)

Reference (Deposit): Dover, J.A., and Miyaoka, R.T., 1988, Reinterpreted geologic map and fossil data, Charley River quadrangle, east-central Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-2004, 2 sheets, scale 1:250,000.


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