Pleasant Creek

The Pleasant Creek is a zinc and lead 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: Pleasant Creek  

State:  Alaska

County:  na

Elevation:

Commodity: Zinc, Lead

Lat, Long: 65.177, -141.05300

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 Pleasant Creek

Pleasant Creek MRDS details

Site Name

Primary: Pleasant Creek


Commodity

Primary: Zinc
Primary: Lead
Secondary: Copper
Secondary: Cobalt
Secondary: Arsenic
Secondary: Silver
Secondary: Antimony


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: Mississippi Valley, Appalachian Zn


Orebody

Not available


Structure

Not available


Alterations

Alteration Type: L
Alteration Text: The alteration at the Pleasant Creek prospects includes serpentization, silicification, and quartz veining.


Rocks

Not available


Analytical Data

Not available


Materials

Ore: Sphalerite
Ore: Pyrite
Ore: Galena
Gangue: Serpentine
Gangue: Quartz


Comments

Comment (Exploration): Status = Active

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

Comment (Deposit): Other Comments = This property 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): Geologic Description = Rock units in the prospect area are of Late Precambrian age and include a thick unit of basalt and redbeds with an interlayered sequence of massive carbonate rocks and conglomerate (DiMarchi and others, 1993). Carbonate rocks include the Pack Formation, a massive dolomite that lies unconformably over the Pleasant Creek Formation of dolomitic limestone, quartzite, and shale. Numerous facies changes and iron-rich zones characterize the prospect area. All of the units are folded along a northeast-trending anticlinal structure which is probably sympathetic to the larger scale Cathedral Creek arch. The prospect area also contains numerous northeast-trending thrust faults and two major high-angle faults, having displacements of 700 to 1,500 feet. A northeast-trending andesite dike swarm cuts across all of the map units in the area (DiMarchi and others, 1993). The prospect hosts two types of breccia: (1) areally extensive collapse breccias related to karsting in the carbonate units; and (2) an areally limited breccia related to faulting along the margins of the andesite dikes. Small iron oxide gossans along the breccias may increase with depth. Silicification and quartz veining are common in both breccia types, and serpentine is found rarely in fractures in the dolomite (DiMarchi and others, 1993). Mineralization at Pleasant Creek consists of a breccia body of unrotated dolomite fragments coated with pyrite in an open-space-fill matrix of coarse dolomite and massive pyrite; very fine grained, light colored sphalerite infilling brecciated pyrite; and late galena cubes (Andres and others, 1977). Soil sampling, rock sampling, and geologic mapping programs have been conducted at the Pleasant Creek prospects (DiMarchi and others, 1993).

Comment (Workings): Workings / Exploration = Soil sampling, rock sampling, and geologic mapping programs have been conducted at the Pleasant Creek prospects (DiMarchi and others, 1993).

Comment (Deposit): Model Name = Plutonic-related Pb-Zn?, Carbonate-hosted Zn? (Cox and Singer, 1986; model 32b)


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): Andrews, Tom, Bigelow, C.G., Fernette, J.P., Jirik, R., Kretschmar, U., Kretschmar, D., Lessman, J., McOuat, M., Martin, W., Ruzicka, J., Sandrock, G., Skyllingstad, P., Yinger, M., 1977, 1976 Annual progress report, Doyon project volume 1a, blocks 1, 4, 5, 7, 8: Anchorage, Alaska, WGM, Inc., p. 7-1 to 7-23. (Report held by Doyon, Limited, Fairbanks, Alaska.)

Reference (Deposit): Schmidt, J.M., 1997, Shale-hosted Zn-Pb-Ag and barite deposits of Alaska, in Goldfarb, R.J., and Miller, L.D., eds., Mineral Deposits of Alaska, 1997: Economic Geology Monograph 9, p. 35-65.


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