The Top is a gold, silver, and zinc 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.
Top MRDS details
Site Name
Primary: Top
Commodity
Primary: Gold
Primary: Silver
Primary: Zinc
Location
State: Alaska
District: Hyder
Land Status
Not available
Holdings
Not available
Workings
Not available
Ownership
Not available
Production
Not available
Deposit
Record Type: Site
Operation Category: Unknown
Operation Type: Unknown
Years of Production:
Organization:
Significant: N
Physiography
Not available
Mineral Deposit Model
Model Name: Polymetallic veins
Orebody
Form: SEE DEPOSIT DESCRIPTION COMMENTS
Structure
Not available
Alterations
Not available
Rocks
Not available
Analytical Data
Not available
Materials
Not available
Comments
Comment (Deposit): TIME (ALLDRICK, 1993).
Comment (Workings): THE DEPOSIT HAS BEEN EXPOSED BY SURFACE TRENCHING FOR ABOUT 450 FEET. SAMPLES COLLECTED BY THE U.S. BUREAU OF MINES IN 1992 OR 1993 (MAAS AND OTHERS, 1995, P. 258) CONTAIN UP TO 48.03 PPM AU, 100.8 PPM AG, AND 10.3% ZN.
Comment (Location): THE TOP PROSPECT IS IN SECTION 23 AT AN ELEVATION OF ABOUT 1500 FEET ON THE WEST SIDE OF MINERAL HILL, 0.3 MILE DUE WEST OF ITS HIGHEST POINT (MAAS AND OTHERS, 1995, P. 254 AND FIG. 66). THE LOCATION IS ACCURATE WITHIN ABOUT 0.1 MILE.
Comment (Deposit): THE COUNTRY ROCKS IN THE AREA OF THE TOP PROSPECT ARE PELITIC METASEDIMENTARY AND SUBORDINATE ANDESITIC METAVOLCANIC STRATA OF THE JURASSIC OR OLDER MESOZOIC HAZELTON GROUP; THE TRIASSIC TEXAS CREEK GRANODIORITE, WHICH UNDERLIES AND LOCALLY INTRUDES THE HAZELTON; AND THE EOCENE HYDER QUARTZ MONZONITE, WHICH INTRUDES THE HAZELTON AND TEXAS CREEK ROCKS(SMITH, 1977; KOCH, 1996). ACCORDING TO MAAS AND OTHERS (1995, P. 254, 258), THE DEPOSIT CONSISTS OF DISSEMINATED AND SEMI-MASSIVE PYRITE, SPHALERITE, AND TETRAHEDRITE, AND A QUARTZ-SULFIDE VEIN. THE DEPOSIT IS HOSTED IN HAZELTON VOLCANIC ROCKS AND HAS BEEN EXPOSED FOR A LENGTH OF ABOUT 450 FEET. MAAS AND OTHERS (P. 254) SUGGEST THAT THIS DEPOSIT IS JURASSIC IN AGE, BASED ON SIMILARITIES IN MINERALOGY, STRUCTURAL SETTING, AND HOSTROCK, TO ISOTOPICALLY-DATED JURASSIC DEPOSITS ELSEWHERE IN THE HYDER DISTRICT (FOR EXAMPLE, SEE BC065, BC067). IF SO, THE DEPOSIT IS CONTEMPORANEOUS, AT LEAST IN PART, WITH ISLAND-ARC VOLCANISM IN HAZELTON
Comment (Geology): MAAS AND OTHERS (1995, P. 254) SUGGEST THAT THIS DEPOSIT IS JURASSIC IN AGE, BASED ON SIMILARITIES IN MINERALOGY, STRUCTURAL SETTING, AND HOSTROCK, TO ISOTOPICALLY-DATED JURASSIC DEPOSITS ELSEWHERE IN THE HYDER DISTRICT (FOR EXAMPLE, SEE BC065, BC067). IF SO, THE DEPOSIT IS CONTEMPORANEOUS, AT LEAST IN PART, WITH ISLAND-ARC VOLCANISM IN HAZELTON TIME (ALLDRICK, 1993).
References
Reference (Deposit): Maas, K. M., Bittenbender, P. E., and Still, J. C., 1995, Mineral investigations in the Ketchikan mining district, southeastern Alaska: U. S. Bureau of Mines Open-File Report 11-95, 606 p.
Reference (Deposit): Koch, R. D., 1996, Reconnaissance geologic map of the Bradfield Canal quadrangle, southeastern Alaska: U.S. Geological Survey Open-File Report 81-728A, 35 p.,1 sheet, scale 1:250,000.
Reference (Deposit): Smith, J.G., 1977, Geology of the Ketchikan D1 and Bradfield Canal A-1 quadrangles, southeastern Alaska: U.S. Geological Survey Bulletin 1425, 49 p.
Reference (Deposit): Alldrick, D. J., 1993, Geology and metallogeny of the Stewart mining camp, northwestern British Columbia: British Columbia Department of Mines and Petroleum Resources Bulletin no. 85, 105 p., 2 plates."
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