Vote for your favorite mineral in #MinCup26! - Sphalerite vs. Anorthite
Both zinc ore Sphalerite and calcium plagioclase feldspar Anorthite have perfect cleavage that will split cleanly if you hit them with a hammer, but only one can claim a larger split of your votes!
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Highway Prospect, Kantishna Mining District, Denali Borough, Alaska, USAi
Regional Level Types
Highway ProspectProspect
Kantishna Mining DistrictMining District
Denali BoroughBorough
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
63° 23' 52'' North , 150° 19' 55'' West
Latitude & Longitude (decimal):
Köppen climate type:
Mindat Locality ID:
197975
Long-form identifier:
mindat:1:2:197975:9
GUID (UUID V4):
0


The site is in Denali National Park and Preserve.
Location: The location corner of the Highway claim (Cobb, 1980 [OFR 80-363]) was reported by Reed (1933, p. 284) to be on the northwest ridge of Bald Mountain at an elevation of 4600 feet. He also reported other mineralization in the same area 'near the northwest base of Bald Mountain and above the east side of the Thorofare River.' For this record, the approximately located site represents mineral deposits on the northwest side of Bald Mountain. The Highway claim is number 41 of Cobb (1972 [MF 366]).
Geology: The northwest flank of Bald Mountain is underlain by Paleozoic, calcareous sedimentary rocks cut by numerous sills of mid-Tertiary porphyritic granodiorite. The mountain is about 1/2 mile north of the main east-west Contact fault of the Mt. Eielson district. The main granodiorite intrusion forms a small, wedge-shaped mass north of the fault (Reed, 1933, plate 22). The Highway claim was prospected by two small pits that exposed a sphalerite-bearing deposit. Reed (1933, p. 284) stated that the northwest base of Bald Mountain, including the area of the Highway claim, is appreciably mineralized. The mineralization is Oligocene, roughly contemporaneous with the Eocene or Oligocene emplacement age of the granodiorite (Reed and Lanphere, 1974; Decker and Gilbert, 1978; Cole, 1998).
Workings: The area was prospected by Ben Cleary around 1931. Cleary excavated small pits that disclosed sphalerite. There apparently has been no further exploration of the deposit.
Age: The mineralization is Oligocene, roughly contemporaneous with the Eocene or Oligocene emplacement age of the granodiorite (Reed and Lanphere, 1974; Decker and Gilbert, 1978; Cole, 1998).

Commodities (Major) - Zn
Development Status: None
Deposit Model: Replacement deposit or zinc-bearing skarn (Cox and Singer, 1986; models 19a, 18

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


Mineral List


1 valid mineral.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
Sphalerite2.CB.05aZnS

List of minerals for each chemical element

SSulfur
S SphaleriteZnS
ZnZinc
Zn SphaleriteZnS

Other Databases

Link to USGS - Alaska:MM161

Other Regions, Features and Areas containing this locality


This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

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