The Mount Hurst is a chromium 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.
Mount Hurst MRDS details
Site Name
Primary: Mount Hurst
Commodity
Primary: Chromium
Location
State: Alaska
District: Ophir
Land Status
Not available
Holdings
Not available
Workings
Not available
Ownership
Not available
Production
Not available
Deposit
Record Type: Site
Operation Category: Occurrence
Operation Type: Unknown
Years of Production:
Organization:
Significant:
Physiography
Not available
Mineral Deposit Model
Model Name: Podiform chromite (minor)
Orebody
Not available
Structure
Not available
Alterations
Not available
Rocks
Not available
Analytical Data
Not available
Materials
Ore: Chromite
Ore: Spinel
Comments
Comment (Deposit): Model Name = Podiform chromite (Cox and Singer, 1986; model 8a)
Comment (Workings): Workings / Exploration = The U.S. Bureau of Mines first investigated Mt. Hurst as a potential source of chromic oxide and platinum-group metals in 1981. Since then, there have been staking and minor exploration programs by private interests.
Comment (Reference): Primary Reference = Roberts, 1984
Comment (Deposit): Other Comments = See also Boob Creek (OP013).
Comment (Geology): Geologic Description = Mt. Hurst is composed of chromite- and chrome spinel-bearing ultramafic rocks surrounded by lower Paleozoic crystalline limestone, schist, slate, phyllite, quartz, and chert. A nearby upper Paleozoic sequence of greenstone, metavolcanic rocks, tuff, and chert-bearing sedimentary rocks suggests a possible ophiolitic origin for the ultramafic rocks (Roberts, 1984). The ultramafic rocks at Mt. Hurst are crudely layered; certain layered zones are traceable for more than 2 miles. Rock types include dunite, wehrlite, harzburgite, lherzolite, and clinopyroxenite. One outcrop of dunite has been altered to carbonate, quartz, and talc. At least two minor occurrences of basalt and one outcrop of gabbro are also present (Roberts, 1984). Chromitite samples collected from the Mt. Hurst area are anomalous in platinum (0.014 - 0.026 ounce per ton) and palladium (0.003 ounce per ton). Wehrlite samples also contained minor amounts of platinum. Altered dunite samples contained elevated concentrations of mercury, antimony, arsenic, and silver. Coalescent or banded chromite is present almost exclusively within dunite layers in wehrlite (Roberts, 1984). Heavy-mineral concentrates panned from three separate drainages on the flanks of Mt. Hurst respectively contained 1474 ppb platinum, 1508 ppb platinum, and 2674 ppb gold (Roberts, 1984). The largest chrome spinel occurrence in the Mt. Hurst area is at this site (Roberts, 1984, locality 10). It is in a chromite band in a light orange-brown dunite lens in well-layered, light-green wehrlite. The chromite band trends northeast for about 30 feet; the southern end disappears beneath vegetation, soil and talus. It pinches and swells from 6 to 30 inches thick over 30 feet. Concentrations of chrome spinel within the chromite band vary from 30 to 80% of the rock. Chromitite samples from this locality contain about 30% chromic oxide (Roberts, 1984). The chrome spinel occurrences on Mt. Hurst appear to be very sparse and variable in size and quality. The presence of detectable platinum and palladium in sediments shed from the ultramafic rocks at Mt. Hurst (see Boob Creek, OP013) suggests a potential for paleo-placers (Roberts, 1984).
References
Reference (Deposit): Roberts, W.S., 1984, Economic potential for chromium, platinum, and palladium in the Mount Hurst ultramafics, west-central Alaska: U.S. Bureau of Mines Open-File Report 84-22, 52 p.
Reference (Deposit): Foley, J.Y., Burns, L.E., Schneider, C.L., and Forbes, R.B., 1989, Preliminary report of platinum group element occurrences in Alaska: Alaska Division of Geological and Geophysical Surveys Public Data File 89-20, 32 p., 1 map sheet, scale 1:2,500,000.
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.