Mount Hawkins

The Mount Hawkins is a chromium mine located in Kittitas county, Washington.

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 Hawkins

State:  Washington

County:  Kittitas

Elevation:

Commodity: Chromium

Lat, Long: 47.44167, -120.98250

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 Hawkins

Mount Hawkins MRDS details

Site Name

Primary: Mount Hawkins
Secondary: Crowe
Secondary: Gallagher Head
Secondary: Skipper;


Commodity

Primary: Chromium


Location

State: Washington
County: Kittitas


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: N


Physiography

General Physiographic Area: Pacific Mountain System
Physiographic Province: Cascade-Sierra Mountains
Physiographic Section: Northern Cascade Mountains


Mineral Deposit Model

Not available


Orebody

Not available


Structure

Not available


Alterations

Not available


Rocks

Name: Serpentinite
Role: Host
Age Type: Host Rock
Age Young: Late Jurassic


Analytical Data

Not available


Materials

Ore: Chromite
Gangue: Serpentine


Comments

Comment (Location): IN DREW CREEK DRAINAGE ON THE SOUTHEAST SLOPE OF HAWKINS MOUNTAIN, NEAR A SMALL LAKE

Comment (Production): THE MOUNT HAWKINS PRODUCED ABOUT 15 TONS OF ORE DURING WORLD WAR II (HUNTTING, 1956, P. 37-38).

Comment (Geology): THE INGALLS COMPLEX IS AN OPHIOLITE COMPLEX OF MIDDLE TO LATE JURASSIC AGE (MILLER, 1985, P. 27-42).


References

Reference (Deposit): FRIZZELL, V.A., JR.; TABOR, R.W.; BOOTH, D.B.; ORT, K.M.; WAITT, R.B., 1984, PRELIMINARY GEOLOGIC MAP OF THE SNOQUALMIE PASS 1:100,000 QUADRANGLE, WASHINGTON: U.S. GEOLOGICAL SURVEY OPEN-FILE REPORT 84-693, 42 P., 1 PL.

Reference (Deposit): HUNTTING, M. T., 1956, INVENTORY OF WASHINGTON MINERALS-PART II, METALLIC MINERALS: WASHINGTON DIVISION OF MINES AND GEOLOGY BULLETIN 37, V. 1, 428 P.; V. 2, 67 P.

Reference (Deposit): MILLER, R. B., 1985, THE OPHIOLITIC INGALLS COMPLEX, NORTH-CENTRAL CASCADE MOUNTAINS, WASHINGTON: GEOLOGICAL SOCIETY OF AMERICA BULLETIN, V. 96, NO. 1, P. 27-42.

Reference (Deposit): WDGER OF 90-18


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