Hurricane

The Hurricane is a manganese and iron mine located in Clallam county, Washington at an elevation of 3,999 feet.

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: Hurricane

State:  Washington

County:  Clallam

Elevation: 3,999 Feet (1,219 Meters)

Commodity: Manganese, Iron

Lat, Long: 48.00639, -123.50333

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 Hurricane

Hurricane MRDS details

Site Name

Primary: Hurricane


Commodity

Primary: Manganese
Primary: Iron


Location

State: Washington
County: Clallam


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: Pacific Border Province
Physiographic Section: Olympic Mountains


Mineral Deposit Model

Not available


Orebody

Not available


Structure

Not available


Alterations

Not available


Rocks

Name: Basalt
Role: Associated
Age Type: Associated Rock
Age Young: Eocene

Name: Basalt
Role: Associated
Age Type: Host Rock
Age Young: Eocene


Analytical Data

Not available


Materials

Ore: Rhodonite
Ore: Hausmannite
Ore: Bementite


Comments

Comment (Location): UNSURVEYED, ELEV. 4000 FT., ABOUT 2.7 MILES EAST-SOUTHEAST OF ELWHA RANGER STATION AND 0.3 MILES EAST-NORTHEAST OF GRIFF.

Comment (Development): ECON.COM: PRODUCED ABOUT 1000 TONS OF ORE (HUNTTING, 1956, P. 255).

Comment (Deposit): AREA IS UNDERLAIN BY HIGHLY ALTERED BASALT CONTAINING INTERCALATED PODS OR LENSES OF RED LIMESTONE (DATA FROM U.S.G.S. MRDS, 1990). THE CRESCENT FORMATION, WHICH HOSTS MANGANESE MINERALIZATION ON THE OLYMPIC PENNINSULA, CONSISTS OF PALEOCENE? AND EOCENE PILLOW BASALTS COMPOSITIONALLY SIMILAR TO OCEAN RIDGE BASALTS. ASSOCIATED PELAGIC LIMESTONES INDICATE DEPOSITION IN DEEP WATER (SNAVELY, 1987, P. 306-308). ; INFO.SRC : 1 PUB LIT


References

Reference (Deposit): WDGER OFR 90-18.

Reference (Deposit): GARRISON, R.E., 1973, SPACE-TIME RELATIONS OF PELAGIC LIMESTONES AND VOLCANIC ROCKS, OLYMPIC PENNINSULA, WASHINGTON: GEOLOGICAL SOCIETY OF AMERICA BULLETIN, V. 84, NO. 2, P. 583-594.

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): MAGILL, E.A., 1960, MANGANESE DEPOSITS OF THE OLYMPIC PENNINSULA, WASHINGTON: U.S. BUREAU OF MINES REPORT OF INVESTIGATIONS 5530, 82 P.

Reference (Deposit): SNAVELY, P.D., JR., 1987, TERTIARY GEOLOGIC FRAMEWORK, NEOTECTONICS, AND PETROLIUM POTENTIAL OF THE OREGON-WASHINGTON CONTINENTAL MARGIN. IN SCHOLL, D.W.; GRANTZ, ARTHUR; VEDDER, J.G., GEOLOGY AND RESOURCES POTENTIAL OF THE CONTINENTAL MARGIN OF WESTERN NORTH AMERICA AND ADJACENT OCEAN BASINS--BEAUFORT SEA TO BAJA CALIFORNIA: CIRCUM-PACIFIC COUNCIL FOR ENERGY AND MINERAL RESOURCES EARTH SCIENCE SERIES , V. 6, P. 305-335.

Reference (Deposit): SOREM, R.K.; GUNN, D.W., 1967, MINERALOGY OF MANGANESE DEPOSITS, OLYMPIC PENNINSULA, WASHINGTON: ECONOMIC GEOLOGY, V. 62, NO. 1, P. 22-56.


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