Cle Elum River Iron

The Cle Elum River Iron is a nickel, chromium, and iron 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: Cle Elum River Iron

State:  Washington

County:  Kittitas

Elevation:

Commodity: Nickel, Chromium, Iron

Lat, Long: 47.43139, -121.05444

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 Cle Elum River Iron

Cle Elum River Iron MRDS details

Site Name

Primary: Cle Elum River Iron
Secondary: Cle Elum River North Deposit
Secondary: Cle Elum River South Deposit
Secondary: Balfour Guthrie;


Commodity

Primary: Nickel
Primary: Chromium
Primary: Iron


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: Sandstone
Role: Host
Age Type: Host Rock
Age Young: Late Jurassic


Analytical Data

Not available


Materials

Ore: Garnierite
Ore: Magnetite
Ore: Hematite
Ore: Millerite
Gangue: Serpentine


Comments

Comment (Location): ON BOTH SIDES OF THE CLE ELUM RIVER

Comment (Production): THERE IS NO RECORDED PRODUCTION

Comment (Geology): IRON MINERALS ARE CONCENTRATED AT THE SERPENTINIZED PERIDOTITE-SWAUK FORMATION CONTACT.

Comment (Reserve-Resource): DRILLING (AVERAGE FROM 52 HOLES) INDICATES A RESERVE OF 6.25 MILLION TONS OF 40.82% FE, 0.83% NI, AND 2.4% CR2 O3 (HUNTTING, 1956, P. 197).


References

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): SHEDD, SOLON; JENKINS, O.P.; COOPER, H.H., 1922, IRON ORES, FUELS, AND FLUXES OF WASHINGTON: WASHINGTON DIVISION OF GEOLOGY BULLETIN 27, 160 P., 1 PL.

Reference (Deposit): WDGER OFR 90-18

Reference (Deposit): BROUGHTON, W. A., 1944, ECONOMIC ASPECTS OF THE BLEWETT-CLE ELUM IRON ORE ZONE, CHELAN AND KITTITAS COUNTIES, WASHINGTON: WASHINGTON DIVISION OF GEOLOGY REPORT OF INVESTIGATIONS 12, 42 P., 7 PL.

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.


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