The Woodcock Mtn Laterite is a nickel mine located in Josephine county, Oregon at an elevation of 1,322 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
Elevation: 1,322 Feet (403 Meters)
Commodity: Nickel
Lat, Long: 42.1203, -123.67860
Map: View on Google Maps
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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.
Woodcock Mtn Laterite MRDS details
Site Name
Primary: Woodcock Mtn Laterite
Secondary: Woodcock Mtn Nickel Deposit
Secondary: Woodcock Mountain Laterite
Commodity
Primary: Nickel
Secondary: Chromium
Secondary: Cobalt
Tertiary: Iron
Location
State: Oregon
County: Josephine
District: Waldo
Land Status
Land ownership: Mixed
Note: the land ownership field only identifies whether the area the mine is in is generally on public lands like Forest Service or BLM land, or if it is in an area that is generally private property. It does not definitively identify property status, nor does it indicate claim status or whether an area is open to prospecting. Always respect private property.
Holdings
Type: Other
Type: Located Claim
Workings
Type: Surface
Ownership
Owner Name: California Nickel Corp
Percent: 5.00
Home Office: California
Info Year: 1979
Owner Name: Inspiration Devel Co
Percent: 15.00
Home Office: Arizona
Info Year: 1979
Owner Name: Hanna Mining Co
Percent: 80.00
Home Office: Ohio
Info Year: 1979
Production
Not available
Deposit
Record Type: Site
Operation Category: Prospect
Operation Type: Surface
Mining Method: Strip-Hillside
Discovery Year: 1941
Years of Production:
Organization:
Significant: Y
Physiography
General Physiographic Area: Pacific Mountain System
Physiographic Province: Pacific Border Province
Physiographic Section: Klamath Mountains
Mineral Deposit Model
Not available
Orebody
Not available
Structure
Not available
Alterations
Not available
Rocks
Not available
Analytical Data
Not available
Materials
Unknown: Kaolinite
Unknown: Chlorite
Unknown: Ilmenite
Unknown: Goethite
Unknown: Gibbsite
Unknown: Garnierite
Unknown: Enstatite
Unknown: Diaspore
Unknown: Chromite
Unknown: Chalcedony
Unknown: Talc
Unknown: Spinel
Unknown: Serpentine
Unknown: Nontronite
Unknown: Montmorillonite
Unknown: Magnetite
Unknown: Limonite
Comments
Comment (Reserve-Resource): QUANTITY ESTIMATES TAKEN FROM B-BIB Q800-Q805 ASSAY FE- 1977
Comment (Reserve-Resource): FIELD OP. FIRST QUARTER FY 1980 INCLUDES THIS IN ILLINOIS VALLEY NICKEL LATERITE DEPOSITS W/EXTENSIVE DATA BASE REVISION AND REVISED MINE COSTING DUE. OWNERS:HANNA MINING CO.>80%,INSPIR. DEV. CO.>15%,CAL. NI CO.> 5%. OTHER NAMES:WOODCOCK MTN. NI DEP.
Comment (Production): PA= NI FROM EIGHT DOLLAR MTN LATERITE. PB= CO DITTO PC= CR DITTO PE= NI FROM WOODCOCK MTN LATERITE. PF= CO DITTO PG= CR DITTO PI= NI FROM ROUGH AND READY LATERITE. PJ= CO DITTO PK= CR DITTO
Comment (Ownership): CALIFORNIA NICKEL CORP. IS A SUBSIDIARY OF NI-CAL DEVELOPMENTS LTD. (A CANADIAN FIRM).
Comment (Geology): LATERITE SHOULD BE A MINERAL ENTRY; IT IS PROCESSED FOR COMMODITY CONTENT. SAPROLITE SHOULD BE A MINERAL ENTRY; IT IS PROCESSED FOR COMMODITY CONTENT. MAGHEMITE IS NOT IN MINERAL TABLE. RECENT RESEARCH INDICATES MOST OF THE NICKEL (AND PRESUMABLY THE COBALT) IS INCLUDED IN THE GOETHITE LATTICE. NICKEL AND COBALT ARE RELEASED FROM THE PARENT MINERALS AND RECOMBINED IN THE IRON OXIDES. OLIVINE IS THE PROBABLE SOURCE OF NICKEL. SOURCE OF COBALT IS UNKNOWN.
Comment (Production): PROPERTY HAS NOT PRODUCED (1979).
Comment (Deposit): LOCATION IS POINT OF ENTRY TO PROPERTY AT TURNOFF FROM WEST SIDE ROAD. NICKEL AND COBALT ARE ENTERED AS COPRODUCTS RECOVERY OF COBALT AND NICKEL IS NECESSARY FOR PRODUCTION AT CURRENT PRICES (1979).
Comment (Geology): THE SHAPE OF THE LATERITE AREAS IS GENERALLY TABULAR, BOTTOM IS HIGHLY IRREGULAR.
Comment (Geology): UNSPEC SEDIMENTARY FOR LACK OF AN APPROPRIATE ENTRY FOR LATERITE. LATERITIC SOIL COMPOSED OF HYDROUS FE-OXIDES, CLAY MINERALS, AND POSSIBLE GARNIERITE WITH RESIDUAL SILICA AND CHROMITE. SAPROLITE, THE CLAY-RICH WEATHERED HOST ROCK, IS A SIGNIFICANT, BUT VARIABLE, PERCENTAGE OF THE RESOURCE. CANNOT BE ENTERED IN L DATA SET.
References
Reference (Reserve-Resource): RALPH C. KIRBY, ASSISTANT DIRECTOR - METALLURGY);
Reference (Reserve-Resource): USBM REPORT, JANUARY 1978.
Reference (Reserve-Resource): *CONFIDENTIAL DATA*
Reference (Deposit): OR. DEPT. GEOL. AND MIN. INDUST. BULLETIN 14-C, 1942,
Reference (Deposit): VOL. 2, P. 224.
Reference (Deposit): OR. DEPT. GEOL. AND MIN. INDUST. MISC. PAPER 20, 1978,
Reference (Deposit): P. 43.
Reference (Reserve-Resource): WILLIAMS, J.F. AND LINDSEY, D.S., NICKEL DEPOSITS IN THE
Reference (Reserve-Resource): WESTERN UNITED STATES (A REPORT AND APPRAISAL FOR
Oregon Gold
"Where to Find Gold in Oregon" looks at the density of modern placer mining claims along with historical gold mining locations and mining district descriptions to determine areas of high gold discovery potential in Oregon. Read more: Where to Find Gold in Oregon.
