| Deposit ID | 10047945 |
|---|---|
| MRDS ID | M700309 |
| Record type | Site |
| Current site name | Skunk Creek No. 19 Claim |
| Related records | 10204209 |
| Geographic coordinates: | -123.87766, 47.37257 (WGS84) |
|---|---|
| Elevation | 442 |
| Location accuracy | 1000(meters) |
| Relative position | ABOUT 3.3 MI NORTH-NORTHWEST OF BURNT HILL LOOKOUT. ABOUT 6.5 MI SOUTH OF QUINAULT LAKE, Estimated At Prospect Symbol Shown On Topo Map |
Political divisions (FIPS codes)
Grays Harbor(county)
Washington(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Stevens Creek(quadrangle 1:24,000 scale)
Shelton(quadrangle 1:100,000 scale)
Seattle(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Queets-Quinault(hydrologic unit)
Washington Coastal(hydrologic accounting unit)
Oregon-Washington Coastal(hydrologic subregion)
Pacific Northwest(hydrologic region)
Federal lands
Olympic National Forest(National Forest)
National Forest FS(Type of land area)
FS(Federal land areas administered by FS)
| Country | State | County |
|---|---|---|
| United States | Washington | Grays Harbor |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Willamette | 022N | 009W | 30 | NW4 | Washington |
| Commodity | Importance |
|---|---|
| Manganese Critical | Primary |
| Iron | Secondary |
| Materials | Type of material |
|---|---|
| Bementite | Ore |
| Goethite | Ore |
| Hematite | Ore |
| Limonite | Ore |
| Pyrolusite | Ore |
| Rhodonite | Ore |
| Chlorite | Gangue |
| Pyrite | Gangue |
| Quartz | Gangue |
| Result | ASSAY: 18.1% MN, 17.5% FE |
|---|
| Model code | 100 |
|---|---|
| USGS model code | 24c.3 |
| Deposit model name | Volcanogenic Mn, Olympic Peninsula |
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Argillite |
| Rock unit name | Crescent Formation;Crescent Formation |
| Rock description | Crescent Formation;Crescent Formation |
| (1) | -123.87766, 47.37257 |
|---|
| General form | LENS |
|---|---|
| Strike | N60W |
| Dip | 45SW (AVERAGE DIP) |
| Thickness | 9.14M |
| Length | 30.48M |
| Development status | Past Producer |
|---|---|
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | No |
| Ownership category | National Forest |
|---|---|
| Area name | In Olympic National Forest |
| Type | Owner |
|---|---|
| Owner | Consolidated Minerals Corp., Seattle, Wa. |
| Year | 1952 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Material | ORE MN | ||||||||||||||
| Accuracy | Accurate | ||||||||||||||
| Description | Ap_Grade: ^19.5% Mn | ||||||||||||||
| |||||||||||||||
| Year | 1953 | ||||||||||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Material | ORE MN FE | ||||||||||||||||||||||||||||
| Accuracy | Accurate | ||||||||||||||||||||||||||||
| Description | Ap_Grade: ^18.1% Mn, 17.5% Fe, 33% Sio2 | ||||||||||||||||||||||||||||
| |||||||||||||||||||||||||||||
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | M700309 |
MAGILL, E.A., 1960, MANGANESE DEPOSITS OF THE OLYMPIC PENINSULA, WASH.: U.S. BUREAU OF MINES REPORT OF INVESTIGATIONS 5530, P. 71-73, 77.
DERKEY, R.E., JOSEPH, N.L., AND LASMANIS, RAYMOND, 1990, METAL MINES OF WASHINGTON - PRELIMINARY REPORT: WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES OPEN-FILE REPORT 90-18, P. 103.
MAGILL, 1960
| Subject category | Comment text |
|---|---|
| Deposit | A HIGHLY SILICEOUS MANGANIFEROUS LENS OCCURS IN AN ALTERED BASALT. THE LENS HAS A MAXIMUM THICKNESS NEAR THE CENTER IS 30 FT AND THINS TOWARD THE EDGES. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JUL-82 | Lawson, William A. (Evarts, Russell C.) | U.S. Geological Survey | |
| Updater | 01-NOV-92 | Peterson, Jocelyn A. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.