| Deposit ID | 10019713 |
|---|---|
| MRDS ID | DC11198 |
| Record type | Site |
| Current site name | Chloride Mine |
| Geographic coordinates: | -113.50649, 46.78878 (WGS84) |
|---|---|
| Location accuracy | 100(meters) |
| Relative position | ON MAIN DIVIDE 3 MI SW OF COPPER CLIFF., .1 Km Radius, .1 Km Radius, .1 Km Radius |
Political divisions (FIPS codes)
Missoula(county)
Montana(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Mineral Ridge(quadrangle 1:24,000 scale)
Missoula East(quadrangle 1:100,000 scale)
Butte(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Upper Clark Fork(hydrologic unit)
Pend Oreille(hydrologic accounting unit)
Kootenai-Pend Oreille-Spokane(hydrologic subregion)
Pacific Northwest(hydrologic region)
| Country | State | County |
|---|---|---|
| United States | Montana | Missoula |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Montana Principal | 012N | 015W | 17,20 | Montana |
| Commodity | Importance |
|---|---|
| Silver | Primary |
| Lead | Secondary |
| Materials | Type of material |
|---|---|
| Galena | Ore |
| Quartz | Gangue |
| Host or associated | Host | ||||
|---|---|---|---|---|---|
| Rock type | Sedimentary Rock > Carbonate > Limestone | ||||
| Rock unit name | Jefferson Limestone | ||||
| Rock description | Jefferson Limestone | ||||
| |||||
| (1) | -113.50649, 46.78878 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | Bearmouth Overthrust |
| Type of structure | Local |
| Structure description | Garnet Stock |
| General form | PIPE |
|---|---|
| Thickness | 1.22M |
| Length | 6.1M |
| Development status | Past Producer |
|---|---|
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | No |
| District name | Garnet Range Area |
|---|
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | DC11198 |
USGS BULL 660, P. 229, 230.
MBMG BULL 8, P. 32.
| Subject category | Comment text |
|---|---|
| Deposit | PIPELIKE FORMS ARE VERTICAL OR INCLINED . ALONG ONE OR MORE ZONES IN WHICH ROCKS WERE FRACTURED OR CRUSHED, THE LIMESTONE HAS BEEN EXTENSIVELY REPLACED BY SILICA. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-MAR-74 | Unknown | U.S. Geological Survey | |
| Updater | 01-APR-81 | Wise, Kristine K. (Elliott, James E.) | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.