| Deposit ID | 10103007 |
|---|---|
| MRDS ID | M020898 |
| Record type | Site |
| Current site name | Kelso Mine |
| Alternate or previous names | Condor, Cully and Hoyes, Tejon Ranch |
| Related records | 10212417 |
| Geographic coordinates: | -118.75731, 34.83278 (WGS84) |
|---|---|
| Relative position | 7 MILES EAST OF LEBEC, SE SIDE OF TEHACHAPI MTS., HEADWATERS OF ALAMOS CR. |
Political divisions (FIPS codes)
Kern(county)
California(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Lebec(quadrangle 1:24,000 scale)
Lancaster(quadrangle 1:100,000 scale)
Los Angeles(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Antelope-Fremont Valleys(hydrologic unit)
Northern Mojave(hydrologic accounting unit)
Northern Mojave-Mono Lake(hydrologic subregion)
California(hydrologic region)
| Country | State | County |
|---|---|---|
| United States | California | Kern |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| San Bernardino | 009N | 018W | 23 | California |
| Commodity | Importance |
|---|---|
| Zinc Critical | Primary |
| Copper | Secondary |
| Lead | Secondary |
| Silver | Secondary |
| Result | 30 - 33 % ZN FROM TWO CLOSELY SPACED FRACTURES |
|---|
| Host or associated | Associated | ||
|---|---|---|---|
| Rock type | Plutonic Rock > Granitoid > Granite | ||
| |||
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Carbonate > Limestone |
| (1) | -118.75731, 34.83278 |
|---|
| Strike | N 30 E |
|---|---|
| Dip | STEEP NW |
| Width | 1.83M |
| Development status | Past Producer |
|---|---|
| Commodity type | Metallic |
| Significant | No |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | M020898 |
TROXEL, B.W. AND MORTON, P.K., 1962 , MINES AND MINERAL RESOURCES OF KERN COUNTY, CA; COUNTY REPT. 1 ; CA. DIV. OF MINES AND GEOLOGY, P. 346 - 347
| Subject category | Comment text |
|---|---|
| Deposit | ZINC MINERALIZATION APPEARS TO HAVE PENETRATED THE LIMESTONE ALONG FRACTURES. THE TWO PRINCIPAL FRACTURES ARE 4 FT. APART AND A THIRD FRACTURE IS ABOUT 30 FT. FARTHER NE OF THEM. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-DEC-1978 | Fraticelli, L. A. (Albers, J.) | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.
These are landing pages for further research — the state agencies don't currently expose per-mine deep links.