| Deposit ID | 10109756 |
|---|---|
| MRDS ID | M100144 |
| Record type | Site |
| Current site name | Hines Deposit |
| Geographic coordinates: | -120.70655, 36.36689 (WGS84) |
|---|---|
| Elevation | 1158 |
| Relative position | APPROXIMATELY LOCATED ON PLATE 3 OF REFERENCE NO. 1 |
Political divisions (FIPS codes)
San Benito(county)
California(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
San Benito Mountain(quadrangle 1:24,000 scale)
Coalinga(quadrangle 1:100,000 scale)
Monterey(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Pajaro(hydrologic unit)
Central California Coastal(hydrologic accounting unit)
Central California Coastal(hydrologic subregion)
California(hydrologic region)
| Country | State | County |
|---|---|---|
| United States | California | San Benito |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Mount Diablo | 018S | 012E | 7,8,17 | California |
| Commodity | Importance |
|---|---|
| Chromium Critical | Primary |
| Materials | Type of material |
|---|---|
| Chromite | Ore |
| Uvarovite | Ore |
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Metamorphic Rock > Serpentinite | ||
| Rock unit name | Franciscan;Panoche | ||
| Rock description | Franciscan;Panoche | ||
| |||
| (1) | -120.70655, 36.36689 |
|---|
| General form | LENSE, POD |
|---|
| Development status | Producer |
|---|---|
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | No |
| District name | New Idria |
|---|
| Ownership category | Private |
|---|
| Type | Owner |
|---|---|
| Owner | K. J. Hines |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | M100144 |
WALKER, G.W. AND GRIGGS, A.B., 1953, GEOLOGICAL INVESTIGATIONS OF CHROMITE IN CALIFORNIA.: CALIF. DIVISION OF MINES BULLETIN 134, PART 2, CHAPT. 2, P. 54,55,80
| Subject category | Comment text |
|---|---|
| Deposit | CHROMITE DEPOSITS OCCUR IN A SERPENTINE MASS 12.5 MILES LONG AND 3 TO 4.5 MILES WIDE. MOST OF CHROMITE IS FOUND IN FLOAT BOULDERS SCATTERED ON HILLSIDES AND IN GRAVELS OF ADJOINING CREEKS. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JUN-1981 | Oster, Karel L. (Albers, John P.) | 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.