| Deposit ID | 10013310 |
|---|---|
| MRDS ID | D009533 |
| Record type | Site |
| Current site name | Spar Hill Mine |
| Alternate or previous names | Pine Canyon Fluorspar Prospects: Claims, Spar Hill, Spar Hill Nos. 1,2 and 3, Spar Hill Deposit |
| Related records | 10223194 |
| Geographic coordinates: | -108.47923, 32.6229 (WGS84) |
|---|---|
| Elevation | 2027 |
| Relative position | ABOUT 16.5 MILES S 48 W OF SILVER CITY. |
Political divisions (FIPS codes)
Grant(county)
New Mexico(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Burro Peak(quadrangle 1:24,000 scale)
Silver City(quadrangle 1:100,000 scale)
Silver City(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Animas Valley(hydrologic unit)
Upper Gila(hydrologic accounting unit)
Upper Gila(hydrologic subregion)
Lower Colorado(hydrologic region)
Federal lands
Gila National Forest(National Forest)
National Forest FS(Type of land area)
FS(Federal land areas administered by FS)
| Country | State | County |
|---|---|---|
| United States | New Mexico | Grant |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| New Mexico | 019S | 016W | 27 | S2 | New Mexico |
| Commodity | Importance |
|---|---|
| Fluorine-Fluorite Critical | Primary |
| Materials | Type of material |
|---|---|
| Fluorite | Ore |
| Quartz | Gangue |
| Host or associated | Associated | ||||||
|---|---|---|---|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite | ||||||
| Rock unit name | Burro Mountain Granite | ||||||
| Rock description | Burro Mountain Granite | ||||||
| |||||||
| Host or associated | Host |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite |
| Host or associated | Host |
|---|---|
| Rock type | Plutonic Rock > Granitoid > Granite |
| (1) | -108.47923, 32.6229 |
|---|
| Type of structure | Local |
|---|---|
| Structure description | Deposits Occur Along The Northeast Striking Spar Hill Fault. |
| General form | LENSES, PODS |
|---|---|
| Strike | N 60 E |
| Dip | 70 NW |
| Thickness | 6.1M |
| Length | 152.4M |
| Width | 15.24M |
| Development status | Past Producer |
|---|---|
| Commodity type | Non-metallic |
| Deposit size | Small |
| Significant | No |
| Discovery year | 1941 |
| Discoverer | Marshall N. Kuykendal |
| Year of first production | 1942 |
| Year of last production | 1945 |
| District name | Burro Mountains District: Pine Canyon Area, Tyrone Mining District |
|---|
| Ownership category | National Forest |
|---|
| Type | Operator |
|---|---|
| Owner | Marshall N. Kuykendall |
| Home office | Lordsburg, N.M. |
| First year | 1958 |
| Type | Owner |
|---|---|
| Owner | Marshall N. Kuykendall |
| Home office | Lordsburg, N.M. |
| First year | 1966 |
| Year | 1940 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Period | Early 1940'S | ||||||||||||||
| Accuracy | Accurate | ||||||||||||||
| Description | Cp_Grade: ^Average Grade 52.5% Caf2. | ||||||||||||||
| |||||||||||||||
| Type of workings | Surface/Underground |
|---|---|
| Length | 27.43M |
| Overall depth | 15.24M |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | D009533 |
ROTHROCK, H.E., JOHNSON, C.H., AND HAHN, A.D., 1946 NMBMMR BULL 21, P. 74-75
GILLERMAN, E., 1952 USGS BULL 973-F, P. 277-278
GILLERMAN, E., 1964 NMBMMR BULL 83, P. 66
WILLIAMS, F.E., 1966 USBM IC-8307, P. 66-67
MCANULTY, W.N., 1978 NMBMMR MEM 34, P. 17
HEDLUND, D.C., 1978 USGS MISC. FIELD STUDIES MAP MF-1040
NMBMMR GENERAL FILE DATA
WILLIAMS, F.E., 1966, P. 67.
| Subject category | Comment text |
|---|---|
| Deposit | THIS RECORD CONTAINS DATA FROM RECORD D009828 BY RONALD G. WORL WHICH HAS BEEN DELETED FROM MRDS. ; INFO.SRC : 1 PUB LIT; 2 UNPUB REPT |
| Deposit | AT THE EASTERN END OF THE CLAIM GROUP ON THE SPAR HILL CLAIM, FLUORSPAR OCCURS AS REPLACEMENT FILLING IN A SHATTERED ZONE AND AS CEMENTING MATERIAL IN A BRECCIATED ZONE ALONG A FAULT THAT STRIKES N60E AND DIPS TO NW IN PRECAMBRIAN GRANITE AND TERTIARY RHYOLITE. THE FAULT CAN BE TRACED FOR ABOUT 500 FT. THE MINERALIZED ZONE RANGES IN WIDTH FROM A FEW INCHES AT EITHER END OF THE EXPOSED OUTCROP TO AS MUCH AS 20 FT IN THE BRECCIA ZONE. EASTWARD FROM THE BRECCIA ZONE, FLUORSPAR OCCURS AS CREVICE-AND-FRACTURE-FILLING FOR ABOUT 75 FT WHERE A NW TRENDING CROSS-FAULT CUTS OFF THE VEIN AT THE WESTERN END. THE VEIN, DILUTED BY QUARTZ, PINCHES OUT, PARTICULARLY IN RHYOLITE HOST ROCK. FOUR UNPATENTED CLAIMS IN THE 1940'S. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JUL-1982 | Menzie, David | New Mexico Bureau of Mines and Mineral Resources | |
| Updater | 01-JAN-1983 | Haug, Jerry L. (Worl, Ronald G.) | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.