| Deposit ID | 10048772 |
|---|---|
| MRDS ID | MP25795 |
| Record type | Site |
| Current site name | Yellow Aster Mine |
| Geographic coordinates: | -117.66229, 35.35749 (WGS84) |
|---|
Political divisions (FIPS codes)
Kern(county)
California(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Johannesburg(quadrangle 1:24,000 scale)
Cuddeback Lake(quadrangle 1:100,000 scale)
Trona(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 |
|---|---|---|---|---|---|
| Mount Diablo | 030S | 040E | 2 | California |
| Commodity | Importance |
|---|---|
| Gold | Primary |
| Silver | Primary |
| Materials | Type of material |
|---|---|
| Gold | Ore |
| Host or associated | Associated |
|---|---|
| Rock type | Plutonic Rock > Granitoid > Quartz Monzonite |
| Host or associated | Host |
|---|---|
| Rock type | Plutonic Rock > Granitoid > Quartz Monzonite |
| Host or associated | Host |
|---|---|
| Rock type | Metamorphic Rock > Schist |
| (1) | -117.66229, 35.35749 |
|---|
| Strike | NW-SE; NE-SW |
|---|---|
| Dip | 30NE-90; 30-35NW |
| Thickness | 22.86M |
| Strike | NW-SE; NE-SW |
|---|---|
| Dip | 30NE-90; 30-35NW |
| Development status | Producer |
|---|---|
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | No |
| Discovery year | 1895 |
| Type | Operator |
|---|---|
| Owner | Anglo-American Mining Corp. |
| Home office | San Francisco, Ca |
| First year | 1933 |
| Type | Owner |
|---|---|
| Owner | Yellow Astre Mining And Milling Co. |
| First year | 1949 |
| Type of workings | Surface/Underground |
|---|---|
| Length | 24139.5M |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | MP25795 |
TUCKER, W.B., SAMPSON, R.J., AND OAKESHOTT, G.B., 1949, MINERAL RESOURCES OF KERN COUNTY: CALIFORNIA JOURNAL OF MINES AND GEOLOGY, V. 45, NO. 2, P. 237, PL. 17.
CALIFORNIA DIVISION OF MINES AND GEOLOGY, BULLETIN 95, P. 121-125.
CALIFORNIA JOURNAL OF MINES AND GEOLOGY, VOL. 29, P. 335-338.
CALIFORNIA JOURNAL OF MINES AND GEOLOGY, VOL. 14, P. 514.
CALIFORNIA JOURNAL OF MINES AND GEOLOGY, VOL. 36, P. 38.
CALIFORNIA JOURNAL OF MINES AND GEOLOGY, VOL. 29, P. 335, CALIFORNIA DIVISION OF MINES AND GEOLOGY, BULLETIN 95, P. 125, CALIFORNIA JOURNAL OF MINES AND GEOLOGY, VOL. 14, P. 514, CALIFORNIA JOURNAL OF MINES AND GEOLOGY, VOL. 36, P. 38.
| Subject category | Comment text |
|---|---|
| Deposit | PLACERS OCCUR ALONG GULCHES THAT DRAIN THE WESTERN SLOPES OF THE DOME ROCK MOUNTAINS: INCLUDES THE GOODMAN ARROYO AND ARROYO LA PAZ AND THEIR TRIBUTARIES. FERRAR GULCH CONTAINED THE RICHEST AND MOST PRODUCTIVE GRAVELS OF THE DISTRICT. |
| Deposit | THE OREBODY IS A NETWORK OF QUARTZ VEINS AND STRINGERS IN QUARTZ MONZONITE AND SCHIST. THE GOLD OCCURS BOTH IN THESE VEINS OF QUARTZ AND STRINGERS AND IN THE QUARTZ-MONZONITE ADJACENT TO THE VEINS. THE PRESENT LOW-GRADE OREBODY CONSISTS OF A TGRIANGULAR BLOCK OF MINERALIZED QUARTZ MONZONITE, WHICH IS BOUNDED ON THE EAST BY THE HANGING WALL FAULT, ON THE NORTH BY THE JUPITER FAULT AND ON THE SOUTHWEST BY THE FOOTWALL FAULT. THIS OREBODY IS ABOUT 800 FT IN WIDTH, 1000 FT IN LENGTH AND WAS WORKED DOWN TO THE THIRD LEVEL. THERE ARE 6 PARALLEL VEINS THAT HAVE BEEN DEVELOPED INTHIS AREA WHICH STRIKE NORTHWEST AND SOUTHEAST. THE DIPS VARY FROM 30 NORTHEAST TO VERTICAL. THE JUPITER FAULT STRIKES N 75 E., DIPPING TO NORTH AT AN ANGLE OF 40; THE HANGING WALL FAULT STRIKES N 30 W, DIPPING 45 DEGREE NE; THE FOOTWALL FAULT STRIKES N 60 W, DIPPING 40 NE. THE HIGH-GRADE OREBODIES FORMERLY MINED OCCURRED ALONG VERICAL FISSURES AND FRACTURE ZONES AND ALSO BENEATH THE LOW-DIPPING PREMINERAL FAULTS |
| Deposit | WHICH BOUND THE PRESENT LOW-GRADE OREBODY ON THE NORTH AND EAST. THE VERTICAL OREBODIES STRIKE NORTHWEST AND VARY IN WIDTH FROM SMALL VEINS TO OVER 75 FT. THE LARGEST OREBODIES OCCURRED IN THE NORTHWEST FISSURES AND FRACTURE ZONES AND HAD A LENGTH OF ABOUT 800 FT AND A THICKNESS OF 20 FT TO 75 FT. THE RAND VERTICAL VEIN WAS WORKED FOR A LENGTH OF 500 FT., AND HAD AN AVERAGE WIDTH OF 15 FT. IT WAS WORKED TO A DEPTH OF 400 FT. THE PRICE VEIN WAS WORKED FOR A LENGTH OF 500 FT. THE AVERAGE WIDTH WAS 10 FT AND IT WAS MINED TO A DEPTH OF 400 FT. THE OREBODIES THAT OCCUR AS MINERALIZED ZONES UNDERLYING THE PRE-MINERAL FAULTS POSSESS WELL-DEFINED HANGING WALLS FORMED BY THE GOUGE ALONG THE FAULT. THIS ORE IS COMPOSED OF MINERALIZED COUNTRY ROCK USUALLY QUARTZ MONZONITE AND SCHIST, WITH VERY LITTLE VEIN QUARTZ. OREBODIES OF THIS TYPE OCCURRED BENEATH JUPITER FAULT, ALONG THE LINE OF THE MIDWAY TUNNEL. THEY WERE FROM 200 FT TO 300 FT IN LENTH AND VARIED FROM 4 FT TO 16 FT IN THICKNESS. A |
| Deposit | NEW OREBODY HAS BEEN DEVELOPED ON THE NORTH SIDE OF THE GLORY HOLE ALONG THE JUPITER FAULT ABOUT 100 FT IN ELEVATION ABOUT THE RAND LEVEL. A TUNNEL HAS BEEN DRIVEN SOUTHWEST 300 FT. AT 100 FT SOUTHWEST OF THE PORTAL, A SHOOT OF ORE WAS ENCOUNTERED WHICH HAS BEEN DEVELOPED FOR 200 FT IN LENGTH. THE VEIN VARIES IN WIDTH FROM 4 FT TO 13 FT. IT STRIKES NORTHEAST AND DIPS 30 TO 35 TO THE NORTH. THE FOOTWALL IS QUARTZ-MONZONITE. ON THE FOOTWALL THREE IS A CARBONIZED GOUGE 6 TO 12 INCHES THICK. THE MINERALIZED QUARTZ OCCURS ABOVE THE GOUGE. AVERAGE VALUE OF THE ORE EXTRACTED IS REPORTED TO $6 PER TON. SEVERAL RAISES HAVE BEEN PUT UP IN THIS SHOOT OF ORE FOR A DISTANCE OF 115. |
| Deposit | 47 PATENTED CLAIMS AND 6 UNPATENTED CLAIMS. 796 ACRES. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-MAR-1981 | Nelson, Scott C. (Albers, John, P.) | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.
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