| Deposit ID | 10095453 |
|---|---|
| MRDS ID | M051058 |
| Record type | Site |
| Current site name | Unnamed Prospect Vhne-009r |
| Geographic coordinates: | -111.51098, 32.37733 (WGS84) |
|---|
Political divisions (FIPS codes)
Pima(county)
Arizona(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Silver Bell West(quadrangle 1:24,000 scale)
Silver Bell Mountains(quadrangle 1:100,000 scale)
Tucson(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Aguirre Valley(hydrologic unit)
Santa Cruz(hydrologic accounting unit)
Middle Gila(hydrologic subregion)
Lower Colorado(hydrologic region)
| Country | State | County |
|---|---|---|
| United States | Arizona | Pima |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Gila and Salt River | 012S | 008E | 15 | Arizona |
| Commodity | Importance |
|---|---|
| Copper | Tertiary |
| Materials | Type of material |
|---|---|
| Chrysocolla | Ore |
| Malachite | Ore |
| Host or associated | Associated | ||||
|---|---|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Quartz Latite | ||||
| |||||
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock |
| (1) | -111.51098, 32.37733 |
|---|
| Strike | N 60 E |
|---|---|
| Dip | STEEP S |
| Development status | Occurrence |
|---|---|
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | No |
| District name | Silver Bell District |
|---|
| Ownership category | BLM Administrative Area |
|---|
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | M051058 |
DOCKTER, R. D., 1976 , FIELD EXAM
| Subject category | Comment text |
|---|---|
| Deposit | NEAR AND ON CONTACT OF K SEDIMENTS WITH RHYOLITE? DIKE |
| Deposit | SELVAGE OF CHLORITE ALONG VEIN SUGGESTS HYDROTHERMAL BIOTITE. CHALCOPYRITE & CHALCOCITE IN 1-2' VEINWORKS CUTTING CRET IN PROSPECT. IN SHAFT ARE COPPER STAINS (PROBABLY EXOTIC) ALONG FAULT CUTTING THE DIKE. DIKE IS PROBABLY POST MINERAL. NO GOOD LIMONITE STAINS OR BOXWORK INDICATED IN IT. ALTERATION MAY BE POTASSIC BUT PROBABLY PROPYLITIC AND LIGHT. ; INFO.SRC : 3 FIELD OBSERV |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-APR-1976 | Dockter, Roger D. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.
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