| Deposit ID | 10027195 |
|---|---|
| MRDS ID | M002440 |
| Record type | Site |
| Current site name | Dives Mine |
| Alternate or previous names | Saxon, Padre Kino |
| Related records | 10137344 |
| Geographic coordinates: | -114.58662, 33.11618 (WGS84) |
|---|---|
| Elevation | 274 |
| Relative position | 1.5 MILES NORTHEAST OF THE RED CLOUD MINE. |
Political divisions (FIPS codes)
La Paz(county)
Arizona(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Picacho(quadrangle 1:24,000 scale)
Trigo Mountains(quadrangle 1:100,000 scale)
Salton Sea(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Imperial Reservoir(hydrologic unit)
Lower Colorado(hydrologic accounting unit)
Lower Colorado(hydrologic subregion)
Lower Colorado(hydrologic region)
Federal lands
Bureau of Land Management(Bureau of Land Management AZ)
Bureau of Land Management AZ BLM(Type of land area)
BLM(Federal land areas administered by BLM)
| Country | State | County |
|---|---|---|
| United States | Arizona | La Paz |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Gila and Salt River | 003S | 023W | 36 | SW | Arizona |
| Commodity | Importance |
|---|---|
| Silver | Primary |
| Lead | Secondary |
| Zinc Critical | Tertiary |
| Manganese Critical | Tertiary |
| Strontium | Tertiary |
| Barium-Barite Critical | Tertiary |
| Iron | Tertiary |
| Materials | Type of material |
|---|---|
| Cerussite | Ore |
| Hematite | Ore |
| Pyrolusite | Ore |
| Smithsonite | Ore |
| Barite | Gangue |
| Celestite | Gangue |
| Host or associated | Associated | ||||
|---|---|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Intermediate Volcanic Rock > Andesite | ||||
| |||||
| Host or associated | Host |
|---|---|
| Rock type | Metamorphic Rock > Schist |
| (1) | -114.58662, 33.11618 |
|---|
| Type of structure | Local |
|---|---|
| Structure description | A Fault Zone Seperates Andesitic And Rhyolitic Lavas, Breccias, And Tuffs On The West From Schist And Granite On The East. The Main Fault Strikes N20w And Dips 60 Sw, Is Joined Near The Center Of The Claim By A Branch Fault That Strikes N10w. These Faults Contain Veins Of Similar Character, But The Main One Is Wider, Longer, And More Strongly Mineralized |
| General form | VUGS & IRREGULAR MASSES |
|---|---|
| Length | 609.6M |
| Width | 3.05M |
| Development status | Past Producer |
|---|---|
| Commodity type | Both |
| Deposit size | Small |
| Significant | No |
| District name | Silver District |
|---|
| Ownership category | BLM Administrative Area |
|---|
| Year | 1920 | |||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Period | 1919-1920 | |||||||||||||||||||||
| Accuracy | Estimate | |||||||||||||||||||||
| Description | Cp_Grade: ^48% Pb, 67 Oz Ag/Ton | |||||||||||||||||||||
| ||||||||||||||||||||||
| Type of workings | Unknown |
|---|---|
| Length | 13.72M |
| Overall depth | 26.21M |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | M002440 | |
| U.S. Bureau of Mines | Minerals Availability System | MAS | 0040271354 |
WILSON, E.D.; 1933; GEOLOGY AND MINERAL DEPOSITS OF SOUTHERN YUMA COUNTY ARIZONA: ARIZ. B.M. BULLETIN 134, P. 62.
KEITH, S.B., 1978, INDEX OF MINING PROPERTIES IN YUMA COUNTY, ARIZONA; ARIZONA BUREAU OF MINES BULLETIN 192, P. 178.
PHILLIPS, K.A., ARIZONA INDUSTRIAL MINERALS: ARIZONA DEPARTMENT OF MINES AND MINERAL RESOURCES MINERAL REPORT 3, 185 P.
A.B.M. BULLETIN 134, P. 62; KEITH, S.B., 1978.
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-APR-1972 | Gere, W. | U.S. Geological Survey | |
| Updater | 01-OCT-1979 | Hall, R. K. (Creasey, S. C.) | U.S. Geological Survey | |
| Updater | 01-APR-1993 | Orris, Greta 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.