| Deposit ID | 10021966 |
|---|---|
| MRDS ID | DE01759 |
| MAS/MILS ID | 0400550011 |
| Record type | Site |
| Current site name | Mangum Copper Prospects |
| Alternate or previous names | Lobaris Prospect |
| Point of reference | Geographic coordinates: | Elevation | UTM | Precision | Relative position | Point location |
|---|---|---|---|---|---|---|
| Plant | -99.49676, 34.78149 (WGS84) | 477 | 100 | GO SW OF MANGUM ON U.S. HWY 34 ABOUT 0.5 MI. AFTER CROSSING BRIDGE OVER SALT FORK, TURN S. ABOUT 5 MI. TURN ESE ABOUT 0.9 MI TO MILL SITE ON TOP OF HAYSTACK GYPSUM HILL, FOLLOWING WINDING UNIMPROVED ROAD. THE MEADOWS COPPER SHALE SHOULD CROP OUT ABOUT 600 FT S. OF THE MILL. THE ROAD INTO THE MILL PROBABLY CROSSES THE BED AT ABOUT 0.35 MI FROM THE ENTRANCE. | ||
| (click for info) | ||||||
| Ore Body | -99.51868, 34.7832 (WGS84) | 100 | location unverified, but appears to be in area of disturbances on Google Earth and Microsoft Maps imagery. | |||
Political divisions (FIPS codes)
Greer(county)
Oklahoma(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Hester(quadrangle 1:24,000 scale)
Altus(quadrangle 1:100,000 scale)
Lawton(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Lower Salt Fork Red(hydrologic unit)
Salt Fork Red(hydrologic accounting unit)
Red Headwaters(hydrologic subregion)
Arkansas-White-Red(hydrologic region)
Federal lands
ST(Federal land areas administered by ST)
| Country | State | County |
|---|---|---|
| United States | Oklahoma | Greer |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Indian | 004N | 022W | 34 | NW OF NE OF NE | Oklahoma |
| Indian | 004N | 22W | 28 | C of SE | Oklahoma |
| Commodity | Importance |
|---|---|
| Copper | Primary |
| Lead | Tertiary |
| Silver | Tertiary |
| Cobalt Critical | Tertiary |
| Nickel Critical | Tertiary |
| Uranium | Tertiary |
| Vanadium Critical | Tertiary |
| Zinc Critical | Tertiary |
| Materials | Type of material |
|---|---|
| Chalcocite | Ore |
| Malachite | Ore |
| Shale | Gangue |
| Result | 0.5-3.0% CU (AVERAGE 1%) FROM MEADOWS COPPER SHALE, LEAD (20-90 PPM), SILVER (24-45 PPM), COBALT (15-40 PPM), NICKEL (35-65 PPM), URANIUM (70-100 PPM), VANADIUM (100-140 PPM), AND ZINC (300-400 PPM) |
|---|
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Shale |
| Rock unit name | Meadows Copper Shale Bed of the Flowerpot Shale |
| Rock description | Meadows Copper Shale |
| Plant (1) | -99.49676, 34.78149 | |
|---|---|---|
| Ore Body (2) | -99.51868, 34.7832 |
| Type of structure | Regional |
|---|---|
| Structure description | Gentle Dip W. About 5-10 Ft/Mi |
| Name | MEADOWS COPPER SHALE |
|---|---|
| General form | TABULAR |
| Strike | N-S |
| Dip | W. 5-10 FT/MI |
| Thickness | 0.46M |
| Length | 9655.8M |
| Width | 4827.9M |
| Depth to top | 0M |
| Development status | Past Producer |
|---|---|
| Commodity type | Metallic |
| Deposit size | Medium |
| Significant | No |
| Discovery year | 1965 |
| Discoverer | Lobaris Copper Co. (of Ardmore, Okla.). Bob Allen, John Hoard, and John Warren |
| Production years | none |
| District name | Red Bed District |
|---|
| Ownership category | Private |
|---|
| Type | Operator |
|---|---|
| Owner | Lobaris Copper Co. (Built pilot mill In Nw-NE-NE-34-4N-22W) |
| Type | Owner |
|---|---|
| Owner | J. N. Meadows |
| Type of workings | Surface |
|---|---|
| Name of workings | LOBARIS COPPER CO. |
| Area | 3885HA |
| Overall length | 9655.8M |
| Overall width | 4827.9M |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | DE01759 | |
| Oklahoma Geological Survey | OGS | OGS | OK-GRE-01 | |
| U.S. Bureau of Mines | Minerals Availability System | MAS | 0400550011 | = newMRDS 10224482, merged and deleted. |
Johnson, K.S., 1976, Permian copper shales of southwestern Oklahoma, in Johnson and Croy, eds., Stratiform copper deposits of the midcontinent region, A symposium: Oklahoma Geological Survey Circular 77, p. 3-14.
Lockwood, R.P., 1976, Geochemistry and prtrology of some Oklahoma red-bed copper occurrences, in in Johnson and Croy, eds., Stratiform copper deposits of the midcontinent region, A symposium: Oklahoma Geological Survey Circular 77, p. 61-68.
STROUD, R.B., MCMAHAN, A.B., STROUP, R.K., AND HIBPSHMAN, M.H., 1970, U.S. BUREAU OF MINES REPORT OF INVESTIGATIONS 7422, 103 P. (P. 38).
HANSEN, R.F., JR., 1958, UNIVERSITY OF OKLAHOMA, M.S. THESIS, 101 P.
LOCKWOOD, R.P., 1972, UNIVERSITY OF OKLAHOMA, PH.D. DISSERTATION, 125 P.
| Subject category | Comment text |
|---|---|
| Deposit | THE DEPOSIT OCCURS OVER 23 SQUARE MILES OR MORE, BUT ONLY 12-15 SQUARE MILES MAY BE PRODUCTIVE. |
| Deposit | BECAUSE OF A LARGE AMOUNT OF OXIDIZED ORE, THEY SOLD THEIR INTERESTS, AND THE AREA IS INACTIVE AND UNLEASED. |
| Deposit | LOCKWOOD (1972; 1976) AND JOHNSON (1976) GIVE DETAILS. HANSEN (1958) DID THE GEOLOGY. STROUD AND OTHERS (1970, P. 38) COLLECTED 11 SAMPLES (C-4 TO C-14) FROM MEADOWS BED IN SW-27, NW-10-4N-22W; AND NE-2, SE-5, NW-8, NW-12, 3N-22W, WITH ANALYSES RANGING FROM 0.02 TO 1.00% CU. |
| Deposit | Discovery Year: EARLY 1965 |
| Deposit | "the Mangum deposit is currently under development: it averages about 14 inches (36 cm) thick and about 1 percent copper" (Johnson, 1976, p. 3). |
| Deposit | "The Mangum deposit is a copper shale nearly identical to that at Creta, but it generally is more oxidized and occurs in a slightly higher bed of the Flowerpot shale. Test pits have been dug and preliminary concentration tests made on the ore, and a mill is being built on the properties." (Johnson, 1976, p. 4). |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-DEC-92 | Fay, Robert O. | Oklahoma Geological Survey | |
| Reporter | 18-NOV-83 | Oklahoma Geological Survey | Oklahoma Geological Survey | From deleted record 10224482 (MAS 0400550011) |
| Editor | 26-APR-10 | Wilson, Anna B. | U.S. Geological Survey | merged and deleted duplicate record 10224482 (MAS 0400550011) |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.