| Deposit ID | 10090807 |
|---|---|
| MRDS ID | D005063 |
| Record type | Site |
| Current site name | Desloge Land |
| Geographic coordinates: | -90.91206, 37.812 (WGS84) |
|---|---|
| Elevation | 335 |
| Relative position | LOCATED 11 MILES S.W. OF IRONDALE |
Political divisions (FIPS codes)
Washington(county)
Missouri(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Palmer(quadrangle 1:24,000 scale)
Farmington(quadrangle 1:100,000 scale)
Rolla(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Meramec(hydrologic unit)
Upper Mississippi-Meramec(hydrologic accounting unit)
Upper Mississippi-Kaskaskia-Meramec(hydrologic subregion)
Upper Mississippi(hydrologic region)
Federal lands
Mark Twain National Forest(National Forest)
National Forest FS(Type of land area)
FS(Federal land areas administered by FS)
| Country | State | County |
|---|---|---|
| United States | Missouri | Washington |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| 5th Principal | 036N | 002E | 30 | Missouri |
| Commodity | Importance |
|---|---|
| Iron | Primary |
| Materials | Type of material |
|---|---|
| Clay | Gangue |
| Host or associated | Host |
|---|---|
| Rock type | Unconsolidated Deposit > Clay, Mud |
| (1) | -90.91206, 37.812 |
|---|
| General form | BOULDERS |
|---|---|
| Depth to top | 0M |
| Development status | Occurrence |
|---|---|
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | No |
| District name | Southeast Missouri District |
|---|
| Ownership category | Private |
|---|
| Type | Owner |
|---|---|
| Owner | H. Desloge |
| Home office | Desloge, Mo. |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | D005063 |
CRANE, G.W. 1912, THE IRON ORES OF MISSOURI, MISSOURI BUR. OF MINES AND GEOLOGY, 2D SER, V. 10, P. 345
| Subject category | Comment text |
|---|---|
| Deposit | THE OUTCROP CONSISTS OF BOULDERS OF SECONDARY LIMONITE SCATTERED FOR A DISTANCE OF A QUARTER OF A MILE ON THE N.E. TRENDING RIDGE. NO CHERT OR SAND WAS OBSERVED ASSOCIATED WITH THE ORE. THE ORE VARIES IN TEXTURE FROM DENSE TO SLIGHTLY CELLULAR, THE SMALL CAVITIES OF THE LATTER BEING USUALLY FILLED WITH RED CLAY. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JUL-1980 | Schneider, Norma J | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.