| Deposit ID | 10072191 |
|---|---|
| MRDS ID | W016790 |
| Record type | Site |
| Current site name | Pilot Knob |
| Geographic coordinates: | -90.63344, 37.61923 (WGS84) |
|---|---|
| Elevation | 457 |
| Relative position | 5 MILES SOUTH AND SLIGHTLY EAST OF IRON MOUNTAIN |
Political divisions (FIPS codes)
Iron(county)
Missouri(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Ironton(quadrangle 1:24,000 scale)
Farmington(quadrangle 1:100,000 scale)
Rolla(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Upper St. Francis(hydrologic unit)
St. Francis(hydrologic accounting unit)
Lower Mississippi-St. Francis(hydrologic subregion)
Lower Mississippi(hydrologic region)
| Country | State | County |
|---|---|---|
| United States | Missouri | Iron |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| 5th Principal | 034N | 004E | 29 | S2 | Missouri |
| Commodity | Importance |
|---|---|
| Iron | Primary |
| Materials | Type of material |
|---|---|
| Magnetite | Ore |
| Apatite | Gangue |
| Barite | Gangue |
| Chalcopyrite | Gangue |
| Feldspar | Gangue |
| Fluorite | Gangue |
| Quartz | Gangue |
| Tourmaline | Gangue |
| Result | SHIPMENTS FOR SIX MONTHS IN 1885 AVERAGED 58.11 % FE, 17.02 % SILICA, 0.013 % PHOSPHORUS, 2.59 % ALUMINA, 0.077 % SULPHUR, 0.015 % LIME, AND 0.015 % MAGNESIA ( STEIDTMANN, 1933 ). RANGE: FE 66.83 % - 43.03 %, SILICA 3.62 % - 30.65 %, SULPHUR 0.07 % - 0.098 %, PHOSPHORUS 0.014 % - 0.021 % ( WINSLOW, 1894 ). |
|---|
| Host or associated | Associated | ||||
|---|---|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite | ||||
| |||||
| Host or associated | Host |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite |
| (1) | Elvins Group - (including Derby-Doerun Dolomite, Davis Formation), Bonneterre Dolomite |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | St. Francois Mountains |
| Type of structure | Local |
| Structure description | Footwall Porphyry Dips About 17 Degrees Sw Without Any Marked Undulations. The Beds Above The Contact Are Conformable. |
| General form | ROUGHLY PEAR-SHAPED |
|---|---|
| Thickness | 42.67M |
| Length | 457.2M |
| Width | 274.32M |
| Depth to top | 0M |
| Development status | Prospect |
|---|---|
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | No |
| Discovery year | 1835 |
| Year of first production | 1848 |
| Ownership category | Private |
|---|
| Type | Operator |
|---|---|
| Owner | Pilot Knob Pellet Co |
| Year | 1933 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Period | 1848 To 1933 | ||||||||||||||
| Material | ORE | ||||||||||||||
| Accuracy | Estimate | ||||||||||||||
| Description | Cp_Grade: ^45 To 50 % Fe | ||||||||||||||
| |||||||||||||||
| Type of workings | Underground |
|---|---|
| Overall depth | 416.05M |
| Overall length | 457.2M |
| Overall width | 274.32M |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | W016790 |
CRANE, G.W., 1912 , THE IRON ORES OF MISSOURI: MISSOURI BUREAU OF MINES AND GEOLOGY, 2D SER., V. 10 , P. 121 - 131 .
HAYES, W.C. AND GUILD, PHILIP W., 1967 , METALLIC MINERAL RESOURCES IN: MINERAL AND WATER RESOURCES OF MISSOURI, V. 43 , 2D SERIES, P. 82 - 83 .
STEIDTMANN, E., 1933 , THE IRON DEPOSITS OF PILOT KNOB, MISSOURI: 16TH INT. GEOL. CONG. GUIDEBOOK 2 , P. 68 - 73 .
WINSLOW, A., HAWORTH, E., NASON, F., 1894 , A REPORT ON THE IRON MOUNTAIN SHEET INCLUDING PORTIONS OF IRON, ST. FRANCOIS AND MADISON COUNTIES: MISSOURI GEOLOGICAL SURVEY, V. 9 , SHEET REPT. NO. 3 , P. 61 - 66 .
US BUREAU OF MINES, 1978
| Subject category | Comment text |
|---|---|
| Deposit | MEASUREMENTS TAKEN ALONG THE FOOTWALL OF THE BIG CUT: S 90 DEG E, 15 DEG S (WEST END OF CUT); N 63 DEG W, 27 DEG S (NEAR MIDDLE OF CUT); N 35 DEG W, 17 DEG S (SOUTHEAST END OF CUT). BOTH VERTICAL AND INCLINED JOINTS ARE PROMINENT. CONGLOMERATE ORE IS NEARLY 200 FT THICK IN PLACES. NO ONE ATTEMPTED TO MINE THE BOULDER ORE ( 1912 ). ORE ALSO OCCURS IN COMPARATIVELY SMALL VEINS OF HEMATITE. ONE STRIKES NE-SW AND IS VERTICAL. SURFACE BOULDER AND CONGLOMERATE ORES CONSTITUTE THE MOST IMPORTANT ORE RESERVES AT PILOT KNOB. ORE OCCURS IN TWO BEDS. UPPER ORE BED RANGES FROM 10 TO 20 FT IN THICKNESS. THE LOWER ORE BED RANGES FROM 5 TO 30 FT IN THICKNESS. CONGLOMERATE ORE EXTENDS OVER 400,000 SQ FT (ESTIMATED). |
| Deposit | ROCKS ON PILOT KNOB ARE DISTINCTLY STRATIFIED NEAR THE SUMMIT. BEDS HAVE A DIP ABOUT 13 DEG SW. ; INFO.SRC : 1 PUB LIT |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JAN-1976 | Weeks, Robert | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.