Clark Mine, Crawford County, Missouri, USAi
Regional Level Types | |
---|---|
Clark Mine | Mine |
Crawford County | County |
Missouri | State |
USA | Country |
This page is currently not sponsored. Click here to sponsor this page.
Latitude & Longitude (WGS84):
37° 59' 17'' North , 91° 19' 30'' West
Latitude & Longitude (decimal):
Locality type:
Köppen climate type:
Nearest Settlements:
Place | Population | Distance |
---|---|---|
Steelville | 1,699 (2017) | 3.4km |
Cuba | 3,374 (2017) | 10.8km |
Leasburg | 334 (2017) | 11.8km |
Bourbon | 1,621 (2017) | 19.8km |
West Sullivan | 119 (2017) | 24.9km |
This mine is located two miles northeast of Steelville and is situated upon the west face of the point of a hill projecting southeast from a high ridge. Like the Griffith mine, it is marked by a well defined sink structure. The area of the sink is shown by a rim of pitching Roubidoux sandstone, encircling it on three sides; the larger diameter extending northeast-southwest. The rim is not exposed for a short distance across the south end of the sink. Within this area one open cut, two shafts, and several shallow pits have been sunk.
The open cut, which is about 100 feet long, 40 feet wide, and 10 feet deep, was made on the north end of the rim where the latter crosses the highest point of the hill. Considerable soft red ore has been mined from this cut. The ore was found in a layer 12 inches or more thick between heavy beds of quartzitic chert and sandstone which dip about 25° toward the center of the sink.
A shallow pit located about 200 feet southeast of the cut exposes the cast rim of the sink but shows very little ore. A 70 foot pit, 30 feet east of the shallow pit and just outside of the rim of the sink, shows only ocherous, decomposed cotton rock and a soft, silicious clay that may represent decomposed chert and limestone. A 102 foot shaft, located about 100 feet southwest of the 70 foot pit, and well within the area of the sink, shows, throughout its depth, decomposed chert and quartzitic sandstone enclosing occasional thin seams of ore. The best seam of ore occurs at a depth of 72 feet and consists of 6 inches of hard blue hematite containing some sand and chert. The dip of the formation is strongly to the west, toward the middle of the sink.
A shallow pit sunk on the southeast edge of the rim shows some soft red ore and a cherty, ferruginous rim rock pitching to the northwest. In the ravine near the base of the west slope of the hill, are many shallow pits from which considerable hard, blue, silicious ore has been mined.
With the exception of the 102 foot shaft, the prospecting here has not been deep and has afforded little knowledge of the extent of the ore body. A position upon the hillside about midway between the open cut at the northeast end of the sink and the shallow diggings in the ravine at its base is suggested as the best point for further prospecting. On the whole, the well developed sink structure and the several showings of ore mark the property as worthy of a thorough investigation.
An analysis of the soft, red ore showed 55.37% iron and 0.075% Phos.
The open cut, which is about 100 feet long, 40 feet wide, and 10 feet deep, was made on the north end of the rim where the latter crosses the highest point of the hill. Considerable soft red ore has been mined from this cut. The ore was found in a layer 12 inches or more thick between heavy beds of quartzitic chert and sandstone which dip about 25° toward the center of the sink.
A shallow pit located about 200 feet southeast of the cut exposes the cast rim of the sink but shows very little ore. A 70 foot pit, 30 feet east of the shallow pit and just outside of the rim of the sink, shows only ocherous, decomposed cotton rock and a soft, silicious clay that may represent decomposed chert and limestone. A 102 foot shaft, located about 100 feet southwest of the 70 foot pit, and well within the area of the sink, shows, throughout its depth, decomposed chert and quartzitic sandstone enclosing occasional thin seams of ore. The best seam of ore occurs at a depth of 72 feet and consists of 6 inches of hard blue hematite containing some sand and chert. The dip of the formation is strongly to the west, toward the middle of the sink.
A shallow pit sunk on the southeast edge of the rim shows some soft red ore and a cherty, ferruginous rim rock pitching to the northwest. In the ravine near the base of the west slope of the hill, are many shallow pits from which considerable hard, blue, silicious ore has been mined.
With the exception of the 102 foot shaft, the prospecting here has not been deep and has afforded little knowledge of the extent of the ore body. A position upon the hillside about midway between the open cut at the northeast end of the sink and the shallow diggings in the ravine at its base is suggested as the best point for further prospecting. On the whole, the well developed sink structure and the several showings of ore mark the property as worthy of a thorough investigation.
An analysis of the soft, red ore showed 55.37% iron and 0.075% Phos.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsCommodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.Mineral List
1 valid mineral.
Rock Types Recorded
Note: data is currently VERY limited. Please bear with us while we work towards adding this information!
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
ⓘ Hematite Formula: Fe2O3 Reference: U.S. Geological Survey,2005, Mineral Resources Data System: U.S Geological Survey,Reston, Virginia |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 4 - Oxides and Hydroxides | |||
---|---|---|---|
ⓘ | Hematite | 4.CB.05 | Fe2O3 |
References
Sort by
Year (asc) Year (desc) Author (A-Z) Author (Z-A) In-text Citation No.Crane, G.W. (1912) The Iron Ores of Missouri. Missouri Bureau of Geology and Mines, Second Series, Volume 10: 211.
Other Regions, Features and Areas containing this locality
North America PlateTectonic Plate
- Mazatzal DomainDomain
This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to
visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders
for access and that you are aware of all safety precautions necessary.