Mine Index 10069406   Yingling Mining Company,  Rose Creek Fluorspar Mines,Conley,Smee Shafts

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S-T-R 11-11S-7E
County: Hardin
Quadrangle: Herod
District: Fluorspar District
Subdistrict: Rose Creek Subdistrict

Mine Index Number: 10069406

ISGS ID: 9020 MSHA ID:
MAS ID: MRDS ID: W006923
Company Name: Yingling Mining Company
Mine/Site Name: Rose Creek Fluorspar Mines, Conley, Smee Shafts
Active/Abandoned: Abandoned
Start Date: Unknown End Date: Unknown
Commodity Type: Metallic, Non-Metallic
Commodity: Fluorspar, Lead, Zinc
Minerals Present: Galena, Fluorine
Type of Mine: Unknown
District: Fluorspar District Subdistrict: Rose Creek Subdistrict
County: Hardin
Section/Township/Range: 11-11S-7E
Latitude,Longitude: 37.57424,-88.40782
Unit(s) Mined: Chesterian Series, Glen Dean Limestone, Renault Limestone
Feature(s) Mined:
MRDS Link: https://mrdata.usgs.gov/mrds/show-mrds.php?dep id=10069406
Mindat link:

Primary source


Denny, F.B., W.J. Nelson, J.R. Breeden, and R.C. Lillie, 2020, Mines in the Illinois portion of the Illinois-Kentucky Fluorspar District: Illinois State Geological Survey, Circular 604, 73 p. and map.


Discussion

The Rose Creek Mines were operated by the Yingling Mining Company from 1942 to 1948 (Davis 1943, 1950) These mines were also called the Yingling Mines (Burmeister 1952) In 1942, Harve Smee sunk the Smee Shaft to 100 feet and drove drifts at the 50- and 100-foot levels (Burmeister 1952) The Conley Shaft was originally sunk to 90 feet (Burmeister 1952) but was later deepened to more than 300 feet. The vein lies along a fault trending N55°E and dipping 80°SE (Weller et al. 1952) Ozark-Mahoning mine maps indicated that the Conley Shaft was located in the middle of the mine workings. Working levels at 155, 215, 285, and 350 feet extended to the northeast and southwest along the fault away from the Conley Shaft. The Smee Shaft was at the northeast end of the mine and was also worked at the 50-foot level. The Minerva Oil Company commenced underground drilling in 1952, and the company reported low-grade ore below the 350-foot level between the main fault and the hanging wall fault. Most all of the exploration borings were drilled in a northwesterly or southeasterly direction to intersect a northeasterly striking fault or vein. Ozark-Mahoning maps suggest that a parallel fault, hosting 40% to 60% CaF2 ore, was present to the southeast and that between the two faults, lower grade mineralization attaining 15% to 20% CaF2 was present (Figure 10). Production at this mine from 1942 to 1949 was 8,500 tons of 60% CaF2 ore and 3,450 tons of 35% to 50% CaF2 ore (Burmeister 1952) In 1951, the Yingling Mining Company sold the Rose Creek property to the Minerva Oil Company (Holtzinger and Arundale 1955) Ozark-Mahoning mine maps indicate that additional ore was present along the master fault and in an east orebody. Minerva Oil Company reserve calculations from 1953 detailed that an additional 324,000 tons was possible along the master fault and that 97,000 tons was possible along the east orebody. Although the east orebody was 160 feet thick, with the top at 230 feet below the surface, the ore was low grade in sandstone and averaged about 19.6% CaF2. A hanging wall orebody was also present southeast of the Conley Mine workings. More information is needed to determine whether the low-grade ore was ever mined.


Mine Data/Information


Mine Data

Host and associated rocks

Host or associated Associated
Rock type Plutonic Rock
Rock unit name Mafic Dikes And Breccia Bodies
Rock description Mafic Dikes And Breccia Bodies
Stratigraphic age (youngest) Early Permian
Stratigraphic age (youngest) Early Permian
Stratigraphic age (youngest) Mississippian
Stratigraphic age (youngest) Mississippian
Host or associated Host
Rock type Sedimentary Rock > Carbonate > Limestone
Rock unit name Limestone
Rock description Limestone

Ore Body Information

General form LINEAR
Strike N 55 DEG E
Dip 80 DEG SE

References

  • Burmeister, H.L., 1952, Knox and Yingling fluorite mines, Hardin County, Illinois: U.S. Bureau of Mines, Report of Investigations 4856, 8 p.
  • Davis, H.W., 1943, Fluorspar and cryolite, in F.M. Shore, ed., Minerals yearbook 1941: U.S. Department of the Interior, Bureau of Mines, Economics and Statistics Service, p. 1399–1416.
  • Davis, H.W., 1950, Fluorspar and cryolite, in E.W. Pehrson and A.F. Matthews, eds., Minerals yearbook 1948: U.S. Department of the Interior, Bureau of Mines, Economics and Statistics Division, p. 525–544.
  • Holtzinger, J.E., and J.C. Arundale, 1955, Fluorspar and cryolite, in J.J. Forbes, ed., Minerals yearbook 1952: Metals and minerals (except fuels), Volume I: U.S. Department of the Interior, Bureau of Mines, Minerals Division, p. 418–431.
  • Weller, J.M., R.M. Grogan, and F.E. Tippie, 1952, Geology of the fluorspar deposits of Illinois: Illinois State Geological Survey, Bulletin 76, 147 p.
  • BAXTER, J. W., DESBOROUGH, G. A. AND SHAW, C. W., 1967, AREAL GEOLOGY OF THE ILLINOIS FLUORSPAR DISTRICT, PART 3: ILL. STATE GEOL. SURV. CIRC. 413, 41 P. (Reference from the USGS MRDS System)
  • 1942 GEOLMAP ILL. STATE GEOLOGICAL SURVEY, J. M. WELLER (Reference from the USGS MRDS System)
  • 1961 GEOLMAP ILL. STATE GEOLOGICAL SURVEY, G. A. DESBOROUGH (Reference from the USGS MRDS System)
  • MC GINNIS, L. D. AND BRADBURY, J. C., 1964, AEROMAGNETIC STUDY OF THE HARDIN COUNTY AREA, ILLINOIS: ILL. STATE GEOLOGICAL SURVEY CIRC. 363, 12 P. (Reference from the USGS MRDS System)

External Links

Mineral Resources Data System (MRDS) USGS Link
https://mrdata.usgs.gov/mrds/show-mrds.php?dep_id=10069406https://mrdata.usgs.gov/mrds/show-mrds.php?dep id=10069406