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Pea Ridge Mine, Sullivan, Washington Co., Missouri, USA
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Latitude: 38°7'34"N
Longitude: 91°2'51"W
 
 
A former Fe mine located near Meramec State Park and 13.8 km (8.6 miles) SE of Sullivan. Owned by the St. Joe Domestic Metals Corp, a subsidiary of the Fluor Corp. Produced 1.3 million tons of ore pellets (1984). Mine was closed and flooded in 2001.

Rare earth elements (REE)−bearing breccia pipes cut through the Pea Ridge massive magnetite-iron orebody. The Pea Ridge deposit is hosted by Precambrian volcanic rocks of the St. Francois terrane of southeastern Missouri. The magnetite-rich orebody is interpreted as a high-temperature, magmatic-hydrothermal deposit (Sidder and others, 1993) in ash-flow tuffs and lavas, which may have formed in the root of a volcanic caldera (Nuelle and others, 1991). Four mapped REE-bearing breccia pipes steeply crosscut the magnetite-hematite orebody and its altered rhyolite host rock. Exposed portions of the breccia pipes are as much as 60 m (197 ft) in horizontal length and as much as 15 m (49 ft) in width; the pipes extend below the mined levels to an undetermined depth (Seeger and others, 2001). Rare earth elements–bearing minerals in the breccia pipes include monazite, xenotime, and minor bastnasite and britholite. The REE concentrations reported in the breccia pipes are consistently high but variable. Nuelle and others (1992, p. A1) state, “Total REE oxide content of samples of the groundmass material, which are not diluted with lithic fragments, average about 20 weight percent.” Seeger and others (2001, p. 2) state, “Total REE oxide concentrations of grab samples range from about 2.5 to 19 weight percent.” Bulk sampling by the U.S. Bureau of Mines found REE oxides concentrations ranging from 7 to 25 weight percent and an average of 12 weight percent (Vierrether and Cornell, 1993).
A populated place (town).

Mineral List

Actinolite
Afwillite
Albite
'Allanite'
Altaite
Anatase
Andradite
Anhydrite
Antigorite
'Apatite'
Baryte
'Bastnäsite'
Bazzite
'Biotite'
Bornite
Britholite-(Ce)
Calcite
Cassiterite
Chalcocite
Chalcopyrite
Chamosite
'Chlorite Group'
Cobaltite
Covellite
Dolomite
Epidote
'Feldspar Group'
Fluorapatite
Fluorite
Galena
Glauconite
Gold
var: Electrum
Grunerite
Gypsum
Hematite
Hematite
var: Martite

Hessite
'Hornblende'
'Hypersthene'
Magnetite
Melonite
Millerite
Molybdenite
'Monazite'
Muscovite
Orthoclase
Palygorskite
'Parisite'
Pyrite
Quartz
var: Amethyst
Riebeckite
Rutile
Sepiolite
'Serpentine Group'
Sphalerite
Sylvanite
'Synchysite'
Tengerite-(Y)
Thorite
Titanite
Topaz
'Tourmaline'
Tremolite
Vesuvianite
'Xenotime'
Xenotime-(Y)
Zircon
Zoisite


70 entries listed. 53 valid minerals.

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References

Mining Annual Review (1985): 325.

C. W. Whitten and R. J. Yancey (1991) Characterization of the Rare-earth Mineralogy at the Pea Ridge Deposit, Missouri. USBM Report of Investigations 9331.

Vierrether and Cornell (1993).

Rocks and Minerals (1998): 73(2) (March-April 1998).

USGS Open File Report 2010-5220.

Grauch, R.I., Verplanck, P.L., Seeger, C.M., Budahn, J.R., and Van Gosen, B.S. (2010): Chemistry of Selected Core Samples, Concentrate, Tailings, and Tailings Pond Waters: Pea Ridge Iron (-Lanthanide-Gold) Deposit, Washington County, Missouri. USGS Open-File Report 10-1080.

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