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Mine detail: Graham-Snyder Mine
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North America
United States
Illinois
Jo Daviess
Previously called ''
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Location
Lat / long:
42.47918, -90.43067
Resource(M)
Primary:
Zinc
Tertiary:
Lead
Ore:
Sphalerite
Gangue:
Calcite, Dolomite, Pyrite, Quartz
Discovery year:
1946
Production
Operation type:
Unknown
Production size:
Yes
Development status:
Past Producer
Production years:
194701953; REOPENED IN 1955, AND IN OPERATION IN JUN 1957.
First production started:
1947
Geology
Host rock:
Quimbys Mill Member, Platteville Formation;Stewartville Member, Galena Dolomite
Host type:
Limestone,Dolomite
Associated rock:
Spechts Ferry
Associated type:
Shale,Limestone
Structure:
Southeast Of Wisconsin Dome And On The Gentle West Limb Of Wisconsin Arch. To The South Is Illinois Basin And To The West And Southwest Is Forest City Basin. A Few Minles South O Fthe Zinc-Lead District Is Westward-Trending Savanna-Sabula Anticline. Regional Strike Is N 85 W And The Dip Is South.
Tectonic:
Stable Sedimentary Platform Having Later Mild Regional Deformation Sufficient To Produce Major And Minor Folds, Faults, Fracture Zones, And Joints.
Alteration processes:
Leaching, Silicification, Dolomitization
References
MRDS
W800154
DEP
10086277
Reference
{Deposit:: HEYL, A.V., AGNEW, A.F., LYONS, E.J., AND BEHRE, C.H., JR., 1959, THE GEOLOGY OF THE UPPER MISSISSIPPI VALLEY ZINC-LEAD DISTRICT: U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 309, 310 P}{Production:: HEYL AND OTHERS, 1959.}
Reporter
Hedgman, Cheryl (Cannon, W.F.), Sutphin, David M., Mason Jr., G.T.