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Feldman and Winkelman Gypsum pits (Feldman Quarry; National Gypsum Co. Mine), PZ Ranch area, Dudleyville area, Pinal County, Arizona, USAi
Regional Level Types
Feldman and Winkelman Gypsum pits (Feldman Quarry; National Gypsum Co. Mine)Group of Pits
PZ Ranch area- not defined -
Dudleyville areaArea
Pinal CountyCounty
ArizonaState
USACountry

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Latitude & Longitude (WGS84):
32° 52' 41'' North , 110° 41' 31'' West
Latitude & Longitude (decimal):
Type:
Group of Pits
Nearest Settlements:
PlacePopulationDistance
Dudleyville959 (2011)13.1km
Winkelman346 (2017)14.2km
Hayden650 (2017)16.6km
Mammoth1,487 (2017)17.9km
Kearny2,038 (2017)28.5km
Mindat Locality ID:
47706
Long-form identifier:
mindat:1:2:47706:5
GUID (UUID V4):
c25a18b1-e58a-4101-8d69-16e2517bafac


A Gypsum occurrence located in secs. 26, 27 & 33, T6S, R16E, about 3¼ miles S of Dudleyville, on the East side of the San Pedro River, about 8½ miles South of Winkleman. Operated by the National Gypsum Co. and the Superior Companies.

Mineralization is thick beds of lacustrine gypsum deposits on both sides of the river. Gypsum is white to greyish white, granular to microcrystalline gypsum beds. The beds are 2.44 meters thick hosted in clay, mud, silt, diatomite and shale. They dip 3E.

This deposit may be extensive in area. It is exposed near the surface where it was mined, but, it is buried to the S and E and eroded away to the W and N except in isolated residual hills. Diatomite occurs as interbeds in the gypsum. In this area, a zone at least 100 feet thick contains thick (1-8 feet), massive, white to grayish white, granular to microcrystalline, flat-lying gypsum beds. The gypsum beds are separated by thin layers of calcareous and gypsiferous shale and silt.

The shale is calcareous to gypsiferous. The lacustrine basin occupies at least 18 square miles, principally along the east side of the San Pedro River, and dips about 3E. An exploration hole drilled to evaluate one of the deposits intersected a continuous 300 foot thick formation of interbedded clay and gypsum. Correlation with other drill holes suggests that the section of clay and gypsum may be more than 595 feet thick. Aravaipa Creek bisects the deposit. North of the creek, massive gypsum with clay partings (30-50 feet thick) is being mined.

The gypsum ore is drilled and blasted; then the broken gypsum is loaded and hauled to crushing plants where the minus 3/8 inch fraction is screened off. The final product contains 92% gypsum and less than 4% insolubles.

Assay data: Mostly 90% + gypsum. Reserves and resources are not estimated but are probably in the multimillion ton range.

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2 valid minerals.

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List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
Opal4.DA.10SiO2 · nH2O
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
Gypsum7.CD.40CaSO4 · 2H2O

List of minerals for each chemical element

HHydrogen
H GypsumCaSO4 · 2H2O
H OpalSiO2 · nH2O
OOxygen
O GypsumCaSO4 · 2H2O
O OpalSiO2 · nH2O
SiSilicon
Si OpalSiO2 · nH2O
SSulfur
S GypsumCaSO4 · 2H2O
CaCalcium
Ca GypsumCaSO4 · 2H2O

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Link to USGS MRDS:10060185

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