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Edison Cement Co. Quarry (Tilcon quarry), White Township, Warren County, New Jersey, USAi
Regional Level Types
Edison Cement Co. Quarry (Tilcon quarry)Quarry
White TownshipTownship
Warren CountyCounty
New JerseyState
USACountry

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Latitude & Longitude (WGS84):
40° 49' 14'' North , 75° 1' 4'' West
Latitude & Longitude (decimal):
Type:
Nearest Settlements:
PlacePopulationDistance
Buttzville146 (2017)1.6km
Bridgeville106 (2017)1.9km
Oxford1,090 (2017)3.1km
Brookfield675 (2017)3.6km
Belvidere2,607 (2017)5.1km
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
ClubLocationDistance
Monroe County Earth Science AssociationStroudsburg, Pennsylvania24km
Morris Museum Mineralogical SocietyMorristown, New Jersey45km
Mindat Locality ID:
12506
Long-form identifier:
mindat:1:2:12506:5
GUID (UUID V4):
91b21de3-7d18-452d-adb7-cbc5166183f7


A limestone quarry in coarse-grained Precambrian marble.
Located about 2 miles NW of Oxford. This is another of Thomas Alva Edison's business ventures connected with his Portland Cement industry. The quarry was dormant for many years prior to the mid 1970's when it was worked by the Oxford Stone Co. who also operated a nearby quarry in gneiss.

In the 1980's the property was acquired by Millington Quarry Co. and turned into a major operation. Millington's holdings, along with those of many other aggregate producers in the region, were acquired by Tilcon in the 1990's. Tilcon is the current operator (2008).

The quarry is opened in the largest outcropping area of Precambrian marble south of the Franklin - Sterling Hill area 25 airline miles to the northeast. Proterozoic marble is best known in the Reading Prong Highlands in the Lime Crest and Franklin/Sterling Hill, NJ and northward to the Amity, NY area. However, marble outcrops sporadically along the northwest margin of the Reading Prong from its principal outcrop area southwestward into Pennsylvania. The marble exposed along the northwestern edge of the Reading Prong is now interpreted (Volkert, 2004) as a carbonate shelf on the margin of a back arc basin. The marble at Oxford is at least broadly equivalent to the Franklin marble in its type area. At Oxford the rock generally contains far fewer concentrations of silicate minerals. The spinel and corundum assemblages present at Lime Crest and elsewhere in the Franklin marble are very rare or absent at Oxford.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


8 valid minerals.

Rock Types Recorded

Note: data is currently VERY limited. Please bear with us while we work towards adding this information!

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Alphabetical List Tree Diagram

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
β“˜Graphite1.CB.05aC
Group 2 - Sulphides and Sulfosalts
β“˜Sphalerite2.CB.05aZnS
β“˜Chalcopyrite2.CB.10aCuFeS2
β“˜Galena2.CD.10PbS
β“˜Pyrite2.EB.05aFeS2
Group 3 - Halides
β“˜Fluorite3.AB.25CaF2
Group 5 - Nitrates and Carbonates
β“˜Calcite5.AB.05CaCO3
Group 9 - Silicates
β“˜Diopside9.DA.15CaMgSi2O6

Other Regions, Features and Areas containing this locality


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