|Latitude & Longitude (WGS84):||39° 22' 27'' North , 76° 52' 3'' West|
|Latitude & Longitude (decimal):||39.37432,-76.86768|
|Köppen climate type:||Cfa : Humid subtropical climate|
Opening in Cockeysville Marble. Rocks present are fine grained dolomitic marble and coarser grained calcite marble with local calc-silicate areas, lenses of phlogopite schist and pegmatite pods.
Currently (2018) operated by Bluegrass Materials.
16 valid minerals.
This geological map and associated information on rock units at or nearby to the coordinates given for this locality is based on relatively small scale geological maps provided by various national Geological Surveys. This does not necessarily represent the complete geology at this locality but it gives a background for the region in which it is found.
Click on geological units on the map for more information. Click here to view full-screen map on Macrostrat.org
541 - 2500 Ma
|Wissahickon Formation; Lower Pelitic Schist|
Age: Proterozoic (541 - 2500 Ma)
Stratigraphic Name: Wissahickon Formation
Description: (Formerly mapped as oligoclase facies of Wissahickon Formation.) Medium- to coarse-grained biotite-oligoclase-muscovite-quartz schist with garnet, staurolite, and kyanite; fine- to medium-grained semipelitic schist; and fine-grained granular to weakly schistose psammitic granulite; psammitic beds increase upward; apparent thickness 5,500 feet or more.
Reference: Horton, J.D., C.A. San Juan, and D.B. Stoeser. The State Geologic Map Compilation (SGMC) geodatabase of the conterminous United States. doi: 10.3133/ds1052. U.S. Geological Survey Data Series 1052. 
1000 - 1600 Ma
|Mesoproterozoic crystalline metamorphic rocks|
Age: Mesoproterozoic (1000 - 1600 Ma)
Reference: Chorlton, L.B. Generalized geology of the world: bedrock domains and major faults in GIS format: a small-scale world geology map with an extended geological attribute database. doi: 10.4095/223767. Geological Survey of Canada, Open File 5529.