Bare Hills Serpentine Quarry East, Bare Hills, Baltimore Co., Maryland, USA
|Latitude & Longitude (WGS84):||39° 23' 13'' North , 76° 39' 31'' West|
|Latitude & Longitude (decimal):||39.38687,-76.65868|
|Köppen climate type:||Cfa : Humid subtropical climate|
Abandoned serpentine quarry- "Produced block serpentine for building and decorative stone, including some verde antique, and crushed serpentine for roads and concrete." Active in the 1890's by the Lake Chrome and Mineral Company and in the 1920's by Lewis O. Stern.
9 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
|Paleozoic - Proterozoic|
252.17 - 2500 Ma
Age: to Permian (252.17 - 2500 Ma)
Description: Chiefly serpentinite with partly to completely altered dunite, peridotite, pyroxenite, and massive to schistose soapstone; talc-carbonate rock and altered gabbro are common in some bodies.
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.