Cockeysville Marble | |
---|---|
Stratigraphic range: Precambrian, Cambrian, or Ordovician | |
Type | metamorphic |
Unit of | Glenarm Supergroup |
Underlies | Wissahickon Formation |
Overlies | Setters Formation |
Thickness | about 750 feet[1] |
Lithology | |
Primary | marble |
Location | |
Region | Piedmont of Maryland |
Type section | |
Named for | Cockeysville, Maryland |
Named by | Williams and Darton, 1892[2] |
The Cockeysville Marble is a Precambrian, Cambrian, or Ordovician marble formation in Baltimore, Carroll, Harford and Howard Counties, Maryland. It is described as a predominantly metadolomite, calc-schist, and calcite marble, with calc-gneiss and calc-silicate marble being widespread but minor.[1]
The extent of this formation was originally mapped in 1892[2] within Baltimore County.