Cockeysville Marble
| Cockeysville Marble | |
|---|---|
| Stratigraphic range: Precambrian, Cambrian, or Ordovician | |
Polished slab of the marble from Cockeysville. Width of slab inside black border is approximately 10.7 cm. | |
| Type | metamorphic |
| Unit of | Glenarm Supergroup |
| Underlies | Wissahickon Formation |
| Overlies | Setters Formation |
| Thickness | about 750 feet |
| Lithology | |
| Primary | marble |
| Location | |
| Region | Piedmont of Maryland |
| Type section | |
| Named for | Cockeysville, Maryland |
| Named by | Williams and Darton, 1892 |
The Cockeysville Marble is a Precambrian, Cambrian, or Ordovician marble formation in Baltimore, Carroll, Harford and Howard Counties, Maryland. It also occurs in two locations in northern Delaware. It is described as a predominantly metadolomite, calc-schist, and calcite marble, with calc-gneiss and calc-silicate marble being widespread but minor.
The extent of this formation was originally mapped in 1892 within Baltimore County by G. H. William, who also named it Cockeysville Marble.
Due to its historical significance, it was proposed in 2020 to include it as a Global Heritage Stone Resource, a designation that provides international recognition of natural stone resources that have achieved widespread utilization in human culture.