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. The extent of this formation was originally mapped in 1892 within Baltimore County.
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| - 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. The extent of this formation was originally mapped in 1892 within Baltimore County. (en)
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- Cambrian
- Carroll County, Maryland
- Beaver Dam, Maryland
- Precambrian
- Quarry Lake (Maryland)
- Baltimore County, Maryland
- Marble
- Howard County, Maryland
- Maryland
- Cockeysville, Maryland
- Piedmont (United States)
- Baltimore County, Maryland
- Washington Monument
- Washington Monument (Baltimore)
- Dolomite (rock)
- Schist
- Geology of Maryland
- Howard County, Maryland
- Gneiss
- Harford County, Maryland
- Harford County, Maryland
- Wissahickon Formation
- Silicate
- Marble
- Marriottsville, Maryland
- Martin Marietta Inc.
- Ordovician
- Carroll County, Maryland
- Setters Formation
- List of types of marble
![http://dbpedia.org/resource/File:Cockeysville_Formation_Massive_Metadolostone_Mbr.jpg](http://dbpedia.org/resource/File:Cockeysville_Formation_Massive_Metadolostone_Mbr.jpg) |
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| - Precambrian, Cambrian, or Ordovician (en)
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| - Polished slab of the marble from Cockeysville. Width of slab inside black border is approximately 10.7 cm. (en)
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| - Piedmont of Maryland (en)
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| - 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. The extent of this formation was originally mapped in 1892 within Baltimore County. (en)
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| - Williams and Darton, 1892 (en)
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