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The Woodstock Quartz Monzonite is a Silurian or Ordovician quartz monzonite pluton in Baltimore County, Maryland. It is described as a massive biotite-quartz monzonite which intrudes through the Baltimore Gneiss at a single locality surrounding the town of Granite, Maryland. The extent of this intrusion was originally mapped in 1892 as the "Woodstock granite". It was given its current name in 1964 by C. A. Hopson. Hopson grouped the Woodstock Quartz Monzonite with the Ellicott City Granodiorite and the Guilford Quartz Monzonite as "Late-kinematic intrusive masses."

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  • The Woodstock Quartz Monzonite is a Silurian or Ordovician quartz monzonite pluton in Baltimore County, Maryland. It is described as a massive biotite-quartz monzonite which intrudes through the Baltimore Gneiss at a single locality surrounding the town of Granite, Maryland. The extent of this intrusion was originally mapped in 1892 as the "Woodstock granite". It was given its current name in 1964 by C. A. Hopson. Hopson grouped the Woodstock Quartz Monzonite with the Ellicott City Granodiorite and the Guilford Quartz Monzonite as "Late-kinematic intrusive masses." Woodstock granite has been used in the Capitol Building, the Library of Congress, and in buildings in Baltimore. (en)
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  • 38122822 (xsd:integer)
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  • 11479 (xsd:nonNegativeInteger)
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  • 1095685873 (xsd:integer)
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dbp:age
  • Silurian or Ordovician (en)
dbp:area
  • ~400 Ha (en)
dbp:caption
  • Photographed on a boulder in Granite, Maryland (en)
dbp:country
dbp:extent
  • Western Baltimore County (en)
dbp:name
  • Woodstock Quartz Monzonite (en)
dbp:namedby
  • Williams and Darton, 1892 (en)
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dbp:period
  • Paleozoic (en)
dbp:prilithology
dbp:region
  • Piedmont of Maryland (en)
dbp:type
  • igneous (en)
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  • The Woodstock Quartz Monzonite is a Silurian or Ordovician quartz monzonite pluton in Baltimore County, Maryland. It is described as a massive biotite-quartz monzonite which intrudes through the Baltimore Gneiss at a single locality surrounding the town of Granite, Maryland. The extent of this intrusion was originally mapped in 1892 as the "Woodstock granite". It was given its current name in 1964 by C. A. Hopson. Hopson grouped the Woodstock Quartz Monzonite with the Ellicott City Granodiorite and the Guilford Quartz Monzonite as "Late-kinematic intrusive masses." (en)
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  • Woodstock Quartz Monzonite (en)
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