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Granite Historic District is a national historic district in Granite, Baltimore County, Maryland, United States. It comprises the focus of a rural quarrying community located in the Patapsco Valley of western Baltimore County, Maryland. It includes two churches, a school, a social hall, former commercial buildings, and houses and outbuildings ...
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.
Beaver Dam, Maryland, a now "flooded marble quarry in Cockeysville, Maryland, that has been used as a swimming location since the 1930s. Source of dolomitic marble known specifically as Cockeysville Marble for the Washington Monument in Washington, D.C. and many other purposes in the eastern U.S. Greenspring Quarry, now a lake, Pikesville, Maryland
Granite is an unincorporated community in Baltimore County, Maryland, United States. [1] Originally known as Waltersville, it was renamed Granite in recognition of its principal product (the Woodstock Quartz Monzonite was quarried). The village was the center of this industry, which during its peak in the late 19th century provided building ...
The Grace Methodist Episcopal Church in Baltimore City, an example of a building built in part from "Falls Road blue gneiss." The name Baltimore Gneiss was first used by George Huntington Williams in 1892 [5] to describe the variety of widely distributed gneisses in the Baltimore area.
The Walters/Blunt family of Waltersville (later Granite, Maryland) "founded the local quarrying industry circa 1820." [6]The 1898 account of Edward B. Mathews of the Maryland Geological Survey [5] of the quarries at Granite (formerly known as Waltersville) begins with boulders attracting the attention of "several enterprising men from New Hampshire," (Sweatt, Putney, and Riddle) who commenced ...
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