The
dolomitic marble is known to geologists as
Cockeysville Marble. It was considered some of the finest quality in the world according to government experts, noted for its purity of color and hardness suitable for building material and monuments.
Benjamin Latrobe ranked the Cockeysville stone over Italian
Carrara marble. Stone was loaded onto wagons and pulled by oxen to the nearby
Northern Central Railway in Cockeysville. The quarry site was connected to a rail spur in around 1866 to facilitate moving the massive columns for the expansion of the
United States Capitol. In 1878,
Hugh Sisson ("Marble King of Baltimore"), acquired the property and other surrounding quarries and began using the latest technology of machine-powered derricks, shovels, and diamond bit drills, significantly increasing production. For many other notable buildings, the stone is only identified as being "Cockeysville Marble" or coming from Baltimore County (Hannibal 2020 for a comprehensive list). While the specific quarry is unknown in these cases, it could have come from the Beaver Dam quarry. Marble was also used in numerous homes, businesses, and cemeteries, including Baltimore's iconic rowhouse
marble steps. About a half mile south lies Texas Quarry, a large active quarry operated by
Martin Marietta. It is located in the former town of
Texas, Maryland, which later merged into Cockeysville. Texas Quarry is of a similar age to the Beaver Dam quarries and was also a major producer of building marble. Its most notable use was for the Washington Monument, where a visible difference in the stone reveals the two quarries' distinct contributions. The whiter marble of the monument's bottom 152 feet came from Texas Quarry, while the warmer-toned marble of the next 390 feet is from Beaver Dam quarry. Today, Texas Quarry primarily produces aggregates such as gravel. ==Lake==