The site is underlain by metamorphic bedrock consisting primarily of garnet and quartz rich biotite schist. It is encountered at about 78 feet bgs.The bedrock is dominated by foliation striking northeast-southwest and dipping to the south between 60 and 90 degrees with joints generally orienting and dipping in the same direction. Two bedrock ridges cross the site from northeast to southwest.

The overburden consists of glacial deposits and weathered bedrock.

Overburden groundwater is found in the sand with the water table being about 10 feet bgs. The vertical gradient is downward.

• Fractured Bedrock

The 1,1,2-Trichloro-1,2,2-trifluoroethane (Freon 113) plume in the bedrock was about 780 feet wide at its widest and 1,600 feet long.

• Trichloroethene (27 µg/L)
• 1,1,2-Trichloro-1,2,2-Trifluoroethane (1,400 µg/L)

• Pump and Treat

New York State Groundwater Quality Standards.

Since start up the plume has been greatly reduced in size and most wells are nondetect.

http://www.epa.gov/region02/waste/fsibmtj.htm