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Brine from springs in and around the southern end of Onondaga Lake, from former brine wells dug or drilled at the lakes' edge, and from wells that tapped halite (common salt) beds near Tully, N.Y., 15 miles south of Syracuse, were used commercially from the late 1700's through the early 1900's for salt production. The rapid development of this industry in tie 18th and 19th centuries led to the nicknaming of Syracuse as "The Salt City." The brine originates from halite beds of the Salina C roup shales of central New York. The dissolution of halite by ground water creates a brine that moves through an unconsolidated basal aquifer northward to the springs near Syracuse. This report briefly presents the history of salt production in the Syracuse area, explains the origin of the halite deposits and the ground-water flow paths from the halite beds to Onondaga Lake, and discusses the need to understand the hydrogeology of the Onondaga Valley and potential changes in water quality (specifically salt water) in relation to current remediation of Onondaga Lake and other contaminated sites in the Onondaga Creek watershed.

Salt production in Syracuse, New York ("The Salt City") and the hydrogeology of the Onondaga Creek Valley