History
Fayetteville Green Lake (FGL) was the first lake in North America identified as meromictic, and is the best studied meromictic lake in the world with records dating back to 1839. Green Lake was referred to as Lake Sodom by Lardner Vanuxem, who was the first to study Green Lake in 1839, and the presence of sulfide in the deeper waters of the lake was known by 1849. FGL is believed to have formed as a plunge pool during the late Wisconsin stage of glaciation at the base of a waterfall formed by the retreating glaciers, which is the reason for its extreme depth relative to a small surface area. The outflow for FGL runs underneath the Erie Canal, which is located within 300m of the north shore of the lake. FGL is currently located in Green Lakes State Park, and since 1933 large quantities of sand have been dumped on the shore of the north end to create a swimming area.
Read more about this topic: Green Lake (New York)
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