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Cayuga Lake (pronounced either "kA-'yü-g&" or "kI-'yü-g&") is the longest of western New York's glacial Finger Lakes, and is the second largest in surface area (marginally smaller than Seneca Lake) and volume. It is just under 40 miles long. Its average width is 1.7 miles, and it is 3.5 miles wide at its widest point near Aurora. It is approximately 435 feet deep at its deepest point.
LocationThe lake has one small island near Union Springs, Frontenac Island, which is one of only two islands in all of the Finger Lakes.
Villages and settlements along the east shore of Cayuga Lake include Myers, King Ferry, Aurora, Levanna, Union Springs, and Cayuga. Settlements along the west shore of the lake include Sheldrake, Poplar Beach, and Canoga. Geographical characteristicsCayuga Lake is located at ; 116.4 m above sea level. Its depth, steep east and west sides with shallow north and south ends is typical of the Finger Lakes, as they were carved by glaciers during the last ice age. Length: 61.4 km
The north end is dominated by shallow mudflats and is an important stopover for migratory birds, where Montezuma National Wildlife Refuge is located. The southern end is also shallow and often freezes during the winter. Human impactImage:CayugaLake.jpg Winter view of the southern end of Cayuga Lake The fish population is managed and substantial sport fishing is practised, including smelt, lake trout and smallmouth bass fishing. Cayuga lake is very popular among recreational boaters. A large state marina and boat launch is located at the southern end of the lake in Ithaca (Allan H. Treman State Marine Park, the largest inland marina in New York). There are two yacht clubs on the western shore: Ithaca Yacht Club a few miles north of Ithaca, and Red Jacket Yacht Club just south of Canoga. There are several other marinas and boat launches scattered along the lake shore. The lake is used both for drinking water and waste disposal, although this is no longer legal and very uncommon. There are also several lake source cooling systems that are in operation on the lake, whereby cooler water is pumped from the depths of the lake, warmed, and circulated in a closed system back to the surface. One of these systems, which is operated by Cornell University and began operation in 2000, was controversial during the planning and building states for potential negative environmental impact; however, all the environmental impact reports and scientific studies have shown that the Cornell lake source cooling system has not yet and will not likely have any measurably significant environmental impact. Furthermore, Cornell's system pumps significantly less warm water back into the lake than others further north which have been operating for decades. Trivia
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