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Map showing Seneca Lake and the other Finger Lakes in relation to Lake Ontario and upstate New York For comparison, Scotland's famous Loch Ness is 22.5 miles (36.2 km) long, 1.7 miles (2.7 km) wide, has a surface area of 21.8 square miles (56 km 2 ), an average depth of 433 feet (132 m), a maximum depth of 744.6 feet (227.0 m), and total volume ...
Senecaville Lake is a reservoir in Guernsey and Noble Counties, Ohio. It is located approximately 13 miles (21 km) southeast of Cambridge near the village of Senecaville, Ohio. The lake is popular among recreation and fishing enthusiasts. It is often referred to locally as Seneca Lake.
The capacity of the lake is 4.5 billion gallons (17 million m 3). [3] The lake was created by the construction of a dam on Little Seneca Creek. It was built to provide an emergency water supply for the metropolitan Washington, D.C. area, and it also provides a recreational amenity for the public. [4]
Seneca Lake State Park is a 141-acre (0.57 km 2) state park located in Seneca County, New York in the United States. [5] The park is at the north end of Seneca Lake , one of the Finger Lakes . The park is south of and between Geneva and Waterloo .
The Seneca River begins at Geneva in Seneca County, as the outflow of Seneca Lake, [6] flowing east past Waterloo and Seneca Falls.Skirting the northern end of Cayuga Lake at the Montezuma Marsh, it turns north, receiving the Clyde River from the west, forming the Seneca–Cayuga county line, then the border of Cayuga and Wayne counties.
Alcove Reservoir; Allegheny Reservoir; Amawalk Reservoir; Ashokan Reservoir; Basic Creek Reservoir; Beacon Reservoir, Dutchess County; Beacon Reservoir, Putnam County; Blake Falls Reservoir
The Cayuga–Seneca Canal is a canal in New York, United States. It is now part of the New York State Canal System. The canal connects the Erie Canal to Cayuga Lake and Seneca Lake and is approximately 20 miles (32 km) long. A multi-use trail runs beside a portion of the canal.
Map of the Finger Lakes. The lake depth, with steep east and west sides and shallow north and south ends, is typical of the Finger Lakes, as they were carved by glaciers during the last ice age. The water level is regulated by the Mud Lock at the north end of the lake. It is connected to Lake Ontario by the Erie Canal and Seneca Lake by the ...