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About 18,000 years ago, Connecticut, Long Island Sound, and much of Long Island were covered by a thick sheet of ice, part of the Late Wisconsin Glacier. About 3,300 feet (1,000 m) thick in its interior and about 1,300 to 1,600 feet (400 to 500 m) thick along its southern edge, it was the most recent of a series of glaciations that covered the ...
[1] [2] It travels under the Long Island Sound between Westchester County and Long Island; this undersea section is roughly 8 miles (13 km) in length (the entire line is roughly 26 miles (42 km) long). [3] [1] [4] The average depth of the undersea section is 10–15 feet (3.0–4.6 m) below the Long Island Sound's seabed. [1]
The Cross-Sound Cable can transmit a maximum power of 330 MW at a voltage of +/- 150 kV DC. The maximum current for Cross-Sound Cable is 1175 amperes.The Cross-Sound Cable is not simply a pair of underwater HVDC cables; rather it is a bundle of cables that includes the HVDC transmission lines and fiber-optic cables for phone and Internet data transfer.
Long Island Sound at night, with nearby settlements marked. The Long Island Sound link is a proposed bridge or tunnel that would link Long Island, New York, to Westchester County or Connecticut, across Long Island Sound east of the Throgs Neck Bridge. The project has been studied and debated since the mid-20th century.
The Y-50 Cable (also known as the Dunwoodie–Glenwood Line) is an undersea and underground high voltage electric transmission cable between Westchester County and Long Island via the Long Island Sound and Hempstead Harbor in New York, United States.
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The fore-edge lake formed by glacial meltwater expanded to be about the same size as present-day Long Island Sound; it may have been connected at times with similar freshwater lakes in Block Island Sound and Buzzards Bay, while sea level was low. The fairly shallow average depth of 78 feet (24 m) of today's Long Island Sound is the result of ...