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  2. Titus Mill-Pond & New York State Tidal Wetlands - Wikipedia

    en.wikipedia.org/wiki/Titus_Mill-Pond_&_New_York...

    Titus Mill Pond & New York State Tidal Wetlands is located at the northeastern end of New Rochelle Harbor in the city of New Rochelle in Westchester, New York. The waters in the harbor and pond flow from Long Island Sound , with tides up to eight feet in the inlet and with no fresh water stream entering into it.

  3. List of tide mills on Long Island - Wikipedia

    en.wikipedia.org/wiki/List_of_tide_mills_on_Long...

    Lloyd Harbor, New York: Van Wyck-Lefferts Tide Mill: Tide mill: About 1793 The Van Wyck-Lefferts Tide Mill is a historic tide mill located at Lloyd Harbor in Suffolk County, New York. It was built about 1793 and is a 3+1⁄2-story, gable-roofed, timber-framed rectangular building little altered since the early 19th century.

  4. Tide table - Wikipedia

    en.wikipedia.org/wiki/Tide_table

    Tide tables, sometimes called tide charts, are used for tidal prediction and show the daily times and levels of high and low tides, usually for a particular location. [1] Tide heights at intermediate times (between high and low water) can be approximated by using the rule of twelfths or more accurately calculated by using a published tidal ...

  5. Van Wyck-Lefferts Tide Mill - Wikipedia

    en.wikipedia.org/wiki/Van_Wyck-Lefferts_Tide_Mill

    Van Wyck-Lefferts Tide Mill (/ v æ n ˈ w aɪ k / van WYKE) is a historic tide mill located at Lloyd Harbor in Suffolk County, New York. It was built about 1793 and is a 3 + 1 ⁄ 2-story, gable-roofed, timber-framed rectangular building little altered since the early 19th century. The property also includes the earthen mill dam with sluice ...

  6. Tide - Wikipedia

    en.wikipedia.org/wiki/Tide

    The water stops rising, reaching a local maximum called high tide. Sea level falls over several hours, revealing the intertidal zone; ebb tide. Oscillating currents produced by tides are known as tidal streams or tidal currents. The moment that the tidal current ceases is called slack water or slack tide. The tide then reverses direction and is ...

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  8. Long Island Sound - Wikipedia

    en.wikipedia.org/wiki/Long_Island_Sound

    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 ...

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