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  2. Tide table - Wikipedia

    en.wikipedia.org/wiki/Tide_table

    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 ...

  3. Tide - Wikipedia

    en.wikipedia.org/wiki/Tide

    Tide. Simplified schematic of only the lunar portion of Earth's tides, showing (exaggerated) high tides at the sublunar point and its antipode for the hypothetical case of an ocean of constant depth without land, and on the assumption that Earth is not rotating; otherwise there is a lag angle. Solar tides not shown.

  4. Tidal range - Wikipedia

    en.wikipedia.org/wiki/Tidal_range

    Tidal range. Tidal range is the difference in height between high tide and low tide. Tides are the rise and fall of sea levels caused by gravitational forces exerted by the Moon and Sun, by Earth's rotation and by centrifugal force caused by Earth's progression around the Earth-Moon barycenter. Tidal range depends on time and location.

  5. Earth tide - Wikipedia

    en.wikipedia.org/wiki/Earth_tide

    Earth tide. Earth tide (also known as solid-Earth tide, crustal tide, body tide, bodily tide or land tide) is the displacement of the solid earth 's surface caused by the gravity of the Moon and Sun. Its main component has meter-level amplitude at periods of about 12 hours and longer. The largest body tide constituents are semi- diurnal, but ...

  6. Tide pool - Wikipedia

    en.wikipedia.org/wiki/Tide_pool

    A tide pool in Porto Covo, west coast of Portugal. A tide pool or rock pool is a shallow pool of seawater that forms on the rocky intertidal shore. These pools typically range from a few inches to a few feet deep and a few feet across. [1] Many of these pools exist as separate bodies of water only at low tide, as seawater gets trapped when the ...

  7. Amphidromic point - Wikipedia

    en.wikipedia.org/wiki/Amphidromic_point

    An amphidromic point, also called a tidal node, is a geographical location where there is little or no difference in sea height between high tide and low tide; it has zero tidal amplitude for one harmonic constituent of the tide. [2] The tidal range (the peak-to-peak amplitude, or the height difference between high tide and low tide) for that ...

  8. Tidewater, Oregon - Wikipedia

    en.wikipedia.org/wiki/Tidewater,_Oregon

    Coordinates and elevation from United States Geological Survey [1] Tidewater is an unincorporated community in Lincoln County, Oregon, United States located on the Alsea River east of Waldport on Oregon Route 34 . Tidewater was named because it is near the head of the tide of the Alsea River. [2] Tidewater post office was established in 1878.

  9. Slack tide - Wikipedia

    en.wikipedia.org/wiki/Slack_tide

    Slack tide or slack water is the short period in a body of tidal water when the water is completely unstressed, and there is no movement either way in the tidal stream. It occurs before the direction of the tidal stream reverses. [1] Slack water can be estimated using a tidal atlas or the tidal diamond information on a nautical chart. [2]

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