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- Q432343 subject Q6274556.
- Q432343 subject Q8864259.
- Q432343 abstract "Slack water, which used to be known as 'the stand of the tide', is a short period in a body of tidal water when the water is completely unstressed, and therefore no movement either way in the tidal stream, and which occurs before the direction of the tidal stream reverses. Slack water can be estimated using a tidal atlas or the tidal diamond information on a nautical chart. It is a common misconception that the time of slack water occurs at high and low water, that is, at the greatest and lowest height of tide. In fact, the time of slack water, particularly in constricted waters, does not occur at high and low water, and in certain areas, such as Primera Angostura, the ebb may run for up to three hours after the water level has started to rise, and the flood may run for three hours after the water has started to fall. Thornton Lecky, writing in 1884, illustrates the phenomenon with an inland basin of infinite size, connected to the sea by a narrow mouth. Since the level of the basin is always at mean sea level, the flood in the mouth starts at half tide, and its velocity is at its greatest at the time of high water, with the strongest ebb occurring conversely at low water.".
- Q432343 wikiPageWikiLink Q1096878.
- Q432343 wikiPageWikiLink Q1323629.
- Q432343 wikiPageWikiLink Q1324526.
- Q432343 wikiPageWikiLink Q1542568.
- Q432343 wikiPageWikiLink Q23384.
- Q432343 wikiPageWikiLink Q2485919.
- Q432343 wikiPageWikiLink Q35715.
- Q432343 wikiPageWikiLink Q36124.
- Q432343 wikiPageWikiLink Q36687.
- Q432343 wikiPageWikiLink Q408.
- Q432343 wikiPageWikiLink Q4918.
- Q432343 wikiPageWikiLink Q613334.
- Q432343 wikiPageWikiLink Q6274556.
- Q432343 wikiPageWikiLink Q654068.
- Q432343 wikiPageWikiLink Q7243412.
- Q432343 wikiPageWikiLink Q728502.
- Q432343 wikiPageWikiLink Q7760830.
- Q432343 wikiPageWikiLink Q7800782.
- Q432343 wikiPageWikiLink Q7800785.
- Q432343 wikiPageWikiLink Q8864259.
- Q432343 wikiPageWikiLink Q922298.
- Q432343 comment "Slack water, which used to be known as 'the stand of the tide', is a short period in a body of tidal water when the water is completely unstressed, and therefore no movement either way in the tidal stream, and which occurs before the direction of the tidal stream reverses. Slack water can be estimated using a tidal atlas or the tidal diamond information on a nautical chart.".
- Q432343 label "Slack water".