Information for "Traits:TidalStrength"
Basic information
Display title | Traits:TidalStrength |
Default sort key | TidalStrength |
Page length (in bytes) | 959 |
Page ID | 9522 |
Page content language | en - English |
Page content model | wikitext |
Indexing by robots | Allowed |
Number of redirects to this page | 0 |
Counted as a content page | Yes |
Page protection
Edit | Allow all users (infinite) |
Move | Allow all users (infinite) |
Edit history
Page creator | Josbut (talk | contribs) |
Date of page creation | 13:59, 24 November 2014 |
Latest editor | Harveytw (talk | contribs) |
Date of latest edit | 14:28, 1 June 2015 |
Total number of edits | 4 |
Total number of distinct authors | 4 |
Recent number of edits (within past 90 days) | 0 |
Recent number of distinct authors | 0 |
Page properties
Transcluded templates (11) | Templates used on this page:
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... more about "TidalStrength"
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The horizontal movement of water associate … The horizontal movement of water associated with the meteorological, oceanographical and topographical factors. High water flow rates result in areas where water is forced through or over restrictions for example narrows or around protruding offshore rocks. Tidal streams are associated with the rise and fall of the tide where as currents are defined as residual flow after the tidal element is removed (Hiscock, 1996). tidal element is removed (Hiscock, 1996). +
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