 | John Walker (geographer to the East India company.) - 1858 - 260 páginas
...Southampton, and there is no fall of consequence until the tide begins to slack at Spithead; but when the tide makes to the eastward at Spithead, the water falls...Southampton. After low water the tide rises pretty steadily for 7 hours, which may be considered as the proper high water ; it then ebbs for an hour about 9 inches,... | |
 | 1862 - 670 páginas
...Portland, there are -what are termed the first and second high -waters. This double high water is probahly caused by the tidal stream at Spithead, for, as long...falls rapidly at Southampton. After low water, the tiderises there pretty steadily for 7 hours, which mny be considered as the Jirst or proper high water... | |
 | Admiralty hydrogr. dept - 1863 - 288 páginas
...and there is no fall of consequence until the tide begins to slack at Spithead ; but when the tide makes to the eastward at Spithead, the water falls rapidly at Southampton (see p. 135). After low water the tide rises pretty steadily for about 65 hours, which may be considered... | |
 | 1865 - 916 páginas
...and as far to the westward as Portland, there are what are termed the first and sccunil high waters. This double high water is probably caused by the tidal...falls rapidly at Southampton. After low water, the tiderises there pretty steadily for 7 hours, which may be considered as the first or proper high water... | |
 | 1869 - 728 páginas
...Solent, and as far to the westward as Portland, there are what are termed iaeßrst and secom/high waters. This double high water is probably caused by the tidal...falls rapidly at Southampton. After low water, the tiderises there pretty steadily for 7 hours, which may be considered as the first or proper high water... | |
 | sir Frederick George D. Bedford - 1875 - 542 páginas
...and as far to the Westward as Portland, there are what are termed the./? rst and second high waters. This double high water is probably caused by the tidal...makes to the Eastward at Spithead, the water falls at Southampton. After low water, the tide rises there steadily for 7 hours, which may be considered... | |
 | Sir Frederick George Denham Bedford - 1875 - 532 páginas
...Spithead, for, as long as that stream runs strong to the Westward the tide is kept up in Southa1i()ton water, and there is no fall, of consequence, until...makes to the Eastward at Spithead, the water falls at Southampton. After low water, the tide rises there steadily for 7 hours, which may be considered... | |
 | 1882 - 764 páginas
...runs restward the tido is kept up in Southampton water, and there is no fall of consequence until the to slack at Spithead, but when the stream makes to the eastward at Spithead the wnler falls rapidly n. After low water, the tide rises there prettjr steadily for 7 hours, which may... | |
 | 1876 - 746 páginas
...runs stward the tide is kept up in Southampton water, and there is no fall of consequence until the i slack at Spithead, but when the stream makes to the eastward at Spithead the water fulls rapidlj . After low water, the tide rises there pretty steadily for 7 hours, which may be considered... | |
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Portland, there are what are termed the first and sccunil high waters. This double high water is probably caused by the tidal stream at Spithead, for, as long as that stream runs strong to the westward the tide is kept up in Southampton water, and there... 