The History of Lynn, Vol. 1 [of 2]Richards, William
History
The History of Lynn, Vol. 1 [of 2]
Richards, William
Fens, The (England); King's Lynn (England)
Things appear to have continued pretty much in this favourable state,
till sometime after the erection of the Sluices at Denver; which by
preventing the tides from going further up into the country, as before,
proved very prejudicial to the harbour and Navigation of Lynn; and the
effects are felt, it seems, and much complained of to this day. The free
admission of the tides, and the natural course of the freshes are said to
have kept other rivers open and navigable; and this appears to have been
the case with the Ouse itself, while it possessed those advantages, or
till the adventurers erected the said sluices across its channel, which
are thought to have proved so very prejudicial, not only to the
navigation of Lynn, Cambridge, &c. but even to the draining of the Fen
districts and Marshland.
Before the erection of those sluices, the tide is said to have gone up
the rivers a very great way. Into the Ouse, and Grant, or Cam, it went,
according to _Badeslade_, five miles above their junction, or 48 above
Lynn; into the Larke, or Mildenhall river, eight miles above its month,
or 42 above Lynn; into the lesser Ouse, or Brandon river, ten miles above
its mouth, or 36 above Lynn; into the Wessey, or Stoke river, six miles
above its mouth, or 24 above Lynn; and into the Nene, seven miles above
its mouth, or 23 above Lynn. {24a}—These rivers are said to be then
completely supplied with water from the sea, in the driest seasons, to
serve for inland navigation.—The Nene, to Well, Marsh, and Peterborough,
&c. with vessels of 15 tuns in the driest times: the Ouse, with vessels
of 40 tuns, 36 miles, at least, from Lynn, in ordinary neap tides; and to
Huntingdon, St. Neots, Bedford, and even as far as 90 miles from Lynn,
with vessels of 15 tuns. The tides then raised the waters at Salters
Lode 12 feet above low-water mark. These waters in their return scoured
the channel, and kept it clear and deep. This seems to have been the
case before the erection of the sluices; but whether it would have
continued so to this time, may, perhaps, be doubted. Badeslade and
Kinderly seem to have entertained different and opposite opinions on the
subject; as the reader may see by consulting their respective
publications.
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