The Life of Henry Bradley Plant: Founder and President of the Plant System of Railroads and Steamships and Also of the Southern Express CompanySmyth, G. Hutchinson (George Hutchinson)
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The Life of Henry Bradley Plant: Founder and President of the Plant System of Railroads and Steamships and Also of the Southern Express Company
Smyth, G. Hutchinson (George Hutchinson)
Plant family; Plant, Henry Bradley, 1819-1899
“The Goodwin sands, about five miles off the coast of Kent, were at one
time a portion of the mainland itself and the property of Earl Goodwin.
But the sea has swallowed them up.
“The coast of Norfolk is minus three villages which it once
possessed--Shipden, Eccles, and Wimpwell--all of which have been taken
into the arms of the encroaching ocean. The Cromer of to-day stands
miles inland of the original Cromer.
“Auburn and Harlburn, two Yorkshire villages, once promised to develop
into seaport towns of considerable importance; but, like the will of
Canute, the will of the inhabitants of these villages was ignored by the
rising sea, and Auburn and Harlburn now exist in mere names and
sand-banks.
“Dunwich, on the coast of Suffolk, is gradually being swallowed up.
Every now and then the inhabitants move a distance inland, rebuild their
houses and shops and wait patiently and philosophically for the next
“notice to quit” from the sea. Many other seaside places have suffered
or are suffering a similar fate.
“It may be argued, on the other hand, that some seaside towns are
gradually becoming inland towns by the failure of the sea to ‘come up to
the mark,’ and running out only to run in for a shorter distance.
Winchelsea, Sandwich, Rye, and Southport are all suffering in this way.
Winchelsea and Rye were originally two of our cinque ports, but the sea
has left them standing high and dry. Sandwich was once a highly
important seaport town. It now stands two or three miles inland.
“The sea is leaving Southport quite in the lurch--so much so indeed that
the inhabitants have had to sink extensive lakes down on the beach to
keep the sea from running off altogether and leaving merely an ordinary
inland town.
“But the extension of our island in this way is very much less than the
encroachment of the sea at other points, and while our land is certainly
becoming more extensive in one direction, it is contracting, and with
much greater rapidity, in some other. And the ultimate effect may be
that our mountain peaks may form small islands, and eventually be
pointed out by posterity as ‘the position in which Great Britain is
reputed to have stood.’”
Public-domain text, read in full here on John Shaqi.
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