England -- Description and travel; London (England) -- Description and travel; Thames River (England)
Northfleet, formerly a small village straggling up the side of a
chalk hill, is now to all intents a suburb of Gravesend, so largely
has each grown in recent years. Here, officially at any rate, are
situated (about a mile to the west of Gravesend proper) those notorious
Rosherville Gardens which in the middle of last century made Gravesend
famous, and provided Londoners with a plausible reason for a trip down
the River. The gardens were laid out in 1830 to 1835 by one Jeremiah
Rosher, several disused chalk-pits being used for the purpose; and here
the jovial Cockney visitors regaled themselves within quaint little
arbours with tea and the famous Gravesend shrimps, and later danced to
the light of Chinese lanterns till it was time to return citywards from
the day’s high jinks.
The Dockyard at Northfleet, constructed towards the end of the
eighteenth century, was at one time a place of considerable importance,
for here were built and launched numbers of fine vessels, both on
behalf of the Royal Navy and of the East India Company. Now it has
dwindled to comparative insignificance. Indeed, from a shipping point
of view, the only interest lies in the numerous and familiar tan-sailed
barges of the Associated Portland Cement Manufacturers; for Northfleet
is one of the main centres of the cement industry so far as the
Thames-side is concerned—an industry which is in evidence right along
this stretch till the chalk hills end at Greenhithe, the town from
which Sir John Franklin set out in 1845 on his illfated expedition to
the North-West Passage.
At Grays (or Grays Thurrock, as it is more properly called), on the
Essex bank, are numbers of those curious subterranean chalk caves which
are a feature of most of the chalk uplands on both sides of the River,
and which have caused so much discussion among the archæologists. These
consist of vertical shafts, 3 or 4 feet in diameter, dug down through
anything from 50 to 100 feet of sand into the chalk below, where they
widen out into caves 20 or more feet long. As many as seventy-two of
them have been counted within a space of 4 acres in the Hangman’s Wood
at Grays. What they were for no one can tell. All sorts of things
have been conjectured, from the fabulous gold-mines of Cunobeline to
the smugglers’ refuges of comparatively modern times. One thing is
certain: they are of tremendous age. Probably they were used by their
makers mainly as secret storehouses for grain. They are commonly called
Dene-holes or Dane-holes, and are said to have served as hiding-places
in that hazardous period when the Danes made life in the valley
anything but pleasant. But this, while it may have been true, in no way
solves the mystery of their origin.
Public-domain text, read in full here on John Shaqi.
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