A book of the west. Volume 1, Devon : $b being an introduction to Devon and CornwallBaring-Gould, S. (Sabine)
History
A book of the west. Volume 1, Devon : $b being an introduction to Devon and Cornwall
Baring-Gould, S. (Sabine)
Devon (England)
One James Robertson and a companion were at that hour crossing the
fields which then extended over this tract, and stumbled across a
slight ridge of gravel, which at first they thought must have been
made by some boys, but one of them stepping on to it, down sank
his leg, and his companion had to pull him out of a yawning chasm.
Next moment they saw that the whole surface of turf was starred and
splitting in all directions, and they fled for their lives. The
sound of the rending of the rocks they described as being much like
that of the tearing of cloth or flannel. Two other members of the
coastguard, who were stationed on the beach, now saw something begin
to rise out of the sea like the back of a gigantic whale; at the
same time the shore of shingles on which they stood lifted and fell,
like the heaving of a breast in sleep. The water was thrown into
violent agitation, foaming and spouting, and great volumes of mud
rushed up from below. The great back rose higher and ever higher,
and extended further till at last it formed a huge reef at a little
distance from the beach. This ridge was composed of the more solid
matter, chert and other pebbles, that had been in the sand under
the chalk, and which by the sinking of the chalk was squeezed out
like so much dough. It remained as a reef for some years, but has
now totally disappeared, having been carried away by the waves.
As the great chasm was formed, the masses from the sides falling
in were, as it were, mumbled and chewed up in the depths, and to
the eyes of the frightened spectators sent forth flashes of light;
they also supposed that an intolerable stench was emitted from the
abyss. But this was no more than the odours given out by the violent
attrition of the cherty sandstone and chalk grinding against each
other as they descended.
Throughout the 26th the subsided masses of the great chasm continued
sinking, and the elevated reef gradually rising; but by the evening
of that day everything had settled very nearly into the position in
which it remains at present, although edges have since lost their
sharpness and minor rents have been choked.
A writer whose reminiscences have been recently published describes
briefly the aspect of the place after the sinkage.
"I rode over to see this huge landslip. The greater part of a
farm had subsided a hundred feet or more. Hedges and fields,
with their crops of turnips, etc., were undisturbed by the fall,
and broken off sharply from the ground a hundred feet above.
There was a rather dislocated ridge on the shore, which formed
a sort of moraine to the slip. On this part were some cottages
twisted about, but still holding together, and having their
gardens and even their wells attached; yet the shock of the
falling mass had been so great as to cause the upheaval of an
island off shore."
Public-domain text, read in full here on John Shaqi.
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