A Guide to the Mount's Bay and the Land's End: Comprehending the topography, botany, agriculture, fisheries, antiquities, mining, mineralogy and geology of West Cornwall — John Shaqi
A Guide to the Mount's Bay and the Land's End: Comprehending the topography, botany, agriculture, fisheries, antiquities, mining, mineralogy and geology of West CornwallParis, John Ayrton
History
A Guide to the Mount's Bay and the Land's End: Comprehending the topography, botany, agriculture, fisheries, antiquities, mining, mineralogy and geology of West Cornwall
Paris, John Ayrton
Cornwall (England : County) -- Guidebooks
Notwithstanding the supposed moisture of the Mount's Bay, the
air is not less fit for respiration, nor less beneficial to the
valetudinarian, than that of drier situations. The porous nature of
the shelfy substratum soon disposes of any excess of water; so that,
after a short cessation of rain, the invalid may safely venture abroad
to enjoy the delightful walks which surround the bay; at the same
time, the numerous promontories which distinguish this coast, promote
a constant circulation of breezes around their extremities, so that
mists seldom linger, and we never experience those sultry calms, or
suffocating fogs, which not unfrequently infest other parts of our
island.
As Cornwall is directly exposed to the expanse of the Atlantic ocean,
lying south-west of it, we cannot be surprised that the winds, which
blow so generally from that quarter, should occasionally produce
very violent storms. Their approach is frequently predicted by
the experienced fisherman, from the agitation of the water along
shore, a phenomenon which is called a "_ground swell_;" and which is
probably occasioned by a storm in the Atlantic, with the wind west;
in which case, as the storm proceeds eastward, the waves raised by
it will outgo the wind, and reach the eastern coast long before it.
A tremendous instance of this kind occurred, during the residence
of the author of these pages, on the night of Sunday, January 19th,
1817. The storm assumed the character of a hurricane, and acting in
conjunction with a spring tide, impelled the waves with such fury,
that they actually broke over the mast heads of the vessels which
were lying within Penzance harbour, and bore down every thing before
them; two of the four pillars recently erected for the reception of
a light were thrown down, and several of the foundation stones of the
pier removed. The windows of the bath-house were demolished, and the
whole of its furniture washed into the sea. The green between Penzance
and Newlyn was torn up, and several boats, lying on the strand were
actually carried into the neighbouring meadows. The towns of Newlyn and
Mousehole suffered corresponding damage, and several of their houses
were washed away. The road between Marazion and St. Michael's Mount
was torn from its lowest foundation, and stones of more than a ton
in weight, though clamped together with massy iron, were severed and
removed from their situation. The turnpike road between Penzance and
Marazion was, in many places, buried with sand; and in others, broken
up by the violence of the waves, and covered by the sea to the depth of
from three to five feet. Had the violence of the storm lasted but a few
hours longer, who will venture to say that the two channels would not
have been united by the inundation of the low land which constitutes
the isthmus, and the district of the Land's end been converted into an
island!
Public-domain text, read in full here on John Shaqi.
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