Henry Smeaton: A Jacobite Story of the Reign of George the First. — John Shaqi
Henry Smeaton: A Jacobite Story of the Reign of George the First.James, G. P. R. (George Payne Rainsford)
General
Henry Smeaton: A Jacobite Story of the Reign of George the First.
James, G. P. R. (George Payne Rainsford)
Jacobite Rebellion, 1715 -- Fiction
The place to which I allude is a little bay, taking somewhat the form
of a horse-shoe, and indenting the land deeply. It is formed by a high
headland, on the south western side, which shelters it from the
prevailing winds. The face of this promontory, to its very extreme
point, is one precipitous cliff of cold grey stone, varying from six
to nine hundred feet in height, rugged and broken indeed, but
apparently pathless; and bold would be the man who should attempt to
scale it; still bolder he who should seek to descend from the height
above. This is called Ale Head; and the opposite limb of the bay
consists of another promontory, not so steep or precipitous, indeed,
but still lofty and scarped enough, which bears the name of Ale Down.
Neither does it project so far into the sea from the general line of
coast, which trends away to the eastward at no very abrupt angle.
Protected thus on three sides by very high ground, and with only a
somewhat narrow opening in one direction, the waters of that bay,
during the greater part of the year, are as soft and tranquil as a
dream of heaven; but they are very deep also, for the cliffs run down
far below the low water-mark. Standing on the heights above, I have
looked down, and beheld the sea lying beneath my feet, as smooth as a
mirror and as blue as a sapphire. A hundred-gun ship could anchor in
that bay, within pistol-shot of the cliffs of Ale Head.
Between the higher promontory and the lower, however, is a deep dell.
I must not call it a valley; for the sides are too steep, and the
concavity too narrow, to admit of that name. Down this dell flows a
strong deep stream of beautifully clear water, over a rooky bed, from
which a large quantity of sand is carried down, forming a soft dry
landing-place, where the dell opens upon the bay. This little beach is
not at all extensive, being, from the foot of the rock on the one side
to the base of the hill on the other, not more than two hundred yards
wide, and perhaps forty in depth. Through the centre of it flows the
stream into the sea; and, twice a-day, ocean comes up to meet its
tributary, covering by far the greater part of the sands.
Public-domain text, read in full here on John Shaqi.
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