This section is from the book "A Library Of Wonders And Curiosities Found In Nature And Art, Science And Literature", by I. Platt. Also available from Amazon: A library of wonders and curiosities.
The next object that claims our regard is The Cave of Fingal, or An-ua-vine, in the Island of Staffa. From Faujas St. Fond's Travels in England, Scotland, and the Hebrides.
"This superb and magnificent monument of a grand subterraneous combustion, the date of which has been lost in the lapse of ages, presents an appearance of order and regularity so wonderful, that it is difficult for the coldest observer, and a peison the least sensible to the phenomena which relate to the convulsions of the globe, not to be singularly astonished by this prodigy, which may be considered as a kind of natural palace.
"To shelter myself from all critical observation on the emotions which I experienced while contemplating the most extraordinary of any cavern known, I shall borrow the expressions of him who first described it. Those who are acquainted with the character of this illustrious naturalist,
Sir Joseph Banks, will not be apt to accuse him of being liable to be hurried away by the force of a too ardent imagination; but the sensation which he felt at the view of this magnificent scene was such, that it was impossible to escape a degree of just enthusiasm.
"The impatience which every body felt to see the wonders we have heard so largely described, prevented our morning's rest; every one was up and in motion before the break of day, and with the first light arrived at the south-west part of the island, the seat of the most remarkable pillars. We were no sooner arrived at this place, than we were struck with a scene of magnificence which exceeded our expectation, though formed as we thought upon the most sanguine foundations The whole of that end of the island is supported by ranges of natural pillars, mostly above fifty feet high, standing in natural colonnades, according as the bays or points of land formed themselves, upon a firm basis of solid shapeless masses of rock. In a short time we arrived at the mouth of the cave, the most magnificent, I suppose, that has ever been described by travellers.
The mind can hardly form an idea of any thing more magnificent than such a space, supported on each side by ranges of columns, and roofed by the bottoms of those from which they have been broken, in order to form it, between the angles of which a yellow stalagmitic matter has exuded; this serves to define the angles precisely, and at the same time vary the colour with a great deal of elegance, and, to render it still more agreeable, the whole is lighted from without; so that the farthest extremity is very plainly seen from the outside, and the air within, being agitated by the flux and reflux of the tides, is perfectly dry and wholesome, entirely free from the vapours with which natural caverns in general abound."
The following description of the same place by Mr. Troil, s also worthy of our notice:"How splendid (says this prelate) do the porticos of the ancients appear in our eyes, from the ostentatious magnificence of the descriptions we have received of them! and with what admiration are we seized, on seeing even the colonnades of our modern edifices! but when we behold the cave of Fingal, formed by nature in the isle of Staflfa, it is no longer possible to make a comparison, and we are forced to acknowledge that this piece of architecture, executed by nature, far surpasses that of the Louvre, that of St. Peter at Rome, and even what remains of Palmira and Pestum, and all that the genius, the taste, and the luxury of the Greeks, were ever capable of inventing." - Letters on Iceland.
Such also was the impression made by the cave of Fingal, on Sir Joseph Banks, and on the Bishop of Linckcaeping.
"I have seen many ancient volcanoes, and have given de scriptions of several superb basaltic causeways and delightful caverns in the midst of lavas; but I have never found any thing which comes near this, or can bear any comparison with it, either for the admirable regularity of the columns, the height of the arch, the situation, the forms, the elegance of this production of nature, or for its resemblance to the master-pieces of art, though this had no share in its construction. It is therefore not at all surprising that tradition should have made it the abode of a hero.
"This amazing monument of nature is thirty-five feet wide at the entrance, fifty-six feet high, and a hundred and forty feet long.
"The upright columns which compose the frontispiece, are of the most perfect regularity. Their height, to the beginning of the curvature, is forty-five feet.
"The arch is composed of two unequal segments of a circle, which form a sort of natural pediment.
"The mass which crowns, or rather which forms the roof, is twenty feet thick in the lowest part. It consists of small prisms, more or less regular, inclining in all directions, closely united and cemented underneath, and in the joints, with a yellowish white calcareous matter, and some zeolitic infiltra-tions, which give this fine ceiling the appearance of mozaic work.
"The sea reaches to the very extremity of the cave. It is fifteen feet deep at the mouth; and its waves, incessantly agitated, beat with great noise against the bottom and walls of the cavern, and every where break into foam. The light also penetrates through its whole length, diminishing gradually inwards, and exhibiting the most wonderful varieties of colour.
"The right side of the entrance presents, on its exterior part, a vast amphitheatre, formed of different ranges of large truncated prisms, the top of which may be easily walked on. Several of these prisms are jointed, that is, concave on the one side, and convex on the other; and some of them are divided by simple transverse intersections.
"These prisms, consisting of a very durable and pure black basaltes, are from one to three feet in diameter. Their forms are triangular, tetrapedral, pentagonal, and hexagonal; and some of them have seven or eight sides. I saw several large prisms, on the truncatures of which are distinctly traced the outlines of a number of smaller prisms; that is, these prisms are formed of a basaltes, which has a tendency to subdivide itself likewise into prisms. I had before observed the same phenomenon in the basaltic prisms of Vivarais.
 
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