The Cruise of the Betsey: or, A Summer Ramble Among the Fossiliferous Deposits of the Hebrides. With Rambles of a Geologist or, Ten Thousand Miles Over the Fossiliferous Deposits of ScotlandMiller, Hugh
Philosophy
The Cruise of the Betsey: or, A Summer Ramble Among the Fossiliferous Deposits of the Hebrides. With Rambles of a Geologist or, Ten Thousand Miles Over the Fossiliferous Deposits of Scotland
Miller, Hugh
Geology -- Scotland
authoritatively deciding whether the inscription was a work of man or a
sport of nature. He stood between his two conclusions, like our
Edinburgh antiquarians between the two fossil Maries of Gueldres; and,
richer in eloquence than most of the philosophers his contemporaries,
was quite prepared, in his uncertainty, to give gilded mounting and a
purple pall to both.
"Should it be no other than a sport of nature," he concludes, "the
reputation which the stone bears in this country deserves that we should
have given a description of it. If, on the other hand, what is on it be
an inscription, though it certainly does not possess the beauty of the
sculpture of Greece or Rome, it very possibly has the advantage of being
the oldest in the universe. The country in which it is found is
inhabited only by a race of men who live like beasts in the forests. We
cannot imagine that they can have ever had any memorable event to
transmit to posterity, nor, if ever they had had, that they could have
invented the means. Nor can it be conceived that this country, with its
present aspect, ever possessed more civilized inhabitants. The rigor of
the climate and the barrenness of the land have destined it for the
retreat of a few miserable wretches, who know no other. It seems,
therefore, that the inscription must have been cut at a period when the
country was situated in a different climate, and before some one of
those great revolutions which, we cannot doubt, have taken place on our
globe. The position that the earth's axis holds at present with respect
to the ecliptic, occasions Lapland to receive the sun's rays very
obliquely: it is therefore condemned to a long winter, adverse to man,
as well as to all the productions of nature. No great movement,
possibly, in the heavens was necessary, however, to cause all its
misfortunes. These regions may formerly have been those on which the sun
shone most favorably; the polar circles may have been what now the
tropics are, and the torrid zone have filled the place occupied by the
temperate." Pretty well, Monsieur, for a philosopher! The various
attempts made to unriddle the real history of graphic granite are,
however, scarce less curious than the speculations connected with what
may be termed its romance. It seems to be generally held, since the days
of old Hutton, who, in his "Theory of the Earth," discussed the subject
with his usual ingenuity, that the feldspathic basis of the stone first
crystallized, leaving interstices between the crystals, partaking of a
certain regularity of form,--a consequence of the regularity of the
crystals themselves,--and of a certain irregularity from the eccentric
dispositions which these manifest in their position and relations to
each other; and that these interstices, being afterwards filled up with
quartz, form the characters of the rock,--characters partaking enough of
the first element of _regularity_ to present their peculiar graphic
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