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
And the boulder continued to exist for
centuries still later as a nameless stone, on which the tall gray heron
rested moveless and ghost-like in the evenings, and the seal at mid-day
basked lazily in the sun. And then there came a night of fierce tempest,
in which the agonizing cry of drowning men was heard along the shore.
When the morning broke, there lay strewed around a few bloated corpses,
and the fragments of a broken wreck; and amid wild execrations and loud
sorrow the boulder received its name. Such is the probable history,
briefly told, because touched at merely a few detached points, of the
huge _Clach Malloch_. The incident of the second voyage here is of
course altogether imaginary, in relation to at least this special
boulder; but it is to second voyages only that all our positive evidence
testifies in the history of its class. The boulders of the St. Lawrence,
so well described by Sir Charles Lyell, voyage by thousands every
year;[18] and there are few of my northern readers who have not heard of
the short trip taken nearly half a century ago by the boulder of Petty
Bay, in the neighborhood of Culloden.
A Highland minister of the last century, in describing, for Sir John
Sinclair's Statistical Account, a large sepulchral cairn in his parish,
attributed its formation to an _earthquake_! Earthquakes, in these
latter times, are introduced, like the heathen gods of old, to bring
authors out of difficulties. I do not think, however,--and I have the
authority of the old critic for at least half the opinion,--that either
gods or earthquakes should be resorted to by poets or geologists,
without special occasion: they ought never to be called in except as a
last resort, when there is no way of getting on without them. And I am
afraid there have been few more gratuitous invocations of the earthquake
than on a certain occasion, some five years ago, when it was employed by
the inmate of a north-country manse, at once to account for the removal
of the boulder-stone of Petty Bay, and to annihilate at a blow the
geology of the Free Church editor of the _Witness_. I had briefly stated
in one of my papers, in referring to this curious incident, that the
boulder of the bay had been "borne nearly three hundred yards outwards
into the sea by an enclasping mass of ice, in the course of a single
tide." "Not at all," said the northern clergyman; "the cause assigned is
wholly insufficient to produce such an effect. All the ice ever formed
in the bay would be insufficient to remove such a boulder a distance,
not of three hundred, but even of _three_ yards." The removal of the
stone "_is referrible to an_ EARTHQUAKE!" The country, it would seem,
took a sudden lurch, and the stone tumbled off. It fell athwart the flat
surface of the bay, as a soup tureen sometimes falls athwart the table
of a storm-beset steamer, vastly to the discomfort of the passengers,
and again caught the ground as the land righted. Ingenious, certainly!
Public-domain text, read in full here on John Shaqi.
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