The Old Red Sandstone; or, New Walks in an Old Field — John Stuart Mill — John Shaqi
The Old Red Sandstone; or, New Walks in an Old Field
John Stuart Mill · en
I know not a more instructive walk for the young geologist than
that furnished by the two miles of shore along which this section
extends. Years of examination and inquiry would fail to exhaust it.
It presents us, I have said, with the numerous organisms of the
Lower Old Red Sandstone; it presents us also, towards its western
extremity, with the still more numerous organisms of the Lower and
Upper Lias; nor are the inflections and faults which its strata
exhibit less instructive than its fossils or its vast denuded hollow.
I have climbed along its wall of cliffs during the height of a
tempestuous winter tide, when waves of huge volume, that had begun to
gather strength under the night of the Northern Ocean, were bursting
and foaming below; and as the harder pebbles, uplifted by the surge,
rolled by thousands and tens of thousands along the rocky bottom, and
the work of denudation went on, I have thought of the remote past,
when the same agents had first begun to grind down the upper strata,
whose broken edges now projected high over my head on the one hand,
and lay buried far under the waves at my feet on the other. Almost
all mountain chains present their abrupter escarpements to the sea,
though separated from it in many instances by hundreds of miles--a
consequence, it is probable, of a similar course of denudation, ere
they had attained their present altitude, or the plains at their
feet had been elevated over the level of the ocean. Had a rise of a
hundred feet taken place in this northern district in the days of
Cæsar, the whole upper part of the Moray Frith would have been laid
dry, and it would now have seemed as inexplicable that this roof-like
ridge should present so rugged a line of wall to the distant sea,
as that the Western Ghauts of India should invariably turn their
steepest declivities to the basin of the Indian Ocean, or that, from
the Arctic Circle to the southern extremity of Patagonia, the huge
mountain-chain of America should elevate its dizzy precipices in the
line of the Pacific.