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
mineral springs of the Strath have their rise, and to which they owe
their peculiar qualities.
After walking on for about eight miles, through noble woods and a lovely
country, I struck from off the high road at the pretty little village of
Evanton, and pursued the course of the river Auldgrande, first through
intermingled fields and patches of copsewood, and then through a thick
fir wood, to where the bed of the stream contracts from a
boulder-strewed bottom of ample breadth, to a gloomy fissure, so deep
and dark, that in many places the water cannot be seen, and so narrow,
that the trees which shoot out from the opposite sides interlace their
branches atop. Large banks of the gray boulder-clay, laid open by the
river, and charged with fragments of dingy sandstone and dark-colored
breccia, testify, along the lower reaches of the stream, to the near
neighborhood of the ichthyolitic member of the Old Red; but where the
banks contract, we find only its lowest member, the Great Conglomerate.
This last is by far the most picturesque member of the system,--abrupt
and bold of outline in its hills, and mural in its precipices. And
nowhere does it exhibit a wilder or more characteristic beauty than at
the tall narrow portal of the Auldgrande, where the river,--after
wailing for miles in a pent-up channel, narrow as one of the lanes of
old Edinburgh, and hemmed in by walls quite as perpendicular, and
nearly twice as lofty,--suddenly expands, first into a deep brown pool,
and then into a broad tumbling stream, that, as if permanently affected
in temper by the strict severity of the discipline to which its early
life had been subjected, frets and chafes in all its after course, till
it loses itself in the sea. The banks, ere we reach the opening of the
chasm, have become steep, and wild, and densely wooded; and there stand
out on either hand, giant crags, that plant their iron feet in the
stream; here girdled with belts of rank succulent shrubs, that love the
damp shade and the frequent drizzle of the spray; and there hollow and
bare, with their round pebbles sticking out from the partially
decomposed surface, like the piled-up skulls in the great underground
cemetery of the Parisians. Massy trees, with their green fantastic roots
rising high over the scanty soil, and forming many a labyrinthine recess
for the frog, the toad, and the newt, stretch forth their gnarled arms
athwart the stream. In front of the opening, with but a black deep pool
between, there lies a midway bank of huge stones. Of these, not a few of
the more angular masses still bear, though sorely worn by the torrent,
the mark of the blasting iron, and were evidently tumbled into the chasm
from the fields above. But in the chasm there was no rest for them, and
so the arrowy rush of the water in the confined channel swept them down
till they dropped where they now lie, just where the widening bottom
first served to dissipate the force of the current. And over the sullen
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