Scenes and legends of the north of Scotland : $b or, The traditional history of Cromarty — John Stuart Mill — John Shaqi
Scenes and legends of the north of Scotland : $b or, The traditional history of Cromarty
John Stuart Mill · en
There rises within the bay, to the height of nearly a hundred feet
over the sea level, a green sloping bank, in some places covered with
wood, in others laid out into gardens and fields. We may trace it at a
glance all along the shores of the firth, from where it merges into the
southern Sutor, till where it sinks at the upper extremity of the bay
of Udoll; and, fronting it on the opposite side, we may see a similar
escarpment, winding along the various curves and indentations of the
coast--now retiring far into the country, along the edge of the bay of
Nigg--now abutting into the firth, near the village of Invergordon.
The Moray and Dornoch firths are commanded by resembling ramparts
of bank of a nearly corresponding elevation, and a thorough identity
of character; and, as in the Firth of Cromarty, the space between
their bases and the shore is occupied by a strip of level country,
which in some places encroaches on the sea in the form of long low
promontories, and is hollowed out in others to nearly the base of the
escarpment. Wherever we examine, we find data to conclude, that in
some remote era this continuous bank formed the line of coast, and
that the plain at its base was everywhere covered by the waters of the
sea. We see headlands, rounded as if by the waves, advancing the one
beyond the other, into the waving fields and richly-swarded meadows
of this lower terrace; and receding bays with their grassy unbeaten
shores comparatively abrupt at the entrance, and reclining in a flatter
angle within. We may find, too, everywhere under the vegetable soil
of the terrace, alternate layers of sand and water-worn pebbles,
and occasionally, though of rarer occurrence, beds of shells of the
existing species, and the bones of fish. In the valley of Munlochy,
the remains of oyster-beds, which could not have been formed in less
than two fathoms of water, have been discovered a full half mile from
the sea; beds of cockles still more extensive, and the bones of a
porpoise, have been dug up among the fields which border on the bay of
Nigg; similar appearances occur in the vicinity of Tain; and in digging
a well about thirty years ago, in the western part of the town of
Cromarty, there was found in the gravel a large fir-tree, which, from
the rounded appearance of the trunk and branches, seems to have been
at one time exposed to the action of the waves. In a burying-ground
of the town, which lies embosomed in an angle of the bank, the sexton
sometimes finds the dilapidated spoils of our commoner shell-fish
mingling with the ruins of a nobler animal; and in another inflection
of the bank, which lies a short half mile to the east of the town,
there is a vast accumulation of drift peat, many feet in thickness, and
the remains of huge trees.