Celtic Scotland : $b A history of ancient Alban. Volume 1 (of 3), History and ethnologySkene, W. F. (William Forbes)
History
Celtic Scotland : $b A history of ancient Alban. Volume 1 (of 3), History and ethnology
Skene, W. F. (William Forbes)
Celts -- Scotland; Civilization, Celtic; Scotland -- Antiquities, Celtic; Scotland -- History -- To 1603
Proceeding farther north, the great series of the mountain ranges,
stretching from the south-west to the north-east, present one continuous
barrier, intersected indeed by rivers forming narrow and easily defended
passes, but exhibiting the appearance of a mighty wall, which separates
a wild and mountainous region from the well-watered and fertile plains
and straths on the south and east; and, while the latter have been at
all times exposed to the vicissitudes of external revolution, and the
greatly more important and radical change from the silent progress of
natural colonisation, the recesses of the Highlands have ever proved the
shelter and protection of the descendants of the older tribes of the
country, and the limit to the advance of a stranger population.
[Illustration:
MAP
SHEWING
MOUNTAIN CHAINS
_W. & A.K. Johnston, Edinburgh & London._
]
The territory which forms the modern kingdom of Scotland is thus thrown
by its leading physical features into three great compartments. First,
the districts extending from the Solway, the Cheviots, and the Tweed, on
the south, to the Firths of Forth and Clyde on the north; secondly, the
low country extending along the east coast from the Forth as far as the
Moray Firth, and lying between the sea and the great barrier of the
Grampians; and thirdly, the Highland or mountainous region on the
north-west.
[Sidenote: Mountain chains.]
In each of these great districts natural boundaries are again found
exercising their influence on the subordinate political divisions.
[Sidenote: The Cheviots.] In the first of these great compartments, the
lofty range of the Cheviots, which forms the southern boundary and
presents a steep face to the north, extends from the Cheviot Hill on the
north-east by Carter Fell to Peel Fell on the south-west; and from
thence a range of hills, sometimes included in the general name of the
Cheviots, separates the district of Liddesdale from that of Teviotdale,
and has its highest point in the centre of this part of the island, in a
group of hills termed the Lowthers, where the four great rivers of the
Tweed, the Clyde, the Annan, and the Nith, take their rise. From thence
it extends westward to Loch Ryan, separating the waters which pour their
streams into the Solway Firth from those which flow to the north. From
the centre of this range a smaller and less remarkable chain of hills
branches off, which, running eastward by Soutra and Lammermoor, end at
St. Abb’s Head, at the entrance to the Firth of Forth, separating the
tributaries of the Tweed from the streams which flow into the Firth of
Forth. In the centre of the island, a barren and hilly region divides
the districts watered by the rivers flowing into the east sea from those
on the west coast.
Public-domain text, read in full here on John Shaqi.
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