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The universal geography : earth and its inhabitants

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j engineers<br />

CHAPTER XIV.<br />

NORTHERN SCOTLAND.<br />

(<strong>The</strong> CorxTiES of Perth, Forfab, Kincardine, Aberdeen, Banff, Elgin, Nairn, Inverness, Ross<br />

AND Cromarty, Sutherl<strong>and</strong>, Caithness, Orkney, Shetl<strong>and</strong>, <strong>and</strong> Argyll.)<br />

General Features.<br />

riTS is a portion of tlie British Isl<strong>and</strong>s which, compared with Engl<strong>and</strong><br />

<strong>and</strong> Southern Scotl<strong>and</strong>, is but thinly populated. In <strong>its</strong> great geo-<br />

graphical features, <strong>its</strong> relief, contours, <strong>and</strong> coast-line, it resembles<br />

Sc<strong>and</strong>inavia rather than any other part of Great Britain. If<br />

the sea once more flooded the broad plain stretching from the<br />

Forth to the Clyde, <strong>its</strong> character of insularity would hardly become more apparent<br />

than it is now. Upper Caledonia is, in foct, a large isl<strong>and</strong>, with smaller isl<strong>and</strong>s<br />

for <strong>its</strong> satellites.<br />

Far more elevated in the mean than Engl<strong>and</strong>, nearlj' the whole of it is<br />

occupied by mountains ; <strong>and</strong> these mountains form ranges, which extend almost<br />

without an exception from the south-west to the north-east. In the south this<br />

Highl<strong>and</strong> region is bounded by the Strathmore, or " Great Valley," through which<br />

the plain of the Forth is extended north-eastward towards Montrose <strong>and</strong> Stone-<br />

haven. <strong>The</strong> vallej'S of the Dee, Doveran, Spey, Findhorn, <strong>and</strong> Nairn run parallel<br />

with that plain towards the German Ocean, <strong>and</strong> the remarkable fissure of<br />

Glenmore, which connects Loch Eil with the Inverness Firth, extends in the<br />

same direction. <strong>The</strong>re are few fissures in Europe which in rigidity of contour can<br />

compare with this "Great Glen" of Scotl<strong>and</strong>, which, 100 miles in length, joins<br />

the Atlantic to the German Ocean. If the Dee were to rise but 100 feet, the<br />

northern extremity of Scotl<strong>and</strong> would be separated from the remainder of the<br />

Highl<strong>and</strong>s, <strong>and</strong> the chain of lakes <strong>and</strong> rivers now occupying the glen converted<br />

into a narrow strait of the sea of uniform width. <strong>The</strong> ocean would then follow<br />

the path apparently traced for it in the Caledonian Canal. <strong>The</strong> execution of that<br />

work was greatly facilitated by the existence of the river Ness, which falls into<br />

Inverness Firth, <strong>and</strong> Loch Ness, which occupies the centre of the isthmus. AU the<br />

had to do was to excavate a canal 22 miles in length, <strong>and</strong> to furnish it<br />

VOL.' IV. z

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