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Campsie Fells
A historical perspective, drawn from the Ordnance Gazetteer
of Scotland: A Survey of Scottish Topography, Statistical, Biographical and
Historical, edited by
Francis H. Groome
and originally published in parts by Thomas C. Jack, Grange Publishing Works,
Edinburgh between 1882 and 1885.
This edition is copyright © The Editors of the Gazetteer for Scotland,
2002-2013.
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ampsie Fells, a portion of the Lennox Hills, or a range of heights, which, extending east-north-eastward from Dumbarton to Stirling, measure about 25 miles in extreme length, and 8 in mean breadth. They are interrupted, for a mile or more, by the valley of the Blane, whence to Dumbarton they bear the name of Kilpatrick Hills; and they are called, in their various portions east-north-eastward, the Killearn, the Campsie, the Kilsyth, the Fintry, the Dundaff, and the Gargunnock Hills. The Campsie Fells are the most prominent portion of the entire range. Beginning at the upper valley of the Blane, they extend about 8 miles eastward to Bin Burn, on the boundary between Campsie and Fintry parishes, and to the eastern skirt of Brown Hill at the boundary between Campsie and Kilsyth parishes; they include a section of Strathblane parish, sometimes called the Strathblane Hills; and sometimes they are likewise regarded as including the Killearn and the Fintry portions of the Lennox Hills. Their highest summit is Earls Seat (1894 feet); they offer great attractions to at once the lovers of romantic scenery, geologists, and botanists; and they overlook most of the great strath of the Forth and Clyde Canal, and command beyond extensive and magnificent views of the Lowlands. See Campsie.
An accompanying 19th C. Ordnance Survey map is
available.
Note: This text has been made available
using a process of scanning and
optical character recognition. Despite manual checking, some typographical
errors may remain. Please remember this description dates from
the 1880s; names may have changed, administrative divisions will certainly be
different and there are known to be occasional errors of fact in the original
text, which we have not corrected because we wish to maintain its integrity.
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