LONDONDERRY TOPOGRAPHY

From A Topographical Dictionary of Ireland, 1837

In form the county approaches to an equilateral triangle: its greatest length is from the point of Magilligan, at the mouth of Lough Foyle, nearly southward, to the vicinity of Coagh, a distance of 32 ½ miles. Although by no means distinguished for picturesque beauty, its surface presents many varieties of form, from the flat alluvial lands along its rivers to the wildest mountains. The latter form its central portion, extending in various chains, covered chiefly with heath, from near the sea-coast to the southern limit. Sawel mountain, in the south, attains an elevation of 2236 feet; Slieve Gallion rises to the height of 1730 feet; Carntogher, near the source of the Roe, 1521 feet; Donald's Hill, east of the same river, 1315 feet; Benyevenagh, forming the termination of that range towards the sea, 1260 feet; and Legavannon, between the Roe and the Faughan, 1289 feet.

Even in these wild regions there are secluded vales, called by the inhabitants "slacks," in which are often found charming spots of fertile soil and romantic scenery. The principal of these are, Faughanvale, where there are some romantic waterfalls; Muff-glen, which, with the beautiful glen of the Ness, affords mountain passes from the Foyle to the Faughan; Laughermore, between the Roe and the Faughan, which commands various fine prospects, and has in its vicinity numerous traces of ancient forests; Lissane, with some deep romantic glens; Feeny, between the higher parts of the Roe and the Faughan, into which several other glens open, of which the most beautiful is Fin-glen; the neighbouring slacks of Moneyniceny and Carntogher; that of Ballyness, leading into the wild district of Glenullen; that of Dunmore, between Coleraine and Newtown-Limavady; and that of Druim-na-Gullion, to the north. The most extensive and diversified view in this part of Ireland, is that from the summit of Benyevenagh, near the mouth of the Roe, from which mountain the huge masses of fallen strata form successive terraces descending to the sandy flats bounded by Lough Foyle and the ocean.

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