The Physical Geology Geography of Ireland

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but the Ovvenmore has constantly deepened its channel, so as to prevent the course of the stream from being diverted.
Oilier rivers in the South-west. As regards the course of the rivers in the S. W. Of Ireland, it will be observed they are directly regulated by the geolo- FIG. 21.
Diagram to illustrate the formation of the river-valleys of the South- west of Ireland.
Crook- Dunmanus Bantry Kenmare Killarney haven Bay Bay River Lakes 8, Old Red Sandstone forming the mountain arches, c, Carbonif
...erous beds forming intervening synclinal valleys. The curved line touching the summits of the arches represents the old 'plane of marine denudation. ' gical structure of the country. They occupy the synclinal troughs of Carboniferous beds which lie alongside the great arches of Old Red Sandstone. The former have ultimately become valleys as well as synclinal troughs, both because of their original position after the flexures were produced, and of their greater destructibility ; the softer shales and slates, and the soluble limestones having yielded to River Valleys.

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