Clackmannan and Kinross . rapid rate, and the valley would, so tospeak, eat its way up stream. Progressing in this manner,it might tap the head waters of other streams draining theOchil face, and the river, increasing thus in volume anderosive power, would continue the process by which thedivide or water-parting gets pushed further and furtherback until it not only has captured the streams drainingthe southern face of the Ochils but has also tapped thehead-waters of a river running in the transverse valleybehind the Blairdenon-to-Whitewisp ridge. This latterriver, now represented by the upper
Clackmannan and Kinross . rapid rate, and the valley would, so tospeak, eat its way up stream. Progressing in this manner,it might tap the head waters of other streams draining theOchil face, and the river, increasing thus in volume anderosive power, would continue the process by which thedivide or water-parting gets pushed further and furtherback until it not only has captured the streams drainingthe southern face of the Ochils but has also tapped thehead-waters of a river running in the transverse valleybehind the Blairdenon-to-Whitewisp ridge. This latterriver, now represented by the upper course of the Devon,.
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Keywords: ., bookcentury1900, bookdecade1910, bookidclackmannank, bookyear1915
