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The Highland Border Ridge of North-east Ireland
Published online by Cambridge University Press: 01 May 2009
Summary
The Highland Border Ridge is a present day positive physiographic element whose activity can be traced back to Devonian time. A change from a distant Lower Dalradian to a nearby Middle and Upper Dalradian source area during Lower Old Red Sandstone times reflects the initial development of the ridge. A model for ridge uplift is outlined and some of its implications discussed.
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- Copyright © Cambridge University Press 1970
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