File:GSG GLA FIG 30 05.jpg

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English: Figure 30.5. Stratigraphical sketch section, illustrating the nature of the subSil urian unconformity in the Girvan district, which is believed to reflect submarine channelling across pre-Silurian fault blocks: basement faulting has not only controlled Ordovician sedimentation but the effects continue into the Silurian.
From: Lawson, J.D. and Weedon, D.S. (editors). 1992. Geological excursions around Glasgow & Girvan. Glasgow : Geological Society of Glasgow.
source Glasgow Geological Society
author Glasgow Geological Society


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© 1992. Geological Society of Glasgow. All rights reserved. Published by the Geological Society of Glasgow. For all uses of the images please contact the Geological Society Glasgow. [1]

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