File:GSG GLA FIG 33 03.jpg

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English: Figure 33.3. Composite W-E section formerly exposed at Junction 27 on the M8 motorway near Paisley, showing a roche moutonnee (of dolerite) overlain by till which, in turn, is overlain by laminated clay and fossiliferous marine sediments (Clyde Beds) deposited during the Windermere Interstadial. The overlying layer of fine sandy silt alternating with sand probably represents land conditions. The conditions under which the uppermost bed, of sandy clay, accumulated are uncertain. Adapted from Aspen & Jardine 1968, Figure 1.
From: Lawson, J.D. and Weedon, D.S. (editors). 1992. Geological excursions around Glasgow & Girvan. Glasgow : Geological Society of Glasgow.
source Geological Society of Glasgow
author Geological Society of Glasgow


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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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