File:GSG GLA FIG 16 13.jpg

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Summary

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English: Figure.16.13. Map of the floodbasins sediments. The lithologies are mapped as set out in the legend, but in addition an interpretation of these lithologies is given by the following codes: Cs-crevasse splays; De-deltas; ch =channels. In this notation deltas (which are the result of crevasse sands building onto the floodplains) are a combination of two gradational or interfingering lithologies- medium grain-size sandstone and pebbly sandstone. Rose diagrams refer to the cross stratification dip directions O n-number of readings, L=vector magnitude a (which is inversely related to the standard deviation of spread of the data). The diagram total cross strata (overbank) refers to dip directions of the cross strata in the sandstone 0 sheets which have originated as sandstone crevasse splays i.e. De and Cs.
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

Licencing

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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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