File:Waterloo - geograph.org.uk - 454845.jpg

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Summary

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English: Waterloo The rock strata on the shore here have been tilted by tectonic movements, so that the dark mudstones laid down on top of the paler ones appear alongside one another. The foreground strata are Triassic, and beyond the old outfall pipe the presence of ammonite fossils marks the transition upwards into the Jurassic.
Date
Source From geograph.org.uk
Author Anne Burgess
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Anne Burgess / Waterloo / 
Anne Burgess / Waterloo
Camera location54° 51′ 35.9″ N, 5° 48′ 20″ W  Heading=337° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

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This file is licensed under the Creative Commons Attribution-Share Alike 2.0 Generic license.
Attribution: Anne Burgess
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31 May 2007

54°51'35.86"N, 5°48'19.80"W

heading: 337 degree

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Date/TimeThumbnailDimensionsUserComment
current16:49, 4 February 2011Thumbnail for version as of 16:49, 4 February 2011640 × 490 (142 KB)GeographBot== {{int:filedesc}} == {{Information |description={{en|1=Waterloo The rock strata on the shore here have been tilted by tectonic movements, so that the dark mudstones laid down on top of the paler ones appear alongside one another. The foreground strata a

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