File:FANG FIG 03.jpg

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Summary

description
English: Figure 3 Marginal drainage channel, Walton Hill, Cupar, formed by meltwater flowing eastwards at the margin of Stratheden ice during the retreat stages of the Late Devensian ice sheet.
From: MacGregor, A.R. Third Edition. 1996. Fife and Angus geology: an excursion guide. Edinburgh:The Pentland Press.
source A.R. MacGregor
author A.R. MacGregor

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{{subst:Custom license marker added by UW}} © Copyright A.R. MacGregor. All rights reserved.

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current22:40, 21 February 2019Thumbnail for version as of 22:40, 21 February 20191,095 × 670 (205 KB)Scotfot (talk | contribs)User created page with UploadWizard

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