File:FANG FIG 17.jpg

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Summary

description
English: Figure 17 Bishop Hill, Loch Leven from Balnethill farm. The summit is capped by quartz-dolerite of the Midland Valley Sill. The steep face is composed of Carboniferous sediments passing down into sediments of the Stratheden Group. Kinnesswood Row is the gully on the right.
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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current21:48, 21 February 2019Thumbnail for version as of 21:48, 21 February 20191,098 × 748 (271 KB)Scotfot (talk | contribs)User created page with UploadWizard

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