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.
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| 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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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 22:48, 21 February 2019 | | 1,098 × 748 (271 KB) | Scotfot (talk | contribs) | User created page with UploadWizard |
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