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Date/Time | Thumbnail | Dimensions | User | Comment | |
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current | 13:38, 5 June 2014 | 1,000 × 787 (214 KB) | Dbk (talk | contribs) | The upper cliffs of Aonach Dubh (pale) are rhyolite lavas resting on lavas of basic andesite, all of Lower Old Red Sandstone age. An t-Sron (on right) is composed principally of granite forming the Glen Coe Ring Fault Intrusion. The Glen Coe Ring Fault... |
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