A Geological Wall to show the rock strata after the Moine Thrust event as it is Today. SCO 8552
Knockan Crag is a line of cliffs in Assynt, Scotland 21 kilometres (13 mi) north of Ullapool. The name is an anglicisation of the Gaelic Creag a' Chnocain meaning 'crag of the small hill'. The Moine Thrust runs through the crag and there is a small visitor centre providing interpretation and artwork that explains the background to the 'Highlands Controversy' concerning the geology of the area During the 19th century prominent geologists conducted a prolonged and bitter debate about the fault line exposed here. The argument was primarily between Roderick Murchison and Archibald Geikie on the one hand and James Nicol and Charles Lapworth on the other. This was finally resolved by the work of Ben Peach and John Horne whose 1907 paper on the subject remains a classic text. The main issue was that the Moine schists at the top of the crag appeared to be older than the Cambrian and Ordovician rocks such as Durness limestone lower down. Murchison and Geikie believed the sequence was wrong and that the Moine schists must be the younger rocks. The conundrum was explained by the action of a thrust fault - this being the first to be discovered anywhere in the world. The older rocks had been moved some 70 kilometres to the west over the top of the younger rocks due to tectonic action. A monument to Peach and Horne's work was erected by the international geological community at Inchnadamph a few miles to the north.
Size: 6063px × 4035px
Location: Knockan Crag, Inverpolly. Assynt Geological Park. Elphin. Sutherland. Scotland.
Photo credit: © David Gowans / Alamy / Afripics
License: Licensed
Model Released: No
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