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Map of the Great Glen Fault and other late Caledonian strike-slip faults in Scotland and northwestern Ireland. The Great Glen Fault is a strike-slip fault that runs through the Great Glen in Scotland. Occasional moderate tremors have been recorded over the past 150 years.
The Great Glen hosts the most prominent fault in the British Isles, the Great Glen Fault. It originated towards the end of the Caledonian Orogeny (around 430-390 million years ago), and cuts diagonally across the Highlands from Fort William to Inverness.
Jan 20, 2024 · The Great Glen Fault is a significant geological feature that covers the Southwest to the Northeast across the Scottish Mainland running from Fort William to Inverness, in an almost straight line.
The Great Glen Fault: the swinging pendulum of displacement estimates. The striking geomorphological aspect of the Great Glen of Scotland is its ruler-straight NE–SW trend for 200 km defined by a relatively narrow, steep-sided valley with hundreds of metres of relief.
The Great Glen Fault is a major geological feature that traverses southwest to northeast across the Scottish mainland from Fort William to Inverness.
Jun 24, 2021 · fault zone deformations. The Great Glen Fault Zone (GGFZ), located within the lower Paleozoic Caledonian orogenic belt of British Isles (Figures la and lb), is often cited as an example of a major strike-slip fault with a long-lived history of reactivation, following Kennedy [1946] and Holgate [1969]. It is
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In Scotland, the largest effect of the Caledonian Orogeny is the Great Glen Fault, a former transform fault over 300 miles long which now contains Loch Ness. Other Caledonian faults include the Moine Thrust, Highland Boundary Fault and Southern Uplands fault.
