Ruins and monasteries on deep lakes. Achetez neuf ou d'occasion The Great Glen (An Gleann Mor) follows 80 miles of lochs and rivers from Glencoe and Fort William in the south to Inverness in the north. Il est divisé en deux: Highlands Ecossais en Grampian Mountains sud-est et les hauts plateaux du nord-ouest au nord-ouest. Continue NE along the A82 towards North Laggan. Request PDF | On Jan 1, 2010, Martyn Stewart published The Great Glen Fault | Find, read and cite all the research you need on ResearchGate (c) Fault contact between Jurassic and Devonian strata. Great Glen Fault . The Great Glen Fault (GGF) is a major transcurrent fault zone of Caledonian inheritance that initially experienced sinistral motion during Paleozoic times and later reactivated as a dextral system during Cenozoic times. Position. Journal. (a) Panoramic view that shows the sigmoidal shape of Jurassic folds next to Great Glen Fault (GGF). It is shown that mylonite is extremely rare in the plane of the Great Glen fault, and that horizontal slickensides or friction-grooves directed along the Glen are virtually absent. The Great Glen can be reached via Inverness Airport and by train or bus to Inverness and Fort William. The Great Glen Fault is a long strike-slip (transcurrent) fault that runs through its namesake the Great Glen (Glen Albyn) in Scotland. The Great Glen Fault trends NNE-SSW across northern Scotland. The Great Glen Fault is a long strike-slip fault that runs through its namesake the Great Glen in Scotland.The fault is actually much longer, and over 400 million years old. According to previous studies, the Great Glen Fault developed as a left-lateral strike-slip fault during the Caledonian Orogeny (Ordovician to Early Devonian). It's a fantastic natural route through the Scottish Highlands, with exceptional scenery and gorgeous forests. Fig. The Great Glen, a major geological fault line cutting diagonally across the Highlands from Fort William to Inverness, is the defining geographic feature of the north of Scotland. It formed towards the end of the Caledonian orogeny associated with the collision between the Laurentia and Baltic tectonic plates at the end of the Silurian continuing into the Early Devonian (likely age range 430–390 Ma (million years)). (0.0 km) #2 Aberchalder Uk Place Updated: 2019-12-24 Aberchalder is a small settlement and estate at the northern end of Loch Oich in the Scottish Highlands and is in the Highland council area of Scotland. Many translated example sentences containing "Great Glen fault" – German-English dictionary and search engine for German translations. However, the fault is actually much longer and over 400 million years old. Moinian rocks SE of the Great Glen Fault, severely altered by fault-zone fluids. The fault line separates Scotland geologically with the rocks on either side of Loch Lochy being quite different in composition and age. Just before the road turns sharp left to cross the swing-bridge at the head of Loch Oich, take the road on the right to the Great Glen Water Park. Aller à : navigation, rechercher. The Great Glen Fault has a long movement history. The bottom of the fault is largely covered with lakes, which are now connected by canals. The GGF developed as a left-lateral fault during the Caledonian Orogeny (Ordovician to Early Devonian). Distance: 0.0 mi. We discuss additional evidence for this later phase. The Great Glen Fault (GGF) trends NNE-SSW across all of Northern Scotland, separating two Neoproterozoic supergroups (Moine and Dalradian). The Great Glen (Scottish Gaelic: An Gleann Mòr [an ˈklaun̪ˠ ˈmoːɾ]), also known as Glen Albyn (from the Gaelic Gleann Albainn "Glen of Scotland" [ˈklaun̪ˠ ˈaɫ̪apən]) or Glen More (from the Gaelic Gleann Mòr), is a glen in Scotland running for 62 miles (100 km) from Inverness on the edge of Moray Firth, in an approximately straight line to Fort William at the head of Loch Linnhe. However, it then reactivated right-laterally in the Tertiary. Great_glen_fault.png ‎ (144 × 250 pixels, taille du fichier : 7 Kio, type MIME : image/png) Ce fichier provient de Wikimédia Commons. Fichier; Historique du fichier; Utilisation du fichier; Pas de plus haute résolution disponible. THE Great Glen Fault was shown by W. Q. Kennedy 1 to be a sinistral tear fault on which a displacement of about 65 miles has occurred since Middle Old Red Sandstone time. The stretch between Fort William and Inverness is one of the most scenic drives in Scotland. This shape is diagnostic of right-lateral slip along the Great Glen Fault. It extends in both directions beyond mainland Scotland. Published: 21 June 1974; Great Glen Fault. Comparisons of pre-Caledonian basement complexes, folded cover successions, and late Caledonian intrusive suites occurring in the Northern and Grampian Highlands on either side of the fault reveal a … Noté /5. The fault line itself formerly continued to the South West through what is today Canada and the United States. It extends in both directions beyond mainland Scotland. Journal of the Geological Society, 158(5), pp.821-830. The great glen fault in the Shetland area. The Great Glen Fault is a long strike-slip fault that runs through its namesake the Great Glen in Scotland.The fault is actually much longer, and over 400 million years old. Ecossais en Grampian Mountains sud-est et les hauts plateaux du nord-ouest au nord-ouest in Fault... A giant crack that runs the length of Scotland: the Great Glen Fault a. 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