great glen fault

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. The Great Glen Fault is probably the best known of the fault zones. You can walk, cycle and canoe the Great Glen Way, or drive along the A82 and explore dozens of waymarked trails as you go. The GGF developed as a left-lateral fault during the Caledonian Orogeny (Ordovician to Early Devonian). The stretch between Fort William and Inverness is one of the most scenic drives in 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. This shape is diagnostic of right-lateral slip along the Great Glen Fault. The deep fault splits the Scottish Highlands diagonally from coast to coast. 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. 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 … We discuss additional evidence for this later phase. 1 Location; 2 History; 3 See also; 4 References Location. Request PDF | On Jan 1, 2010, Martyn Stewart published The Great Glen Fault | Find, read and cite all the research you need on ResearchGate Andrew Marr takes to the sky in a microlight over a giant crack that runs the length of Scotland: the Great Glen Fault. Position. The fault line separates Scotland geologically with the rocks on either side of Loch Lochy being quite different in composition and age. The Great Glen Fault trends NNE-SSW across northern Scotland. #1 Great Glen Fault Unclassified Updated: 2020-05-09 The Great Glen Fault is a long strike-slip fault that runs through its namesake the Great Glen in Scotland. 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. We discuss additional evidence for this later phase. The Great Glen Fault cuts across the Highlands and is provided its name by the Great Glen that it runs through. Fichier:Great glen fault.png. 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. 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. People of all fitness levels can complete the Great Glen Way's low-level walking trails in 5-10 days, or focus on the stretches around Fort William and Loch Ness. Journal. Position. The Great Glen Fault (GGF) trends NNE-SSW across all of Northern Scotland, separating two Neoproterozoic supergroups (Moine and Dalradian). Retrouvez Articles on Geography of Ireland, Including: Extreme Points of Ireland, Great Glen Fault, Irish Grid Reference System, Thomond, Caledonian Ocean, Drom et des millions de livres en stock sur Amazon.fr. The great glen fault in the Shetland area. The fault line itself formerly continued to the South West through what is today Canada and the United States. We agree with him that the aeromagnetic map2 distinguishes regions of shallow and deep magnetic basement by the smoothness of the contours. Noté /5. The Great Glen Fault is a long strike-slip (transcurrent) fault that runs through its namesake the Great Glen (Glen Albyn) in Scotland. (b) Calcite veins right-laterally offsetting Jurassic strata. 8. Mountain bikers with good fitness levels can tackle it in 1-3 days. Structure and early kinematic history of the Great Glen Fault Zone, Scotland M. Stewart • and R. A. Strachan Department of Geology, Oxford Brookes University, Headington, Oxford R. E. Holdsworth Reactivation Research Group, Department of Geological Sciences, University of Durham, England Abstract. However, the fault is actually much longer and over 400 million years old. 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. Photographs of Jurassic outcrops at Port-an-Righ. Retrouvez Geography of Inverness Geography of Inverness: Loch Ness, Moray Firth, Great Glen Fault, Glen Affric, Carn Loch Ness, Moray Firth, Great Glen Fault, G et des millions de livres en stock sur Amazon.fr. According to previous studies, the Great Glen Fault developed as a left-lateral strike-slip fault during the Caledonian Orogeny (Ordovician to Early Devonian). Caledonian Channel: East-West connection for boats . Ruins and monasteries on deep lakes. Aller à : navigation, rechercher. It extends in both directions beyond mainland Scotland. (a) Panoramic view that shows the sigmoidal shape of Jurassic folds next to Great Glen Fault (GGF). (c) Fault contact between Jurassic and Devonian strata. The Great Glen Fault trends NNE–SSW across northern Scotland. Constraints on early sinistral displacements along the Great Glen Fault Zone, Scotland: structural setting, U-Pb geochronology and emplacement of the syn-tectonic Clunes tonalite. Great_glen_fault.png ‎ (144 × 250 pixels, taille du fichier : 7 Kio, type MIME : image/png) Ce fichier provient de Wikimédia Commons. Il peut être utilisé par d'autres projets. The Great Glen fault, for which a strike-slip displacement of about 2,000 km is proposed from paleomagnetic data by Van der Voo and Scotese, transects the metamorphic Caledonides of Scotland. Achetez neuf ou d'occasion Moinian rocks SE of the Great Glen Fault, severely altered by fault-zone fluids. Achetez neuf ou d'occasion Thomson, K. and Hillis, R. R. Tertiary structuration and erosion of the Inner Moray Firth 1995 - Geological Society, London, Special Publications . Continue NE along the A82 towards North Laggan. The Great Glen Fault has a long movement history. Fichier; Historique du fichier; Utilisation du fichier; Pas de plus haute résolution disponible. It's a fantastic natural route through the Scottish Highlands, with exceptional scenery and gorgeous forests. However, it then reactivated right-laterally in the Tertiary. Grave doubt is consequently thrown on the alleged horizontal displacement in the fault zone. 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. Contents. However, it then reactivated right-laterally in the Tertiary. According to previous studies, the Great Glen Fault developed as a left-lateral strike-slip fault during the Caledonian Orogeny (Ordovician to Early Devonian). Noté /5. The Great Glen can be reached via Inverness Airport and by train or bus to Inverness and Fort William. Journal of the Geological Society, 158(5), pp.821-830. 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. Le Great Glen suit le chemin d'un grand faute géologique connue sous le nom Great Glen Fault. Story: The Great Glen Fault Duration: 4:47 . (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. Distance: 0.0 mi. The bottom of the fault is largely covered with lakes, which are now connected by canals. Abstract: WE apologize to Dr Flinn for any disquiet we may have caused by omitting to refer to his recent paper1. Fig. Published: 21 June 1974; Great Glen Fault. 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