A fault is where tectonic plates meet. The powerful dislocation which intersects Scotland along the line of the Great Glen has, in the past, been regarded by most geologists as a normal or dip-slip fault with a predominant vertical downthrow to the south-east. Great Glen Fault . Great Glen (englisch; dt. after A-levels including undergraduate and further degrees The Great Glen Fault is a long strike-slip fault that runs through its namesake, the Great Glen, in Scotland. adshelp[at]cfa.harvard.edu The ADS is operated by the Smithsonian Astrophysical Observatory under NASA Cooperative Agreement NNX16AC86A Tectonic faults and volcanoes in Scotland? Updates on outreach activities, information about how the geosciences interact with society, details of policy related meetings, consultation responses, and policy briefing notes. The Great Glen Fault is a long strike-slip fault that runs through its namesake the Great Glen in Scotland.. It consists of a zone of crushed rock (now represented mainly by indurated cataclasite) up to 0.5 km wide, flanked by zones of minor faulting and shattering. The tectonic complexities associated with this configuration require further evaluation. This website uses cookies to give you the best user experience. Order publications, find out about the Lyell Collection and read guidelines for preparing a paper or submitting a book proposal. The North Anatolian fault stretches across northern Turkey and its movement is strike-slip in nature just like the ancient movement seen at the Great Glen Fault in Scotland. Der Great Glen Fault hat eine lange Bewegungsgeschichte. Many translated example sentences containing "Great Glen fault" – German-English dictionary and search engine for German translations. The Great Glen Fault is a long strike-slip fault that runs through its namesake the Great Glen in Scotland. Part of the fault runs through Cape Breton Highlands National Park. 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)). Kennedy showed that the fault had moved sideways – as a so-called strike-slip (or wrench) fault. Viele übersetzte Beispielsätze mit "great Glen fault" – Deutsch-Englisch Wörterbuch und Suchmaschine für Millionen von Deutsch-Übersetzungen. The Great Glen Fault has a long movement history. Loch Ness was formed after that by glaciers. If this discrepancy is correct, lines of major transcurrent dislocation have yet to be identified either in the North Atlantic continental shelves and margins or in eastern North America, and the Great Glen fault was not the main locus of offset between Britain and North America. The bottom of the fault is largely covered with lakes, which are now connected by canals. A 6th century abbey along the way marks the … The Great Glen Fault had its final phase of movement during the Late Cretaceous to Early Tertiary. Search the events calendar for forthcoming conferences and events, and view past meeting resources. Information and resources for teachers and students from The Glen runs along: * River Ness * Loch Dochfour * Loch Ness * River Oich * … primary education onwards; for those making careers choices It consists of a zone of crushed rock (now represented mainly by indurated cataclasite) up to 0.5 km wide, flanked by zones of minor faulting and shattering. The fault runs along the boundary between ...continue reading, © 2012 The Geological Society of London, registered charity, number: 210161, Get involved in our plate tectonics competition, Accredited CPD and training course listings, Accreditation of Company Training Schemes, Quarterly Journal of Engineering Geology and Hydrogeology, Geochemistry Exploration Environment Analysis, Proceedings of the Yorkshire Geological Society, Transactions of the Edinburgh Geological Society, Transactions of the Geological Society of Glasgow, Accredited degrees and university departments, Instructions for reviewers and publishers. 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. 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. Coordinates: .mw-parser-output .geo-default,.mw-parser-output .geo-dms,.mw-parser-output .geo-dec{display:inline}.mw-parser-output .geo-nondefault,.mw-parser-output .geo-multi-punct{display:none}.mw-parser-output .longitude,.mw-parser-output .latitude{white-space:nowrap}57°05′N 4°46′W / 57.08°N 4.76°W / 57.08; -4.76, "Structure and early kinematic history of the Great Glen Fault Zone, Scotland", "A geotraverse through the Appalachians of northern Newfoundland", "Post-glacial activity and earthquakes of the Great Glen Fault (Scotland)", https://en.wikipedia.org/w/index.php?title=Great_Glen_Fault&oldid=997735577, Creative Commons Attribution-ShareAlike License, This page was last edited on 2 January 2021, at 00:07. Captions. 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