great glen fault

If you continue without changing your settings we'll assume you are happy to receive all GSL cookies. The Great Glen Fault is such an important feature both geologically and topographically that it has attracted special attention and has an extensive literature. The Great Glen Fault is a long strike-slip (transcurrent) fault that runs through its namesake the Great Glen (Glen Albyn) in Scotland. Aligned northeast to southwest, the Great Glen Fault extends further southwest in a straight line through Loch Linnhe and the Firth of Lorne, and then on into northwestern Ireland, directly through Lough Swilly, Donegal Bay and Clew Bay as the Leannan Fault. The Great Glen Fault is such an important feature both geologically and topographically that it has attracted special attention and has an extensive literature. The Great Glen is a huge valley, eroded by glaciers more than 10,000 years ago. The stretch between Fort William and Inverness is one of the most scenic drives in Scotland. Order publications, find out about the Lyell Collection and read guidelines for preparing a paper or submitting a book proposal. at university; and for those seeking professional Information about the Geological Society’s internationally acclaimed books and journals for authors, editors, librarians and readers. The mountain of Lochnagar … The Great Glen follows a line of rocks weakened by fault that moved between 400 and 300 million years ago. Although it is known that the north west and south east … 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. Fortunately, none of the modern day infrastructure has been affected by the tremors, as the latest one to affect Inverness and the surrounding area occurred in September 1901 and was approximately a 5.0 magnitude quake. Erosion along the fault zone during Quaternary glaciation formed the famous Loch Ness. [1] The second main phase of movement was during the Carboniferous, this time with a dextral sense. The Great Glen Fault line is a well-known geological fault which cuts through the Scottish Highlands and was active from 430 million to 2 million years ago. 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 exact timing is uncertain, but associated folds within the Devonian are cut by members of the Late Carboniferous to Early Permian dyke swarm. Location. A reconsideration of the entire problem now suggests that this view is no longer tenable and that the dislocation is, in reality, a lateral-slip or wrench fault with a horizontal … 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 Great Glen Fault is a long strike-slip fault that runs through its namesake the Great Glen in Scotland. The movement at that time was sinistral (left-lateral), the same as the closely related set of faults sub-parallel to the main part of the Great Glen Fault, which include the Strathconon Fault and Strathglass Faults to the northwest and the Laggan Fault, Tyndrum Fault, and Ericht-Laidon Fault to the southeast. Many translated example sentences containing "Great Glen fault" – German-English dictionary and search engine for German translations. The Glen has always been a natural travelling route in the Highlands of Scotland, and incorporates the Caledonian Canal and A82 road. 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. 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. 5459, p. 777. 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. Published: 21 June 1974; Great Glen Fault. This website uses cookies to give you the best user experience. To the northeast the fault connects to the Walls Boundary Fault and the associated Melby Fault and Nestings Fault, before becoming obscured by the effects of Mesozoic rifting to the north of Shetland.[1]. It formed towards the end of the Caledonian orogeny (mountain building) associated with the collision between the Laurentia and Baltic tectonic plates at the end of the Silurian period continuing into the Early Devonian (likely age range - 430-390 Ma (million years)). The fault is actually much longer, and over 400 million years old. Es bildete sich gegen Ende der kaledonischen Orogenese, die mit der Kollision zwischen den tektonischen Platten von Laurentia und Baltikum am Ende des Silur verbunden war und sich bis ins frühe Devon fortsetzte (wahrscheinlich Altersgruppe 430–390 Ma (Millionen Jahre)). Published: 21 June 1974; Great Glen Fault. Structured data. In the Highlands, earthquakes are linked to seismic activity along the ancient Great Glen Fault, a zone of fractures in two blocks of rock that are moving slowly in opposite directions. However, the fault is actually much longer and over 400 million years old. „Großes Tal“ von schottisch-gälisch gleann mòr), auch Glen More genannt, ist eine tektonische Verwerfung (Great Glen Fault), die mitten durch Schottland verläuft und das schottische Hochland in die Grampian Mountains und die Northwest Highlands unterteilt. Like other major fault zones around the world, the Great Glen has a long history of reactivation. The displacement is estimated to be 64 miles (104 km).[3]. adshelp[at]cfa.harvard.edu The ADS is operated by the Smithsonian Astrophysical Observatory under NASA Cooperative Agreement NNX16AC86A 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. (uk) rdfs:label: Great Glen Fault … Andrew Marr takes to the sky in a microlight over a giant crack that runs the length of Scotland: the Great Glen Fault. Great Glen Fault Download PDF. Keep up to date with activities, news and events and find out how Fellows can get involved. Geologists will tell you that the Great Glen divides the North of Scotland along a line from Fort William to Inverness and that the fault is a very old feature and has been active since Mid Devonian times (c.400 million years ago). The Great Glen Fault has a long movement history. Great Glen Fault Download PDF. Location. STORETVEDT, K. M. 1974. The Aspy Fault is a strike-slip fault that runs through 40 km of Cape Breton, Nova Scotia and is often thought to be a part of the Cabot Fault/ Great Glen Fault system of Avalonia. A huge rift valley was formed when the northwestern and southeastern sides of the fault slid in opposite directions for more than sixty miles, while the present landscape was shaped by glaciers that retreated only around 8000 BC. 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. Der Great Glen Fault hat eine lange Bewegungsgeschichte. During supercontinent Pangea, the Aspy Fault in the Cape Breton Highlands was likely connected to Scotland's Great Glen Fault, home to Loch Ness. 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. 249, Issue. Grave doubt is consequently thrown on the alleged horizontal displacement in the fault zone. To change your cookie settings, select the option below and follow the instructions. Search our collection of printed books, maps and journals, e-resources, bibliographic databases and archives. 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. A fault is where tectonic plates meet. The Great Glen Fault is a long strike-slip (transcurrent) fault that runs through its namesake the Great Glen (Glen Albyn) in Scotland.However, the fault is actually much longer and over 400 million years old. The bottom of the fault is largely covered with lakes, which are now connected by canals. These instructions are also obtainable from the privacy & cookies link at the bottom of any GSL page. It extends in both directions beyond mainland Scotland. 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 … And yes, moderate tremors have been felt in the area. Great Glen Fault . The Great Fault. File; File history; File usage on Commons; File usage on other wikis; No higher resolution available. primary education onwards; for those making careers choices Loch Ness was formed after that by glaciers. Jump to navigation Jump to search. Viele übersetzte Beispielsätze mit "great Glen fault" – Deutsch-Englisch Wörterbuch und Suchmaschine für Millionen von Deutsch-Übersetzungen. An Gleann Mòr, (The Great Glen), is a large geological fault, which runs for over 100 kilometres from Inverness, on the Moray Firth, to Fort William, at the head of Loch Linnhe. 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. The Great Glen Fault . The Great Glen Fault is a long strike-slip fault that runs through its namesake the Great Glen in 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)). 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 extends in both directions beyond mainland Scotland. The Great Glen Fault is a long strike-slip fault that runs through its namesake, the Great Glen, in Scotland. Loch Ness is the largest and most famous of the lakes. The Great Glen Fault had its final phase of movement during the Late Cretaceous to Early Tertiary. Find out about the benefits of membership, and how we can help you achieve and maintain Chartered status. Die Verwerfung ist seismisch aktiv. The Great Glen Fault is a long strike-slip fault that runs through its namesake, the Great Glen, in Scotland. 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 Great Glen Fault has a long movement history. The Geological Society offers grades of membership for every stage of your career, from student to retirement. Part of the fault runs through Cape Breton Highlands National Park. Lawrence. Updates on outreach activities, information about how the geosciences interact with society, details of policy related meetings, consultation responses, and policy briefing notes. Information on our Specialist and Regional groups, Joint Associations and Networks. Tectonic faults and volcanoes in Scotland? File:Great glen fault.png. geosciences training or exploring lifelong learning Aligned northeast to southwest, the Great Glen Fault extends further southwest in a straight line through Loch Linnhe and the Firth of Lorne, and then on into northwestern Ireland, directly through Lough Swilly, Donegal Bay and Clew Bay as the Leannan Fault. Aligned northeast to southwest, the Great Glen Fault … The fault is mostly inactive today, but occasional moderate tremors have been recorded over the past 150 years which has meant that seismic buffers are built into the Kessock Bridge carrying the A9 out of Inverness. On the Northern Highlands side of the fault the zones of shattering extend up to about 1 km beyond the crush-zone. The Great Glen Fault has a long movement history. English. A zone of shattered rock along the length of the fault is prone to erosion and this has given rise to the development of the most extensive valley in Scotland, the Great Glen ( Glen Mor ). Jedes Jahrhundert gibt es mehrere Erdbeben mit der Stärke 4 auf der Richterskala. Great Glen - Loch Linnhe - Firth of Lorn - Inverness - Aspy Fault - Kessock Bridge - Loch Ness - Fault (geology) - Scotland - Ireland - Lough Foyle - Donegal Bay - Clew Bay - Shetland - North America - Atlantic Ocean - Mid-Atlantic Ridge - Newfoundland (island) - Gulf of Saint Lawrence - Caledonian orogeny - Laurentia - Baltic Shield - Silurian - Devonian - Carboniferous The Great Glen Fault is a long strike-slip fault that runs through its namesake the Great Glen in Scotland. This website uses cookies to give you the best user experience. Great_glen_fault.png ‎ (144 × 250 pixels, file size: 7 KB, MIME type: image/png) File information. It formed towards the end of the Caledonian orogeny (mountain building) associated with the collision between the Laurentia and Baltic tectonic plates at the end of the Silurian period continuing into the Early Devonian (likely age range - 430-390 Ma (million years)). Moving to the west of Speyside, in the area called the Grampian Highlands, which lies between the Highland Boundary Fault to the south and the Great Glen Fault to the north, is an area that stretches from the islands of Islay and Jura in the south-west to the Buchan coast in the north-east. Great Glen (englisch; dt. The Great Glen Fault is a long strike-slip fault that runs through its namesake the Great Glen in Scotland.. opportunities. You have disabled cookies which will render many features of the GSL website unusable. Kennedy showed that the fault had moved sideways – as a so-called strike-slip (or wrench) fault. The fault continues on the North American side of the North Atlantic Ocean, but is no longer part of a contiguous fault, as the complete fault was broken when the Mid-Atlantic Ridge formed 200 million years ago. 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 hosts the most prominent fault in the British Isles, the Great Glen Fault. 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)). A 6th century abbey along the way marks the … It was one of the first such structures to gain wide acceptance and in the years before plate tectonics was established, was important evidence for large-scale lateral earth movements. Within the area there are many igneous intrusions of granitic, basic, and ultrabasic composition. (en) Розлом Грейт-Глен - що прямує долиною Грейт-Глен, Шотландія. Ruins and monasteries on deep lakes. To change your cookie settings, select the option below and follow the instructions. These instructions are also obtainable from the privacy & cookies link at the bottom of any GSL page. [2] It is at least 300 miles (480 km) long. Caledonian Channel: East-West connection for boats . The glen is … Captions. The contrast between the rocks flanking this Leannan fault is very marked. These glaciers carved the valley below present day sea level, forming a series of deep lakes, the largest and most famous of which is Loch Ness. 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. How did the Great Glen Fault originate? The deep fault splits the Scottish Highlands diagonally from coast to coast. Visible from space, the Great Glen is a huge valley in the Scottish Highlands, eroded by glaciers more than 10,000 years ago. Great Glen Fault.Nature, Vol. The Great Glen Fault has a long movement history. The Leannan fault is directly in line with the Great Glen fault and the possibility that it is a continuation of this structure is discussed. Discover and access geoscience information resources via one of the world’s premier Earth science libraries. The tectonic complexities associated with this configuration require further evaluation. after A-levels including undergraduate and further degrees Search the events calendar for forthcoming conferences and events, and view past meeting resources. This broken rock has guided erosion to form the deep linear depression of the G… Grave doubt is consequently thrown on the alleged horizontal displacement in the fault zone. Huw finds out... _____ Anturus Education make educational videos to … Geoscientist is the Fellowship magazine of the Geological Society: with news about science, people, the Society, features, reviews, opinion, letters and forthcoming events. Founded in 1807, we are the oldest geological society in the world. They are often valleys because the rock has been fractured by pressure and movement and weathers more easily. It follows a geological fault known as the Great Glen Fault, and bisects the Scottish Highlands into the Grampian Mountains to the southeast and the Northwest Highlands to the northwest. From Wikimedia Commons, the free media repository. The Glen runs along: * River Ness * Loch Dochfour * Loch Ness * River Oich * … 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. The fault is actually much longer, and over 400 million years old. All this, and more, can be found sooner here, in our online version. The Geological Society of London is the UK's national society for geoscience, providing support to over 12,000 members in the UK and overseas. The North American side of the fault runs through the length of northwestern Newfoundland, Canada, as the Cabot Fault (Long Range Fault) and on into the Gulf of St. The Great Glen Fault is a tear or strike-slip fault with a displacement estimated at 64 miles (104 km). Request PDF | On Jan 1, 2010, Martyn Stewart published The Great Glen Fault | Find, read and cite all the research you need on ResearchGate Information and resources for teachers and students from These glaciers carved the valley below present-day sea level, forming a series of deep lakes. Enquire about room hire and conference facilities at Burlington House.

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