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- Cleveland_Dyke abstract "The Cleveland Dyke (or Armathwaite Dyke) is an igneous intrusion which extends from Galloway in southern Scotland through County Durham in northern England to the North York Moors in North Yorkshire. The dyke is associated with volcanism which took place at the Isle of Mull igneous centre in western Scotland during the early Palaeogene Period at a time of regional crustal tension associated with the opening of the north Atlantic Ocean and which resulted in the intrusion of innumerable dykes. The Cleveland Dyke has been dated to 55.8+/- 0.9 Ma. Though generally from 22-28 m wide, in places it is up to 30 m wide and has been mapped over a distance of 430 km. It is the most significant of a swarm of such intrusions associated with the Mull centre which extend southeastwards through this region, the others being the Acklington Dyke and the Blyth and Sunderland subswarms of Northumberland and Tyne and Wear.It was thought traditionally that the entire dyke comprising some 85 km3 of rock was emplaced as a single pulse of magma over a few days, moving southeastwards from Mull but also rising vertically through the country rock, this mechanism leading in places to the development of en echelon segments of dyke. However, more recent work suggests that vertical emplacement as a series of thin blades of magma from a series of high level chambers within the crust is more likely. Offsets of the alignment occur within Scotland where the dyke crosses Caledonide fault systems. The dyke is composed of basaltic andesite which is amygdaloidal in places.The dyke has been worked for roadstone at numerous localities including Barrock Fell near Armathwaite in Cumbria and at both Cockfield Fell and Bolam in County Durham. Setts for road construction were made from the dyke at Langbaurgh.".
- Cleveland_Dyke wikiPageID "40644039".
- Cleveland_Dyke wikiPageLength "3029".
- Cleveland_Dyke wikiPageOutDegree "31".
- Cleveland_Dyke wikiPageRevisionID "680077322".
- Cleveland_Dyke wikiPageWikiLink Acklington_Dyke.
- Cleveland_Dyke wikiPageWikiLink Amygdule.
- Cleveland_Dyke wikiPageWikiLink Armathwaite.
- Cleveland_Dyke wikiPageWikiLink Atlantic_Ocean.
- Cleveland_Dyke wikiPageWikiLink Basaltic_andesite.
- Cleveland_Dyke wikiPageWikiLink Bolam,_County_Durham.
- Cleveland_Dyke wikiPageWikiLink Caledonian_orogeny.
- Cleveland_Dyke wikiPageWikiLink Category:Geology_of_Scotland.
- Cleveland_Dyke wikiPageWikiLink Category:Geology_of_Yorkshire.
- Cleveland_Dyke wikiPageWikiLink Cockfield,_County_Durham.
- Cleveland_Dyke wikiPageWikiLink Construction_aggregate.
- Cleveland_Dyke wikiPageWikiLink County_Durham.
- Cleveland_Dyke wikiPageWikiLink Cumbria.
- Cleveland_Dyke wikiPageWikiLink Dike_(geology).
- Cleveland_Dyke wikiPageWikiLink Dike_swarm.
- Cleveland_Dyke wikiPageWikiLink Dyke_(geology).
- Cleveland_Dyke wikiPageWikiLink England.
- Cleveland_Dyke wikiPageWikiLink Fault_(geology).
- Cleveland_Dyke wikiPageWikiLink Galloway.
- Cleveland_Dyke wikiPageWikiLink Igneous_rock.
- Cleveland_Dyke wikiPageWikiLink Intrusion.
- Cleveland_Dyke wikiPageWikiLink Isle_of_Mull.
- Cleveland_Dyke wikiPageWikiLink Langbaurgh,_North_Yorkshire.
- Cleveland_Dyke wikiPageWikiLink Magma.
- Cleveland_Dyke wikiPageWikiLink Mull.
- Cleveland_Dyke wikiPageWikiLink North_York_Moors.
- Cleveland_Dyke wikiPageWikiLink North_Yorkshire.
- Cleveland_Dyke wikiPageWikiLink Northumberland.
- Cleveland_Dyke wikiPageWikiLink Palaeogene.
- Cleveland_Dyke wikiPageWikiLink Paleogene.
- Cleveland_Dyke wikiPageWikiLink Scotland.
- Cleveland_Dyke wikiPageWikiLink Sett_(paving).
- Cleveland_Dyke wikiPageWikiLink Tyne_and_Wear.
- Cleveland_Dyke wikiPageWikiLink Volcanism.
- Cleveland_Dyke wikiPageWikiLinkText "Cleveland Dyke".
- Cleveland_Dyke wikiPageWikiLinkText "Cleveland".
- Cleveland_Dyke hasPhotoCollection Cleveland_Dyke.
- Cleveland_Dyke wikiPageUsesTemplate Template:Reflist.
- Cleveland_Dyke subject Category:Geology_of_Scotland.
- Cleveland_Dyke subject Category:Geology_of_Yorkshire.
- Cleveland_Dyke hypernym Intrusion.
- Cleveland_Dyke type Mountain.
- Cleveland_Dyke comment "The Cleveland Dyke (or Armathwaite Dyke) is an igneous intrusion which extends from Galloway in southern Scotland through County Durham in northern England to the North York Moors in North Yorkshire. The dyke is associated with volcanism which took place at the Isle of Mull igneous centre in western Scotland during the early Palaeogene Period at a time of regional crustal tension associated with the opening of the north Atlantic Ocean and which resulted in the intrusion of innumerable dykes.".
- Cleveland_Dyke label "Cleveland Dyke".
- Cleveland_Dyke sameAs m.0xnq3bn.
- Cleveland_Dyke sameAs Q16949199.
- Cleveland_Dyke sameAs Q16949199.
- Cleveland_Dyke wasDerivedFrom Cleveland_Dyke?oldid=680077322.
- Cleveland_Dyke isPrimaryTopicOf Cleveland_Dyke.