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- Neath_Disturbance abstract "The Neath Disturbance is a geological structure which stretches across south Wales from Swansea Bay northeastwards as far as Hereford in western England. It consists of a series of both faults and associated folds which were active during the mountain-building period known as the Variscan orogeny. This line of weakness probably featured in the earlier Caledonian Orogeny and perhaps reflects a more ancient line of weakness in the basement rocks.The Disturbance gives rise to a lineament crossing the region, that is to say that it is responsible for a number of significant landscape features along its 100 km length. Prominent amongst these is the Vale of Neath, a deep valley incised by a glacier during the ice ages along this line of weakness in the Earth's crust and now occupied by the River Neath between Pontneddfechan and Swansea Bay. The hill of Moel Penderyn also lies on the Disturbance a little further east. A part of the Vale of Grwyne north of The Sugarloaf and the northeast-southwest aligned section of the Monnow valley on the English/Welsh border are also excavated along this line of weakness.The Neath Disturbance is possibly the southernmost geological feature within Britain which can be described as following the Caledonoid trend. The phrase describes a suite of major geological structures associated with the closure of the former Iapetus Ocean in the middle Palaeozoic Era and giving rise to the Caledonian orogeny or mountain-building period. The Cribarth or Swansea Valley Disturbance and the Carreg Cennen Disturbance are similar features found a little further north in south Wales. The Bala Fault, Menai Strait Fault, Southern Uplands Fault, Highland Boundary Fault and Great Glen Fault are other major Caledonoid structures of Britain.".
- Neath_Disturbance wikiPageID "21033767".
- Neath_Disturbance wikiPageLength "2462".
- Neath_Disturbance wikiPageOutDegree "33".
- Neath_Disturbance wikiPageRevisionID "550396551".
- Neath_Disturbance wikiPageWikiLink Bala_Fault.
- Neath_Disturbance wikiPageWikiLink Basement_(geology).
- Neath_Disturbance wikiPageWikiLink Caledonian_orogeny.
- Neath_Disturbance wikiPageWikiLink Carreg_Cennen_Disturbance.
- Neath_Disturbance wikiPageWikiLink Category:Geology_of_Wales.
- Neath_Disturbance wikiPageWikiLink Cribarth_Disturbance.
- Neath_Disturbance wikiPageWikiLink England.
- Neath_Disturbance wikiPageWikiLink Fault_(geology).
- Neath_Disturbance wikiPageWikiLink Fold_(geology).
- Neath_Disturbance wikiPageWikiLink Geological_structure_of_Great_Britain.
- Neath_Disturbance wikiPageWikiLink Glacier.
- Neath_Disturbance wikiPageWikiLink Great_Glen_Fault.
- Neath_Disturbance wikiPageWikiLink Grwyne_Fawr.
- Neath_Disturbance wikiPageWikiLink Hereford.
- Neath_Disturbance wikiPageWikiLink Highland_Boundary_Fault.
- Neath_Disturbance wikiPageWikiLink Iapetus_Ocean.
- Neath_Disturbance wikiPageWikiLink Ice_age.
- Neath_Disturbance wikiPageWikiLink Lineament.
- Neath_Disturbance wikiPageWikiLink Menai_Strait_Fault.
- Neath_Disturbance wikiPageWikiLink Moel_Penderyn.
- Neath_Disturbance wikiPageWikiLink Paleozoic.
- Neath_Disturbance wikiPageWikiLink Pontneddfechan.
- Neath_Disturbance wikiPageWikiLink River_Monnow.
- Neath_Disturbance wikiPageWikiLink River_Neath.
- Neath_Disturbance wikiPageWikiLink Southern_Uplands_Fault.
- Neath_Disturbance wikiPageWikiLink Sugar_Loaf,_Monmouthshire.
- Neath_Disturbance wikiPageWikiLink Swansea_Bay.
- Neath_Disturbance wikiPageWikiLink Swansea_Valley.
- Neath_Disturbance wikiPageWikiLink Vale_of_Neath.
- Neath_Disturbance wikiPageWikiLink Variscan_orogeny.
- Neath_Disturbance wikiPageWikiLink Wales.
- Neath_Disturbance wikiPageWikiLinkText "Dinas Fault".
- Neath_Disturbance wikiPageWikiLinkText "Neath Disturbance".
- Neath_Disturbance wikiPageUsesTemplate Template:Reflist.
- Neath_Disturbance subject Category:Geology_of_Wales.
- Neath_Disturbance hypernym Structure.
- Neath_Disturbance type Building.
- Neath_Disturbance comment "The Neath Disturbance is a geological structure which stretches across south Wales from Swansea Bay northeastwards as far as Hereford in western England. It consists of a series of both faults and associated folds which were active during the mountain-building period known as the Variscan orogeny.".
- Neath_Disturbance label "Neath Disturbance".
- Neath_Disturbance sameAs Q6984492.
- Neath_Disturbance sameAs m.05b4g7z.
- Neath_Disturbance sameAs Q6984492.
- Neath_Disturbance wasDerivedFrom Neath_Disturbance?oldid=550396551.
- Neath_Disturbance isPrimaryTopicOf Neath_Disturbance.