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- Myddfai_Steep_Belt abstract "The Myddfai Steep Belt is a geological structure which affects rocks of Silurian and Devonian age in mid Wales. It extends for tens of miles across country from near Carmarthen northeastwards via Mynydd Myddfai, Mynydd Bach Trecastell and Mynydd Epynt to the vicinity of Llangammarch Wells. Within this linear zone, the rock beds have been tilted steeply to the southeast. The folding took place in late Silurian to early Devonian times. This structure gives rise to a series of landscape features along its length, not least the steep northwest-facing scarps of the hills and ranges mentioned above. Indeed, the feature can be seen as a significant lineament in aerial and satellite views of Wales.The Steep Belt effectively marks the southeastern edge of the intensely folded region of the Caledonian Orogenic Belt in central Wales. A series of major folds and faults affect the Ordovician and Silurian rocks to its northwest whilst folding and faulting of the Devonian rocks to its southeast is much more subdued. The Steep Belt forms a part of a much longer feature which extends from Pembrokeshire as far as Shropshire and Cheshire and is sometimes referred to as the Pontesford Lineament. The Lineament includes the Pontesford-Linley Fault, the Clun Forest Disturbance and the Red Rock Fault Zone which marks the eastern edge of the Cheshire basin.".
- Myddfai_Steep_Belt wikiPageID "21254774".
- Myddfai_Steep_Belt wikiPageLength "1948".
- Myddfai_Steep_Belt wikiPageOutDegree "21".
- Myddfai_Steep_Belt wikiPageRevisionID "684607961".
- Myddfai_Steep_Belt wikiPageWikiLink Caledonian_orogeny.
- Myddfai_Steep_Belt wikiPageWikiLink Carmarthen.
- Myddfai_Steep_Belt wikiPageWikiLink Category:Geography_of_Carmarthenshire.
- Myddfai_Steep_Belt wikiPageWikiLink Category:Geography_of_Powys.
- Myddfai_Steep_Belt wikiPageWikiLink Category:Geology_of_Wales.
- Myddfai_Steep_Belt wikiPageWikiLink Cheshire.
- Myddfai_Steep_Belt wikiPageWikiLink Devonian.
- Myddfai_Steep_Belt wikiPageWikiLink Lineament.
- Myddfai_Steep_Belt wikiPageWikiLink Llangammarch_Wells.
- Myddfai_Steep_Belt wikiPageWikiLink Mynydd_Bach_Trecastell.
- Myddfai_Steep_Belt wikiPageWikiLink Mynydd_Epynt.
- Myddfai_Steep_Belt wikiPageWikiLink Mynydd_Myddfai.
- Myddfai_Steep_Belt wikiPageWikiLink Ordovician.
- Myddfai_Steep_Belt wikiPageWikiLink Pembrokeshire.
- Myddfai_Steep_Belt wikiPageWikiLink Shropshire.
- Myddfai_Steep_Belt wikiPageWikiLink Silurian.
- Myddfai_Steep_Belt wikiPageWikiLink Structural_geology.
- Myddfai_Steep_Belt wikiPageWikiLink Wales.
- Myddfai_Steep_Belt wikiPageWikiLink Wem-Bridgemere-Red_Rock_Fault_System.
- Myddfai_Steep_Belt wikiPageWikiLinkText "Myddfai Steep Belt".
- Myddfai_Steep_Belt wikiPageUsesTemplate Template:Reflist.
- Myddfai_Steep_Belt subject Category:Geography_of_Carmarthenshire.
- Myddfai_Steep_Belt subject Category:Geography_of_Powys.
- Myddfai_Steep_Belt subject Category:Geology_of_Wales.
- Myddfai_Steep_Belt hypernym Structure.
- Myddfai_Steep_Belt type Building.
- Myddfai_Steep_Belt comment "The Myddfai Steep Belt is a geological structure which affects rocks of Silurian and Devonian age in mid Wales. It extends for tens of miles across country from near Carmarthen northeastwards via Mynydd Myddfai, Mynydd Bach Trecastell and Mynydd Epynt to the vicinity of Llangammarch Wells. Within this linear zone, the rock beds have been tilted steeply to the southeast. The folding took place in late Silurian to early Devonian times.".
- Myddfai_Steep_Belt label "Myddfai Steep Belt".
- Myddfai_Steep_Belt sameAs Q16931768.
- Myddfai_Steep_Belt sameAs m.05c27n7.
- Myddfai_Steep_Belt sameAs Q16931768.
- Myddfai_Steep_Belt wasDerivedFrom Myddfai_Steep_Belt?oldid=684607961.
- Myddfai_Steep_Belt isPrimaryTopicOf Myddfai_Steep_Belt.