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- Cribarth_Disturbance abstract "The Cribarth Disturbance is a geological structure forming a lineament which stretches across south Wales from Swansea up the Swansea Valley then northeastwards to Brecon and beyond. It consists of both a series of 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. It is also known (in part) as the Tawe Valley Disturbance or the Swansea Valley Disturbance.".
- Cribarth_Disturbance wikiPageID "21035414".
- Cribarth_Disturbance wikiPageRevisionID "550397376".
- Cribarth_Disturbance hasPhotoCollection Cribarth_Disturbance.
- Cribarth_Disturbance subject Category:Geology_of_Wales.
- Cribarth_Disturbance comment "The Cribarth Disturbance is a geological structure forming a lineament which stretches across south Wales from Swansea up the Swansea Valley then northeastwards to Brecon and beyond. It consists of both a series of 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.".
- Cribarth_Disturbance label "Cribarth Disturbance".
- Cribarth_Disturbance sameAs m.05b50_v.
- Cribarth_Disturbance sameAs Q5184877.
- Cribarth_Disturbance sameAs Q5184877.
- Cribarth_Disturbance wasDerivedFrom Cribarth_Disturbance?oldid=550397376.
- Cribarth_Disturbance isPrimaryTopicOf Cribarth_Disturbance.