Neath Disturbance
id:
neath-disturbance-296-1476470
title:
Neath Disturbance
text:
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
brand slug:
wiki
category slug:
encyclopedia
description:
Geological structure in Great Britain
original url:
https://en.wikipedia.org/wiki/Neath_Disturbance
date created:
date modified:
2022-10-12T18:44:17Z
main entity:
{"identifier":"Q6984492","url":"https://www.wikidata.org/entity/Q6984492"}
image:
fields total:
13
integrity:
14