Cleveland Dyke
id:
cleveland-dyke-236-16451013
title:
Cleveland Dyke
text:
The Cleveland Dyke is an igneous intrusion which extends from Galloway in southern Scotland through Cumbria and 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
brand slug:
wiki
category slug:
encyclopedia
description:
Geological feature across England and Scotland
original url:
https://en.wikipedia.org/wiki/Cleveland_Dyke
date created:
date modified:
2023-03-24T18:38:30Z
main entity:
{"identifier":"Q16949199","url":"https://www.wikidata.org/entity/Q16949199"}
image:
fields total:
13
integrity:
14