Topographical areas of Yorkshire
id:
topographical-areas-of-yorkshire-310-5139025
title:
Topographical areas of Yorkshire
text:
In Yorkshire there is a very close relationship between the major topographical areas and the geological period in which they were formed. The Pennine chain of Hills in the west is of Carboniferous origin. The central vale is Permo-Triassic. The North York Moors in the north-east of the county are Jurassic in age while the Yorkshire Wolds to the south east are Cretaceous chalk uplands. The plain of Holderness and the Humberhead levels both owe their present form to the Quaternary ice ages. Much
brand slug:
wiki
category slug:
encyclopedia
description:
original url:
https://en.wikipedia.org/wiki/Topographical_areas_of_Yorkshire
date created:
date modified:
2022-03-28T12:27:09Z
main entity:
{"identifier":"Q7824962","url":"https://www.wikidata.org/entity/Q7824962"}
image:
{"content_url":"https://upload.wikimedia.org/wikipedia/commons/0/0a/Yorksgeology.jpg","width":549,"height":451}
fields total:
13
integrity:
14