Northumberland Trough
id:
northumberland-trough-264-9410405
title:
Northumberland Trough
text:
The Northumberland Trough, also known as the Northumberland Basin, is an element of the structural geology of northern England, the origin of which dates back to the Carboniferous period when a block and basin province was established throughout the Pennine region. The trough is an ENE-WSW aligned half-graben, an asymmetric depositional basin. It is defined to the south by the Stublick and Ninety Fathom faults, which separate the trough from the Alston Block. To the north, where its depth is lea
brand slug:
wiki
category slug:
encyclopedia
description:
original url:
https://en.wikipedia.org/wiki/Northumberland_Trough
date created:
date modified:
2023-07-23T22:22:00Z
main entity:
{"identifier":"Q85789787","url":"https://www.wikidata.org/entity/Q85789787"}
image:
fields total:
13
integrity:
13