North Pennine Batholith
id:
north-pennine-batholith-307-2500711
title:
North Pennine Batholith
text:
The North Pennine Batholith, also known as the Weardale Granite is a granitic batholith lying under northeast England, emplaced around 400 million years ago in the early Devonian. The batholith consists of five plutons, the Tynehead, Scordale, Rowlands Gill, Cornsay and Weardale plutons. The Weardale Granite pluton is the largest and the only one that has been proved (sampled), after the Rookhope Borehole confirmed Martin Bott's hypothesis that a large negative gravity anomaly under Weardale rep
brand slug:
wiki
category slug:
encyclopedia
description:
Granite batholith under northeast England
original url:
https://en.wikipedia.org/wiki/North_Pennine_Batholith
date created:
date modified:
2024-04-06T17:04:47Z
main entity:
{"identifier":"Q7056311","url":"https://www.wikidata.org/entity/Q7056311"}
image:
{"content_url":"https://upload.wikimedia.org/wikipedia/commons/b/b9/3D_Weardale_Granite.png","width":4000,"height":2224}
fields total:
13
integrity:
15