Northern Harz Boundary Fault
id:
northern-harz-boundary-fault-309-12957421
title:
Northern Harz Boundary Fault
text:
The Northern Harz Boundary Fault is a geological fault where the Harz Block, which consists of rocks formed during the Palaeozoic Era and folded in the course of Hercynian mountain building, borders on the Subhercynian Basin or Harz Foreland. The fault is also known in English as the Harz North Rim Fault or Harznordrand Thrust (Fault). The northern edge of the Harz is oriented in a Hercynian (WNW-ESE) direction and runs from Neuekrug-Hahausen via Langelsheim, Goslar, Bad Harzburg, Ilsenburg, Wer
brand slug:
wiki
category slug:
encyclopedia
description:
original url:
https://en.wikipedia.org/wiki/Northern_Harz_Boundary_Fault
date created:
date modified:
2023-06-15T09:40:35Z
main entity:
{"identifier":"Q1488852","url":"https://www.wikidata.org/entity/Q1488852"}
image:
{"content_url":"https://upload.wikimedia.org/wikipedia/commons/c/c9/Harznordrandstoerung_Langenberg.jpg","width":801,"height":534}
fields total:
13
integrity:
14