Aroley Formation
id:
aroley-formation-281-11716038
title:
Aroley Formation
text:
The Couches de l’Aroley are a sedimentary formation deposited during the Early Cretaceous. They consist of calcitic schists with dolomite clasts interbedded with finegrained conglomerates. The whole sequence is about 100 m thick. The Couches de l’Aroley are the lowest of the three post-rift sequences deposited in the Valais ocean. It overlies syn-rift sequences of the Brèches du Grand Fond Group. The Aroley Formation can be found within the following nappes: External Valais
Moûtiers unit
Roc de
brand slug:
wiki
category slug:
encyclopedia
description:
original url:
https://en.wikipedia.org/wiki/Aroley_Formation
date created:
date modified:
2023-01-29T14:32:30Z
main entity:
{"identifier":"Q5175949","url":"https://www.wikidata.org/entity/Q5175949"}
image:
{"content_url":"https://upload.wikimedia.org/wikipedia/commons/2/2f/Pierre_Avoi.JPG","width":3008,"height":2000}
fields total:
13
integrity:
14