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- Aroley_Formation abstract "The Couches de l’Aroley (short: Aroley Formation) are a sedimentary formation deposited during the Early Cretaceous (Barremian to Aptian). 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 ValaisMoûtiers unitRoc de l'Enfer unitPetit St. Bernard unitInternal ValaisVersoyen unitThe type locality is the Massif de la Pierre Avoi, in Saxon, Valais, Switzerland. The formation is named after a "Plan Aroley" which lies below the Pierre Avoi. It was first described by Rudolf Trümpy 1952.The Couches de l’Aroley can be correlated with the Klus Formation and the Tristel Formation found in eastern Switzerland, the Engadin window and the Tauern window.".
- Aroley_Formation thumbnail Pierre_Avoi.JPG?width=300.
- Aroley_Formation wikiPageID "38602661".
- Aroley_Formation wikiPageRevisionID "579018585".
- Aroley_Formation caption "Pierre Avoi is the type locality of the Aroley formation.".
- Aroley_Formation country France.
- Aroley_Formation name "Couches de l’Aroley".
- Aroley_Formation namedfor "Plan Aroley".
- Aroley_Formation otherlithology "Fine conglomerate".
- Aroley_Formation overlies Brèches_du_Grand_Fond_Group.
- Aroley_Formation period "Barremian".
- Aroley_Formation prilithology "Calcitic schist".
- Aroley_Formation region Savoie.
- Aroley_Formation thickness "6000.0".
- Aroley_Formation type Formation_(stratigraphy).
- Aroley_Formation underlies Marmontains_Formation.
- Aroley_Formation unitof "Valais trilogy".
- Aroley_Formation subject Category:Geology_of_France.
- Aroley_Formation subject Category:Geology_of_Switzerland.
- Aroley_Formation subject Category:Geology_of_the_Alps.
- Aroley_Formation point "45.696144 6.734438".
- Aroley_Formation type SpatialThing.
- Aroley_Formation comment "The Couches de l’Aroley (short: Aroley Formation) are a sedimentary formation deposited during the Early Cretaceous (Barremian to Aptian). 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.".
- Aroley_Formation label "Aroley Formation".
- Aroley_Formation sameAs m.0r4xwrj.
- Aroley_Formation sameAs Q5175949.
- Aroley_Formation sameAs Q5175949.
- Aroley_Formation lat "45.696144".
- Aroley_Formation long "6.734438".
- Aroley_Formation wasDerivedFrom Aroley_Formation?oldid=579018585.
- Aroley_Formation depiction Pierre_Avoi.JPG.
- Aroley_Formation isPrimaryTopicOf Aroley_Formation.