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- Marmontains_Formation abstract "The Couches des Marmontains are a sedimentary formation deposited during the middle Cretaceous (Albian to Cenomanian). It consists of sandstones and black shales. The formation is 5 to 30 m thick. The Couches des Marmontains overly the Couches de l’Aroley and underlie the Couches de Saint Christophe. All three units together make up the post-rift sequence of the Valais ocean. Outcrops can be found north of Bourg-Saint-Maurice.The Couches des Marmontains can be found in the following nappes:External ValaisMoûtiers unitRoc de l'Enfer unitPetit St. Bernard unitInternal ValaisVersoyen unitThe type locality and namesake of the formation is the mountain Marmontains (45.88263°N 7.108412°E / 45.88263; 7.108412) and the Val Ferret in Orsières, Canton Valais, Switzerland. It was first described in 1955 by Rudolf Trümpy.The Marmontains Formation can be correlated with the Valzeina Formation of Graubünden and black shales in the Engadine.".
- Marmontains_Formation wikiPageID "38598102".
- Marmontains_Formation wikiPageRevisionID "556715786".
- Marmontains_Formation country France.
- Marmontains_Formation name "Couches des Marmontains".
- Marmontains_Formation namedfor "L’arête des Marmontains".
- Marmontains_Formation overlies Couches_de_l’Aroley_Formation.
- Marmontains_Formation period "Albian".
- Marmontains_Formation region Savoie.
- Marmontains_Formation thickness "1800.0".
- Marmontains_Formation type Formation_(stratigraphy).
- Marmontains_Formation underlies Saint_Christophe_Formation.
- Marmontains_Formation unitof "Valais trilogy".
- Marmontains_Formation subject Category:Geology_of_France.
- Marmontains_Formation subject Category:Geology_of_Switzerland.
- Marmontains_Formation subject Category:Geology_of_the_Alps.
- Marmontains_Formation point "45.696144 6.734438".
- Marmontains_Formation type SpatialThing.
- Marmontains_Formation comment "The Couches des Marmontains are a sedimentary formation deposited during the middle Cretaceous (Albian to Cenomanian). It consists of sandstones and black shales. The formation is 5 to 30 m thick. The Couches des Marmontains overly the Couches de l’Aroley and underlie the Couches de Saint Christophe. All three units together make up the post-rift sequence of the Valais ocean.".
- Marmontains_Formation label "Marmontains Formation".
- Marmontains_Formation sameAs m.0r4wlkj.
- Marmontains_Formation sameAs Q5175951.
- Marmontains_Formation sameAs Q5175951.
- Marmontains_Formation lat "45.696144".
- Marmontains_Formation long "6.734438".
- Marmontains_Formation wasDerivedFrom Marmontains_Formation?oldid=556715786.
- Marmontains_Formation isPrimaryTopicOf Marmontains_Formation.