Taillefer Massif

Taillefer Massif

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← Previous revision Revision as of 13:38, 19 April 2026
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{{Infobox mountain
{{Infobox mountain
| name = Taillefer massif
| name = Taillefer Massif
| native_name = {{Native name|fr|Massif du Taillefer}}
| native_name = {{Native name|fr|Massif du Taillefer}}
| map_image = Massif des Alpes map-fr.svg
| map_image = Massif des Alpes map-fr.svg
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| photo = Massif du Taillefer Chamrousse.jpg
| photo = Massif du Taillefer Chamrousse.jpg
}}
}}
The '''Taillefer massif''' ({{Langx|fr|Massif du Taillefer}}) is a massif in the [[French Alps]] located in the [[Isère|Isère department]].
The '''Taillefer Massif''' ({{Langx|fr|Massif du Taillefer}}) is a massif in the [[French Alps]] located in the [[Isère|Isère department]].


== Geography ==
== Geography ==
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== Geology ==
== Geology ==
The Taillefer massif is predominantly a crystalline massif, similar to the Belledonne, to which it serves as an extension.{{Cite book |url=https://www.google.co.in/books/edition/Transactions/uQPxAAAAMAAJ?hl=en&gbpv=0&bsq=massif%20du%20taillefer%20belledonne |title=Transactions |date=1962 |publisher=Waltman |pages=82 |language=fr}} In contrast, the western chain of [[Sénépy]] and the Conest mountain consists of slightly clayey limestones from the [[Lower Lias]] period. Additionally, the western flank features outcrops of calcschists from the [[Upper Lias]] period.{{Cite book |url=https://www.google.co.in/books/edition/Comptes_rendus_des_s%C3%A9ances_de_l_Acad%C3%A9m/qwCb8QkYoxEC?hl=en&gbpv=0&bsq=massif%20du%20taillefer%20Lias%20sup%C3%A9rieur%20calcschistes |title=Comptes rendus des séances de l'Académie des sciences: Sciences naturelles. Série D |date=1979 |publisher=Gauthier-Villars |language=fr}}
The Taillefer Massif is predominantly a crystalline massif, similar to the Belledonne, to which it serves as an extension.{{Cite book |url=https://www.google.co.in/books/edition/Transactions/uQPxAAAAMAAJ?hl=en&gbpv=0&bsq=massif%20du%20taillefer%20belledonne |title=Transactions |date=1962 |publisher=Waltman |pages=82 |language=fr}} In contrast, the western chain of [[Sénépy]] and the Conest mountain consists of slightly clayey limestones from the [[Lower Lias]] period. Additionally, the western flank features outcrops of calcschists from the [[Upper Lias]] period.{{Cite book |url=https://www.google.co.in/books/edition/Comptes_rendus_des_s%C3%A9ances_de_l_Acad%C3%A9m/qwCb8QkYoxEC?hl=en&gbpv=0&bsq=massif%20du%20taillefer%20Lias%20sup%C3%A9rieur%20calcschistes |title=Comptes rendus des séances de l'Académie des sciences: Sciences naturelles. Série D |date=1979 |publisher=Gauthier-Villars |language=fr}}


== References ==
== References ==