Roignais

Refuge de Presset is a refuge in the Alps.

Aiguille du Grand Fond is a mountain of Savoie, France. It lies in the Beaufortain Massif range. It has an elevation of 2,920 metres above sea level.

Pierra Menta is a mountain of Savoie, France. It lies in the Beaufortain Massif range. It has an elevation of 2,714 metres above sea level.

The Pointe de la Terrasse (2,881 m) is a mountain in the Beaufortain Massif in Savoie, France.

The Grande Paréi (2,705 m, sometimes written Grande Parei) is a mountain in the Beaufortain massif in Savoie, France. The Beaufortain is situated about 20 km South-West of Mont Blanc.

Les Chapelles (French pronunciation: [le ʃapɛl]; Arpitan: Lé Tsapéle) is a commune in the Savoie department in the Auvergne-Rhône-Alpes region in south-eastern France.

Valezan (French pronunciation: [valzɑ̃]; Arpitan: Valzan) is a former commune in the Savoie department in the Auvergne-Rhône-Alpes region in south-eastern France. On 1 January 2016, it was merged into the new commune of La Plagne Tarentaise.

The Brèches du Grand Fond Group is a group of stratigraphic formations in France that were deposited between the Middle Jurassic and the Early Cretaceous. The deposition was contemporaneous to the rifting of the Valais ocean, and overlies the pre-rift rocks along an angular unconformity. The Brèches du Grand Fond Group is overlain by the post-rift sequences Couches de l’Aroley, Couches des Marmontains and the Couches de Saint Christophe.The Brèches du Grand Fond Group consists of two formations that are found in the External Valais units, the younger Pyramides Calcaires Formation and the older Dent d'Arpire Formation. The deposition of these two units was roughly contemporaneous to the deposition of the Brèches du Collet des Rousses and the Complexe Antéflysch Formation of the Internal Valais units.In general the Brèches du Grand Fond Group consists of coarse grained clastic sediments composed of pre-rift lithologies. Outcrops can be studied The Brèches du Grand Fond Group can be found within the following nappes: External ValaisMoûtiers unit Roc de l'Enfer unitOutcrops occur to the northwest of Bourg-Saint-Maurice.

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 unit Roc de l'Enfer unit Petit 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.

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 Valais Moûtiers unit Roc de l'Enfer unit Petit St. Bernard unit Internal Valais Versoyen 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.

The Couches de Saint Christophe are a sedimentary formation deposited between the Late Cretaceous and the Paleogene. It is a very monotonous sequence of calcitic sandstones and black schists. These are interpreted as a turbidite sequence. The average thickness of the unit is 500 m. The Couches de Saint Christophe are a post-rift sequence that overlies the Couches des Marmontains.The Couches de Saint Christophe occupy the following nappes: External ValaisMoûtiers unit Roc de l'Enfer unit Petit St. Bernard unitInternal ValaisVersoyen unitLarge outcrops of the Couches de Saint Christophe crop out north of Bourg-Saint-Maurice.The type locality of the formation is the Val de Bagnes in the canton Valais of Switzerland. It was first described by Rudolf Trümpy in 1952. The formation is named after a chapel (46.094905°N 7.200371°E / 46.094905; 7.200371) to the northwest of Verbier.The Saint Christophe Formation can be correlated with the Sassauna Formation found in Graubünden and calcareous flysch found in the Engadine.

La Côte-d'Aime (French pronunciation: [la kot dɛm], literally The Slope of Aime; Arpitan: La Kouha d’Éma) is a former commune in the Savoie department in the Auvergne-Rhône-Alpes region in south-eastern France. On 1 January 2016, it was merged into the new commune of La Plagne Tarentaise.It lies in the heart of the Tarentaise valley.