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puy+griou Latitude and Longitude:

45°04′49″N 2°42′22″E / 45.08028°N 2.70611°E / 45.08028; 2.70611
From Wikipedia, the free encyclopedia
Puy Griou
Highest point
Elevation1,690 m (5,540 ft)
Coordinates 45°04′49″N 2°42′22″E / 45.08028°N 2.70611°E / 45.08028; 2.70611
Geography
Puy Griou is located in France
Puy Griou
Puy Griou
France
Location Cantal departement, France
Parent range Mounts of Cantal ( Massif Central)

The Puy Griou is a summit at an altitude of 1,690 meters in the Mounts of Cantal, located on the ridge line between the valleys of the Cère and the Jordanne [ fr], partially situated in the municipalities of Saint-Jacques-des-Blats and Mandailles.

Toponymy

The summit is called "Puei Griu" in Aurillac Occitan. In this dialect, griu comes from griea, which means "difficult to climb." [1] In the Occitan auvergnat spoken further north of the mountain, it is called Puei de Grion. [2]

Geology

Due to its position in the center of the Monts du Cantal and its very slender conical shape, Puy Griou was long considered to be the eroded chimney of the Cantal volcano. However, it has since lost this status, and geologists now consider it to be a phonolite dome occupying a central position similar to other peaks in the massif such as Roc d'Hozières [ fr]. It is believed to have formed approximately 6 million years ago, following the paroxysmal eruptive phases experienced by the Cantal between 8.5 Ma and 6.5 Ma. [3] During the cold periods of the recent Quaternary, repeated freeze-thaw cycles fractured the rock into slabs, forming a scree mantle. [4]

Access

The GR 400 follows the ridge line between the Col du Pertus and the Col de Rombière, near the ski resort of Le Lioran. At the foot of the dome, a trail veers southward, allowing for the ascent of the final 200 meters of elevation gain. [5] [6]

References

  1. ^ Lhermet, Jean (1931). Contribution à la lexicologie du dialecte aurillacois (in French). E. Droz. p. 19. ISBN  978-2-600-02902-5.
  2. ^ Roux, Jean (2004). L'auvergnat de poche (in French). Assimil. p. 246. ISBN  978-2-7005-0319-7.
  3. ^ Graveline, François; Brunel, Janine (1996). Cantal: la saga d'un volcan (in French). Editions Debaisieux. p. 96. ISBN  978-2-9509180-4-8.
  4. ^ "Comprendre la géologie du volcan cantalien | Carlades". Carlades – Office du tourisme (in French). 2020-02-28. Retrieved 2024-04-08.
  5. ^ "GR® 400 : le tour du volcan cantalien – Mon GR®". www.mongr.fr. Retrieved 2024-04-08.
  6. ^ "Le Puy Griou – Les Boissines | Auvergne Destination". www.auvergne-destination.com (in French). 2019-12-04. Retrieved 2024-04-08.

External links


puy+griou Latitude and Longitude:

45°04′49″N 2°42′22″E / 45.08028°N 2.70611°E / 45.08028; 2.70611
From Wikipedia, the free encyclopedia
Puy Griou
Highest point
Elevation1,690 m (5,540 ft)
Coordinates 45°04′49″N 2°42′22″E / 45.08028°N 2.70611°E / 45.08028; 2.70611
Geography
Puy Griou is located in France
Puy Griou
Puy Griou
France
Location Cantal departement, France
Parent range Mounts of Cantal ( Massif Central)

The Puy Griou is a summit at an altitude of 1,690 meters in the Mounts of Cantal, located on the ridge line between the valleys of the Cère and the Jordanne [ fr], partially situated in the municipalities of Saint-Jacques-des-Blats and Mandailles.

Toponymy

The summit is called "Puei Griu" in Aurillac Occitan. In this dialect, griu comes from griea, which means "difficult to climb." [1] In the Occitan auvergnat spoken further north of the mountain, it is called Puei de Grion. [2]

Geology

Due to its position in the center of the Monts du Cantal and its very slender conical shape, Puy Griou was long considered to be the eroded chimney of the Cantal volcano. However, it has since lost this status, and geologists now consider it to be a phonolite dome occupying a central position similar to other peaks in the massif such as Roc d'Hozières [ fr]. It is believed to have formed approximately 6 million years ago, following the paroxysmal eruptive phases experienced by the Cantal between 8.5 Ma and 6.5 Ma. [3] During the cold periods of the recent Quaternary, repeated freeze-thaw cycles fractured the rock into slabs, forming a scree mantle. [4]

Access

The GR 400 follows the ridge line between the Col du Pertus and the Col de Rombière, near the ski resort of Le Lioran. At the foot of the dome, a trail veers southward, allowing for the ascent of the final 200 meters of elevation gain. [5] [6]

References

  1. ^ Lhermet, Jean (1931). Contribution à la lexicologie du dialecte aurillacois (in French). E. Droz. p. 19. ISBN  978-2-600-02902-5.
  2. ^ Roux, Jean (2004). L'auvergnat de poche (in French). Assimil. p. 246. ISBN  978-2-7005-0319-7.
  3. ^ Graveline, François; Brunel, Janine (1996). Cantal: la saga d'un volcan (in French). Editions Debaisieux. p. 96. ISBN  978-2-9509180-4-8.
  4. ^ "Comprendre la géologie du volcan cantalien | Carlades". Carlades – Office du tourisme (in French). 2020-02-28. Retrieved 2024-04-08.
  5. ^ "GR® 400 : le tour du volcan cantalien – Mon GR®". www.mongr.fr. Retrieved 2024-04-08.
  6. ^ "Le Puy Griou – Les Boissines | Auvergne Destination". www.auvergne-destination.com (in French). 2019-12-04. Retrieved 2024-04-08.

External links


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