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Geological Formation

Baïgorry Valley

Valleys

The Baïgorry Valley is a valley in the Pyrenees through which flows the Nive des Aldudes, a tributary of the Nive River. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

Connections

Associated With

Paleozoic, Eras
Source Baïgorry Valley (Wikipedia)
Permian, Eras
Source Baïgorry Valley (Wikipedia)
Sandstone, Materials
Source Baïgorry Valley (Wikipedia)
Triassic, Eras
Source Baïgorry Valley (Wikipedia)

Caused By

Erosion, Processes

Wikidata P31 formation-type mapped to formative process Erosion via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Baïgorry Valley

In Discipline

Geomorphology, Disciplines

Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Baïgorry Valley
In the Other Atlases

Found In

France

Also in Geography Atlas: where this subject is found.

Source Wikidata: Baïgorry Valley
Sources
Baïgorry Valley (Wikipedia)
  • Lead section
    The Baïgorry Valley is a valley in the Pyrenees through which flows the Nive des Aldudes, a tributary of the Nive River.
  • Associated With: Paleozoic, Article text, age Paleozoic
    The Baïgorry Valley lies within an ancient massif composed of Paleozoic rocks dating from 550 to 250 million years ago.
  • Associated With: Permian, Article text, age Permian
    To the northwest, the watershed dividing the Nive and Bidassoa river basins follows the crest of a Permian-Triassic cuesta in the Baztan region, formed of pink sandstone.
  • Associated With: Triassic, Article text, age Triassic
    To the northwest, the watershed dividing the Nive and Bidassoa river basins follows the crest of a Permian-Triassic cuesta in the Baztan region, formed of pink sandstone.
  • Associated With: Sandstone, Article text, rock Sandstone
    To the northwest, the watershed dividing the Nive and Bidassoa river basins follows the crest of a Permian-Triassic cuesta in the Baztan region, formed of pink sandstone.
View the Source
Wikidata: Baïgorry Valley
Wikidata Q3554046, class allow-list match (w-wdresolver-0926)View the Source
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