File:Villeneuve lac et Canigou.jpg

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Summary

Description
English: The lake, now dammed and used as a reservoir, lies in a deflation pan. That is a natural, circular, shallow depression caused by the removal of fairly loose, mainly Pliocene, sediment by wind erosion, during very cold, windy phases of the Quaternary period. It is the largest of a number of such deflation pans in this area.
See: Calvet, Marc; Delmas, Magali; Gunnell, Yanni; Laumonier, Bernard. 2022. Geology and Landscapes of the Eastern Pyrenees: A Field Guide with Excursions (pp. 323-324). Springer International Publishing. Kindle Edition.
Français : Le lac, aujourd'hui endigué et utilisé comme réservoir, se trouve dans une "deflation pan". Il s'agit d'une cuvette naturelle circulaire et peu profonde causée par l'enlèvement de sédiments assez meubles, principalement du Pliocène, par l'érosion éolienne, pendant les phases très froides et venteuses du Quaternaire. Il s'agit de la plus grande des nombreuses cuvettes de ce genre de ce secteur de la plaine du Roussillon.
Voir : B. Laumonier et al., Notice explicative de la feuille Argelès-sur-Mer - Cerbère (1097) à 1/50 00, BRGM Éditions, Orléans, 2015 (pages 7, 62 et 95), en ligne à : http://ficheinfoterre.brgm.fr/Notices/1097N.pdf.
Date
Source Own work
Author Alan Mattingly
Camera location42° 38′ 06.04″ N, 2° 54′ 44.05″ E Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

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Captions

Lac de Villeneuve-de-la-Raho, Pyrénées-Orientales, France. In the distance: Canigou massif.

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26 November 2023

42°38'6.036"N, 2°54'44.050"E

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current21:03, 26 November 2023Thumbnail for version as of 21:03, 26 November 20234,608 × 3,456 (3.32 MB)Alan MattinglyUploaded own work with UploadWizard
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