- Parc naturel régional du Luberon - https://www.parcduluberon.fr/en/ -

Fossil foootprints

Mots clefs
  • Découverte [1]
  • Géologie [2]
  • Sites yielding fossil mammal footprints are rare on a global scale. However, the Luberon region features several examples, including sites in Saignon, Viens, and Manosque. The site of  Viens displays nearly 200 depressions corresponding to mammal footprints over an area of approximately 400 square meters. It is part of the Luberon Geological Nature Reserve.

    Location : Viens
    Site type : formation géologique remarquable
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    • empreinte_3_doigts_c_pnrl_stephane_legal
    • dessin_dalle_viens_c_aline_laage
    • piste_dalle_viens_c_stephane_legal
    • Panneau d'interprétation à la dalle de Viens
      Viens fossil tracks information panel
      © PNRL - Stéphane Legal
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    The Site

    The site, discovered in 1968 by hikers, consists of two slabs from the same geological layer, separated by a trail (GR6-GR97). The smaller slab, located above the path, is about 20 square meters, while the larger one measures approximately 400 square meters. Composed of limestone, this layer is inclined about 15° to the south, with small faults oriented northeast/southwest scattered across its surface. This limestone is of lacustrine-lagoonal origin and dates back approximately 30 million years (La Fayette Limestone Formation, Oligocene, Cenozoic).

    The Footprints

    The limestone layer features numerous depressions (nearly 300) corresponding to mammal footprints. Some are arranged in tracks, allowing the tracing of the movements of now-extinct animals.

    Three-Toed Footprints

    The perissodactyl trackways are referred to as Rhinoceripeda voconcense. These footprints are attributed to a Ronzotherium (a group of rhinoceroses). Notably, a fragment of a Ronzotherium jawbone was found in the clay quarry at Viens.

    Two-Toed Footprints

    About a hundred two-toed footprints (artiodactyls), identified as Megapecoripeda velox, have been highlighted. These footprints are attributed to Entelodonts, ungulates that appeared in Europe at the begigning of the Oligocene.

    Other smaller footprints are attributed to small chevrotains (e.g., Gelocus, Lophiomerix, Bachitherium).

    — Getting to the site of Viens

    The footprint site is located 1 km south of Gignac. Park at the intersection between the road and the GR trail, and take the path heading towards Viens for 500 meters.
    Calculate your route [3]

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    Photo du bandeau : Empreinte fossile à deux doigts sur la dalle de Viens  © PNRL – Stéphane Legal

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    Photo du bandeau : © Prénom Nom