Construction period Néolithique (≈ 4100 av. J.-C.)
Edification of dolmen by neolithic communities.
1950
First scientific reference
First scientific reference 1950 (≈ 1950)
Reporting by Lluis Péricot after discovery.
3 novembre 1958
Classification of historical monuments
Classification of historical monuments 3 novembre 1958 (≈ 1958)
Official protection by ministerial decree.
Aujourd'hui
Aujourd'hui
Aujourd'hui Aujourd'hui (≈ 2025)
Position de référence.
Heritage classified
Dolmen dit Collets de Collioure (cad. CH 225): by order of 3 November 1958
Key figures
Pierre Ponsich - Discoverer of the dolmen
Archaeologist who identified the site around 1950.
Lluis Péricot - First scientific report
Mentioned dolmen in 1950.
Origin and history
The Dolmen des Collets de Cotlliure is a megalithic building located in Argelès-sur-Mer, in the Pyrénées-Orientales. Discovered by Pierre Ponsich, it was first reported in 1950 by Lluis Péricot. This dolmen, considered by Ponsich as a ciste, has a trapezoidal chamber bounded by four orthostates in local slate schist. The largest bedside slab is 1.65 m in length, while the cover table (1.50 m x 0.90 m) has been moved north of the tumulus, not visible today.
The monument is classified as historical monuments by order of 3 November 1958. Its modest architecture, with an opening to the east and a split slab, suggests a funeral vocation typical of Neolithic. The tumulus, partially erased, keeps a slab erect on its southern edge, possible vestige of a peristalith. The excavations and studies carried out in the 20th century, notably by Ponsich and Péricot, made it possible to document this site among the many megaliths of the Pyrénées-Orientales.
The region, rich in prehistoric sites, illustrates the importance of collective funeral practices during the Neolithic period. Dolmens, like that of the Cotlliure Collets, served as burials for sedentary agro-pastoral communities. Their construction of local stones, here from the slate shale, reflects a technical mastery and a complex social organization, characteristic of this period of transition towards the age of metals.
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