First written entry 1897 (≈ 1897)
Published by Paul du Châtellier.
17 octobre 1995
Registration historical monument
Registration historical monument 17 octobre 1995 (≈ 1995)
Legal protection of the site and menhirs.
Aujourd'hui
Aujourd'hui
Aujourd'hui Aujourd'hui (≈ 2025)
Position de référence.
Heritage classified
Menhirs of the alignment as well as the land (soil, subsoil and monuments) on which they are established, namely the whole of Parcel D 136 plus a 10 metre strip of land in Parcel D 1599 throughout the boundary with Parcel D 136, with the exception of contemporary buildings: inscription by order of 17 October 1995
Key figures
Paul du Châtellier - Archaeologist
The site was mentioned in 1897.
Origin and history
Leitan's alignment is a group of five menhirs in local granite, of which only one, measuring about 3 meters high, remains standing today. The other blocks, about 3 meters long, lie in the slope or masked by vegetation. The alignment extends about 40 meters on a north-east/south-west axis, on the municipality of Brennilis, in Finistère.
The site was first mentioned by Paul du Châtellier in 1897 in his Memoirs of the Society of Emulation of the North Coasts. At that time, only one menhir was still trained. The alignment was inscribed as historical monuments on 17 October 1995, thus protecting menhirs and their immediate environment, with the exception of contemporary buildings.
The menhirs of Leitan date from the Protohistory and are listed in the ZPPAU (Zone of Protection of Architectural and Urban Heritage) of Brennilis. Their layout and size suggest a cultural or ritual significance, typical of the megalithic monuments of this period in Brittany. The site is now partially visible, with a location estimated as 'passable' in terms of accuracy.
Paul du Châtellier, 19th century archaeologist, played a key role in the initial documentation of the site. His work, published in 1897, kept a record of the alignment before its condition deteriorated further. The standing menhir, as well as the coated blocks, are made of local granite, a material characteristic of the megalithic constructions of the region.
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