Village of Sceautres
At the foot of the Coiron can be seen a basalt "neck" (mass of volcanic rock), which is surely one of the largest in Europe. In the village remains of its medieval age can be seen on its fortified gate.
At the foot of the Coiron can be seen a basalt "neck" (mass of volcanic rock), which is surely one of the largest in Europe. In the village remains of its medieval age can be seen on its fortified gate.
The first church in Lussas dedicated to Notre Dame was founded in 537, it is one of the 2nd churches that were constructed during the 12th century but destroyed during the 19th century. Therefore, the current church was built not long after that.
From the national roadway 102, the village can be seen with its elegant bell tower, tiled rooftops and the beautiful silhouette of its convent. There are traces of Neolithic life, noting the ancient presence of man in Lavilledieu.
The ruins of the old castle and donjon or tower.
Oppidum de Jastres-Nord is a Gallic oppidum of the barred spur type, overlooking the River Ardèche. On the accessible side, it is defended by a monumental wall showing three stages of construction.
The church of St. Etienne located at the end of the village was constructed during the latter part of the 12th century and may have been built on an earlier structure which has been referred to in writings as of 950AD.
Neolithic dolmen of Mias. Ardèche is one of the departments with the most dolmens. This Breton name means "stone table", they are funerary monuments. They appear in 2500 years before J-C, end of the Neolithic and in the Bronze Age.
Desire when the village was elevated in 1284, the church, dedicated at Saint-Louis benefactor of Vivarais area, was inaugurated in 1297. During his long existence, the church has suffered a lot of reorganizations, the latest in 1995.
This village was fortified at the Middle Ages during the 100 years war and some of its ramparts are still standing today. It is situated on the road leading to Alba at the border of where the black basalt columns and white limestone rock are found.
The church were once part of its fortification which have been referred to as early as 1137. The facade of the actual building has gone through a number of modifications but still has two remaining small towers surrounding it.