Deep in a cleft in the steep, rocky hillside topped by the Eglise Saint-Pierre lies the Fosse Dione, a large karst spring. “Karst Spring” is a term for a spring that represents the end of a large underground river system, typically with a very large discharge. In the case of the Fosse Dione, this spring has an immense capacity, and is deep enough at its mouth (initially 32 meters) that cave divers have dived the cave.
Ironically, much of the local information focuses on the wash house (or laverie) built around it in 1758. Little is made of the spring itself, which is believed to be the reason that this area has been occupied as far back as it has. The presence of this abundant source of pure flowing water certainly explains the choice of the area as an administrative center, the Oppidum of Tomodurum, by the Romans, and explains signs of occupationwell back into the Bronze Age.
The water flows up out of the spring, over a lip in the surrounding wall, and down through a narrow, steep natural course between houses and out to the Armencon. Houses cling to the hillside above it, and a narrow street enters on one side of the cleft, loops over the spring, and back out the other side.
The flow from the spring varies, and was quite low when I visited, reflecting the drought at the time. Still, as you view the pictures, try to imagine the situation one spring in January 1910, when the water flow was so great that the water level in the cleft was two feet above the level of the spring retaining wall!!
In addition to being a natural and historical marvel, it also reflects some of the historical understatement I found from time to time after this, and which I encountered again when I reached Montbard.