The programme explains how rainwater circulates in the limestone massifs and why these massifs are most often deserts.
The water cycle in our area is put in context with comments made during
the tour of the cave, which allows visitors to move around in a karstic
system without getting their feet wet.
Visitors will observe the effects of water erosion, transport and deposit.
The tour of the galleries reveals the tracks left by the water that for
several million years has built up the Clamouse underground system.
We “read” the cave the way we read the two landscapes outside, to
expand students’ vision and get them to ask questions, to provide
interpretative tools that they can reinvest later.
