description Cirque de Baume Overview
Cirque de Baume is a limestone cirque in the Jura Mountains of eastern France. It is described as a steephead valley, a landform in which a valley begins abruptly at a steep enclosed head rather than through a broad glacial basin. The site is known for its prominent rock walls and scenic relief, and it is considered one of the larger examples of this type of formation in the regional Jura landscape. It is of interest to visitors and students of karst and non-glacial geomorphology.
help Cirque de Baume FAQ
Where is Cirque de Baume located?
Cirque de Baume is in the Jura Mountains of eastern France. It is a limestone landform with prominent rock walls and an enclosed valley head.
What type of landform is Cirque de Baume?
It is a cirque described as a steephead valley. The valley begins abruptly at a steep, enclosed head rather than opening through a broad glacial basin.
Is Cirque de Baume a glacial cirque?
The site is described specifically as a steephead valley, so it should not automatically be treated as a classic bowl-shaped glacial cirque. Its limestone geology and abrupt enclosed head are the key features.
What geological features can visitors see at Cirque de Baume?
The most noticeable features are steep limestone walls and the sudden enclosed head of the valley. These give Cirque de Baume a strongly enclosed, rocky landscape in the Jura.
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