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Similar calanques can also be found on the French riviera near Estérel and on the island of Corsica (see Calanques de Piana).

The highest point along the calanques are located at Mount Puget (565 meters)and in the mountains of Marseilleveyre (432 meters).

During these periods of interglacial low sea level, additional steep-sided valleys, which were later flooded to create calanques, along the Mediterranean coastline were formed by fluvial and karst processes.

The calanques have a particular ecosystem, as soil is almost non-existent there, and the limestone cliffs instead contain numerous cracks into which the roots of plants are anchored.

For example, the Rhône River cut a canyon as deep as 576 meters into Cretaceous carbonate strata near its confluence with its tributary the Ardèche.

Fluvial erosion by smaller streams and rivers created numerous other deep, steep-sided valleys in response to the greatly lowered sea level at this time.

However, this excessive use has posed problems of potential damage to this delicate microhabitat.

Its walls are covered with paintings and engravings dating back to between 27,000 and 19,000 BC and depict many terrestrial animals such as bison, ibex, and horses as well as sea animals like seals and auks.

Similarities are seen between calanques, and rias, the river mouths formed along the coast of Brittany in Northern France.

The limestone calanques of the Massif des Calanques lie within the recently created Parc National des Calanques (2012) and include the Calanque de Sormiou, the Calanque de Morgiou, the Calanque d'En-Vau, the Calanque de Port-Pin and the Calanque de Sugiton.

There are additional calanques in the parc, further east along the coast, incised into Cap Canaille.

These calanques formed in very different rock strata, often in layers of cemented pebble conglomerate.

Its walls are covered with paintings and engravings dating back to between 27,000 and 19,000 BC and depict many terrestrial animals such as bison, ibex, and horses as well as sea animals like seals and auks.Similarities are seen between calanques, and rias, the river mouths formed along the coast of Brittany in Northern France.The limestone calanques of the Massif des Calanques lie within the recently created Parc National des Calanques (2012) and include the Calanque de Sormiou, the Calanque de Morgiou, the Calanque d'En-Vau, the Calanque de Port-Pin and the Calanque de Sugiton.There are additional calanques in the parc, further east along the coast, incised into Cap Canaille.These calanques formed in very different rock strata, often in layers of cemented pebble conglomerate.These valleys were either incised by rivers or created by cave collapse as karstic dry valleys when sea level was lower than present.