Abstract

Amplifies an earlier note on the terraces of the Dombes and the Saone, France, giving details of position and altitude of the Pliocene at various points on the Dombes, the relationship between the Quaternary and Pliocene terraces, and terrace features attributable to the relation between subsidence and uplift of the crystalline basement and the advance and retreat of glaciers in the vicinity of Lyons.

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