A high correlation is noted between paleoclimates and facies of fluviatile deposits: fine texture deposits reveal temperate, or fresh temperate biostasical phases: coarse texture deposits reveal cold rhexistasical phases. The phases of vertical
the detritic deposits of A. Efthemia and the oldest breccia on the southern talus of the Parnassus cannot be considered as one and the same thing: the former one is older than the latter. Both Mindelian and Wurmian talus fans are related to rhexistasic crisis