До палеогеографи Північного Поділля у палеоліті

Abstract

In territory Northern Podolia the whole is open “a paleolithic province”. All investigated monuments are fixed in loesses -soils series of anthropogenous adjournment. The paleolith Northern Podolia should be considered as the period which occupies a geological interval of time from the beginning of formation Korshev's (Kaidak's) a mineral soil complex up to Dubno's (Vitachiv's) mineral soil and further to Holocene. Means, dynamics of natural processes should be traced within the framework of this chronological piece. On a background of the general cold snap natural processes varied rhythmically. But these rhythms were not regular in time and differed the duration, and also intensity. Alternations of horizons of losses and minerals testify to it soils. Taking into account results of complex researches, it is possible to track the basic changes of an environment of a paleolith Northern Podolia.