Hudrogeology

Pazynych V. The local untypical alluvium on the Dnipro left bank in the Kaniv-town area.  The article contains examples when the fragmental debris are bedding in the alluvium sands on the left Dnipro-river bank. High altitude for this debris and locations on the surface are appointing on the superflood. The fossils C14 dating show this event had took place near 10800±120 BP. We assuming that superflood reason were the water escape from temporary lake with dimensions close to dimensions of the modern artificial water storage.  The fragmental debris was withdrawn from right steep bank.

It seemed, in 2010 the version of Polissja lake origin was pioneer in the study of the earth's surface reconstruction by vortexes. But in fact the priority belongs C. Wythe Cooke. On the possibility of participating of vortices in the formation Carolina Bays wrote on 1940 in paper “Elliptical bays in South Carolina and the shape of eddies” [Jour. Geology, v. 48, no. 2, p. 205-211].  Full version “Carolina Bays and the Shapes of Eddies” was realized in 1954 [Geological survey professional paper 254-I]. A wider analysis of these publications will be made in the paper dedicated Carolina Base.

When starting a new article about tsunami, it is necessary to once again remember the unexpected response to the first publication. And this must be done for two reasons. Firstly, to provide answers, and secondly, to explain the new approaches that have formed on the basis of the analyzed results. In this case, it is necessary to recall only the first part of the review: "Everything is logical - only where is the source (cause) of the giant tsunami in the Atlantic?