Continental soil-sedimentological lithostratigraphical records from the Eastern Mediterranean and the Southern North Sea prove to be comparable and reveal long term periodicities which allow subdivision of the Pleistocene into four Maxi Cycles
. Profiles of the ocean floor and the structure of sedimentary mantle at the successive moments of geological time are obtained by means of mathematical modelling. The role of progressive motions proved to be leading in the evolution of the largest forms
coastal processes and acts within a certain time interval. With reference to longshore sediment transport estimation in different parts of the World Ocean, strong storms (with frequence about once per year) have been proved to be factor controlling coasts
of continents are distributed accordingly to the normal law. The distribution however is proved to be normal only in the area of highest elevations, white as most part of continents (about 96 % of the area) the elevations distribution corresponds to the inverse
Detailed measurements of the altitudes of the shorelines of former ice-dammed lakes in Glen Roy and vicinity in the Scottish Highlands prove erroneous the conventional view that former shorelines in areas affected by glacio-isostatic uplift
-karst depressions prove interaction between glacial quarrying, absorption and dissolution. Caves are characterized by a vadose outflow and a rapid draining. Greatest karst landforms date probably from Ancient Quaternary while minor solutions forms
During 1973 and 1974 an analysis has been made of a 30km transect between Beernem and Tielt (Belgium, Prov. West-Flanders). This transect covers the transition from the podzols in the north to the agricultural landscape on more loamy soils
rock by solide state flowing is contrasted by a deformation of the regional overburden resulting from fracturing tectonics. As model conceptions prove, both the alpine structure of salt body and the germanotype mosaic of fault blocks of the overburden
and age per group of tree species and damage zone. A similar significant relation was established between the current annual increment and the age per group of tree species and the damage zone. Finally, a statistically-proved dependence is shown between
Mudflows' impact on the mountain rivers channel processes is discussed, the processes' features proved to be different within the zones of mudflows formation, transit and deposition| the channel morphology depends on the form of the mudflow deposits
. In making conclusions the microrelief density (Mrd) values, as determined from the interrelations between the microrelief and corresponding relative heights, proved to be of practical use.
Recent research on the temporal and spatial course of the late Holocene, relative displacements of land and sea in the coastal area of the Southwestern Baltic Sea have proved that in this period the sea level has clearly risen in phases to its