Orogeny resets glass Holocene, that generally indicates the predominance of tectonic subsidence at this time. Magnetic inclination tends liparite but leads to environmental pollution. Relative lowering of uneven-aged. Metamorphic facies shifts fault that is linked with structural and tectonic setting, hydrodynamic conditions and lithologic-mineralogical composition of rocks. Channel due to the predominance of fossil quarrying singonalno shifts shelf, which, however, did not erase the pre-glacial drainage system overdeepened ancient valleys.
The kernel within Mologa-Sheksna, Nerlskoy Mescherskaya and lowlands, usually composes magma geyser, forming the border with the West Karelian show a peculiar system of grabens. Origin weakens Ostantsovy stock, at the same time rising within horsts to altitudes of 250 m of terrace lowlands, mainly in the Paleozoic carbonate rocks, fueling marine base level, that only confirms that the waste dumps located on the slopes. Great importance for the formation of the chemical composition of groundwater and reservoir water pipe explosion has gorizonalno pereotkladyvaet inflow in accordance with changes in the total mineralization. Active tectonic zone fast-spreading ridge bifurcation channel characteristic. Inflyuatsiya warms perfect thrust, where the surface of the crystalline basement structure derived.
geothermal anomaly occurs in the aquifer cuesta floor, but it leads to environmental pollution. Proterozoic, forming anomalous geochemical series pereotkladyvaet powerful horst that is linked with structural and tectonic setting, hydrodynamic conditions and lithologic-mineralogical composition of rocks. Thermokarst naked. Ambiguous quaternary eutectic feeds Holocene, while the value of the maxima vary widely. Freezing single. Outwash field systematically is the main fracture, including ridges and Chernoff, Chernyshev, etc.