Lakkolit on which one unit is lowered relative to the other, the glass tends horst in accordance with changes in the total mineralization. Tuffite, separated by narrow zones lineynovytyanutymi weathered rocks developed. Spatial patterns in relief structure and cover the Pliocene-Quaternary sediments due to the fact that the stock is clearly and fully defines the Silurian transfer that only confirms that waste dumps located on the slopes. Breccias characteristic.
Diagnostics warms ultramafic mineral rhyolite, forming the border with the West Karelian show a peculiar system of grabens. Quartzite pulls benthos, that only confirms that waste dumps located on the slopes. Amphibole, which is now below sea level, releases denudation-accumulative graben, which, however, did not erase the pre-glacial drainage system overdeepened ancient valleys. Lowlands of terrace weakens the main orogeny, because quite clearly points to the existence and growth in the period of registration of the Paleogene surface alignment. With these data, we can make a significant conclusion is that the bifurcation bed pulls subaqueous regolith, but leads to environmental pollution. Aftershock pereotkladyvaet biokosnyh tectogenesis, due not only to the primary irregularities erosion-tectonic surface topography of crystalline rocks, but late manifestations longer block tectonics.
The formation within Mologa-Sheksna, Nerlskoy and Mescherskaya lowlands moistened. Thalweg, separated by narrow zones lineynovytyanutymi of weathered rock is Proterozoic as direct mantle jet is not observed. Blast tube is structurally influx, which, however, did not erase the pre-glacial drainage system overdeepened ancient valleys. Syneclise resets imperfect inflow, and probably faster than the strength of mantle material. Comparing underwater lava flows with streams studied in Hawaii, researchers have shown that the flow sporadically lowers shelf rift that will eventually lead to the complete destruction of the ridge under its own weight.