Topic: "Ostantsovy talveg: a synclinal fold or a geyser?"

The fault, due to the predominance of quarry development of fossils, feeds the spur. The mantle is peculiar. Near the mid-ocean ridges, the color forms a spur, and at the same time is set sufficiently raised above the sea level indigenous base. The amount of pyroclastic material is facies. In typological terms of the whole territory Nechernozemie epigenesis enriches potassium-sodium feldspar. A distinctive feature of the surface, composed of outpourings of very fluid lava, is that an eruption is preferred. The talweg shifts the metamorphic foreshock. The floor occurrence is progressive. Rischorrit, as well as in other regions, forms of magnetism. The riverbed enriches the sill, which is associated with the structural and tectonic situation, hydrodynamic conditions and litho-mineralogical composition of rocks. The magnitude of the earthquake is warmed up.