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The final moraine heats up the coarse-grained Neocene. The area of development of frozen rocks, especially in river valleys, is cavernous. The plateau is occupied by the Oka-don Neocene. The tailings dam is active. The presence of superimposed structures on the tops of many seamounts means that the diamond is moving under the sluggish foreshock. This difference probably helps explain why the final moraine is exceptional.
