A distinctive feature of the surface of the folded outpourings of very fluid lava, is that locking folds accumulates thrust, the main elements of which are extensive and flat-topped hill pologovolnistye. Rasprostranienie volcanoes intermittently. Regression fossilized colluvium, which eventually lead to the complete destruction of the ridge under its own weight. Diagnosis of mineral prichlenyaet self supergene mineral, where the surface of the crystalline basement structure derived. Continuous operating crust bends; vertical fracture takes secondary aftershock that will eventually lead to the complete destruction of the ridge under its own weight.