Individual volcanoes in the Azas Plateau volcanic field include the Derbi-Taiga tuya (), which is formed by several layers of hyaloclastite and lava flows and displays a prominent winged topography. The hyaloclastite layers were formerly considered to be tuffs and reach thicknesses of . Pillow lavas also exist. A system of ancient valleys formed by floods are found near to Derbi-Taiga. Ulug-Arginskii () is a cone that formed exposed in the air. The cone is accompanied by a maar with a lake to the south, and a lava flow from the cone reached in length. Shivit-Taiga with a length of over and a height of is among the biggest volcanoes in the world that formed beneath ice, but Derby-Taiga may be even larger depending on how the size is measured. Shivit-Taiga covers a surface of and is high. This edifice is a stratovolcano and it features two craters with diameters of and . Lava lakes formed in two craters on the volcano. Shivit-Taiga too is accompanied by a topography that indicates that ancient floods passed there. Kokhemskii is and was affected by glacial erosion. Sorug-Chushku-Uzu north of Shivit-Taiga is high.