The volcano is formed from two volcanic cones. The younger of which may be of Holocene age and is constructed in the middle of a caldera marked by a semilunar shape.: Thanks to heavy erosion, lavas and eruption products are mostly found in peripheral parts of the edifice, while in the central area a deep-grounded crystalline core is exposed.: A breach wide and long with an azimuth of 139° lies in the volcano, whose summit has a maximum slope of 25°. The volcano forms a lineament with Saxani and Isluga.