The cinder cones are formed due to the strombolian eruption. The cone-building process is mainly one of ballistic deposition and slumping with some of the fine-grained airfall carried away by wind (McGetchin et al., 1974). The cinder cones are primarily constructed by moderately explosive eruptions, pristine cone morphometry depending principally upon explosive eruptions that are based on pyroclastic size, distribution, ejection velocity, and ejection angle (Settle, 1979).