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Cinder cones are commonly found on the flanks of shield volcanoes, stratovolcanoes, and calderas. For example, geologists have identified nearly 100 cinder cones on the flanks of Mauna Kea, a shield volcano located on the island of Hawaii.inder cones are made of pyroclastic material. Many cinder cones have a bowl-shaped crater at the summit. During the waning stage of a cinder-cone eruption, the magma has lost most of its gas content. This gas-depleted magma does not fountain but oozes quietly into the crater or beneath the base of the cone as lava.
Sunset crater, AZ is a classic example of a cinder cone (note the well defined crater at the top.) Paricutin volcano (1943-1952) in Mexico (with an AA lava flow consuming the village of San Juan Parangaricutrio) is a classic example of a cinder cone. Mt. Capulin New Mexico, is another classic example of a cinder cone.