GEOLOGY

Detailed explanation-1: -Stratovolcano. Stratovolcanoes have relatively steep sides and are more cone-shaped than shield volcanoes . They are formed from viscous, sticky lava that does not flow easily.

Detailed explanation-2: -Composite volcanoes are also called stratovolcanoes. Some geologists avoid the use of the term “stratovolcano” because these volcanoes typically are not stratified and do not consist of orderly layers of lava flows and pyroclastic deposits.

Detailed explanation-3: -Cinder cones are the most common type of volcano in the world. They may look like an idealized depiction of a volcano as they are steep, conical hills that usually have a prominent crater at the top. Cinders at Capulin Volcano. Cinders are small chunks of scoria.

Detailed explanation-4: -There are three basic cone shapes and six eruption types. The three cone shapes are cinder cones, shield cones, and composite cones or stratovolcanoes.

Detailed explanation-5: -Unlike shield volcanoes, composite volcanoes have a distinctly conical shape, with sides that steepen toward the summit. Cinder cones are the smallest, and almost too small to see next to a volcano like Mauna Loa. Eve Cone is a cinder cone on the flanks of Mt.