What are the 3 types of volcanoes?
Individual volcanoes vary in the volcanic materials they produce, and this affects the size, shape, and structure of the volcano. There are three types of volcanoes: cinder cones (also called spatter cones), composite volcanoes (also called stratovolcanoes), and shield volcanoes.
How many types volcanoes are there?
Strictly speaking there are two broad types of volcano, a stratovolcano and a shield volcano, although there are lots of different volcanic features that can form from erupted magma (such as cinder cones or lava domes) as well processes that shape volcanoes.
What are some examples of the 4 types of volcanoes?
What are the Different Types of Volcanoes? Cinder Cone Volcanoes: These are the simplest type of volcano. Composite Volcanoes: Composite volcanoes, or stratovolcanoes make up some of the world’s most memorable mountains: Mount Rainier, Mount Fuji, and Mount Cotopaxi, for example. Shield Volcanoes: These are large, broad volcanoes that look like shields from above – hence the name.
What are the 4 volcano hazards?
4.4 Volcanic Hazards. There are two classes of volcanic hazards, direct and indirect. Direct hazards are forces that directly kill or injure people, or destroy property or wildlife habitat. Indirect hazards are volcanism-induced environmental changes that lead to distress, famine, or habitat destruction.
What are 4 landforms types created by volcanoes?
Volcanic landforms include: Caldera – Cauldron-like volcanic feature formed by the emptying of a magma chamber Cinder cone – A steep conical hill of loose pyroclastic fragments around a volcanic vent Complex volcano – A landform of more than one related volcanic centre Cryptodome – Roughly circular protrusion from slowly extruded viscous volcanic lava
What are the names of different types of volcanoes?
The different types of volcanoes are: composite (or stratovolcanoes), shield, cinder cones and spatter cones. Throughout the world, one can see pictures of the four types of volcanoes, each type indicative of the active underground world we often view as static.