Active volcanoes. Has a recent history of eruptions
Dormant volcanoes. Volcanoes that have not erupted for a very long time, but may erupt in the future
Extinct volcanoes. Are not expected to erupt in the future
Viscosity. The ability and the resistence of the magma to flow.
Viscosity depends on the composition of the magma
True
High temperature
Low viscosity
Low temperature
High viscosity
Highsilica
High viscosity
Low silica
Low viscosity
High viscosity. Viscuos, thicker and features slow moving magma
Highest viscosity. Magma does not move at all due to it's viscosity
Lowestviscosity. Thinner and features fast moving magma
Phreatic. A type of eruption, and is a stream-driven eruption that is caused by the interaction between magma and water, features ash columns, and may be an onset on larger eruption
Plinian. Largest and the most violent type of eruption, its eruption can reach up to 50km (stratosphere) and is capable of emptying the magma chamber, and becomes inactive after it's eruption
Hawaiin. Very fluid, and basaltic fluid, and forms rivers from the vent
Vulcanian. Stronger than strombolian but weaker than pulnian, ejects ashes, characterized by tall columns that reaches up to 20km
Strombolian. The smallest type of explosive eruption, occurs when volcanic gasses pressure is excessively high.
Strombolian is characterized by a fountain of lava, and features slow movement of lava
Mt. Vesuvius erupted in 79 AD
Mt. St. Helens erupted in 1980
Mt. Pinatubo erupted in 1991.
Phreatic. This type of eruption is caused when the water above the magma, and lava is heated.
Phreatomagtic. A violent eruption, that features large columns and very fine ash, high speed and side way emission of pyroclastics
Vulcanian characterized by tall eruptions columns that reaches upto 20km high with pyroclastic flow
Primary factors which affects the magmas viscosity:
The magmas temperature
Chemical composition
The amount of dissolved gassesitcontains
A crater is a funnel shaped at the top of the volcano
Caldera is formed when a part of the wall of a volcano collapses