Pyroclastic (rock & glass fragments) material explosively erupted by a volcano
VolcanicExplosivityIndex (VEI)
Used to describe the explosivity of an eruption, taking into account observable & measurable parameters such as the amount of tephra ejected and eruption cloudheight
DenseRockEquivalent (DRE)
Characterizes the size of an eruption by taking into account the amount of erupted magma, both effusively and explosively, from volume estimates of erupted products (lava and/or tephra)
Eruption types
Magmatic
Phreatic
Phreatomagmatic
Magmatic eruption
Eruption driven by the overpressure created by volcanic gases exsolving from magma
Phreatic eruption
Eruption caused when surface/near-surfacewater is heated by magma, hot rocks, or hot volcanic deposits, resulting in suddenincrease in pressure driving the eruption of watervapor, tephra, but no lava
Phreatomagmatic eruption
Explosive eruption generated by the interaction of magma with abundant surfacewater, resulting in the eruption of watervapor, pyroclasts (from magma and/or surrounding rocks) as well as lava
Lava
Lavaflows
Lavafountains
Lava types
Pahoehoe
A'a
Pillow
A volcano is a vent, hill or mountain from which molten or hotrocks with gaseous material have been ejected, and can also be craters, depressions, hills or mountains formed by removal of pre-existing material or by accumulation of ejected materials