.
Viscosity of magma
Outside temperature
Dissolved gases
It has a low viscosity
It explodes violently
It explodes quietly
It occurs at rifts, and oceanic hot spots such as Hawaii
It has an intermediate viscosity
It has a high viscosity
It sometimes explodes violently
It is located at subduction boundaries
It has a high viscosity
It is very explosive
It is located at continental hot spots such as Iceland
It is produced by shield volcanoes
Material expelled from a volcano during an eruption
The same thing as magma
It gets thrown into the atmosphere and can be blown many miles away.
Can change the global climate
They are microscopic
It can be felt globally.
They are similar to pebbles
They can be 2 - 64 mm. size
They can change global climate
They can be larger than 64 mm in length
Car sized ones can be thrown 1 km, while smaller ones can be thrown 1-5 km away.
Lava bombs have magma inside which explode when they hit the ground
True
False
True
False
True
False
Earthquakes
Tornadoes
Gas emissions
Deformation
Composite volcanoes, andesitic lava, high viscosity, low temperatures, high gas content
Pyroclastic flows, ash plunes, lahars
Occurs at convergent boundaries (o-o, o-c) and at subduction zones
Occur at divergent boundaries
Shield volcanoes, mafic lava, low viscosity, high temperatures
Lava flows, lava fountains, lava pools
Occurs at divergent boundaries and oceanic hot spots
Pyroclastic flows and lahars
Steep sides, usually explosive, pyroclastic materials and lava flows
Ex. Cascade Mountains
Basaltic Lava
Alternating layers of andesitic lava and tephra
Cylindrical shape
Gently sloping sides, ONLY lava flows, quiet eruptions, mafic lava
Hawaii
Steep/gentle sloping sides
Pyroclastic materials and sometimes explosive
Ex. Sunset Crater, AZ
Andesitic and mafic lava and tephra - cinders and lapilli
True
False
Divergent boundaries
Convergent boundaries
Oceanic hotspots
Convergent boundaries (o-o, o-c)
Rifting
Subduction zones
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