Types of volcanoes
There
are three main types of volcanoes
- Active volcanoes which are currently or have recently erupted.
- Dormant volcanoes which have not erupted recently and is expected to erupt at any time.
- Extinct volcanoes which has stopped to erupt and will never erupt again.
On earth, volcanism occurs in several distinct geologic
settings.
The first place of volcanic activities are those areas
associated with the boundaries of the enormous rigid plates that make up the
lithosphere (the crust and upper mantle). The majority of active terrestrial
volcanoes (roughly 80 percent) and related phenomena occur where two
lithospheric plates converge and one overrides the other, forcing it down into
the mantle to be reabsorbed.
A second major site of active volcanism is along the axis of
the oceanic ridge system, where the plates move apart on both sides of the
ridge and magma wells up from the mantle, creating new ocean floor along the
trailing edges of both plates. All of this volcanic activity occurs underwater.
Iceland is the best example. The magma that are erupted along the oceanic
ridges are basaltic in composition.
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