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Earth Science-plates and earthquake
Q1M3W3- EarthSci
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When an oceanic crust converges with a
continental crust, a crack between the crusts underwater, called
trench
, is formed.
Subduction
is the process
by which a plate dives under a less dense plate.
It turns into a hot molten
material which we call
magma.
The column of rising magma is called
a
mantle plume.
a group of volcanoes, called
volcanic arc
This is what we call
tsunamis
, a Japanese term for harbor wave.
This series of volcanoes is called
volcanic island arc
since it is surrounded by water.
Converging continental crusts or
plates result in a
collision zone
, which
could cause shallow earthquakes.
A vertical space that may extend deep down into the lowest
layer of the crust is created, it is a
rift valley.
The force of separation creates a
tension zone.
These materials pile up near the tension zone
forming mountain-like structures called
oceanic ridges.
The filled-up space between the plates becomes a
new seafloor. This process is known as
seafloor spreading.