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All of the following can be found at convergent plate boundaries except
a hot spot
hot magma rising, cooling and then sinking
convection currents
Oceanic crust is more dense
sea floor spreading
divergent plate boundaries
subduction zones
diverging
When a continental plate collides with an oceanic plate, the oceanic plate dives beneath the continental plate. Why?
a hot spot
hot magma rising, cooling and then sinking
convection currents
Oceanic crust is more dense
sea floor spreading
divergent plate boundaries
subduction zones
diverging
What is responsible for tectonic plate movement?
a hot spot
hot magma rising, cooling and then sinking
convection currents
Oceanic crust is more dense
sea floor spreading
divergent plate boundaries
subduction zones
diverging
All of the following can be found at divergent plate boundaries except
a hot spot
hot magma rising, cooling and then sinking
convection currents
Oceanic crust is more dense
sea floor spreading
divergent plate boundaries
subduction zones
diverging
Mid-ocean ridges (rifts) normally form where tectonic plates are
a hot spot
hot magma rising, cooling and then sinking
convection currents
Oceanic crust is more dense
sea floor spreading
divergent plate boundaries
subduction zones
diverging
New sea floor is created at
a hot spot
hot magma rising, cooling and then sinking
convection currents
Oceanic crust is more dense
sea floor spreading
divergent plate boundaries
subduction zones
diverging
The Hawaiian Islands were created by
a hot spot
hot magma rising, cooling and then sinking
convection currents
Oceanic crust is more dense
sea floor spreading
divergent plate boundaries
subduction zones
diverging
Movement of convection currents in the mantle can be described as
a hot spot
hot magma rising, cooling and then sinking
convection currents
Oceanic crust is more dense
sea floor spreading
divergent plate boundaries
subduction zones
diverging
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