body waves
The process of one tectonic plate moving beneath another is called subduction. This usually occurs at convergent plate boundaries where one plate is forced beneath the other due to differences in density. Subduction zones can lead to the formation of deep ocean trenches and volcanic arcs.
When a moving plate collides and is pushed under another plate it is known as a subduction zone. Subduction zones are located at convergent bounties. The plate that is pushed beneath the other plate is then consumed in the asthenosphere.
Subduction. This process occurs at convergent plate boundaries where one lithospheric plate is forced beneath another due to differences in density, causing earthquakes and volcanic activity.
Subduction is a convergent boundary where one tectonic plate moves beneath another plate into the Earth's mantle. This process occurs at plate boundaries where two plates are moving towards each other.
The process of one tectonic plate diving beneath another is called subduction. This often occurs at convergent plate boundaries where one plate is forced beneath the other due to differences in density.
The area where one tectonic plate slides beneath another is called a "subduction zone." This process occurs at convergent plate boundaries, where the denser oceanic plate typically subducts beneath a lighter continental plate or another oceanic plate. Subduction zones are often associated with deep ocean trenches, volcanic activity, and earthquakes.
This process is known as subduction and it typically occurs at convergent plate boundaries where one tectonic plate is forced beneath another due to differences in density. Subduction zones are characterized by deep oceanic trenches and volcanic arcs on the overriding plate.
When one tectonic plate is pushed beneath another plate, it is called subduction. This process occurs at convergent plate boundaries where one plate is denser than the other, causing it to sink into the mantle. Subduction zones are associated with deep ocean trenches and can lead to volcanic activity and earthquakes.
Subduction zones occur at plate boundaries where one oceanic plate descends beneath another. This process leads to the formation of deep oceanic trenches, volcanic arcs, and earthquakes due to the intense pressure and heat generated by the subduction of the oceanic plate.
The process is called subduction. It occurs when one tectonic plate is forced beneath another due to differences in density, typically in convergent plate boundaries. This subduction process is a key driver of plate tectonics.
Subduction.This specific process occurs at a destructive plate margin.The oceanic plate subducts at around 25-45 degrees into the mantle and the friction produced between the two plates triggers earthquakes.
subduction, which is when one tectonic plate is pushed down beneath another tectonic plate.