A destructive plate boundary (usually a subduction zone).
magma
continental-continental collision I think. When I got down to the last one, that was the only answer left.
You are describing a subduction zone, where one tectonic plate moves beneath another due to convergence, resulting in the destruction of the older crust through melting and recycling in the Earth's mantle. This process often leads to the formation of volcanoes and deep ocean trenches.
Convergent boundary...it's on my homework
convergent boundary
Crust is destroyed at the convergent plate boundaries in Earth. In between the oceanic and continental plates, the subduction of the denser oceanic crust takes place.
Niether. At a transform boundary, plates slide past each other, and crust is conserved.
A crust is not destroyed at a divergent boundary, where tectonic plates move away from each other. This movement creates new crust as magma rises to the surface and solidifies.
When tectonic plates converge, they can form features such as mountain ranges, deep-sea trenches, volcanic arcs, and earthquakes. The collision and subduction of plates at convergent boundaries can also lead to the formation of island arcs and continental crust deformation.
When two continental plates converge, a major landform created is a mountain range. The intense pressure and collision between the plates causes the Earth's crust to uplift, forming large mountain ranges such as the Himalayas or the Alps.
When two tectonic plates converge, a subduction zone can form where one plate is pushed beneath the other, creating deep oceanic trenches and volcanic arcs. Another possibility is a collision boundary, where the two plates collide and form mountain ranges due to intense pressure and folding of the Earth's crust.
When two continental plates converge, they can create mountain ranges due to the intense pressure and collision between the plates. This process, known as continental collision, leads to the folding and uplift of the Earth's crust. Examples of mountain ranges formed by this process include the Himalayas, which were created by the collision of the Indian and Eurasian plates. Additionally, seismic activity is common in these regions due to the stress and strain on the crust.