convergent boundary -rift valley
divergent boundary -mid-ocean ridge
Subduction zone.
A deep ocean trench is likely to form where two oceanic plates push together in a convergent boundary. This is because one of the plates subducts beneath the other, creating a deep trench.
A collision boundary (also known as a continent-continent convergent boundary) would most likely create a non-volcanic mountain range. When two continental plates collide, the crust crumples and folds, leading to the formation of mountain ranges like the Himalayas. This process does not typically involve volcanic activity.
A convergent plate collision involving two continental plates is most likely to result in the formation of the most extensive mountain range. This is because the thick and buoyant continental crust resists subduction, leading to intense compression, uplift, and folding that can create large mountain chains like the Himalayas.
A convergent plate boundary would likely form a mountain chain of sedimentary rock. As tectonic plates collide, one plate may be forced beneath the other, leading to the uplift of sedimentary layers and their subsequent compression and deformation, forming mountain ranges.
At a convergent boundary.
Sea floor bassalt and sediments.
Subduction zone.
Where an oceanic plate dives under a continental plate (e.g. just offshore the Washington/Oregon coast, creating a line of explosive volcanos just inland).
At a convergent boundary.
The most likely cause of a volcano is a convergent plate boundary, where one tectonic plate is forced beneath another in the process of subduction. This movement melts rock and generates magma, which can rise to the surface and erupt as a volcano.
Any type of plate boundary can cause an earthquake. That said, areas along convergent, divergent, and transform tectonic plate boundaries are the most likely places for earthquakes to occur.
The effect of subduction at the boundary of two plates is the movement of one tectonic plate under another tectonic plate. This creates a subduction zone, which often occurs in convergent boundaries.
Most likely Because of either a convergent boundary or a transform boundary that caused this.
Mountains are most likely to form at a convergent boundary where two tectonic plates collide, with one plate being forced beneath the other in a process called subduction. The intense pressure and heat generated during this collision cause the crust to deform and uplift, leading to the formation of mountain ranges.
A deep ocean trench is likely to form where two oceanic plates push together in a convergent boundary. This is because one of the plates subducts beneath the other, creating a deep trench.
convergent!