Either both sides of the plates are thrust upwards to form mountains. Or one side is thrust downwards beneath the other, known as subduction.
The tectonic plate boundaries come together and push up on each other to form mountains.
The plates come together
The plate boundary at which plates collide or come together is called a convergent boundary. At convergent boundaries, one plate is typically forced beneath the other in a process known as subduction. This collision can lead to the formation of mountain ranges, deep ocean trenches, and volcanic activity.
Island arcs are formed from the subduction of one oceanic plate beneath another oceanic plate. As the subducted plate melts, magma rises to the surface, creating a chain of volcanic islands parallel to the subduction zone. This process is associated with tectonic plate boundaries and can lead to the formation of island arcs.
When oceanic plates come together, they create a subduction zone where one plate is forced beneath the other. This process forms deep ocean trenches and can lead to the formation of volcanic arcs and islands.
Converging plates come together. They converge together. Diverging plates come apart.
The techtonic plates come together and one plate will go down where the other will go upwards. this is what makes or causes volcanoes
When two tectonic plates come together, they can form a convergent boundary, leading to features such as mountain ranges, deep ocean trenches, or volcanic arcs. The collision of continental plates often creates mountain ranges like the Himalayas, while the subduction of an oceanic plate beneath a continental plate can result in volcanic activity and oceanic trenches. This process is a fundamental aspect of plate tectonics and significantly shapes the Earth's landscape.
No, subduction is not characteristic of diverging plate boundaries. Subduction occurs at converging plate boundaries where one tectonic plate is forced beneath another plate. Diverging plate boundaries are where tectonic plates move away from each other, such as at mid-ocean ridges.
they have convergent plates boundaries and come together rubbing
When tectonic plates converge together at the bottom of the ocean the oceanic plate goes under the continental plate because the oceanic plate weighs more and then the oceanic plate pushes up the continental plate which forms mountains and sometimes the tectonic plates let magma through which goes up through the continental plate and then opens a hole at the top of the mountains called a vent which is where the steam, volcanic ash, debris and lava come out of.
No, volcanic islands typically form at convergent plate boundaries where an oceanic plate subducts beneath another plate, creating intense heat and pressure that leads to volcanic activity. When the magma reaches the surface, it forms volcanic islands.