Subduction zone.
a subduction zone forms
When two plates move towards each other, it is called convergence. The motion during convergence is usually called subduction if one plate is forced beneath the other, or collision if the two plates collide and form mountain ranges.
A convergent boundary is where two tectonic plates move towards each other. The denser plate is typically forced beneath the less dense plate in a process called subduction. This can lead to the formation of mountain ranges, volcanic arcs, and deep ocean trenches.
Convergent boundaries occur where tectonic plates collide or move towards each other. This collision can result in the plates being forced upwards to create mountains or one plate being forced beneath the other in a process called subduction. Earthquakes and volcanic activity are common at convergent boundaries.
Subduction occurs where the oceanic crust bends down towards the mantle at a subduction zone, typically at convergent plate boundaries where two tectonic plates collide. The denser oceanic plate is forced beneath the less dense continental plate, creating a deep trench and volcanic activity. This process contributes to the recycling of Earth's crust and the formation of mountain ranges and volcanic arcs.
At a convergent plate boundary, two tectonic plates are moving towards each other. As the plates collide, one plate is forced beneath the other in a process called subduction. This can lead to the formation of deep ocean trenches, volcanic arcs, and earthquakes.
they collide and create earthquake
fault line
Because it's heading towards us.
a subduction zone forms
One of the way is they move towards each other and converge,or collide
When tectonic plates are pushing towards each other and forming mountains, it is called a convergent boundary. This process usually involves one plate sliding beneath the other, creating intense pressure and leading to the uplift of large landforms like mountain ranges. An example of this is the Himalayas, which were formed by the collision of the Indian and Eurasian plates.
A convergent plate boundary is where two plates move towards each other. This can result in one plate being forced beneath the other in a process called subduction, or the plates can collide and create mountain ranges.
When two plates move towards each other, it is called convergence. The motion during convergence is usually called subduction if one plate is forced beneath the other, or collision if the two plates collide and form mountain ranges.
It seems that the Milky Way and the Andromeda Galaxy will collide, in about 3-4 billion years.
When two continental plates collide, the crust is forced to thicken, creating mountain ranges such as the Himalayas. When a continental plate and an oceanic plate collide, the oceanic plate will subduct beneath the continental plate as it is denser. This will form a subduction zone. In this process, orogenic belts (mountain ranges) are formed near or along the coastline. They can also create deep ocean trenches offshore, and sometimes forming volcanoes as molten material created from the subduction of cold wet crust rises to the surface. An example would be the volcanoes at the Pacific Ring of Fire. When two oceanic plates collide, the denser oceanic plate will subduct beneath the lighter one, forming a subduction zone as well. They can also form (volcanic) island arcs such as the Solomon islands.
In a convergent boundary, tectonic plates move towards each other. As they collide, one plate is forced beneath the other in a process called subduction. This movement can create volcanic arcs, deep ocean trenches, and mountain ranges.