Tectonic plates that are convergent are "crashing into" each other at this collision boundary, and a subduction zone there is possible. One of the plates will "dive under" the other one. This creates uplift, "hot spots" or volcanic "risers" and instability along the boundary. The west coast of the United States is a good example. A link is provided below.
Convergent boundary
The plate tectonic process where one plate moves under another is called subduction. This process occurs at convergent plate boundaries, where the denser oceanic plate typically sinks beneath the less dense continental plate. Subduction zones are associated with deep oceanic trenches and volcanic arcs.
This process is called subduction. It occurs when one tectonic plate moves beneath another plate at a convergent boundary. Subduction zones are associated with deep ocean trenches and volcanic activity.
When tectonic plates push into each other, the boundary where they meet is called a convergent boundary. At convergent boundaries, one plate is forced beneath the other in a process known as subduction, leading to the formation of mountain ranges, earthquakes, and volcanic activity.
When tectonic plates converge, they can form various geological features such as mountain ranges, deep ocean trenches, and volcanoes. This convergent boundary can result in one plate being pushed beneath the other in a process known as subduction.
The type of boundary where one tectonic plate slides under another is called a convergent boundary. This process is known as subduction, where one plate is forced beneath the other due to differences in density.
Convergent boundary
The plate tectonic process where one plate moves under another is called subduction. This process occurs at convergent plate boundaries, where the denser oceanic plate typically sinks beneath the less dense continental plate. Subduction zones are associated with deep oceanic trenches and volcanic arcs.
This process is called subduction. It occurs when one tectonic plate moves beneath another plate at a convergent boundary. Subduction zones are associated with deep ocean trenches and volcanic activity.
Subduction is the process when one tectonic plate moves beneath another plate at a convergent boundary. This movement can lead to the recycling of old oceanic crust back into the mantle.
When tectonic plates push into each other, the boundary where they meet is called a convergent boundary. At convergent boundaries, one plate is forced beneath the other in a process known as subduction, leading to the formation of mountain ranges, earthquakes, and volcanic activity.
When tectonic plates converge, they can form various geological features such as mountain ranges, deep ocean trenches, and volcanoes. This convergent boundary can result in one plate being pushed beneath the other in a process known as subduction.
A region where a plate descends is called a subduction zone. In this type of plate boundary, one tectonic plate is forced beneath another due to differences in density. Subduction zones are commonly associated with volcanic activity and earthquakes.
A convergent boundary is formed when one tectonic plate pushes underneath another. This process is known as subduction, and it can lead to the formation of mountain ranges, deep ocean trenches, and volcanic arcs.
When two tectonic plates collide, it is called a convergent boundary. This collision can result in the plates pushing against each other, causing one plate to be forced beneath the other in a process known as subduction.
The region is called a subduction zone. It occurs at convergent plate boundaries where one tectonic plate is forced below another due to differences in density. This subduction process can lead to volcanic activity and earthquakes.
subduction boundary!!!