Rifts and trenches are produced by divergent and convergent boundaries, respectively. Divergent boundaries occur when tectonic plates move apart, leading to the formation of rift valleys, such as the East African Rift. In contrast, convergent boundaries happen when plates collide, causing one plate to subduct beneath another, resulting in deep ocean trenches, like the Mariana Trench. Each type of boundary is associated with distinct geological features and processes.
Convergent boundaries
A convergent boundary is formed when plates collide. In this type of boundary, one plate is forced beneath the other in a process called subduction. This collision can result in the formation of mountains, volcanic arcs, and deep-sea trenches.
A subduction zone forms arcs of volcanoes and deep-ocean trenches. In this type of plate boundary, one tectonic plate is forced beneath another, generating intense geologic activity that results in volcanic eruptions and the formation of deep trenches in the ocean floor. This process occurs where two plates converge.
A destructive boundary, also known as a subduction zone, is a type of tectonic plate boundary where one plate is being forced beneath another plate. This process can lead to the formation of deep ocean trenches, volcanic arcs, and earthquakes.
A convergent boundary, where two tectonic plates are moving towards each other, creates deep sea trenches. Here, one plate is forced beneath the other in a process called subduction, leading to the formation of these deep underwater features.
Transform Boundary
convergent plate boundary
Convergent boundaries
It Is an east boundry because it is in the east and the way the water in flowing it depends on the people of Africa
When plates collide it is called a convergent boundary.newtest3
When two tectonic plates are pushed together, it forms a convergent boundary. This boundary leads to the creation of mountain ranges and deep ocean trenches.
A convergent boundary is formed when plates collide. In this type of boundary, one plate is forced beneath the other in a process called subduction. This collision can result in the formation of mountains, volcanic arcs, and deep-sea trenches.
A mid-ocean ridge forms at the divergent plate boundary. This boundary initially forms rifts that later on become rift valleys.
A subduction zone forms arcs of volcanoes and deep-ocean trenches. In this type of plate boundary, one tectonic plate is forced beneath another, generating intense geologic activity that results in volcanic eruptions and the formation of deep trenches in the ocean floor. This process occurs where two plates converge.
convergent
A destructive boundary, also known as a subduction zone, is a type of tectonic plate boundary where one plate is being forced beneath another plate. This process can lead to the formation of deep ocean trenches, volcanic arcs, and earthquakes.
A convergent boundary, where two tectonic plates are moving towards each other, creates deep sea trenches. Here, one plate is forced beneath the other in a process called subduction, leading to the formation of these deep underwater features.