A divergent boundary is an area where two neighboring tectonic plates move away from one another. It can also be called a divergent plate boundary, constructive boundary or extensional boundary.
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.
Trenches are typically found at the boundaries of tectonic plates, where one plate is being subducted beneath another. The most well-known trenches are oceanic trenches, found underwater near subduction zones where one tectonic plate sinks beneath another.
Another name for a constructive boundary is a divergent boundary. This type of boundary occurs when two tectonic plates move away from each other, leading to the formation of new crust. It is characterized by volcanic activity and the creation of rift valleys.
When two tectonic plates slide past each other horizontally, the boundary between them is called a transform boundary. This type of boundary is characterized by lateral movement along fault lines, such as the San Andreas Fault in California.
subduction boundary!!!
A. Divergent
divergent
a divergent plate boundary.
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.
A "mid oceanic ridge" A "rift valley" or "graben" A "Constructive Plate Boundary" An "Ocean"
Trenches are typically found at the boundaries of tectonic plates, where one plate is being subducted beneath another. The most well-known trenches are oceanic trenches, found underwater near subduction zones where one tectonic plate sinks beneath another.
Convergent Boundary
tectonic plates. just because they are convergent doesnt change the fact that they are tectonic..
Another name for a constructive boundary is a divergent boundary. This type of boundary occurs when two tectonic plates move away from each other, leading to the formation of new crust. It is characterized by volcanic activity and the creation of rift valleys.
Plate boundaries.
When two tectonic plates slide past each other horizontally, the boundary between them is called a transform boundary. This type of boundary is characterized by lateral movement along fault lines, such as the San Andreas Fault in California.
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.