A "mid oceanic ridge"
A "rift valley" or "graben"
A "Constructive Plate Boundary"
An "Ocean"
A. Divergent
The boundary between two tectonic plates moving together is called a convergent boundary. At this type of boundary, one plate may be forced beneath another in a process known as subduction, leading to geological phenomena such as earthquakes and volcanic activity.
tectonic plates. just because they are convergent doesnt change the fact that they are tectonic..
Plate boundaries.
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.
a divergent plate boundary.
A. Divergent
The boundary between two tectonic plates moving together is called a convergent boundary. At this type of boundary, one plate may be forced beneath another in a process known as subduction, leading to geological phenomena such as earthquakes and volcanic activity.
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.
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.
divergent
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.
Tectonic plates come together at convergent boundaries. Some examples include the boundary between the Pacific Plate and the North American Plate along the west coast of the United States, where the plates are converging and creating the Cascade Range of mountains. Another example is the boundary between the Indian Plate and the Eurasian Plate, where the plates are colliding and creating the Himalayas.
Convergent Boundary
Plate boundaries where plates slide past each other horizontally are called transform boundaries. These boundaries are characterized by lateral movement between tectonic plates, often resulting in earthquakes. An example of a transform boundary is the San Andreas Fault in California.
tectonic plates. just because they are convergent doesnt change the fact that they are tectonic..