A rift valley is a deep faulted structure found along a divergent boundary. It forms as tectonic plates move away from each other, creating a depression in the Earthβs crust. Rift valleys are often associated with volcanic activity and can eventually develop into new ocean basins.
A deep valley where two tectonic plates move apart is called a rift valley. This occurs due to divergent plate tectonics, where the plates separate and magma rises to create new crust. Examples include the East African Rift Valley and the Mid-Atlantic Ridge.
At a convergent boundary, tectonic plates collide and create mountains, deep ocean trenches, and volcanic activity. On the other hand, at a divergent boundary, tectonic plates move apart and cause the formation of rift valleys, mid-ocean ridges, and volcanic activity as new crust is created.
This tectonic boundary is known as a divergent boundary which will cause the formation of normals faults, leading to horst and graben structures. If the tensile stress is maintained and divergence continues, this will form a rift valley and ultimately due to the thinning of the crust, the creation of a new ocean and mid ocean spreading centre.
A convergent plate boundary forms a deep sea trench. This occurs when two tectonic plates are pushed towards each other, causing one to subduct beneath the other, creating a trench in the ocean floor.
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No, rift valleys form along divergent boundaries, where tectonic plates move away from each other. Convergent boundaries are where plates collide, leading to the formation of features like mountains and deep ocean trenches.