You may be referring to graben structures. These are fault bounded blocks of the lithosphere that subside in regions of divergence.
transform and divergent
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 Earth’s crust. Rift valleys are often associated with volcanic activity and can eventually develop into new ocean basins.
Volcanoes at divergent plate boundaries often occur along mid-ocean ridges, where tectonic plates are moving apart. As the plates separate, magma rises to the surface, creating underwater volcanic activity. These volcanic eruptions contribute to the formation of new oceanic crust.
Rift valleys are typically seen on divergent plate boundaries, where tectonic plates are moving apart. Ocean ridges are also commonly found at divergent plate boundaries, where new oceanic crust is formed through volcanic activity along the mid-ocean ridges.
Divergent boundaries are found primarily along mid-ocean ridges, where tectonic plates are moving away from each other. Additionally, divergent boundaries can also occur on continents, leading to the formation of rift valleys.
along divergent boundaries tectonic plates move apart & rifts are created
Earthquakes can, and do, occur at divergent, convergent, and transform plate boundaries.
yes
convergent boundaries, divergent boundaries, transform boundaries and plate boundaries
convergent boundaries, divergent boundaries, transform boundaries and plate boundaries
convergent boundaries, divergent boundaries, transform boundaries and plate boundaries
convergent boundaries, divergent boundaries, transform boundaries and plate boundaries
transform and divergent
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 Earth’s crust. Rift valleys are often associated with volcanic activity and can eventually develop into new ocean basins.
Divergent boundaries are tectonic plate boundaries where two plates move away from each other. This movement results in the upwelling of magma from the mantle, creating new crust. Divergent boundaries are typically found along mid-ocean ridges.
oceanic ridges
Transform, Divergent, and Convergent