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a divergent boundary is where two of earth plates are moving
Sea-floor spreading occurs in places where two tectonic plates are moving away from each other. Magma rises to the surface, creating new crust as the plates separate. This process is a key mechanism driving the movement of Earth's lithosphere.
The Earth's crust is broken up into several lithospheric or tectonic plates. These plates are constantly moving atop the Earth's mantle (semi-solid layer of molten rocks). Based upon their motion, tectonic plates are referred to as converging or diverging. Converging tectonic plates move towards each other and form convergent boundary. Diverging tectonic plates move away from each other and form divergent boundary.
A plate boundary where two plates move away from each other.A plate boundary where two plates move away from each other.
Diverging Plate Boundary
Volcanoes are created mainly at the border of two neighboring plates of earth.
a boundary at which two plates moves past each other horizontally
Diverging plates can create several landforms, most notably mid-ocean ridges, where tectonic plates separate and magma rises to form new oceanic crust. This process can also lead to rift valleys on land, such as the East African Rift, where the land sinks between two diverging plates. Additionally, volcanic activity often occurs along these boundaries, resulting in the formation of new volcanic islands or underwater volcanoes.
The Eyjafjallajökull eruption in 2010 involved the Eurasian and North American tectonic plates in Iceland. The volcano is located along the Mid-Atlantic Ridge, where these two plates are diverging.
No, subduction is not characteristic of diverging plate boundaries. Subduction occurs at converging plate boundaries where one tectonic plate is forced beneath another plate. Diverging plate boundaries are where tectonic plates move away from each other, such as at mid-ocean ridges.
Plates
The mechanism responsible for producing new seafloor between two diverging plates is seafloor spreading. Magma rises from the mantle to fill the gap created by the plates moving apart, solidifies upon contact with seawater, and forms new oceanic crust. This process results in the continuous growth of the ocean floor.