Mid-ocean ridge. A divergent plate boundary.
When two lithospheric plates move apart, a divergent boundary is formed. This process results in the creation of new oceanic crust as magma rises to fill the gap between the plates, forming a mid-ocean ridge.
A mid-ocean ridge is formed when plates diverge or move apart. This is where new crust is created as magma rises to fill the gap created by the separating plates.
Mountains are formed at the boundary where tectonic plates collide or move apart.
At divergent boundaries, mid-ocean ridges are formed as tectonic plates pull apart. At converging boundaries, various geologic features are formed such as trenches, mountains, and volcanic arcs, depending on the type of plates involved (oceanic vs. continental).
When Earth's plates spread apart, it creates a divergent boundary where new oceanic crust is formed as magma rises from the mantle and solidifies. This process leads to the creation of features like mid-ocean ridges and rift valleys.
When two lithospheric plates move apart, a divergent boundary is formed. This process results in the creation of new oceanic crust as magma rises to fill the gap between the plates, forming a mid-ocean ridge.
A mid-ocean ridge is formed when plates diverge or move apart. This is where new crust is created as magma rises to fill the gap created by the separating plates.
It forms a hole but new crust is formed.
Plates move apart on divergent plate boundaries.
Seafloor spreading
Mountains are formed at the boundary where tectonic plates collide or move apart.
When tectonic plates move apart, it creates a divergent boundary. As the plates separate, magma from beneath the Earth's surface can rise up, creating new crust. This process can lead to the formation of volcanic activity and mid-ocean ridges.
Some move away from each other and create massive trenches normally in the sea bed, for example the Mariana Trench - 10,998 m.
The plates dont move.
A rift valley is formed when tectonic plates move apart, creating a gap in the Earth's crust. This process is often associated with divergent boundaries where new crust is formed as magma rises to fill the gap. Rift valleys can be found on land or under the ocean.
At divergent boundaries, mid-ocean ridges are formed as tectonic plates pull apart. At converging boundaries, various geologic features are formed such as trenches, mountains, and volcanic arcs, depending on the type of plates involved (oceanic vs. continental).
At collision, mountains, at separation, long deep holes into the earth.