an earthquake
an earthquake
When divergent boundary plates move apart, magma rises from the mantle to fill the gap, creating new oceanic crust. As the crust cools and solidifies, it forms a series of underwater mountain ranges known as mid-ocean ridges.
A long, linear crack that forms as two tectonic plates move apart is called a mid-ocean ridge. This type of boundary is where new oceanic crust is created as molten rock rises up from the mantle and solidifies along the spreading center. Over time, as the plates continue to move apart, the new crust forms a continuous ridge on the ocean floor.
forms when two {crustal} lithosphere plates move apart.
It forms a hole but new crust is formed.
Plates move apart on divergent plate boundaries.
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.
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.
You are a mid-ocean ridge that forms when tectonic plates move apart and new oceanic crust is created through volcanic activity. This process is known as seafloor spreading, and it results in the formation of new oceanic crust at the mid-ocean ridge.
When two plates move apart from each other, it creates a divergent boundary. Magma from the mantle rises to fill the gap, solidifies, and forms new crust. This process is called seafloor spreading and is responsible for the formation of mid-ocean ridges.
A mid-ocean ridge forms as tectonic plates move apart, creating a gap where magma rises from the mantle to form new crust. This process is known as seafloor spreading and results in the continuous growth of the ocean floor.
The long crack that forms as two tectonic plates move apart is called a rift. It is typically seen in divergent plate boundaries, where the plates separate and magma from the mantle can rise to create new crust. Over time, as the plates continue to move apart, the rift can widen and eventually lead to the formation of a new ocean basin.