The pulling force that causes tectonic plates to move apart, leading to the formation of new lithosphere, is called "tensional force." This force occurs at divergent boundaries, where plates are pushed apart due to mantle convection and the upwelling of magma. As the plates separate, magma rises to fill the gap, solidifying to create new crust.
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.
Convergent: plates move into one another.Divergent: plates move apart.Transform: plates move sideways in relation to each other.
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.
An enormous gap that forms as new ocean crust cools and moves apart is called a mid-ocean ridge. This is a mountain range on the ocean floor where new oceanic crust is created as tectonic plates move away from each other.
Magma wells up as the plates move apart and fill some of the gap.
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.
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.
The pulling force that causes tectonic plates to move apart, leading to the formation of new lithosphere, is called "tensional force." This force occurs at divergent boundaries, where plates are pushed apart due to mantle convection and the upwelling of magma. As the plates separate, magma rises to fill the gap, solidifying to create new crust.
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 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.
Convergent: plates move into one another.Divergent: plates move apart.Transform: plates move sideways in relation to each other.
Because as tectonic plates move away from each other, the ocean floor spreads apart and fills the gap.
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.
They are found at a plate boundary. When two plates move apart (divergent) magma rises through the gap.
An enormous gap that forms as new ocean crust cools and moves apart is called a mid-ocean ridge. This is a mountain range on the ocean floor where new oceanic crust is created as tectonic plates move away from each other.
They are found at a plate boundary. When two plates move apart (divergent) magma rises through the gap.