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.
A divergent boundary is the boundary between two tectonic plates moving apart. At these boundaries, new crust is formed as magma rises up from the mantle to fill the gap created by the plates moving in opposite directions. This process is responsible for the formation of mid-ocean ridges.
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.
Plates move apart at divergent boundaries, also known as spreading centers. This process is usually associated with the formation of new crust as magma rises from the mantle to fill in the gap created by the moving plates. An example of a divergent boundary is the Mid-Atlantic Ridge.
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.
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.
Because as tectonic plates move away from each other, the ocean floor spreads apart and fills the gap.
A divergent boundary is the boundary between two tectonic plates moving apart. At these boundaries, new crust is formed as magma rises up from the mantle to fill the gap created by the plates moving in opposite directions. This process is responsible for the formation of mid-ocean ridges.
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.
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.
Plates move apart at divergent boundaries, also known as spreading centers. This process is usually associated with the formation of new crust as magma rises from the mantle to fill in the gap created by the moving plates. An example of a divergent boundary is the Mid-Atlantic Ridge.