Divergent Boundary
Geologists call the process of tectonic plates breaking apart "rifting." It occurs when the Earth's lithosphere is being pulled apart, causing the plates to separate, creating new ocean basins. Rifting is a key stage in the formation of new tectonic boundaries.
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.
Mid-Ocean ridges are places where tectonic plates are moving apart from each other. This movement results in the creation of new oceanic crust as magma rises and cools at the ridge.
called tectonic plates. These plates can move in different directions, either colliding, moving apart, or sliding past each other. Their movement is responsible for phenomena such as earthquakes, volcanic activity, and the formation of mountain ranges.
Tectonic plates move because of the heat and pressure from the Earth's core, causing convection currents in the mantle that push the plates apart or pull them together.
Places where tectonic plates separate are known as divergent boundaries. At these boundary locations, magma rises from the mantle, forming new crust as the plates move apart.
I'm guessing you're talking about the tectonic plates? Divergence.
Tectonic plates interact at plate boundariesThey move apart at divergent boundaries
Converging plates come together. They converge together. Diverging plates come apart.
Underwater mountain chains that form where two tectonic plates are pulling apart are called mid ocean ridges. The largest is the Mid Atlantic Ridge.
tectonic movement can cause tectonic plates to collide, drift apart, or slide across one another
Yes. Tectonic plates are extremely strong and catastrophic in some cases.
A rift valley.
Geologists call the process of tectonic plates breaking apart "rifting." It occurs when the Earth's lithosphere is being pulled apart, causing the plates to separate, creating new ocean basins. Rifting is a key stage in the formation of new tectonic boundaries.
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.
The process that pushes tectonic plates apart is called seafloor spreading. Magma rises from the mantle through divergent boundaries, creating new oceanic crust. As the new crust forms, it pushes the existing plates away from each other, causing them to move.
Mid-Ocean ridges are places where tectonic plates are moving apart from each other. This movement results in the creation of new oceanic crust as magma rises and cools at the ridge.