Tectonic Plate Movement: An Exciting Geological Phenomenon

How do ridge push and slab pull contribute to the movement of tectonic plates?

a) Ridge push involves the downward force of a ridge, while slab pull involves the sinking of a subducting slab.

b) Ridge push and slab pull both involve the sinking of tectonic plates.

c) Ridge push and slab pull are unrelated geological phenomena.

d) Ridge push and slab pull both cause earthquakes.

Ridge push and slab pull: Key Players in Tectonic Plate Movement

Final answer: Ridge push and slab pull are two processes that contribute to the movement of tectonic plates. Ridge push involves magma pushing the lithosphere at a mid-ocean ridge, while slab pull is the sinking of a subducting plate into the mantle. These forces play a role in the formation of geological features like mountains and earthquakes.

Explanation: Ridge push and slab pull are two essential processes in the movement of tectonic plates. Ridge push occurs when magma pushes the lithosphere at a mid-ocean ridge, causing it to move away. On the other hand, slab pull involves the sinking of a dense subducting plate into the mantle, pulling the rest of the plate along with it.

An example of ridge push can be seen in the movement of the Eurasian Plate away from the Mid-Atlantic Ridge. This movement is due to the force created by magma pushing the lithosphere. As for slab pull, a notable example is the subduction of the Pacific Plate beneath the North American Plate, contributing to the formation of geological features like the Cascade Range in the United States.

These two processes, along with other geological forces, work together to shape the Earth's surface and contribute to phenomena such as mountain formation and seismic activity like earthquakes. Understanding the mechanisms behind ridge push and slab pull is crucial for grasping the complex dynamics of tectonic plate movement.

← Reflecting on centripetal acceleration and gravity in a wheel shaped space station Electric force of attraction between pennies →