Erosion.
The type of weathering that occurs along ocean cliffs is mainly mechanical weathering, caused by processes such as waves crashing against the rocks, causing them to break apart and erode over time. Chemical weathering can also occur due to the saltwater and other chemical reactions taking place along the cliff face.
A rock falls from a high place due to the force of gravity pulling it downward. This force overcomes the rock's inertia and friction with the surface, causing it to accelerate towards the ground. Factors such as tilt of the surface, weathering, and seismic activity can also contribute to rock falls.
Erosion occurs, causing the cliffs to wear down over time. This process can cause the cliffs to become more unstable and eventually lead to landslides or rockfalls. Over time, the cliffs can change shape or even collapse.
Weathering of rocks occur on the outer surface.
Erosion
You can go to the Interpretive Centre and get information about the Cliffs of Moher. Best of all you can go and have a look at the cliffs. While there, you can enjoy the view and take photographs. It is a very special place.
The main form of weathering in a desert is decomposition.
A cliff can change over time by the process of erosion. This process erodes parts of the cliff away slowly and then, when erosion stops taking place to the cliff, the cliff stops changing.
The breaking down of rocks is weathering. Their movement from one place to another place is erosion.
Its a place where dragonflys normally stay, like in weeds and if there babys then in streams. Its a place where dragonflys normally stay, like in weeds and if there babys then in streams.
Weathering does not necessarily have to take place before erosion. While weathering is the breakdown of rocks into smaller particles, erosion is the process of transporting these particles to a new location. Weathering can occur simultaneously with erosion or even after erosion has started.
Freeze-thaw weathering occurs in regions with temperature fluctuations around the freezing point of water. Water seeps into cracks in rocks, freezes, expands, and pushes the rock apart upon thawing. This cycle of freezing and thawing weakens the rock over time, eventually causing it to break apart.