In one way (ice wedging), water gets into cracks in the rock, then freezes. This force can eventually split the rock crystals.
In another (moving ice), a glacier or other large mass of ice moves across the rocks surface. This can scour away loose rock by friction. (It does not require that there be imbedded rocks, but this can also occur, where rocks are pushed together until one breaks.)
Ice-wedging occurs when water seeps into cracks in a rock, freezes, expands, and widens the crack. As the water repeatedly freezes and thaws, the crack will continue to expand due to the pressure exerted by the ice. Over time, this process can cause the rock to break apart into smaller pieces.
When water seeps into a crack in a rock during warm weather and then freezed in cold weather , it expands. And when it expands, it pushes against the sides of the crack forcing it to open wider.
Ice can find its way into cracks and fissures of rock when melted to a liquid state. When it refreezes, it expands, prying the cracks further apart. Moving ice can facilitate the abrasion of existing rock into smaller particles by grinding their surfaces against each other. Moving ice can also pluck rock fragments off of existing rock as it moves.
The mass of ice is typically less dense than rock, so ice typically has a lower mass compared to an equal volume of rock. The exact mass of ice and rock would depend on the volume and density of each material.
The grinding away of rock by rock particles is known as abrasion. This process occurs when particles carried by wind, water, or ice come into contact with the surface of rocks, wearing them down over time.
weather is precipitation rain, hail, snow, ice,e.g. weathering is the wearing away of rock
to melt the ice
by wind,rain,ice,chemical actions,plants,etc.
You have to destroy all the weather changes in the area.
wind because it slowly erodes it.
The roots of certain plants can break or crack into a rock, making the rock more susceptible to frost wedging (ice wedging).
Ice-wedging occurs when water seeps into cracks in a rock, freezes, expands, and widens the crack. As the water repeatedly freezes and thaws, the crack will continue to expand due to the pressure exerted by the ice. Over time, this process can cause the rock to break apart into smaller pieces.
In one way (ice wedging), water gets into cracks in the rock, then freezes. This force can eventually split the rock crystals. In another (moving ice), a glacier or other large mass of ice moves across the rocks surface. This can scour away loose rock by friction. (It does not require that there be imbedded rocks, but this can also occur, where rocks are pushed together until one breaks.)
Weather can be a good example of ice erosion. When the weather gets bad and there is hail, the hail then hits the ground or hits other things that are solid, such as rock walls, or rocky features. When this happens, the hail can sometimes hit as such hard forces to cause a crack, split, break, or hole in these features, thus causing ice erosion.
When water seeps into a crack in a rock during warm weather and then freezed in cold weather , it expands. And when it expands, it pushes against the sides of the crack forcing it to open wider.
When water seeps into a crack in a rock during warm weather and then freezed in cold weather , it expands. And when it expands, it pushes against the sides of the crack forcing it to open wider.
No rock is "weather proof." All forms of rock will eventually be worn away (eroded) by the action of the weather.