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.)
Rocks on mountain tops are exposed to harsher weather conditions, such as wind, rain, and ice, which can break down the rocks more quickly through processes like frost wedging and erosion. Additionally, mountain rocks may experience larger temperature variations, leading to thermal stress that can contribute to faster weathering.
Rocks are typically exposed to more wind, rain, and ice in mountainous regions and coastal areas where there are strong weather patterns and erosion processes at play. These environments experience higher levels of weathering and erosion due to the constant exposure to these elements.
Without an atmosphere or weather, a planet would not have sedimentary rocks. Sedimentary rocks form from the accumulation and compression of sediments by water, wind, or ice - processes that require an active atmosphere and weather system to transport the sediments.
fine grained rock will weaher faster thatn the course grained rock
The science that studies rocks is geology, while the study of weather is meteorology. These two fields often overlap in studying how rocks and weather interact with each other in the Earth's systems.
Ice with rocks in it.
When water in the ground freezes, the ice expands and breaks off very small amounts of rock. The ice causes abrasion of the rocks causing grooves and cracks. Water then enters these openings and freezes causing the rocks to break open, exposing more sides to the weather and continuing the breakdown.
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.)
All weather can and will break up rocks.
Rocks on mountain tops are exposed to harsher weather conditions, such as wind, rain, and ice, which can break down the rocks more quickly through processes like frost wedging and erosion. Additionally, mountain rocks may experience larger temperature variations, leading to thermal stress that can contribute to faster weathering.
Rocks are typically exposed to more wind, rain, and ice in mountainous regions and coastal areas where there are strong weather patterns and erosion processes at play. These environments experience higher levels of weathering and erosion due to the constant exposure to these elements.
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.)
Normally, sedimentary rocks weather more rapidly than igneous or metamorphic rocks due to the ability of water to attack the cementing material and the ability of ice, water and plant roots to attack and separate the depositional layers.
Would you like your drink neat or on the rocks? -->> neat = without ice just as it is on the rocks = with ice
It breaks from ice wedging
they are exposed to more wind,rain,and ice than the rocks at lower elevation
ice and loose rocks