Sand stone is pourous and water gets into it. When it freezes the water expands causing the granuals of sand that make up the sandstone to become disconected from the overal mass of the stone. Freeze and thaw often enough and you have nothing but a pile of sand.
Quartzite and sandstone are composed mainly of quartz which is a very resistant mineral that weathers slowly. As a result, the soil that develops from quartzite or sandstone tends to be nutrient-poor and well-drained due to the lack of easily weathered minerals. It may also be sandy or gravelly in texture.
Generally, arkosic sandstone would travel less distance before deposition compared to quartz sandstone. This is because arkosic sandstone is typically less resistant to weathering and erosion due to its higher content of feldspar, which weathers more easily compared to quartz. Quartz sandstone, being more durable, can travel further before getting deposited.
Sandstone is susceptible to weathering due to its porous nature, allowing water and other elements to penetrate and break down the rock over time. Processes such as freeze-thaw cycles, wind erosion, and chemical weathering can cause the sandstone to deteriorate, leading to the formation of cracks, fractures, and erosion of the rock surface. As a result, the overall structure and integrity of the sandstone can be compromised.
Sandstone typically weathers into sandy soils. These soils generally have poor nutrient retention and water holding capacity, leading to reduced crop productivity. Management problems may include increased erosion, nutrient leaching, and the need for frequent irrigation and fertilization to support plant growth.
Frezing that all I know
frezzer not frezing
i think its granite Above answer is wrong! Granite is VERY hard and weathers slowly. SANDSTONE is very soft and permeable and weathers (erodes) very quickly.
Because it is relatively soft, sandstone is not a good building material for certain things such as houses. It can be used for building other things such as fountains, counter tops and statues.
by frezing it
Quartzite and sandstone are composed mainly of quartz which is a very resistant mineral that weathers slowly. As a result, the soil that develops from quartzite or sandstone tends to be nutrient-poor and well-drained due to the lack of easily weathered minerals. It may also be sandy or gravelly in texture.
When water freezes, it expands, which can lead to the formation of ice within the pores of the sandstone. As the ice expands, it can exert pressure on the surrounding sandstone, potentially causing it to crack or fracture. Over time, repeated cycles of freezing and thawing in the presence of water can contribute to the weathering and deterioration of the sandstone.
Generally, arkosic sandstone would travel less distance before deposition compared to quartz sandstone. This is because arkosic sandstone is typically less resistant to weathering and erosion due to its higher content of feldspar, which weathers more easily compared to quartz. Quartz sandstone, being more durable, can travel further before getting deposited.
Sandstone is susceptible to weathering due to its porous nature, allowing water and other elements to penetrate and break down the rock over time. Processes such as freeze-thaw cycles, wind erosion, and chemical weathering can cause the sandstone to deteriorate, leading to the formation of cracks, fractures, and erosion of the rock surface. As a result, the overall structure and integrity of the sandstone can be compromised.
Sandstone typically weathers at a faster rate compared to granite due to its softer and more porous nature. Sandstone is more susceptible to erosion from wind, water, and other environmental factors, leading to quicker deterioration over time. Granite is a much harder and more resistant rock that is better able to withstand weathering processes.
6 Degrees Celcius.
As the water froze and expanded, it would exert pressure on the surrounding sandstone. This pressure could cause the sandstone to crack or fracture, as the ice expands and pushes against the rock material. Over time, repeated freezing and thawing cycles can lead to weathering and erosion of the sandstone.
Carbon dioxide dissolved in rain water forms a weak acid which slowly weathers limestone, a carbonate which reacts with acids.