Chemical weathering can dissolve the calcite in marble and limestone over time, especially in the presence of acidic rain or groundwater. This can cause the rocks to deteriorate, forming cracks and pits on their surface. The dissolution of calcite can also weaken the structure of the rocks, leading to physical weathering processes like erosion.
carbon dioxide: when it mixes with rain& water will create carbonic acid rain which weathers marble and limestone.so carbonic acid weathers marble and limestone.
The answer is marble because it is like glass and if there were a piece on the ground it could be easily broken but if there were a tornado the tornado couldnt break it. Marble is very fragile.
In wet climates, granite weathers more slowly than limestone because granite is a harder and more resistant rock compared to limestone. The minerals in granite are less susceptible to dissolution by water and chemical weathering processes, leading to slower weathering rates.
Marble weathers faster than feldspar because marble is more susceptible to chemical weathering due to its composition of calcium carbonate, which reacts easily with acidic rainwater. In comparison, feldspar is more resistant to weathering due to its hardness and chemical stability.
in rain and flooding
Limestone and marble.
chemical weathering by acid rain.
carbon dioxide: when it mixes with rain& water will create carbonic acid rain which weathers marble and limestone.so carbonic acid weathers marble and limestone.
No. Calcite is also found in marble, marl, and can occur in small amounts in igneous rocks as a product of chemical weathering.
The answer is marble because it is like glass and if there were a piece on the ground it could be easily broken but if there were a tornado the tornado couldnt break it. Marble is very fragile.
No. Calcite is also found in marble, marl, and can occur in small amounts in igneous rocks as a product of chemical weathering.
Quartz is a mineral that is highly resistant to chemical weathering. Marble is a mineral that is more susceptible to chemical weathering.
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Marble is known as Calcium Carbonate (CaCO3) in terms of chemical formula.
Carbonic acid, which forms when carbon dioxide in the atmosphere dissolves in rainwater, is a major agent of chemical weathering for marble and limestone. When carbonic acid reacts with the calcium carbonate in marble and limestone, it forms calcium bicarbonate which dissolves the rock and causes weathering.
Dissolution by water, especially water acidified by atmospheric carbon dioxide (producing carbonic acid) or soil acids. Marble is composed primarily of the mineral calcium carbonate, modified to crystalline form by metamorphism of the parent limestone. Therefore karst features can develop in marble just as they can in unaltered limestone.
Chemical change