Rainwater is naturally slightly acidic because carbon dioxide from the air dissolves in it. Minerals in rocks may react with the rainwater, causing the rock to be weathered. Some types of rock are easily weathered by chemicals. For example, limestone and chalk are mostly calcium carbonate. When acidic rainwater falls on limestone or chalk, a chemical reaction happens. New, soluble, substances are formed in the reaction. These dissolve in the water, and then are washed away, weathering the rock. -BBC: The rock cycle
The acid well eat at the limestone, Making it look old and decompsed
Sulfuric acid degrades
it is a chemical weathering
Limestone is mainly composed of calcium carbonate. It will react with acids to produce carbon dioxide, a salt and water, and the limestone will slowly dissolve away - an experiment easily performed by pouring vinegar on a piece of limestone. In the outdoors: Acid rain (from industrial pollution mixing with falling rain) cause limestone to dissolve, increasing the natural effect of rain water erosion of rock - forming potholes, caverns - and clints and grykes (fissures) on 'limestone pavements'.
Because rainwater is mildly acidic. Acid in the rainwater dissolves the limestone.
yes
The dissolution of limestone by rainwater containing carbonic acid is the perfect example of chemical weathering.
Under the category of weather, limestone would be most affected by rain. Rain contains carbonic acid which reacts chemically with the calcium carbonate in limestones. Just try putting a drop of vinegar on a piece of limestone and see what happens. Carbonic acid in rainwater is not nearly this concentrated, though, and the effects take much longer to be noticeable. Tropical climates also produce large amounts of vegetation whose plant roots help break limestone apart, creating more surface area for rainwater to attack. Limestone would be least affected in arid climates, where most erosion is in the form of wind particle abrasion.
Rainwater is naturally slightly acidic. The acid in rainwater reacts chemically with the calcium carbonate of limestone, dissolving it. The result is chemically weathered limestone, karst terrains, and cave structures.
Acid in the rainwater causes limestone to dissolve, leaving open spaces, or caves.
Because rainwater dissolves carbon dioxide to produce carbonic acid - a weak acid - but over geological time it can dissolve various types of rock like limestone and thus weather it.
because of acid rain
Chemical weathering processes are particularly effective on limestone landscapes forming because of carbonation. When rainwater combines with acid in the air, limestone is formed.
Chemical(acid in rainwater dissolving limestone), biological (work of animals and plants) and physical (freeze thaw)
Rainwater sinking into limestone
Carbon dioxide dissolved in rain water forms a weak acid which slowly weathers limestone, a carbonate which reacts with acids.