Not quite. Limestone can be quite hard but in any case mechanical erosion is a secondary process consequent upon a sufficiently large conduit forming first.
The primary process is the dissolution of limestone (strictly speaking the calcium carbonate that is its main constituent) by water slightly acidified by absorbing atmospheric carbon dioxide.
The water finds its way through the rock formation by following the tension-cracks, bedding-planes and other discontinuities from sink to rising (spring).
And the term used throughout the English-speaking world is "caving" not "spelunking", which I have heard is actually derisory slang in the US for novice or dilettante cavers. I've mentioned this a few times on Answers by now!
The causes of chemical weathering include exposure to water, oxygen, carbon dioxide, and acids. Erosion is a physical weathering process, not a chemical one.
Chemical weathering
acid rain causes the marbel statues to arode
Weathering from mechanical and chemical means is the process that causes rocks to become smaller and smaller; wind, rain, the sun, the freeze/thaw cycle, moving glaciers, chemical reactions, and gravity are some of the causes of weathering.
It causes chemical weathering because when it touches rocks, the rocks dissolve, forming caves.
The dissolution of limestone by carbonic acid is a chemical process. Carbonic acid reacts with the calcium carbonate in limestone to form calcium bicarbonate, which is soluble in water. This chemical reaction causes the limestone to dissolve.
what chemical weathering called oxidation causes
Oxygen is the major gas that is the cause chemical weathering.
Carbonation, a type of chemical weathering where carbon dioxide in rainwater reacts with limestone to form carbonic acid, is the primary process that creates karst features like caves and sinkholes. Over time, this acidic water dissolves the limestone, creating underground voids and caverns in the process.
Chemical weathering involves the breakdown of rocks through chemical reactions. For example, the gradual dissolution of limestone by acidic rainwater is a common form of chemical weathering. Physical weathering, on the other hand, involves the breakdown of rocks without changing their chemical composition. An example is freeze-thaw weathering, where water seeps into cracks in rocks, freezes, expands, and causes the rocks to break apart over time.
This would usually be caused by the dissolution of soluble rocks such as limestones. Dissolution is a chemical weathering process.
Erosion of limestone can be caused by chemical weathering, where acidic rainwater dissolves the calcium carbonate in limestone, or by physical weathering, where wind, water, or ice break down the rock over time. Human activities like mining and quarrying can also contribute to the erosion of limestone.
The causes of chemical weathering include exposure to water, oxygen, carbon dioxide, and acids. Erosion is a physical weathering process, not a chemical one.
Chemical weathering
Chemical weathering
Chemical weathering
Mechanical weathering is the breakdown of rocks into smaller pieces without altering their chemical composition, usually by processes such as frost wedging or root expansion. Chemical weathering, on the other hand, involves changes in the chemical composition of rocks due to reactions with substances like water, acid rain, or oxygen, leading to the breakdown of minerals.