That would be erosion.
Rocks containing calcium carbonate (Ca CO3), example limestone, tend to weather easily. The acid rain reacts with this component in sedimentary rocks and weaken the bonds between its constituent minerals, making it more susceptible to breaking away from the original portion.
When the rock erodes away, the mass slowly leaves along with the bits that erode away. So as it becomes smaller, it becomes lighter.
Acid does indeed cause weathering. It is a common form of chemical weathering, and is sometimes influenced by humans. It is particularly devastating to basic rocks like limestone which neutralise the acid rain, but at the expense of its own volume, as after the neutralisation, the salt is often washed away and the limestone is consequently worn away.
No. It is a sedimentary rock. However, unlike sandstone which is also a sedimentary rock, it is primarily composed of calcium carbonate which can be eaten away by acid (like acid rain) gradually with time.
The change undergone is physical only. The definition of weathering is the wearing away of rocks in situ. Weathering causes the rocks to "break down", but mostly not to chemically change (the exception being limestone in acid rain).
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'.
Rocks wear away because slowly,wind/water take away tiny pieces of dust and slowly it gets worn away.
Limestone and marble.
The tides and waves slowly wear away at the rocks.
when acid is on limestone to start with there would be a continues fizz. After time acid would were slowly chip and were away the rock.
They Dissolve by fumes and smells, scents and gas or bad fumes and the smells get into the stars slowly washing them away.
Limestone is calcium carbonate and is basic in nature. When added to dilute acid, limestone will dissolve, forming the corresponding calcium salt, water and carbon dioxide. Eg. 2HCl + CaCO3 ---> CaCl2 + H2O + CO2 or H2SO4 + CaCO3 ---> CaSO4 + H2O + CO2 Note: this is infact one of the major problems of acid rains. When acid rain falls on monuments made up of marbles (which is also another form of calcium carbonate), these monuments fade away as the monuments dissolve slowly.
Hard rocks , such as granite, weather more slowly than softer rocks , such as limestone. Differential weathering happens when softer rocks weathers away and leaves harder, more resistant rock behind. The figures below show an example of how differential weathering can shape landscape.
Dissolve is where it fully disappears and then fade is where it slowly goes like a sun bleached cushion a while it starts to go away.
Limestone caves are formed by the dissolution of limestone rocks over thousands of years due to the chemical reaction of rainwater and carbon dioxide. This process creates underground caverns and passages with unique formations such as stalactites and stalagmites. Limestone caves are often popular tourist attractions due to their natural beauty and geological significance.
It's a salt depositary in the original limestone blocks and is slowly being eroded away
Rocks containing calcium carbonate (Ca CO3), example limestone, tend to weather easily. The acid rain reacts with this component in sedimentary rocks and weaken the bonds between its constituent minerals, making it more susceptible to breaking away from the original portion.