Mostly Calcium carbonate(CaCO3)
The colours of limestones vary depending on their chemical composition. An iron content to limestone can give a tinge of iron oxide (rust) colour. The exact chemical composition will depend on the origin and geological process resulting that stone.
You will get marble, a metamorphic rock, from limestone. Marble forms when limestone is subjected to heat and pressure, causing it to recrystallize and change in mineral composition.
alkali and acid
There are two main types of limestone: (1) calcitic limestone, which is mainly composed of calcium carbonate, and (2) dolomitic limestone, which contains a combination of calcium carbonate and magnesium carbonate. These types of limestone have different properties and are used for various applications depending on their composition.
Marble is a type of rock that was once limestone. Through heat and pressure, limestone undergoes metamorphism and transforms into marble, resulting in a harder and more crystalline composition.
Limestone typically does not have a noticeable smell. Sandstone may have a mineral-like smell due to its composition, but it is generally not strong or distinct.
Dolomite and chalk have similar compositions to limestone, as they are all primarily composed of calcium carbonate minerals. Dolomite contains a significant amount of magnesium carbonate in addition to calcium carbonate, while chalk is a type of limestone that is formed from the shells of marine organisms.
Different types of limestone have varying amounts of calcium carbonate due to differences in their formation processes. Factors such as environmental conditions, mineral composition, and the presence of impurities can contribute to variations in calcium carbonate content. Additionally, geological processes such as pressure and temperature can also affect the composition of limestone.
Fossiliferous limestone has larger fossils in the rock and is of biochemical composition where as the oolitic limestone doesn't have any fossils and has a chemical composition. The Oolitic limestone has spherical grains that resemble miniature pearls (they are called ooliths or ooids). Both do effervesce in diluted HCL(acid)
Limestone gets its name from the Latin word "calx" which means lime. Limestone is primarily composed of the mineral calcite, which is a form of calcium carbonate. The name reflects the mineral composition and the fact that it often contains high amounts of lime.
A streak is the color of the powdered mineral left behind when the mineral is rubbed against a hard, rough surface. Limestone typically has a white streak due to its composition of calcium carbonate.
Yes, crushing limestone is a physical change. This is because the chemical composition of limestone remains unchanged during the process of crushing. The size and shape of the limestone particles may change, but the chemical makeup remains the same.