The main substance in limestone is calcium carbonate.
The main compound in limestone is calcium carbonate.
The main processes that affect limestone are weathering, erosion, and dissolution. Weathering breaks down the rock, erosion transports the broken material, and dissolution occurs when rainwater or acidic water dissolves the limestone. These processes can lead to the formation of caves, sinkholes, and other unique landforms.
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.
Limestone is a mineral largely composed of calcium carbonate.
The main types of limestone are chalk, coral limestone, travertine, and tufa. Chalk is soft and white, coral limestone contains coral and other marine organisms, travertine is formed by hot springs, and tufa is a porous rock formed by calcium-rich water.
The chemical formula of limestone is CaCO3.
Pure substance
its heated with something
limestone
Limestone is a type of sedimentary rock that is made up primarily of the mineral calcite, which is a homogeneous substance. Therefore, limestone is considered a homogeneous material.
The main compound in limestone is calcium carbonate.
Limestone is not a pure substance. It is a sedimentary rock composed of various minerals such as calcite, aragonite, and dolomite. These minerals can vary in composition and impurities, making limestone a heterogeneous mixture rather than a pure substance.
Limestone
The main substance used in glassmaking is silica sand, which is heated to high temperatures along with other materials such as soda ash and limestone. These ingredients are melted together to form molten glass, which can then be shaped and cooled to create various glass products.
Limestone and baking soda will.
Limestone is made of calcium carbonate, which is a base when dissolved in water
The main sediment of limestone is calcium carbonate, which is primarily composed of the mineral calcite. It forms from the accumulation and compaction of the remains of marine organisms such as coral, shells, and skeletal fragments.