Bituminous coal is largely the product of ancient plant remains, although some animals would have contributed to a very small percentage of its mass.
anthracite coal is the metamorphic form of bituminous coal which is the sedimentary form. in other words it has been heated under pressure.
bituminous is less hard,and its dull.whereas anthracite is very hard.
Lignite is a low-grade coal with low carbon content and high moisture content, making it less energy-dense than bituminous coal. Bituminous coal, on the other hand, has a higher carbon content and energy density, making it a more valuable and widely-used form of coal for energy production.
Anthracite coal, which is a harder and more carbon-rich coal with a higher energy content.
Actually, any kind of plant/animal could have died to form coal. But not just any type of coal. Bituminous coal, to be exact. This happens when dead plant/animal's remains (though mostly plant, a small percentage of bituminous coal is from animal remains) are buried under a body of water (usually a swamp) and decay there for a while, forming a thick layer. Then it needs to be buried by a lot of 'sediments', usually mud/sand to compress the plant/animal remains into coal.
no not all of them for example like Bituminous coal or coal, is form by plant remains
Anthracite coal is formed by the further metamorphism of bituminous coal. This process involves high pressures and temperatures, which leads to the coal becoming harder and more carbon-rich. Anthracite coal is the highest rank of coal and has a high carbon content and low impurities.
Coal forms from the remains of ancient plants that have been buried and subjected to high pressure and heat over millions of years. As the plant material decomposes and undergoes chemical changes, it transforms into peat, then lignite, sub-bituminous coal, bituminous coal, and finally anthracite coal, with each stage containing less moisture and more carbon.
Yes. Lignite is also known as brown coal. It is not exactly the same as coal (bituminous or anthracite) but it is near the beginning of the process that makes coal. Lignite has about 1/3 to 1/2 the carbon content of coal.
Millions of years of pressure and heat turned decaying animals and plants into coal.
Coal is formed through a process called coalification, where layers of plant material are buried and compressed over millions of years. The plant material is first transformed into peat through decay, then undergoes further compaction and heating to form lignite, then into sub-bituminous coal, bituminous coal, and finally anthracite with increasing pressure and heat. Each layer represents a different stage in the coalification process, resulting in different types of coal.
The protolith of schist is typically shale or slate, which undergoes metamorphism to form schist. The protolith of anthracite coal is primarily bituminous coal, which is subjected to higher temperature and pressure conditions during metamorphism to convert into anthracite coal.