Coal forms from the accumulation of plant material in swampy environments, which decomposes and transforms over time. The lack of coal deposits in rocks older than about 443 million years is due to plate tectonics and the movement of continents, which have caused older coal-bearing rocks to be buried too deep, where the heat and pressure have transformed them into other types of rocks.
Coal has been forming in the Earth for millions of years, with some coal deposits dating back to over 300 million years. The process of coal formation involves the accumulation of plant material in swampy environments, which over time gets buried and compressed to form coal deposits.
Coal deposits are layers of sedimentary rock containing coal, formed from the accumulation of buried plant material over millions of years. These deposits are mined for coal, which is a fossil fuel used for electricity generation and heating. Coal deposits can vary in thickness, quality, and location around the world.
Coal deposits are formed by the remains of plants that were buried and compacted over millions of years. The process involves the accumulation of organic material in swamps and wetlands, which is then subjected to pressure and heat, leading to the formation of coal.
Todays coal was formed millions of years ago. Sum of the earliest coal deposits formed only about 1 million years ago whereas the old deposits are from 300 million years ago. Coal is formed where plant life has died and then eventually sink to the bottom of swampy areas or the water level has risen and covered the dead plant life. Over time as the amount of dead plant life accumulates at the bottom of the swampy area it turns into a dense soggy material known as peat then as the land changed and the pressure upon the peat built due to deeper burial, sandstone and sedimentary rocks that may have formed due to the changing land, the water in the peat is squeezed out and when heat is added from the earths core, the peat is turned into coal.
Coal deposits are commonly referred to as coal seams or coal beds. These are layers of coal that are found buried beneath the Earth's surface.
Coal
Coal has been forming in the Earth for millions of years, with some coal deposits dating back to over 300 million years. The process of coal formation involves the accumulation of plant material in swampy environments, which over time gets buried and compressed to form coal deposits.
Coal deposits are layers of sedimentary rock containing coal, formed from the accumulation of buried plant material over millions of years. These deposits are mined for coal, which is a fossil fuel used for electricity generation and heating. Coal deposits can vary in thickness, quality, and location around the world.
Tertiary coal refers to coal deposits that were formed during the Tertiary Period of geologic time, which occurred between 65 to 2.6 million years ago. These coal deposits are relatively younger compared to those from earlier periods such as the Carboniferous and Permian. Tertiary coals are typically lower in rank and quality compared to older coal deposits.
Most coal deposits were laid down during the Carboniferous period, approximately 360 to 300 million years ago. This period is sometimes referred to as the "Age of Coal" due to the extensive coal-forming swamps and forests that existed during this time.
it is made from once living things when the pangea on the earth moved away
Coal beds formed during the Carboniferous Period, approximately 300 to 360 million years ago. This period was characterized by extensive forests being buried and compressed over time, eventually transforming into coal deposits.
Coal forms from the remains of plants that have been buried and compressed over millions of years. Human fossils would not be found in coal deposits because humans did not exist during the time when the plants that formed the coal were alive. Additionally, the conditions necessary for coal formation are not conducive to the preservation of human remains.
The formation of coal layers happened in many early geological periods, but the Carboniferous Period is especially known for producing them in the US. This period was about 300-350 million years ago.
Coal is a sedimentary rock that forms from the remains of plants that lived in swampy environments millions of years ago. It is typically found in underground deposits known as coal seams or coal beds. Coal can be mined from these deposits to be used as a source of energy.
Coal deposits are formed by the remains of plants that were buried and compacted over millions of years. The process involves the accumulation of organic material in swamps and wetlands, which is then subjected to pressure and heat, leading to the formation of coal.
Todays coal was formed millions of years ago. Sum of the earliest coal deposits formed only about 1 million years ago whereas the old deposits are from 300 million years ago. Coal is formed where plant life has died and then eventually sink to the bottom of swampy areas or the water level has risen and covered the dead plant life. Over time as the amount of dead plant life accumulates at the bottom of the swampy area it turns into a dense soggy material known as peat then as the land changed and the pressure upon the peat built due to deeper burial, sandstone and sedimentary rocks that may have formed due to the changing land, the water in the peat is squeezed out and when heat is added from the earths core, the peat is turned into coal.