organic
Coal is not considered a mineral because it is organic in nature, formed from the remains of plants. Unlike minerals, which are inorganic and have a crystalline structure, coal does not have a consistent chemical composition or crystal structure. This distinction classifies coal as a sedimentary rock rather than a mineral.
Coal contains energy because it is made up of carbon-rich organic compounds that were formed millions of years ago from decaying plant matter. Through a process called carbonization, the energy stored in these organic compounds is trapped within the coal as chemical energy. When the coal is burned, this chemical energy is released as heat and can be harnessed for various applications such as generating electricity or heating.
Limestone is a type of rock that can be either chemical or organic in nature. Chemical limestone is formed through the precipitation of calcium carbonate, while organic limestone is made up of the remains of marine organisms like shells and coral.
While coal is composed of organic materials, it is generally not classified as a mineral because it is formed from plant matter rather than the inorganic processes that create minerals. Minerals are typically crystalline and have a specific chemical composition, which differs from the amorphous nature of coal.
Coal is made from organic matter (plant material) that has undergone a series of geological processes, which distinguishes it from minerals that are inorganic and have a crystalline structure. While coal shares some similarities with minerals in terms of its use and extraction, its organic origin makes it different from minerals in the traditional sense.
Limestone made from shells would be an organic sedimentary rock.
The two main types of sedimentary rocks are clastic (detrital) rocks, which are made of pre-existing rock fragments cemented together, and chemical rocks, which form from minerals that precipitate out of solution.
Clastic sediments are sediments that have particles or pieces of rock (clasts) in them. The clasts can be of igneous, metamorphic or sedimentary rock. Non-clastic sediments are made up of dissolved minerals or organic matter.
Clastic sedimentary rock forms when fragments of preexisting rocks are compacted or cemented together. Organic sedimentary rock forms from the remains of plants or animals. Chemical sedimentary rock forms when minerals precipitate from a solution or settle from a suspension.
Sedimentary rocks are classified as either clastic (composed of fragments of pre-existing rocks), chemical (formed from mineral precipitation), or organic (derived from the remains of plants and animals). These classifications help to understand how the rock was formed and its origin.
Clastic Sedimentary Rock- Sedimnetary rocks formed from fragments of rocks cemented together by minerals such as calcite.Chemical Sedimentary Rock- Sedimentary rocks formed from a solution of minerals (such as halite) and water.Organice Sedimentary Rocks- Sedimentary Rocks formed from the remaints of dead sea animals and seashells.
Most non-clastic sedimentary rocks are made up of minerals that have precipitated from water, such as limestone, which is composed of calcite. Other non-clastic sedimentary rocks include organic-rich rocks like coal and chert, a silica-rich rock formed from the remains of marine organisms.
Clastic sedimentary rocks, like conglomerate and sandstone.
Clastic: These rocks are composed predominantly of broken pieces of older weathered and eroded rocks Non-clastic/ Organic: A sedimentary rock composed of the remains of plants and animals.
Sedimentary rocks can be classified based on their composition, texture, and the way they were formed. Common classifications include clastic, chemical, and organic sedimentary rocks. Clastic rocks are made of fragments of other rocks, while chemical rocks form from dissolved minerals. Organic rocks are made from the remains of plants and animals. Texture can also help classify sedimentary rocks, such as fine-grained, coarse-grained, or conglomerate.
Sedimentary rocks are classified based on their mineral composition, grain size, texture, and the way they were formed. The three main types of sedimentary rocks are clastic, chemical, and organic. Clastic rocks are made up of broken fragments of other rocks, chemical rocks form from precipitation of minerals from water, and organic rocks are formed from the accumulation of plant and animal remains.
Coal is not considered a mineral because it is organic in nature, formed from the remains of plants. Unlike minerals, which are inorganic and have a crystalline structure, coal does not have a consistent chemical composition or crystal structure. This distinction classifies coal as a sedimentary rock rather than a mineral.