The only good example of this is chalk, which is made from the compacted shells of tiny marine organisms called diatoms. Other than that, animal and plant remains do not tend to form rocks, although the hard parts may form fossils.
Sedimentary rock is formed from the cementing of small pieces of older rocks, shells, soil, or dead plants and animals. These fragments, called sediments, can be compacted and cemented together over time to create sedimentary rock. Examples of sedimentary rocks include sandstone, limestone, and shale.
Sedimentary rocks form at or near the Earth's surface through the accumulation and compression of sediments. These sediments can come from the weathering and erosion of pre-existing rocks, as well as from the remains of plants and animals. Over time, these sediments are compacted and cemented together to form sedimentary rocks.
A sedimentary rock forms from rock particles cemented (compacted) together. If the remains of dead plants and animals are preserved in the rock, they become fossils. If the remains break down into carbon, oils, or gases, they become fossil fuels.
Yes, shale is a clastic sedimentary rock composed of clay minerals and other fine-grained particles that have been compacted and cemented together.
Sedimentary rocks formed from the remains of plants and animals are called organic sedimentary rocks. Examples include coal, formed from the remains of plants, and limestone, formed from the shells of marine organisms.
Sedimentary rock is formed from the cementing of small pieces of older rocks, shells, soil, or dead plants and animals. These fragments, called sediments, can be compacted and cemented together over time to create sedimentary rock. Examples of sedimentary rocks include sandstone, limestone, and shale.
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 form at or near the Earth's surface through the accumulation and compression of sediments. These sediments can come from the weathering and erosion of pre-existing rocks, as well as from the remains of plants and animals. Over time, these sediments are compacted and cemented together to form sedimentary rocks.
Sedimentary rock formed from pieces of once living organisms is called organic or biogenic sedimentary rock. This type of rock is made up of the remains of plants or animals that have been compacted and cemented together over time. Examples include limestone, coal, and chalk.
A sedimentary rock forms from rock particles cemented (compacted) together. If the remains of dead plants and animals are preserved in the rock, they become fossils. If the remains break down into carbon, oils, or gases, they become fossil fuels.
Yes, shale is a clastic sedimentary rock composed of clay minerals and other fine-grained particles that have been compacted and cemented together.
Sedimentary rocks formed from the remains of plants and animals are called organic sedimentary rocks. Examples include coal, formed from the remains of plants, and limestone, formed from the shells of marine organisms.
Fossilized plants and animals are often found separately because they have different preservation conditions. Plants are usually preserved in sedimentary rocks, while animals are more commonly found in sedimentary rocks or amber. The chances of both being preserved together in the same location are low due to the specific conditions required for fossilization to occur.
Plants and Animals
Sedimentary rocks are made of various materials such as mineral fragments, organic matter, or chemical precipitates. These materials accumulate over time in layers and become compacted and cemented together to form rocks like sandstone, shale, or limestone.
Coal is a type of sedimentary rock known as a combustible sedimentary rock. It is formed from the remains of plants that have been compacted and altered over millions of years under heat and pressure.
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.