The term that describes the remains or impressions of plants and animals in sedimentary rock is "fossils." Fossils can include a variety of forms, such as preserved bones, shells, imprints, or traces of organisms, providing valuable insights into past life and ecosystems. They are essential for understanding the history of life on Earth and are typically found in sedimentary rock layers where conditions favored their preservation.
The term that describes the remains or impressions of plants and animals in sedimentary rock is "fossils." Fossils can include not only the actual remains of organisms but also their traces, such as footprints, burrows, or imprints. They provide valuable information about past life forms and their environments. Fossils are crucial for understanding the history of life on Earth.
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.
FOSSILS
Sedimentary rock, specifically organic sedimentary rock such as coal or limestone, forms where the remains of plants and animals are deposited in thick layers over time. These rocks are primarily made up of organic material and are created through the compression and cementation of these remains.
Because when the lava killed the animals, their remains stayed in the lava and dried to become sedimentary rock.
Plants and animals contribute to the formation of sedimentary rock through the process of fossilization. When plants and animals die, their remains can become buried in layers of sediment over time. Through pressure and time, these organic remains can undergo the process of mineralization, where their organic material is replaced by minerals, ultimately forming sedimentary rock.
The type of rock that forms where the remains of plants and animals are deposited in thick layers are called organic sedimentary rock.
Such remains are known as fossils if the sediment is changed over eons into a sedimentary rock.
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Sedimentary rocks that are formed partially by animals and plants are called organic sedimentary rocks. These rocks are formed from the accumulation and lithification of the remains or traces of once-living organisms. An example of an organic sedimentary rock is limestone, which is formed from the accumulation of marine organisms' shells and skeletons.
Sedimentary rocks are most likely to contain fossils. This is because sedimentary rocks form from the accumulation and compression of sediments that often include the remains of plants and animals. Over time, these remains can become preserved as fossils within the layers of sedimentary rock.
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.