Fossil remains
Sedimentary rock, specifically organic sedimentary rock, is formed when material from dead plants and animals is deposited and hardened into rock. This process involves the accumulation and compression of organic remains over time. Examples include coal, limestone, and oil shale.
Sedimentary rock forms when material from dead plants and animals, along with other debris, is compacted and cemented over time. This process creates rock layers rich in organic material, such as coal or limestone, from the remains of living organisms.
Through the geophysical pressure on decomposed fossil shells deposited in deep underground layers. FOSSIL FULES ARE MADE UP OF PLANTS AND ANIMALS B- THE ORGANISM MUST BE BURIED IN SEDIMENT SOON AFTER IT DIES.
lorpumete
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.
The type of rock that forms where the remains of plants and animals are deposited in thick layers are called organic sedimentary rock.
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.
The hardened remains of plants and animals are typically bones or fossils. Fossils are the hardened remains that are formed due to pressure from being squished between Earth's layers.
Dead and decayed remains of plants and animals, called Humus.
Tiny remains of animals and plants in streams come from the mountains. When it rains, these remains are washed down the mountains toward the streams.
decomposes break down the remains of dead plants and animals.
The biological accumulation of the skeletal remains of the plants and animals make up the fossils. A fossil refers to the trace of plants or animals that survived in the past.
Sedimentary rock, specifically organic sedimentary rock, is formed when material from dead plants and animals is deposited and hardened into rock. This process involves the accumulation and compression of organic remains over time. Examples include coal, limestone, and oil shale.
A paleontologist studies fossilized remains of plants and animals.
Coal is formed from the remains of plants that lived in swamps and marshes millions of years ago. These organic materials were buried under layers of sediment and compressed over time. Coal deposits are typically found in areas where these conditions existed, such as former swamps and wetlands.
Dirt
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.