A type of rock? Possibly coal, which is decayed plant material, compressed and turned into a 'rock-like' material.
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.
A rock type that forms from particles of other rocks or the remains of plants and animals is called sedimentary rock. These rocks are created through the accumulation and compaction of sediments over time, which can include mineral fragments, organic materials, and other particles. Common examples of sedimentary rocks include sandstone, limestone, and shale. They often contain fossils and provide valuable information about Earth's history.
organic sedimentary
The type of rock that forms when particles from other rocks or the remains of plants and animals are pressed and cemented together is called sedimentary rock. This process typically occurs in layers over time, as sediments accumulate and undergo compaction and lithification. Common examples of sedimentary rocks include sandstone, limestone, and shale. These rocks often contain fossils and provide valuable information about Earth's history.
Sedimentary rock, specifically organic sedimentary rock like coal or limestone, forms from the accumulation and compaction of remains from dead plants and animals over time. These materials can include organic matter such as shells, bones, and plant debris.
Organic sedimentary rock forms when material from dead plants and animals (organic matter) gets deposited and hardens into rocks over time. Examples include coal and some types of limestone.
remains of plants and animals:)
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 rock that forms when layer of particles settle on top of each other and harden is a sedimentary rock.
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.
When soil forms over bare rock, it is made up of weathered rock particles, organic matter from decaying plants and animals, and a mix of minerals and nutrients. Over time, soil formation processes such as weathering, erosion, and biological activity continue to enrich and develop the soil profile.
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.