humus
They could simply become fossils and in other casses decomposition may fully occur to produce humus, or they might just disintegrate the more, then mix up to develop soil. But most times the ultimate result usually ends up in the formation of sedimentary rocks, after the minerals, fossils, humus, regoliths, and soil, all combine and gets hardened over a long period of time.
The process of changing the hard parts of animal or plant remains with minerals is called fossilization. This process can involve the replacement of organic materials with minerals, preserving the structure of the original organism as a fossil for scientific study.
Sedimentary rocks form through the accumulation and compaction of sediments, which can include rock particles, minerals, and organic materials like animal remains. Over time, layers of sediment build up and undergo lithification, a process that involves compaction and cementation, transforming loose materials into solid rock. Additionally, minerals can crystallize from water in the sediment, further contributing to the rock's composition. This multifaceted process allows sedimentary rocks to incorporate a diverse range of materials.
A rock containing organic debris is called a sedimentary rock. This type of rock forms from the accumulation and compression of organic materials like plant and animal remains. Over time, these organic materials become compacted and cemented together to form a rock.
The study of plants and animal remains is known as paleobotany and paleozoology. These fields involve examining fossilized plant and animal remains to understand their anatomy, ecology, evolution, and their interactions with the environment. It provides insights into the history of life on Earth and helps reconstruct ancient ecosystems.
Yes, fossil fuels like coal, oil, and natural gas are formed from the remains of plants and animals that lived millions of years ago. These organic materials underwent a process of decomposition and were subjected to high pressure and temperature over time, leading to the formation of fossil fuels.
fuel is the decayed remains of plant and animal matter after thousands of years. hence the name: fossil fuels.
Humus (Not hummus the dip), compost, or fertilizer. Those are words for decayed plant and animal material.
Soil is composed of mineral particles (like sand, silt, and clay), organic matter (such as decaying plant and animal material), water, and air. These components interact to support plant growth and provide habitats for various organisms. The proportions of these materials can vary, leading to different types of soil.
rock fragments plant and animal remains mineral grains
Decayed matter that becomes part of the soil is called organic matter. This includes leaves, plant material, animal remains, and other organic substances that break down and contribute nutrients to the soil. Organic matter is important for soil fertility and structure.
Sometimes they are referred to as bits of dead plants or animals. Others refer to them as fossils, or organic remains. If it is a decayed organism (either plant OR animal) it might be referred to as 'detritus'. If it's the final remains of a human being, it may be referred to as a corpse.
The Topsoil
humus
Soil is mostly made up of mineral particles (such as sand, silt, and clay), organic matter (decayed plant and animal material), water, and air. These components interact to provide plants with essential nutrients, support, and drainage needed for growth.
Organic matter, such as decaying plant and animal residue, combines with particles of weathered bedrock to make the fertile soil of the Midwest. This process helps provide essential nutrients for plant growth and contributes to the productivity of the region's agriculture.
crude oil
HUmus