tang ina kantutin mo si Saddam
That would be fossils.
biogenic
Biological weathering is called so because it involves the breakdown of rocks and minerals by living organisms like plants, animals, and microorganisms. These organisms play a role in physically or chemically altering the rock structures, leading to their weathering and eventual breakdown. This process is essential in soil formation and ecosystem development.
Organic weathering is the breakdown of rock and minerals through biological processes such as the action of plants, animals, and microorganisms. This type of weathering can occur through processes like root growth, burrowing, and the release of acids by organisms, leading to the decomposition of rocks over time.
Fossils are the preserved remains or traces of plants and animals that lived in the past. Through a process called petrification, minerals replace the organic material in the remains, turning them into rock-like structures over time.
aciod
The type of rock that forms where the remains of plants and animals are deposited in thick layers are called organic sedimentary rock.
Animals can break down rock material through physical weathering, such as digging, scratching, or burrowing. Plants can break down rock material through root growth, where roots penetrate cracks and crevices in rocks, causing them to break apart over time. Both processes contribute to the breakdown of rocks into smaller particles through mechanical means.
Plants weather rocks through root growth, where roots penetrate cracks in the rock causing physical weathering. Animals can weather rocks through activities like burrowing and digging, which can break apart rocks over time through mechanical weathering. Additionally, animal waste can contribute to chemical weathering by altering the composition of the rock.
The type of weathering that includes the effects of animals and plants on the landscape is called biological weathering. This process occurs when living organisms contribute to the breakdown of rocks and minerals through physical actions, such as root expansion or burrowing, as well as through chemical processes, like the release of organic acids. Plants can penetrate rock crevices and, over time, contribute to their disintegration, while animals can disturb soil and rock, facilitating further weathering. Together, these biological activities play a significant role in shaping the Earth's surface.
The rock is called coal.
Fossils is the word