soil erosion
Chat with our AI personalities
Soil can be transported by water, wind, ice, or gravity. Water can carry soil particles in rivers or streams, causing erosion and deposition in new locations. Wind can also pick up and move soil particles, especially in arid or exposed areas. Ice can transport soil through processes like glacial movement or frost heave. Gravity can cause soil to move downhill in mass wasting events like landslides.
Transported soil refers to soil that has been moved from its original location by natural processes like wind, water, or ice. This soil may be deposited in different layers or locations, carrying nutrients and minerals with it. Transported soil can have different characteristics compared to the local soil, depending on its origin and the process of transportation.
Soil that has been moved away from its parent bedrock is called transported soil. This can happen through processes like erosion, weathering, or human activities like construction or agriculture. Transported soil can differ in composition and characteristics from in situ soil.
transported soil....:-)
Transported soil is soil that has been moved from its original location by natural forces such as wind, water, ice, or gravity. This can result in soil deposits with different characteristics and compositions compared to the original soil source. Transported soil plays an important role in shaping landscapes and ecosystems.
Residual soil is formed in situ by weathering of the underlying bedrock, retaining characteristics of the parent material. Transported soil is moved away from its source by erosion or deposition processes, often by wind, water, or ice. Residual soil is typically found in the same location as the parent rock, while transported soil can be found far from its original source.