Sediments that are loosely packed, fine-grained, or located in areas with high water flow or wave action are more likely to be eroded. Additionally, sediments that have been disturbed by human activities or natural processes like intense rainfall or ice melt can also be easily eroded.
hydrates
sedimentation
Yes, that is true. Moraines are piles of eroded sediments that are pushed in front of a glacier as it moves, either as a result of the glacier plucking rocks and debris as it moves or as it deposits material carried by the ice.
Erosion transports sediments from the original source through processes like wind, water, or ice. As the sediments are eroded, they are carried away and eventually deposited in a new location, forming sedimentary deposits.
When metamorphic rock is weathered and eroded, it breaks down into sediments. These sediments can then be transported and eventually compacted and cemented together to form sedimentary rock. The process involves the physical and chemical breakdown of the metamorphic material, leading to the creation of new rock types through sedimentary processes.
Most rivers have eroded and Deposited sediment.
Sedimentation
Sediments
Sediments eroded from mountainsides and transported in streams are an example of the conservation of mass. The total amount of sediment that is eroded from the mountainside remains constant as it is transported by streams to other locations.
Sediment
Approximately 15-20% of sediments eroded from the continents reach beyond coastal regions to the continental shelf and slope. The majority of eroded sediments tend to accumulate and deposit near the coast due to factors such as wave action and currents.
Eroded materials carried by wind or water are called sediment.
hydrates
When sedimentary rocks are weathered and eroded, they turn into sediments. And after compaction and cementation of the sediments, it will turn back into sedimentary rock.
sedimentation
hydrates
Materials eroded from the Abilene area would most likely be deposited downstream in rivers and streams as they flow towards larger bodies of water like lakes or the Gulf of Mexico. These sediments can accumulate in channels, riverbanks, delta regions, or in the floodplains of rivers and streams.