During transport, the physical characteristics of sediments change due to processes like abrasion, sorting, and compaction. As sediments are moved by water, wind, or ice, they tend to become smaller and rounder as edges are worn down. Sorting occurs as sediments are separated by size and weight, often leading to a more uniform grain size in the deposit. Additionally, compaction can increase density and alter the arrangement of particles as sediments settle in new environments.
Copyright © 2026 eLLeNow.com All Rights Reserved.