Newly formed sediments are transported to new locations primarily through natural processes such as water, wind, and ice. Water, in the form of rivers and streams, can carry sediments downstream, while waves and currents in oceans and lakes can redistribute them along Coastlines. Wind can lift and move fine particles over long distances, especially in arid regions. Additionally, glaciers can transport sediments as they advance and retreat, depositing them in new areas as they melt.
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