stratification
Sedimentary rocks with rounded grains typically form from materials that have been transported over long distances by wind, water, or ice, which causes abrasion and rounding of the grains. In contrast, sedimentary rocks with angular grains often form from materials that have not been transported far and have not undergone as much abrasion. Factors like the energy of the transporting agent and the distance traveled can influence the roundness of the grains in sedimentary rocks.
They are called clastic sedimentary rocks.
Stratification as this is a term that describes the layering of rocks and so is not a term that is related to sediment transport (i.e. erosion) but is instead the result of deposition, compaction and cementation.
Ironstone sedimentary rock forms when iron-rich minerals oxidize in a marine or lacustrine environment, producing iron oxide deposits. Over time, these deposits accumulate and harden into ironstone through compaction and cementation processes. Water plays a crucial role in transporting the iron minerals and aiding in the formation of ironstone.
It is then sedimentary rock.
Wind is not a sediment transporting agent.
Air is primary agent
Transported sediments are usually deposited at locations where the transporting medium's energy decreases, such as river deltas, beaches, and the mouths of rivers. The sediment settles out of the transporting medium and accumulates to form sedimentary deposits.
water
Air is not a sediment transporting agent. Sediment transporting agents typically involve water (such as rivers and oceans), ice (glaciers), or wind. Air can carry dust particles, but it does not transport larger sediment particles like water or ice.
a transporting agent, such as water must be present
Sedimentary rocks with rounded grains typically form from materials that have been transported over long distances by wind, water, or ice, which causes abrasion and rounding of the grains. In contrast, sedimentary rocks with angular grains often form from materials that have not been transported far and have not undergone as much abrasion. Factors like the energy of the transporting agent and the distance traveled can influence the roundness of the grains in sedimentary rocks.
only when the fluid transporting the sediments slows down or when glacial ice melts
Water chemically and mechanically weathers sedimentary rocks. It also weathers and erodes all rock types, transporting and depositing the sediments, a step in the formation of sedimentary rock.
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The dropping or settling of eroded materials is called deposition. This process occurs when the energy of the transporting agent (such as water or wind) decreases, causing it to drop the sediment it was carrying and build up sedimentary layers in new locations.
Once it is able to move, displace and change position of light materials and particles of matter it can carry... then, it is definitely an agent of sediment transportation.