Yes, it is possible to estimate how much material was eroded away using methods such as sediment sampling, topographic surveys, and historical data comparison. By measuring changes in landscape features, analyzing sediment deposits in nearby bodies of water, and utilizing techniques like LiDAR for precise topographic mapping, researchers can quantify erosion rates. Additionally, modeling approaches can help estimate the volume of eroded material over time, providing a clearer picture of erosion processes and their impacts.
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it drowns.
Deflation
The depositing or placing of eroded material is called sedimentation. This process occurs when eroded particles settle and accumulate in a new location, often leading to the formation of sedimentary rocks over time.
Igneous Rock
The eroded material from the shield was deposited on the continental margins, where it accumulated and formed sedimentary rocks over time due to compaction and cementation. This material became part of the geological record and can contain important information about Earth's history and past environments.
The harder a material is, the less it will be eroded by mechanic forces like wind and water. Eroded material from one place can also gather another place and form a protective layer.
As a mountain is eroded, the mountain root (the deep-seated portion of the mountain that stabilizes it) may become exposed or covered by eroded material. The root may also be weakened or eroded, contributing to the overall erosion of the mountain.
The eroded particles may be carried by water, wind or ice to other locations like the lowland regions or into the ocean and lakes.The eroded materials build up and under their own pressure gradually become hardened into sedimentary rock.
Erosion, transportation of the eroded material, deposition of this material then lithification.
Erosion, transportation of the eroded material, deposition of this material then lithification.
Depends what the agents of erosion are. For example: If it was ice, the area would be scoured clean. If it were water or wind, the eroded material may have been carried off, leaving only the eroded surface.