The East and Gulf Coasts are submerged and therefore depositional, but the West Coast is emergent and consequently erosive. When contrasting the east and west coasts of the United States, there are numerous different elements to take into account.
<h3>
Compare and contrast the features of the east and west coasts of the United States?</h3>
The west coast is mostly an emergent coastline, whilst the east coast is primarily a submerging coastline. This is one way that the two differ from one another. Wave-cut cliffs and platforms above sea level, which are regularly seen in California, are indicators of emerging coastlines. On the other hand, submerged coastlines are identified by drowned river mouths and other submergence indicators typically found in Maine. Even if these are the 're center' histories, both coasts have undoubtedly undergone numerous periods of emergence and submergence.
While depositional coasts are characterized by significant long-term sediment buildup, erosional coasts are those with little to no sediment. Each of these coastal kinds may experience variations in both time and place. Usually, erosive beaches have considerable relief and steep terrain.
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What erosional and depositional features are more common on each coastline?</h3>
Depositional Feature:
Depositional landforms are the physical manifestation of processes that deposit rocks or sediments after they have been carried there by gravity, wind, or flowing water. Beaches, deltas, glacial moraines, sand dunes, and salt domes are a few examples.
Erosional Feature:
Erosional landforms are any of the various landforms that have been produced on the earth's surface as a result of erosion. Erosion-related landforms include valleys, potholes, river terraces, and embedded Meanders.
Erosional features, such as valleys, are those that remain after sediment has been removed. River deltas and other depositional landforms are created from sediments that are transported from their eroding source and dropped.
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