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Both deltas and alluvial fans are types of depositional land forms formed by flowing rivers. Alluvial fans are formed at foothills where streams flowing from higher level break into foot slope plains of low gradient whereas deltas are formed near mouth of streams where it meets seas or stagnant water bodies.
The two land forms also differ in terms of characteristics of their deposits. Alluvial fans are generally composed of coarse sediments which are not distinguishingly stratified whereas deltas are generally formed by fine deposits.
Factors responsible for formation of alluvial fans:
Factors responsible for formation of deltas:
Economic significance of alluvial fans:
Economic significance of deltas:
By: ABHISHEK KUMAR GARG ProfileResourcesReport error
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