Asian Journal of Plant Science & Research

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Coastal Geography

The coastal backward can be measured and explained by the temporal extent of the waves, the seasons, and other temporal processes of speed. Coastal erosion can be caused by the action of hydraulic, abrasion, impact and corrosion of air and water, and other forces, natural or non-natural. The soft surfaces are broken down much faster than the hard ones, which often lead to global changes such as tunnels, bridges, columns and columns. Over time the coast tends to come out. The soft surfaces are filled with exposed mud on hard surfaces, and rock formation is removed. And abrasion tends to occur in areas with strong winds, loose sand, and soft rocks. The striking of millions of sharp grain of sand creates the effect of sand. This effect helps to turn rocks, smooth and polish. Coastal erosion is the loss or evacuation of land, or the temporary removal of rocks and rocks of the coastline due to the action of waves, currents, currents, storm water, storm water, or other storm effects.

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