Costal Features Along Maracas Bay

Tides often determine the range over which depository is deposited or eroded. Areas with high tidal ranges conquer waves to reach farther up the shore, and areas with lower tidal ranges produce deprossosition at a smaller line of longitude interval. The tidal range is influenced by the size and frame of the coastline. Tides do not typically cause corroding by themselves however, tidal bores can erode as the waves surge up river estuaries from the ocean. 3 Waves erode coastline as they mince on shore releasing their energy the big the wave the more energy it releases and the more sediment it moves.Coastlines with longer shores have more room for the waves to send their energy, while coasts with cliffs and short shore faces give trivial room for the wave energy to be dispersed. In these areas the wave energy disruption against the cliffs is higher, and air and pee are compressed into cracks in the rock, forcing the rock apart, breaking it down. deposition deposited by wave s comes from eroded cliff faces and is go along the coastline by the waves. This forms an abrasion or cliffed coast. Sediment deposited by rivers is the dominant influence on the number of sediment located on a coastline. 4 nowadays riverine deposition at the coast is often impede by dams and other human regulatory devices, which call back the sediment from the stream by causing it to be deposited inland. Like the ocean which shapes them, coasts are a projectile environment with constant change. The Earths natural processes, particularly sea level rises, waves and various weather phenomena, have resulted in the erosion, accretion and reshaping of coasts as well as fill and creation of continental shelves and drowned river valleys