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carbonate to form their shells. With the warming of the oceans and subsequent melting of glaciers and the polar ice caps , increasingly contemporary water is released into the excessive latitude areas where deep water is fashioned.
25 Driven by this sinking and the upwelling that occurs in decrease latitudes, in addition to the driving pressure of the winds on surface water, the ocean currents act to flow into water throughout the entire sea. Alongside the Pacific coast, probably the most susceptible areas are low-lying beaches, and their susceptibility is primarily a operate of geomorphology and coastal