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    Atlantic online dating article

    In this article, however, the Arctic Ocean is considered a separate entity. Perhaps a more appropriate method for determining this boundary is by following the division between the distinctive Arctic and Atlantic water masses: the relatively warm and saline waters of the , an immense median mountain range extending throughout the length of the Atlantic, claiming the centre third of the ocean bed, and reaching roughly 1,000 miles (1,600 km) in breadth.This feature, though of tremendous proportions, is but the Atlantic portion of the world-encircling .

    Consequent movement of the ocean floor and of the continents in opposite directions outward from the ridge is widening the Atlantic basin at an estimated rate of about 0.4 inch (1 cm) to a maximum of about 4 inches (10 cm) per year.As the continents are approached and the rugged Mid-Atlantic Ridge is left behind, an abyssal plain first is encountered, followed by the smooth, undulating surface of the continental rise.These broad embankments, which lie at depths of some 8,000 to 15,000 feet (2,400 to 4,500 metres) at the foot of continents, reach more than 300 miles (500 km) in width off northwestern Africa, , and riverine sediment deposition have contributed to creating the sloping continental rises that are characteristic of the Atlantic basin.A high heat flow, which is associated with the extrusion of magma and with , exists in the rift zone.The crustal material on either side of the ridge is notably younger than that on the corresponding plateaus, indicating an uprising of material from Earth’s mantle onto the crest of the ridge.

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