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Mid- Atlantic Ridge is in which ocean?
A.The Pacific Ocean
B.The Indian Ocean
C.The Atlantic Ocean
D.The Southern Ocean

Answer
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Hint: The Mid-Atlantic Ridge is in effect an enormously lengthy peak row stretching for approximately 10,000miles in a curving aisle from the Arctic Ocean to near the southern tip of Africa. The ridge is midway between the landmasses on either wall of it. The cliffs constructing the hill attain a width of 1,000miles These peaks periodically rise above sea level, accordingly shaping the islands or island coalitions of the Azores, and Tristan da Cunha, Ascension, St. Helena among others.

Complete answer:
We have to remember that the Mid-Atlantic Ridge, torpedo ridge lying along the north-south axis of the Atlantic sea; it dwells the prominent part of the gulf between a sequel of horizontal abyssal plains that proceed to the perimeters of the continental shores.
The Mid Atlantic Ridge, like distinct ocean ridge networks, has expanded as a fallout of the divergent movement between the Eurasian and North American, and African and South American Plates. As the mantle surges towards the exterior below the cliff the burden is bowed (decompression) and the hot gravel begins to partially dissolve. This elicits basaltic volcanoes when an outburst occurs above the covering and specific basalt “pillow lava” in aquatic explosions. In this manner, as the panes shift distant apart a new sea lithosphere is cropped up at the cliff and the ocean basin gets broader. This procedure is understood as “seafloor spreading” and impacts in a proportional alignment of the stones of the ocean bed which get aged with distance from the cliff height.

Hence, the correct answer is option (C).

Note:We have to know that the North American and Eurasian Sheets are strolling off from each other through the caravan of the Mid Atlantic Ridge. The Ridge enlarges into the South Atlantic Ocean between the South American and African Plates. The ocean ridge soars to between 2 to 3 km above the brine bottom. It has a rift valley at its crest imprinting the site at which the two layers are changing positions apart.