Geology of The Pacific Ocean

Geology Of The Pacific Ocean

The Pacific Ocean evolved from the Panthalassic Ocean when Rodinia rifted apart around 750 million years ago. The first ocean floor which is part of the current Pacific Plate, began to the west of the central Pacific, subsequently developing into the largest oceanic plate on Earth.

The tectonic plates continue to move today. The slowest spreading ridge is the Gakkel Ridge on the Arctic Ocean floor which spreads at less that 2.5 cm/yr while the fastest, the East Pacific Rise near Easter Island, has a spreading rate of over 15 cm/yr.

Read more about Geology Of The Pacific Ocean:  History, Geological Origins of The Pacific Islands, Andesite Line, Earthquakes

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