Macquarie Island is an oceanic island in the Southern Ocean, lying 1,500 km south-east of Tasmania and approximately halfway between Australia and the Antarctic continent. The island is the exposed crest of the undersea Macquarie Ridge, raised to its present position where the Indo-Australian tectonic plate meets the Pacific plate. It is a site of major geo-conservation significance, being the only place where rocks from the Earth's mantle (6 km below the ocean floor) are being actively exposed above sea level.

Continent: Oceania
Country: Australia
Category: Natural
Criterion: (VII)(VIII)
Date of Inscription: 1997
Oceanic Crust and Rocks
It is the only island in the world composed entirely of oceanic crust and rocks from the Earth's mantle deep below the surface. Macquarie Island probably began as a spreading ridge under the sea with the formation of new oceanic crust somewhere between 11 million and 30 million years ago.At some stage the spreading halted and the crust began to compress, squeezing rocks upward from deep within the mantle. As the ridge grew it eventually became exposed above the ocean surface about 600,000 years ago. Thus, rocks normally only occurring deep within the Earth's mantle have become exposed on the surface.
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Macquarie Island Australia |
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