Monaco Bank (volcano)

Last updated
Monaco Bank
Summit depth197 m (646 ft) [1]
Location
Location Atlantic Ocean
Coordinates 36°36′N25°53′W / 36.60°N 25.88°W / 36.60; -25.88
Country Portugal
Geology
Type Submarine volcano
Last eruption March 1911

Monaco Bank is a submarine volcano in the Azores, which last erupted in 1911.

Submarine volcano Underwater vents or fissures in the Earths surface from which magma can erupt

Submarine volcanoes are underwater vents or fissures in the Earth's surface from which magma can erupt. Many submarine volcanoes are located near areas of tectonic plate formation, known as mid-ocean ridges. The volcanoes at mid-ocean ridges alone are estimated to account for 75% of the magma output on Earth. Although most submarine volcanoes are located in the depths of seas and oceans, some also exist in shallow water, and these can discharge material into the atmosphere during an eruption. The Kolumbo submarine volcano in the Aegean Sea was discovered in 1650 when it erupted, killing 70 people on the nearby island of Santorini. The total number of submarine volcanoes is estimated to be over 1 million, of which some 75,000 rise more than 1 km above the seabed.

Azores Portuguese archipelago in the North Atlantic Ocean

The Azores, officially the Autonomous Region of the Azores, is one of the two autonomous regions of Portugal. It is an archipelago composed of nine volcanic islands in the North Atlantic Ocean about 1,360 km (850 mi) west of continental Portugal, about 1,500 km (930 mi) west of Lisbon, in continental Portugal, about 1,500 km (930 mi) northwest of Morocco, and about 2,500 km (1,600 mi) southeast of Newfoundland, Canada.

See also

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References

  1. "Monaco Bank". Global Volcanism Program . Smithsonian Institution . Retrieved 2018-01-05.