Submarine Volcanoes

Submarine volcanoes and volcanic vents are common features on certain zones of the ocean floor.

Some are active at the present time and, in shallow water, disclose their presence by blasting steam and rock-debris high above the surface of the sea.

Many others lie at such great depths that the tremendous weight of the water above them results in high, confining pressure and prevents the formation and explosive release of steam and gases.

Even very large, deepwater eruptions may not disturb the ocean surface.

The unlimited supply of water surrounding submarine volcanoes can cause them to behave differently from volcanoes on land.

Violent, steam-blast eruptions take place when seawater pours into active shallow submarine vents.

Lava, erupting onto a shallow sea floor or flowing into the sea from land, may cool so rapidly that it shatters into sand and rubble.

The result is the production of huge amounts of fragmental volcanic debris.

The famous "black sand" beaches of Hawaii were created virtually instantaneously by the violent interaction between hot lava and seawater. Loihi Submarine Volcano - the most recent expression of the hotspot that produces the Hawaiian Island chain - NOAA

On the other hand, recent observations made from deep-diving submersibles have shown that some submarine eruptions produce flows and other volcanic structures remarkable similar to those formed on land.

During an explosive submarine eruption in the shallow open ocean, enormous piles of debris are built up around the active volcanic vent.

Ocean currents rework the debris in shallow water, while other debris slumps from the upper part of the cone and flows into deep water along the sea floor.

Fine debris and ash in the eruptive plume are scattered over a wide area in airborne clouds.

Coarse debris in the same eruptive plume rains into the sea and settles on the flanks of the cone.

Pumice from the eruption floats on the water and drifts with the ocean currents over a large area.


Submarine Volcanoes


Mount Marsili

Europe's largest underwater volcano is active according to the scientists who have been monitoring it for years, but until recently believed it to be dormant. There has never been an eruption of the volcano in recorded history. The Tyrrhenian Project, the national research group studying the volcano, reported its findings last November 27, 1999.

Mt. Marsili, which rises 9,800 feet (3,000 meters) from the seabed in the Tyrrhenian Sea southwest of Naples, is capable of producing huge tidal waves along southern Italy if its activity ever does build to an eruption. According to the researchers, "Il Marsili'" is about 40 miles (65 km) long and 25 miles (40 km) wide. The experts said its tip was only 1,640 feet (500 metres) below the surface of the water.

Michael Marani, the scientist heading up the study of the volcano, said, "Because the Tyrrhenian Sea is the youngest sea in the Mediterranean, it is still unstable and carries elevated risks that must be monitored and understood." He reported that evidence of enormous masses which had probably broken away from the main crater a long time ago were found on the volcanic edge.


In the News ...

Sicily - Volcano larger than Washington, D.C., discovered CNN - June 23, 2006

Underwater Volcano Erupts on Video National Geographic - May 25, 2006
A volcano is seen erupting 1,800 feet beneath the surface of the Pacific Ocean near Guam.

Unraveling the Mysteries of Underwater Volcanoes NOAA - August 21, 2001



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