Submarine volcano

[1] 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 presence of water can greatly alter the characteristics of a volcanic eruption and the explosions of underwater volcanoes in comparison to those on land.

Using Remote Operated Vehicles (ROV), scientists studied underwater eruptions, ponds of molten sulfur, black smoker chimneys and even marine life adapted to this deep, hot environment.

[6] Subsequent scientific investigations revealed the pumice raft originated from the eruption of a nearby submarine volcano, which was directly observed as a volcanic plume in satellite images.

[7] This discovery will help scientists better predict for the precursors of a submarine eruption, such as low-frequency earthquakes or hydrophone data, using machine learning.

Using this method to be able to distinguish the two can help measure the related affects on marine animals and ecosystems, the volume and composition of the lava flow can also be estimated and built into a model to extrapolate potential effects.

In 2009, a video camera and a hydrophone were floating 1,200 metres (3,900 ft) below sea level in the Pacific Ocean near Samoa, watching and listening as the West Mata Volcano erupted in several ways.

Scheme of a submarine eruption.
  1. Water vapor cloud
  2. Water
  3. Stratum
  4. Lava flow
  5. Magma conduit
  6. Magma chamber
  7. Dike
  8. Pillow lava
Pillow lava formed by a submarine volcano
NOAA exploration video showing remnants of underwater tar volcanoes.
Circular plumes from a submarine eruption near Tonga
Deepest ever filmed submarine volcano, West Mata , May 2009. [ 9 ]