Undersea Volcanoes
Naval Meterological and Oceanography Command
03.19.01

It was one of the most spectacular natural occurrences in recent history. Thick, black smoke billowed miles into the sky. Scorching, red lava oozed from a turbulent sea. Molten lava hardened into pumice and cinder, and scientists declared that a modern-day miracle had occurred. In 1963, the island of Surtsey emerged near Iceland from a spot 425 feet below the ocean surface. 
 
Millions of years ago, this miracle was common place as hundreds of volcanic islands, such as the Hawaiian Island chain, were born in oceans throughout the world. Undersea volcanoes are still found in all the oceans with approximately 10,000 of them on the floor of the Pacific Ocean. 
 
Like their counterparts on land, underwater volcanoes are usually cone-shaped. They are frequently grouped together in circles or in long chains known as "rings of fire". 
 
Volcanoes alternate active periods which can last for millions of years with long dormant phases. During active periods, the lava cone builds up and eventually explodes onto the ocean floor as molten rock. The lava solidifies and turns into volcanic rock. 
 
These volcanoes are enormous. Hawaii, the largest mountain on earth, has a relief of 32,024 feet above its base - over 3,000 feet higher than Mt. Everest. 
 
Cone erosion at sea level is the cause of the flat-topped undersea volcanoes known as guyots. Commonly found in the South Pacific, these volcanoes sank, sometimes completely, because the sea floor could no longer support their enormous weight. In some cases, fringing reefs continued to grow upward as the volcano sank, so that all that remained was an atoll - coral islands surrounding a lagoon. 








Naval Meterological and Oceanography Command 
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1100 Balch Boulevard 
Stennis Space Center, Mississippi 39529




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