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New Technology for New Exploration of Hydrothermal Vents

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Alvin samples a black smoker
Courtesy Rob Reves-Sohn,? Woods Hole Oceanographic Institution
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TAG Tour

Jack Cook,? Woods Hole Oceanographic Institution
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» TAG Vent Field

Shelley Dawicki

December 5, 2005

Source: Media Relations


Advances in undersea imaging systems, the development of new vehicles and instruments, and improved seafloor mapping capabilities have enabled scientists to explore areas of the deep sea in unprecedented detail.  One such area is the TAG hydrothermal mound in the North Atlantic Ocean, one of the largest known mineral deposits on the seafloor.

Rob Reves-Sohn , a geologist at Woods Hole Oceanographic Institution (WHOI), will discuss some of the technological advances and present some recent imagery collected at the TAG  hydrothermal vent during a  press conference today at the American Geophysical Union meeting in San Francisco. TAG, for Trans Atlantic Geotraverse, is on the Mid-Atlantic Ridge about 1,900 miles east of Miami at 26°8'N and 44°49'W more than two miles below the ocean's surface.

Since hydrothermal vents were discovered in 1977 on the Galapagos Rift in the eastern Pacific Ocean, vent sites have been found on the mid-ocean ridge around the world.  New sites are found each year, each with unique animal communities and geological/geochemical features. TAG was among the first to be found in the North Atlantic 20 years ago.  
    
Using two-dimensional maps produced from data collected by a research vessel, Reves-Sohn and colleagues produced computer animations of the TAG site, enabling scientists to view it from different perspectives.  Images of the mound and smokers were taken by cameras mounted on the three-person submersible Alvin, operated by WHOI for the American ocean research community.

For centuries, people have mined copper, gold and precious metals on land from mineral deposits that many believe formed on the ocean floor.  At the TAG vent site, a superheated mixture of seawater and toxic chemicals hot enough to melt lead billows out of the seafloor. This fluid, driven by heat from molten magma deep below the earth's crust, erupts into clouds or plumes that rise nearly 1,000 feet above the ocean bottom. Chemical reactions occurring as this hot fluid mixes with cold seawater cause the formation of chimney-like structures called "black smokers." These freestanding chimneys, which commonly reach heights of 100 feet or more, contain minerals similar to those mined on land.

AGU Press Conference:  Monday, December 5 MC Level 2, Room 2012 3 p.m. PST
Diversity of Hydrothermal Systems at Slow Spreading Ocean Ridges

Related AGU Session:  OS33A-1466 New Constraints on the Thermal Power of the TAG Hydrothermal System and the Dynamics of the Water Column Plume




Originally published: December 5, 2005

Last updated: May 23, 2008
 


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