Hydrothermal vents that appear to be producing rare metals found off Okinawa
 
 Mineral clusters projecting from the seabed. (Photo courtesy of the University of Tokyo)
(Mainichi Japan) September 19, 2010
A few active hydrothermal areas found at the bottom of the sea off  the coast of Okinawa Prefecture appear to be producing rare earth  metals, which will likely draw interest to the area as a potential  underwater mine.
The discovery was made by a team of researchers from the University  of Tokyo and other institutes. On Sept. 17, they announced that they had  discovered three areas with hydrothermal eruptions at the bottom of the  ocean about 100 kilometers northwest of the main island of Okinawa. The  team had used an unmanned probe equipped with sensors they developed  that can detect manganese and hydrogen sulfide contained in hot water  released from vents, and over an eight-day period beginning on Sept. 4  used the probe to search an underwater area full of volcanic craters.
In their exploration, the team found three areas at depths of around  500 to 600 meters where water from 43 to 247 degrees centigrade was  erupting. In one of the areas, there were chimney-shaped clusters --  about 50 centimeters in diameter and one to two meters in height -- on  the seabed, which were emitting 121-degree water from their tips. The  clusters are believed to consist of rare earth elements, such as  manganese and antimony.
Such active hydrothermal metal deposits have recently been drawing  researchers' attention as potential mines, spurring them to conduct  explorations for them in the seas around Japan. The team has already  collected the mineral clusters and plans to analyze the types and  content of the metals contained in them.
(Mainichi Japan) September 19, 2010
 
 
 
No comments:
Post a Comment