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Minerals Report - International Seabed Authority

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SUMMARY OF THE PRESENTATION AND DISCUSSIONS ON SEAFLOOR<br />

MASSIVE SULPHIDES DEPOSITS AND THEIR RESOURCE POTENTIAL<br />

Presentation<br />

Professor Peter Herzig, of the Lehrstuhl fur Lagerstattenlehre Institut<br />

fur Mineralogie based in Freiberg/Sachsen, Germany, noted at the beginning<br />

of his presentation that it would overlap in part with Professor Rona’s<br />

presentation, and that his presentation on “Seaflloor massive sulphides<br />

deposits and their resource potential” would reflect the point of view of an<br />

Economic Geologist. He also informed participants that prior to his fifteen<br />

years of experience on seafloor massive sulphides deposits he was a geologist<br />

that specialized in land-based massive sulphides deposits.<br />

Utilizing slides, Professor Herzig reiterated some of the points made<br />

by Professor Rona, showing, inter alia, the principal morphological features of<br />

the modern seafloor: the deep ocean basins with water depths in excess of<br />

5,000m and the occurrence of manganese nodules; sea mount areas of the<br />

Pacific and the occurrence of cobalt-rich manganese crusts deposits, and the<br />

mid-ocean ridge system, comprised of the Mid-Atlantic Ridge, the Red Sea,<br />

the Carlsberg Ridge, the Central Indian Ridge, the Southwest and Southeast<br />

Indian Ridges the East Pacific Rise, the Southeast Pacific Rise and the<br />

Northeast Pacific Rise.<br />

With regard to the mid-ocean ridge system, Professor Herzig noted<br />

that these ridges are to be found across all the major spreading centres of the<br />

world’s oceans, and that with a total length of 55,000 km, the ridge system is<br />

an important morphological feature of the seafloor. He further noted that<br />

ridges also define boundaries, places where new oceanic crusts are being<br />

continuously formed<br />

In relation to crust formation, Professor Herzig informed participants<br />

that rates differed in different parts of the ocean. For example, he noted that<br />

the Mid-Atlantic Ridge is a slow spreading ridge with a spreading rate of only<br />

a few centimetres per year, while the East Pacific Rise, in particular in it’s<br />

INTERNATIONAL SEABED AUTHORITY 145

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