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Minerals Report - International Seabed Authority

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Focussing on sites of sea floor mineralisation that have been<br />

discovered, Dr. Rona informed participants that the first discovery came by<br />

chance in the 1960s in the Red Sea at the same time of the development of the<br />

theory of plate tectonics. Professor Rona described an international Indian<br />

Ocean expedition, during which various ships that were transiting through<br />

the Red Sea coming to and from the Indian Ocean, ran the echo sounders on<br />

their ships in the course of transits, and got reflections from layers within the<br />

water column that were totally anomalous. He pointed out that usually the<br />

reflections from the echo sounders come back from the sea floor. When<br />

samples were taken in the area, it was found that the reflect surfaces were<br />

layers of highly salty metal and rich water at certain places along the axis of<br />

the Red Sea. Dr. Rona explained that the Red Sea is a part of a plate boundary<br />

where sea floor spreading is occurring, i.e. carrying Saudi Arabia and Africa<br />

apart at a slow rate of centimetres per year. Professor Rona further explained<br />

that Saudi Arabia and Africa are about 200 kilometres apart at this time.<br />

Along the axis of the Red Sea where the hot rocks are welling up from the<br />

earth's interior in this submerged plate boundary, there are several deep<br />

basins from which hot springs are welling up from the sea floor. The largest of<br />

these basins is the Atlantis II Deep he pointed out, just west of the sacred city<br />

of Mecca.<br />

Professor Rona remarked that the thick layers of rock salt, formed at a<br />

time when the Red Sea’s circulation was restricted by surrounding<br />

landmasses, represented a special phenomenon. He noted that at that time<br />

there was more inflow and evaporation than inflow. He briefly reviewed the<br />

history of the formation of these deposits; namely the penetration of cold,<br />

heavy seawater into the lithosphere, the subsequent dissolution of metals and<br />

salts into this heavy seawater as it passes through volcanic rocks, the heating<br />

of this body of water by the hot rocks and the up welling of it beneath the axis<br />

of the Red Sea, and its final discharge as a metal rich brine that is heavier than<br />

surrounding seawater. Dr. Rona described this process of concentration of<br />

metals as a most efficient one. He noted that the Red Sea brines deposit is the<br />

largest seafloor hot spring deposit known on earth at this time. With regard<br />

to the resource evaluation of the metals to be found in the Atlantis II Deep,<br />

Professor Rona informed participants that the volume of brines had been<br />

estimated at 94 million tonnes dry weight containing 2 percent zinc and 0.5<br />

INTERNATIONAL SEABED AUTHORITY 96

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