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Minerals Report - International Seabed Authority

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is mainly being used in the oil-based economies of Middle Eastern maritime<br />

states, desalination plants are spreading to other parts of the world. The<br />

element phosphorous is also critical to agriculture and occurs where it has<br />

precipitated from deep seawater as the mineral phosphorite at present and<br />

past locations of up welling along sections of continental shelves primarily<br />

within the trade wind belts (0 to 30 degrees North and South latitude). All<br />

phosphorite is presently mined from land deposits precipitated during higher<br />

stands of sea level in the geological past, but extensive deposits exist on<br />

continental shelves of agriculture-intensive countries like India. He<br />

demonstrated that for metals and non-metals, there are fewer than 20 sites<br />

that have been or are operational in terms of marine mining.<br />

In terms of seafloor mineralisation, he mentioned that the first<br />

discovery was in the Red Sea when in the course of a transit during the<br />

<strong>International</strong> Indian Ocean Expedition in the 1960s, echo sounders got<br />

reflections from layers within the water column that were totally anomalous.<br />

Usually, he remarked, the reflections come back from the seafloor. When<br />

sampling, it was found that the reflectors were layers of highly salty metal<br />

and rich water at certain places along the axis of the Red Sea. The Red Sea it<br />

turns out is a part of a plate boundary where the seafloor is spreading is, i.e.,<br />

moving Saudi Arabia and Africa further apart. Along its axis, hot rocks are<br />

welling up from the earth’s interior in this submerged plate boundary. The<br />

mineral deposits that are to be found in certain basins along it, came about as<br />

a result of the interaction of the hot metal enriched volcanic rocks up welling<br />

at the plate boundary, the restricted circulation of seawater that led to the<br />

deposition/precipitation of thick layers of rock salt in the basins, and down<br />

welling of cold, heavy seawater through the volcanic rocks and rock salt,<br />

forming a metal brine that is both saltier and richer in metals. While there are<br />

several deep basins are to be found in the Red Sea, the Atlantis II Deep, just<br />

west of Mecca is the largest seafloor hot spring deposit known on earth and is<br />

particularly enriched in zinc and is also known to contain silver and gold.<br />

Professor Rona noted that this process was extremely efficient for<br />

concentrating metals since the metals precipitate as particles that collect at the<br />

seafloor, and form the metalliferous sediments of the Red Sea. The latest<br />

estimate of the size of this deposit is 94 million tonnes dry weight with about<br />

2 per cent zinc. Since this deposit is to be found within the 200 n-mile zone of<br />

Saudi Arabia and Sudan, they undertook a joint survey of this deposit in 1979<br />

INTERNATIONAL SEABED AUTHORITY 17

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