It was estimated that if all the then planned
mining projects were allowed to proceed and are in operation by the
mid-Eighties that by the end of the century, several hundred thousand square
miles of the Pacific could be contaminated. Fortunately for economic and
political reasons that prediction was not realized. Yet now nearly half a
century later, that threat now has the potential to be unleashed.
I’m going to step back in time to April 1977 to Pier 32 in Honolulu where I
watched a cargo of potato sized rocks discharge from a Liberian registered
mining ship named the Sedco 445.
John L. Shaw, the President and General Manager of Ocean Management Inc.,
gave me a guided tour of the Sedco 445, the first ship to carry out a deep
sea mining operation.
The Sedco 445 had just returned for a mining site 800 to 1,000 miles
southwest of Hawaii where it had brought up a continuous stream of material
from a depth of 17,000 feet or three miles.
I picked up a rock that resembled a black potato and Mr. Shaw informed me
that each of these rocks took over 200-million years to form on the seabed
and contained up to thirty different minerals with three quarters of the
content of each nodule being nickel.
According to Shaw, the nodules formed over millions of years as falling
debris like sharks’ teeth or fish bones acting as a nuclei to gather trace
minerals. The estimate is that the nodules grow about one millimeter every
thousand years and in some areas of the benthic seabed there are billions of
these potato sized rocks and each one is teeming with minute marine
organisms.
The exploratory voyages were inspired by John L. Mero in 1965 with his
estimate of vast ferromanganese (Fe-Mn) nodules in the Pacific Ocean. He
speculated that the Pacific seabed contained a limitless supply of metals
including manganese, copper, nickel, cobalt, lithium, zinc, and molybdenum.
That was enough to make huge mining interests salivate with the
possibilities for exploitation.
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