A metal-enriched seawater plume entering the western Mediterranean Sea
through the Strait of Gibraltar originates 300 km to the west in the
Rio Tinto estuary of southwestern Spain, Mining of Rio Tinto ore, one
of the largest metal-rich sulfide deposits in the world, started well
before Roman times, Contemporary Rio Tinto waters draining the region
are highly acidic (pH 2.5) with dissolved cadmium, zinc, and copper co
ncentrations 10(5)-10(6) times higher than in uncontaminated surface w
ater of the Gulf of Cadiz, Two dated sediment cores from the Spanish c
ontinental shelf show that metal inputs to the region increased with t
he onset of intensive mining activities during the second half of the
19th century, Although the impact of mining may have decreased over th
e past few decades, the Tinto river and estuary remain highly contamin
ated.