The seabed - an important mineral resource of Slovakia in the future

• Main Authors: Peter Blišťan, Branislav Kršák, Monika Blišťanová, Vojtech Ferencz
• Format: Article in Journal/Newspaper
• Language: English; Slovak
• Published: Technical University of Kosice 2015
• Subjects: Deep Seabed Mineral Resources; Polymetallic Nodules; Interoceanmetal IOM; Clarion-Clipperton Zone; Slovakia; Mining engineering. Metallurgy; TN1-997; Geology; QE1-996.5; Antarc*; Antarctica
• Online Access: https://doi.org/10.3390/ams20040334; https://doaj.org/article/cc2512559a7445d3acef509c42d1437d

In 1987, Slovakia bought part of the ocean bottom with the occurrence of mineral resources future - polymetallic nodules. The polymetallic nodule is a geological term for naming natural features consisting of more than 40 metals and other chemical elements. These special services originated in the ocean for two to three million years and nowadays, they are of main interest for countries whose mineral wealth is little or no available. Nodules contain about 30 % manganese, 1.2 % copper, 1.2 % nickel, 0.2 % cobalt, rare earth elements, etc. The existence of submarine nodules was found by the British ship HMS "Challenger" by oceanographic research in 1872 - 1876. Research and the subsequent mining of nodules were particularly points of interest for Western countries as well as the USSR. Rules for the use of mineral resources of the seabed beyond the limits of national jurisdiction were codified in the Convention on the Law of 1982, which came into force on 16.11.1994, and in the Slovakia on 21.7.1996. The seabed is one of the international space next to the high seas, Antarctica, outer space and celestial bodies, which are not subject to the sovereignty of any state authority.