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- Deep sea nodules, also called polymetallic nodules or manganese nodules, are mineral concretions on the sea bottom formed of concentric layers of iron and manganese hydroxides around a core1. They are potential sources of rare-earth and other critical elements2. Vast areas of the deep-ocean floor are covered with mineral-rich resources such as polymetallic nodules, which contain high grades of manganese, cobalt and nickel – metals required to manufacture batteries for storing renewable energy and powering electric vehicles3.Learn more:✕This summary was generated using AI based on multiple online sources. To view the original source information, use the "Learn more" links.Polymetallic nodules, also called manganese nodules, are mineral concretions on the sea bottom formed of concentric layers of iron and manganese hydroxides around a core. As nodules can be found in vast quantities, and contain valuable metals, deposits have been identified as a potential economic interest.en.wikipedia.org/wiki/Manganese_noduleThe growth of these deep-sea nodules —metallic lumps of manganese, iron, and other metals found in all the major ocean basins—is one of the slowest known geological processes. These ringed concretions, which are potential sources of rare-earth and other critical elements, grow on average just 10 to 20 millimeters every million years.phys.org/news/2020-01-nodules-bottom-sea.htmlVast areas of the deep-ocean floor are covered with mineral-rich resources such as polymetallic nodules. Lying on the seafloor unattached, these nodules contain high grades of manganese, cobalt and nickel – metals required to manufacture batteries for storing renewable energy and powering electric vehicles.allseas.com/activities/deep-seapolymetallicnodulec…
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