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The contracts to explore for manganese nodules are typically for areas up to 75,000 square kilometres (29,000 sq mi), but the total area affected by the extractions is much greater. The extent of physically disturbed seabed area in one mine contract area only can be assumed to be between 200 and 600 square kilometres (77 and 232 sq mi) each ...
The CCZ is regularly considered for deep-sea mining due to the abundant presence of manganese nodules. The CCZ extends around 4,500 miles (7,240 km) East to West [4] and spans approximately 4,500,000 square kilometres (1,700,000 sq mi). [5] The fractures themselves are unusually mountainous topographical features.
Polymetallic nodules on the deep seabed in the CCZ Example of manganese nodule that can be found on the sea floor. Polymetallic nodules are found at depths of 4–6 km (2.5–3.7 mi) in all major oceans, but also in shallow waters like the Baltic Sea and in freshwater lakes. [23] [24] They are the most readily minable type of deep sea ore. [25]
An abundant resource of manganese in the form of manganese nodules found on the ocean floor. [65] These nodules, which are composed of 29% manganese, [ 66 ] are located along the ocean floor . The environmental impacts of nodule collection are of interest.
Nodule is also used for widely scattered concretionary lumps of manganese, cobalt, iron, and nickel found on the floors of the world's oceans. This is especially true of manganese nodules. Manganese and phosphorite nodules form on the seafloor and are syndepositional in origin. Thus, technically speaking, they are concretions instead of nodules ...
This page was last edited on 17 December 2012, at 07:09 (UTC).; Text is available under the Creative Commons Attribution-ShareAlike 4.0 License; additional terms may apply.
The quiet CCZ, as wide as the continental U.S., is home to polymetallic nodules or trillions of potato-size lumps of matter formed over millions of years that contain nickel, manganese, copper, zinc and cobalt, as well as deep water coral, sponges and unusual species ("ghost octopus", crustaceans, worms and sea cucumbers) that in a near light ...
Marine sediment, or ocean sediment, or seafloor sediment, are deposits of insoluble particles that have accumulated on the seafloor.These particles either have their origins in soil and rocks and have been transported from the land to the sea, mainly by rivers but also by dust carried by wind and by the flow of glaciers into the sea, or they are biogenic deposits from marine organisms or from ...