magnanese
Nodules...
it is either apatite, kimberlite magma precipitation minerals calcite or mica
Manganese Nodules.
Manganese Nodules.
Hydrogenetic manganese nodules form over millions of years through the precipitation of metals out of seawater onto small particles or other nodules on the ocean floor. Manganese and other metals accumulate on the nodules as a result of chemical reactions driven by the presence of hydrogen in the deep-sea environment. These nodules grow at very slow rates, about 1-10 millimeters per million years.
Manganese nodules do not directly affect the salinity of ocean water. Salinity is primarily influenced by factors such as evaporation, precipitation, and inputs from rivers and hydrothermal vents. While manganese nodules can impact the distribution of minerals in the ocean floor, they do not play a significant role in altering the overall salinity of the water.
Manganese nodules are an example of hydrogenous sediment, which forms directly from ocean water through chemical precipitation. They are typically found on the deep ocean floor.
Five minerals that may be found in nodules are manganese, iron, cobalt, copper, and nickel. These minerals are commonly found in nodules formed on the ocean floor.
A possible future source of minerals in ocean basins is polymetallic nodules, which are found on the seafloor and contain valuable metals like nickel, copper, cobalt, and rare earth elements. These nodules form over millions of years and are abundant in certain regions, such as the Clarion-Clipperton Zone in the Pacific Ocean. As land-based mineral resources become depleted, deep-sea mining may become more attractive, leading to increased interest in harvesting these nodules. However, this raises environmental concerns regarding the impact on marine ecosystems.
Mineral nodules on the ocean floor are considered a nonrenewable resource because their formation takes millions of years through geological processes, making them extremely slow to replenish. Once harvested, the extraction of these nodules can deplete the resource significantly, as they do not regenerate at a rate that can keep up with human consumption. Furthermore, the environmental impact of mining these nodules can lead to irreversible damage to marine ecosystems, further emphasizing their nonrenewable nature.
An example of authigenic sediment is manganese nodules, which form on the seafloor as a result of chemical precipitation of manganese and iron oxides. These nodules slowly grow over time by accumulating layers of material from seawater.
Nodules of manganese are commonly found on the ocean floor.