Manganese crust is a type of geological formation found on the ocean floor. The word is spelled as /ˈmæŋɡəniːz krʌst/ in the International Phonetic Alphabet. The first part of the word is pronounced with a nasal "ng" sound, followed by the short "a" vowel sound, and a hard "g". The second word "crust" is pronounced with a short "u" sound and a soft "s" at the end. Manganese crusts are valuable due to their high concentrations of manganese, iron, and other trace metals, and are being explored as a potential source of rare earth elements.
Manganese crust is a term used in geological and oceanographic studies to describe a type of mineral coating or encrustation found on the seafloor. It is composed mainly of manganese oxides and hydroxides, but can also contain other metals such as cobalt, nickel, and copper. These crusts typically develop in areas of slow seafloor spreading or volcanic activity, resulting in the deposition of metallic elements from seawater onto hard surfaces.
Manganese crusts form through a slow process known as precipitation, where metal-rich minerals settle out of seawater and accumulate layer by layer over long periods of time. The growth rate of manganese crusts is incredibly slow, estimated to be only a few millimeters per million years. Due to their slow growth, these crusts can reach considerable thicknesses, sometimes exceeding a meter.
Manganese crusts are highly valued for their concentrations of valuable metals. They have attracted commercial interest due to the abundance of rare elements they contain, including but not limited to cobalt, nickel, and rare earth elements. Furthermore, these crusts can provide important insight into the history of the Earth's oceans, as they preserve records of past environmental conditions and changes in seawater composition.
Exploration and extraction of manganese crusts pose significant technological and environmental challenges. Current efforts are focused on developing methods to assess the economic viability of metal recovery, while minimizing potential negative impacts on marine ecosystems.
The word "manganese" originates from the Latin word "magnes", which refers to a magnetic stone or ore. This term was also used to describe minerals such as magnetite and lodestone. The name "magnes" itself is believed to have Greek origins, possibly derived from the Greek region known as Magnesia, where magnetic stones were abundant.
The word "crust" comes from the Old French word "croûte", meaning a hard outer coating or crust. This term later came from the Latin word "crusta", which has a similar meaning. It is often used to describe a hard or encrusted layer that forms on a surface.
Combining these two terms, "manganese crust" refers to a hard, encrusted layer or coating made up of manganese minerals found on the seafloor.