This diagram shows the process by which vents on the ocean floor spew out a cocktail of minerals. Cold sea water enters cracks in an underwater volcano. It descends hundreds of kilometres into the earth, where it is heated as it nears molten rock (magma). The heated sea water also becomes more acidic, and starts to dissolve elements such as manganese, iron, silicon and other minerals from the surrounding rocks. The heated fluid starts to rise, and is eventually expelled through vents on the sea floor. As the hydrothermal fluid mixes with cold sea water, the metals in solution precipitate as fine-grained particles, which form dark-coloured plumes called black smokers. Some of the material that is precipitated falls on the sea floor, and gradually enriches the surrounding area in metals.
Te whakamahi i tēnei tūemi
This item has been provided for private study purposes (such as school projects, family and local history research) and any published reproduction (print or electronic) may infringe copyright law. It is the responsibility of the user of any material to obtain clearance from the copyright holder.
Source: GNS Science