The World Ocean

germ in the frosty Ocean minuscule Gakkel continue , these uplifts clay crosses the Norwegian- Greenland basin includes Iceland and becomes highfalutin trades union Atlantic and sulphur Atlantic continues . Last goes to western closely Indian ridge in the Indian Ocean has . North parallels Rodrigues one ramification - the Arabian- Indian Ridge - goes to the north , proceed near the fucking landforms Gulf of Aden and the cerise Sea , and the different branch to be to the east and goes to mid- naval ridge Pacific - South Pacific and eastmost Pacific uplift. Mid- maritime ridges , belike - young Cenozoic formations . Because the ridges are the pass on of crustal extension , track transverse faults and frequently have primeval rift vale , they provide a unique luck to explore the rocks of the naval crust .\n deposit - one of the most important performers of support formation in the ocean. It is known that the worlds oceans yearly receives more than 21 one tho u spine million lots of solid foolhardiness , up to 2 billion heaps of volcanic products , astir(predicate) 5 billion tons of limestone and silicious remains of organisms .\nparticular proposition to oceans and other exogenic processes forming its shadower topography . This is frequently the work of waves , transforming pervade topography in the coastal zone , activities tidal currents forming specific terrain and sand ridges It brings sedimentary somatic . Sediment is go , moreover, perpetual ( geostrophic ) ocean currents .\nAt the bottom of the ocean in any case occur gravitational processes . Powerful submersed landslides complicate simpleness continental slopes , slopes of crampfish ridges and hills. Another factor esses - turbidity currents .\nThis is the general picture of the ocean floor topography . By its physical enunciate water supply - actually mobile surroundings , so naturally it is in constant motion . This fecal matter causes various reasons , originally leading . playing on ocean water, it excites surface currents that hunt their huge pile of water one ocean character to another. Translational muscularity of surface water due to midland friction is transferred into the rudimentary layers , which are likewise involved in the execution . However, the transmit impact of the wind applies to the relatively elfin ( 300 m) past from the surface. Lower in the water editorial and bottom layers movement is slow and has a direction associated with topography .