what are the main layers of the ocean.?
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The bottom (sometimes called the sea bed)\nThe middle watery bit ( the sea)\nand the foamey wavey part
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How deep is the deepest part of the ocean? Does anything live down there? \n\nWe didn't have to dig very deep to find the answer to this one. We simply typed "deepest part of the ocean" into Yahoo! and uncovered several web pages that answered your question. \nOur first stop was ScienceNet, a British web site that purports to be a one-stop science site. We couldn't dispute that claim after they provided us with the facts of the matter: The Marianas Trench in the Pacific Ocean is 11,033 meters (36,201 feet) below sea level. If Mount Everest were placed inside of this trench, it would disappear. \n\nWe headed back to the search results and saw something that looked very familiar -- our friend Earl, the answer man at Yahooligans!. Turns out Earl had answered the question some time ago and agreed with our earlier finding. He also offered a couple of links to more information on the trench. At Oceanclopedia, we learned that the deepest part of the trench is named Vitjazdepth. The trench was formed when the Pacific plate collided with the Philippine plate, which also resulted in the formation of the nearby island Guam. \n\nTo find out if anything actually lives down there, we swam over to Earth & Sky, a companion site to the popular science radio series. We discovered that plants can't live at such depths because they need sunlight for photosynthesis -- light doesn't penetrate such depths. However, recent photographs from unmanned craft show shrimp-like crustaceans, sea cucumbers, and marine worms. In addition, bacteria flourish on the muddy floors of the trenche
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Are you thinking of the Sargasso Sea?\n\nhttp://en.wikipedia.org/wiki/Sargasso_Sea
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Wind driven surface currents (such as the Gulf Stream) head polewards from the equatorial Atlantic Ocean, cooling all the while and eventually sinking at high latitudes (forming North Atlantic Deep Water). This dense water then flows downhill into the deep water basins, only resurfacing in the northeast Pacific Ocean 1200 years later. Extensive mixing therefore takes place between the ocean basins, reducing differences between them and making the Earth's ocean a global system. On their journey, the water masses piggyback both energy (in the form of heat) and matter (solids, dissolved substances and gases) around the globe. As such, the state of the circulation has a large impact on the climate of our planet.  It's also called thermohaline circulation
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The earth has four layers...\n\nTheCrust, Upper mantle, Lower Mantle and the Core refer to <http://volcano.und.edu/vwdocs/vwlessons/lessons/Earths_layers/Earths_layers1.html>\n\nThe Crust has many hollow parts like caves. Caves connected to the ocean and some undergorund river, near an instict volcano is posible of supporting life.\n\nHumans can live there but not making civilization. Just hiding from dangers on the surface such as crusaders, barbarians, dinasours, wild animals...at the present these caverns is used for safety hiding places from war, nuclear attack and for the one of the most dangerous speicies on earth and that is the Humosapiens.....
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East China Sea, South China Sea, Sea of Japan, Phillipine Sea, Java Sea, Greenland Sea, Sea of Galilee, and the Indian Ocean
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Deep inside the ocean...B-)
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The Earth's oceans are all connected to one another. Until the year 2000, there were four recognized oceans: the Pacific, Atlantic, Indian, and Arctic. In the Spring of 2000, the International Hydrographic Organization delimited a new ocean, the Southern Ocean (it surrounds Antarctica and extends to 60 degrees latitude). \nSee map with location in\nhttp://www.enchantedlearning.com/subjects/ocean/
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good websites...\nAll about te ocean\nhttp://www.noaa.gov/ocean.html\nNOAA Media Contents\nhttp://www.publicaffairs.noaa.gov/reporters.html\nNOAA Library\nhttp://www.lib.noaa.gov/
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There are many links here, including a link to Scripps Oceanographic institue and a section with links, Marine Education (way down at the "m"s-an alphabetical list).\nhttp://www.csulb.edu/library/subj/ocean.html
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Mediterranean Sea\nSouth China Sea \nCoral Sea \nNorth Sea\nIrish Sea\nAdriatic Sea\nAtlantic Ocean\nIndian Ocean\nPacific Ocean\nBest was the Coral Sea - Cairns, North Queensland & the Great Barrier Reef.\nSee it before you die - or it does...\n\nAnd don't do what I did!  All that way & focussing on the reef - I missed the tropical rainforest just inland!
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Yup, definately oceans.
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There are a few main parts to the earth. The earth is like a tootsie pop: a hard crunchy exterior, and it is soft inside. They are in roughly concentric spheres. The main layers of the earth are called the crust, the mantle and the core. \n\nThe outside shell of the earth is called the crust. The crust is about 5-60 kilometers thick and forms about 1% of the volume of the earth. We live on the crust. \n\nUnder the crust is a very large part of the earth called the mantle. The mantle is about 84% of the volume of the earth. The mantle is about 2800 kilometers thick.\n\nInside the mantle, is the soft middle of the earth, called the core. The core is roughly a round ball, and is about 15% of the volume of the earth, and has a radius of about 3400 Km. \n\nOf course, one can get much more detailed, but this is enough to give you a start, so you can understand what you read on the internet.
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1. Atlantic ocean\n2. Pacific ocean\n3. Indian ocean\n4. Mediterranean\n5. China Sea\n6. Coral Seas (Oceania)\n7. Caribbean\n\nHowever, keep in mind that it does have a tone of antiquity thus, To the ancients, "seven" often meant "many," and before the fifteenth century, the many seas of the world were: \nthe Red Sea \nthe Mediterranean Sea \nthe Persian Gulf \nthe Black Sea \nthe Adriatic Sea \nthe Caspian Sea \nthe Indian Ocean
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Here is piece form an encyclopedia...\n\nThe Atlantic may be divided into two basins–North Atlantic Ocean and South Atlantic Ocean–each with a distinct circulation system. The clockwise-moving currents of the North Atlantic (North Equatorial Current, Antilles Current, Gulf Stream, North Atlantic Drift, Canaries Current) and the counterclockwise-moving currents of the South Atlantic (South Equatorial Current, Brazil Current, West Wind Drift, Benguela Current) are separated from each other by the Equatorial Counter Current; the Guinea Current off W Africa is a link between the two systems. At the Grand Banks off Newfoundland heavy fogs form along the front where the warm Gulf Stream meets the cold Labrador Current. The surface waters in the Atlantic's trade wind belts attain the highest salinity known in ocean water.
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It's C), inner, outer, mantle, crust
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SafariX Textbooks Online - Essentials of Oceanography, Eighth EditionThe existence of sea floor spreading was confirmed when the Glomar Challenger began the Deep Sea Drilling Project to sample ocean sediments and the ... \nhttp://www.safarix.com/0131635719/ch04lev1sec9\n\nSpreading of the Ocean Floor: New Evidence -- Vine 154 (3755 ...Sediment Distribution on the Mid-Ocean Ridges with Respect to Spreading of the Sea Floor. J. Ewing and M. Ewing (1967). Science 156: 1590-1592 | Abstract ... \nhttp://www.sciencemag.org/cgi/content/abstract/154/3755/1405\n\nThe Active Part of Charlie-Gibbs Fracture Zone: A Study Using Sonar and Other Geophysical Techniques … - group of 2 »\nR Searle - J. Geophys. Res, 1981 - osti.gov \n... SEA-FLOOR SPREADING; ATLANTIC OCEAN;GEOLOGIC FAULTS;OCEANIC CRUST;PLATE\nTECTONICS;SEDIMENTS;SONAR. ... geophysical instruments has revealed new information ...\nhttp://www.osti.gov/energycitations/product.biblio.jsp?osti_id=6458102\n\nContinental breakup and the onset of ultraslow seafloor spreading off Flemish Cap on the Newfoundland rifted margin \nhttp://geology.geoscienceworld.org/cgi/content/abstract/32/1/93\n\nTransition from continental break-up to punctiform seafloor spreading: how fast, symmetric and … - group of 5 »\nG Corti, JW Van Wijk, M Bonini, D Sokoutis, S … - Geophys. Res. Lett, 2003 -\n http://scholar.google.com/url?sa=U&q=http://www-pord.ucsd.edu/~wilbert/JOLANTE/bestanden%2520Jolante/Corti2003.pdf\n\nI could not find much on it but I hope these links help. If not, just put what your looking for into the search bar to do more research on it. good luck.