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  2. Cosmic ocean - Wikipedia

    en.wikipedia.org/wiki/Cosmic_ocean

    The ocean is boundless, unordered, unorganized, amorphous, formless, dangerous, terrible. In some myths, its cacophony is noted, opposed to the ordered rhythm of the sea. [3] Chaos can be personified as water or by the unorganized interaction of water and fire, The transformation of chaos into order is also the transition from water to land. [4]

  3. Meeting of Waters - Wikipedia

    en.wikipedia.org/wiki/Meeting_of_Waters

    This phenomenon is due to the differences in temperature, speed, and amount of dissolved sediments in the waters of the two rivers. The Rio Negro flows at near 2 km/h (1.2 mph) at a temperature of 28 °C (82 °F), while the Rio Solimões flows between 4 and 6 km/h (2.5–3.7 mph) at a temperature of 22 °C (72 °F). [ 1 ]

  4. Parting of the Waters - Wikipedia

    en.wikipedia.org/wiki/Parting_of_the_Waters

    Parting of the Waters is an unusual hydrologic site at Two Ocean Pass on the Great Divide, within the Teton Wilderness area of Bridger-Teton National Forest, Wyoming, USA. Two Ocean Pass separates the headwaters of Pacific Creek, which flows west to the Pacific Ocean, and Atlantic Creek, which flows east to the Atlantic Ocean.

  5. Ocean stratification - Wikipedia

    en.wikipedia.org/wiki/Ocean_stratification

    The stratified configuration of the ocean can act as a barrier to water mixing, which impacts the efficiency of vertical exchanges of heat, carbon, oxygen, and other constituents. Thus, stratification is a central element of Earth's climate system. Global upper-ocean stratification continued its increasing trend in 2022 and was among the top ...

  6. Marine biogeochemical cycles - Wikipedia

    en.wikipedia.org/wiki/Marine_biogeochemical_cycles

    Water carried into the mantle eventually returns to the surface in eruptions at mid-ocean ridges and hotspots. [131]: 646 Estimates of the amount of water in the mantle range from 1 ⁄ 4 to 4 times the water in the ocean. [131]: 630–634 The deep carbon cycle is the movement of carbon through the Earth's mantle and core.

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  8. Open ocean convection - Wikipedia

    en.wikipedia.org/wiki/Open_ocean_convection

    Open ocean convection is a process in which the mesoscale ocean circulation and large, strong winds mix layers of water at different depths. Fresher water lying over the saltier or warmer over the colder leads to the stratification of water, or its separation into layers. Strong winds cause evaporation, so the ocean surface cools, weakening the ...

  9. Borders of the oceans - Wikipedia

    en.wikipedia.org/wiki/Borders_of_the_oceans

    The borders of the oceans are the limits of Earth's oceanic waters.The definition and number of oceans can vary depending on the adopted criteria. The principal divisions (in descending order of area) of the five oceans are the Pacific Ocean, Atlantic Ocean, Indian Ocean, Southern (Antarctic) Ocean, and Arctic Ocean.