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  2. Ice giant - Wikipedia

    en.wikipedia.org/wiki/Ice_giant

    These envelopes nevertheless limit observation of the ice giants' interiors, and thereby the information on their composition and evolution. [2] Although Uranus and Neptune are referred to as ice giant planets, it is thought that there is a supercritical water-ammonia ocean beneath their clouds, which accounts for about two-thirds of their ...

  3. Sea ice - Wikipedia

    en.wikipedia.org/wiki/Sea_ice

    Broken pieces of Arctic sea ice with a snow cover. Sea ice arises as seawater freezes. Because ice is less dense than water, it floats on the ocean's surface (as does fresh water ice). Sea ice covers about 7% of the Earth's surface and about 12% of the world's oceans.

  4. Sea ice growth processes - Wikipedia

    en.wikipedia.org/wiki/Sea_ice_growth_processes

    Sea ice will deform primarily at fracture points which in turn will form at the points of greatest stress and lowest strength, or where the ratio between the two is a maximum. Ice thickness, salinity and porosity will all affect the strength of the ice. The motion of the ice is driven primarily by ocean currents, though to a lesser extent by wind.

  5. Incoming! Excitement builds for the return of ice giants - AOL

    www.aol.com/news/incoming-excitement-builds...

    One by one, and ever so slowly, an entire flotilla of massive chunks of ice several stories high gradually make t. Residents view the first iceberg of the season as it passes the South Shore, also ...

  6. Ice - Wikipedia

    en.wikipedia.org/wiki/Ice

    Ice that is found at sea may be in the form of drift ice floating in the water, fast ice fixed to a shoreline or anchor ice if attached to the seafloor. [47] Ice which calves (breaks off) from an ice shelf or a coastal glacier may become an iceberg. [48] The aftermath of calving events produces a loose mixture of snow and ice known as Ice ...

  7. Antarctic sea ice - Wikipedia

    en.wikipedia.org/wiki/Antarctic_sea_ice

    Antarctic sea ice is the sea ice of the Southern Ocean. It extends from the far north in the winter and retreats to almost the coastline every summer. [1] Sea ice is frozen seawater that is usually less than a few meters thick. This is the opposite of ice shelves, which are formed by glaciers; they float in the sea, and are up to a kilometre thick.

  8. Ice shelf - Wikipedia

    en.wikipedia.org/wiki/Ice_shelf

    Ice shelves form along coastlines where the ice thickness is insufficient to displace the more dense surrounding ocean water. The boundary between the ice shelf (floating) and grounded ice (resting on bedrock or sediment) is referred to as the grounding line; the boundary between the ice shelf and the open ocean (often covered by sea ice) is ...

  9. Blue whales can reach 100 feet long and weigh up to 330,000 pounds, according to the National Oceanic and Atmospheric Administration.. The ocean giants live in all oceans except the Arctic, NOAA ...