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  2. Ice core - Wikipedia

    en.wikipedia.org/wiki/Ice_core

    An ice core is a core sample that is typically removed from an ice sheet or a high mountain glacier. Since the ice forms from the incremental buildup of annual layers of snow, lower layers are older than upper ones, and an ice core contains ice formed over a range of years. Cores are drilled with hand augers (for shallow holes) or powered ...

  3. Planetary core - Wikipedia

    en.wikipedia.org/wiki/Planetary_core

    A planetary core consists of the innermost layers of a planet. [1] Cores may be entirely liquid, or a mixture of solid and liquid layers as is the case in the Earth. [2] In the Solar System, core sizes range from about 20% (the Moon) to 85% of a planet's radius (Mercury). Gas giants also have cores, though the composition of these are still a ...

  4. Milankovitch cycles - Wikipedia

    en.wikipedia.org/wiki/Milankovitch_cycles

    Antarctic ice cores contain trapped air bubbles whose ratios of different oxygen isotopes are a reliable proxy for global temperatures around the time the ice was formed. Study of this data concluded that the climatic response documented in the ice cores was driven by northern hemisphere insolation as proposed by the Milankovitch hypothesis. [16]

  5. Ice giant - Wikipedia

    en.wikipedia.org/wiki/Ice_giant

    An ice giant is a giant planet composed mainly of elements heavier than hydrogen and helium, such as oxygen, carbon, nitrogen, and sulfur. There are two ice giants in the Solar System: Uranus and Neptune. In astrophysics and planetary science the term "ice" refers to volatile chemical compounds with freezing points above about 100 K, such as ...

  6. Paleoclimatology - Wikipedia

    en.wikipedia.org/wiki/Paleoclimatology

    Paleoclimatology (British spelling, palaeoclimatology) is the scientific study of climates predating the invention of meteorological instruments, when no direct measurement data were available. [1] As instrumental records only span a tiny part of Earth's history, the reconstruction of ancient climate is important to understand natural variation ...

  7. North Greenland Ice Core Project - Wikipedia

    en.wikipedia.org/wiki/North_Greenland_Ice_Core...

    The drilling site of the North Greenland Ice Core Project (NGRIP or NorthGRIP) is near the center of Greenland (75.1 N, 42.32 W, 2917 m, ice thickness 3085). Drilling began in 1999 and was completed at bedrock in 2003. [1] The cores are cylinders of ice 11 centimeters in diameter that were brought to the surface in 3.5-meter lengths.

  8. List of ice cores - Wikipedia

    en.wikipedia.org/wiki/List_of_ice_cores

    Peel et al. list one core for 1988-1989, at 104 m, which is presumably one of the 108 m cores listed by Thompson et al.[ 42] ^ Drilling took place in 1990-1993, 1995-1998, and 2005-2006. Hole 5G reached 2259 m; in 1992 an offset hole, 5G-1, was begun, reaching 3650 m in 2006.[ 54]

  9. Quaternary glaciation - Wikipedia

    en.wikipedia.org/wiki/Quaternary_glaciation

    Quaternary glaciation. Extent of maximum glaciation (in black) in the Northern Hemisphere during the Pleistocene. The formation of 3 to 4 km (1.9 to 2.5 mi) thick ice sheets equate to a global sea level drop of about 120 m (390 ft) The Quaternary glaciation, also known as the Pleistocene glaciation, is an alternating series of glacial and ...