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  2. Sea level rise - Wikipedia

    en.wikipedia.org/wiki/Sea_level_rise

    The world's largest potential source of sea level rise is the East Antarctic Ice Sheet (EAIS). It is 2.2 km thick on average and holds enough ice to raise global sea levels by 53.3 m (174 ft 10 in) [97] Its great thickness and high elevation make it more stable than the other ice sheets. [98]

  3. Past sea level - Wikipedia

    en.wikipedia.org/wiki/Past_sea_level

    Sea levels have been comparatively stable over the past 6,500 years, ending with a 0.50 m sea level rise over the past 1,500 years. For example, about 10,200 years ago the last land bridge between mainland Europe and Great Britain was submerged, leaving behind a salt marsh. By 8000 years ago the marshes were drowned by the sea, leaving no trace ...

  4. Post-glacial rebound - Wikipedia

    en.wikipedia.org/wiki/Post-glacial_rebound

    To form the ice sheets of the last Ice Age, water from the oceans evaporated, condensed as snow and was deposited as ice in high latitudes. Thus global sea level fell during glaciation. The ice sheets at the last glacial maximum were so massive that global sea level fell by about 120 metres. Thus continental shelves were exposed and many ...

  5. Last Glacial Period - Wikipedia

    en.wikipedia.org/wiki/Last_Glacial_Period

    A chronology of climatic events of importance for the Last Glacial Period, about the last 120,000 years The Last Glacial Period caused a much lower global sea level.. The Last Glacial Period (LGP), also known as the Last glacial cycle, occurred from the end of the Last Interglacial to the beginning of the Holocene, c. 115,000 – c. 11,700 years ago, and thus corresponds to most of the ...

  6. Meltwater pulse 1A - Wikipedia

    en.wikipedia.org/wiki/Meltwater_pulse_1A

    Image showing sea level change during the end of the last glacial period. Meltwater pulse 1A is indicated. Meltwater pulse 1A (MWP1a) is the name used by Quaternary geologists, paleoclimatologists, and oceanographers for a period of rapid post-glacial sea level rise, between 13,500 and 14,700 calendar years ago, during which the global sea level rose between 16 meters (52 ft) and 25 meters (82 ...

  7. Last Glacial Maximum - Wikipedia

    en.wikipedia.org/wiki/Last_Glacial_Maximum

    The Last Glacial Maximum (LGM), also referred to as the Last Glacial Coldest Period, [1] was the most recent time during the Last Glacial Period where ice sheets were at their greatest extent 26,000 and 20,000 years ago. [2] Ice sheets covered much of Northern North America, Northern Europe, and Asia and profoundly affected Earth 's climate by ...

  8. Climate tipping points may have been reached already ... - AOL

    www.aol.com/news/climate-tipping-points-may...

    Since the last Ice Age peaked about 20,000 years ago, sea level has risen hundreds of feet. But sea-level rise is not linear; it can happen abruptly. 11,000 years ago sea level rose as much as 15 ...

  9. 8.2-kiloyear event - Wikipedia

    en.wikipedia.org/wiki/8.2-kiloyear_event

    The sea-level data from the Rhine–Meuse Delta indicate a 2–4 m (6 ft 7 in – 13 ft 1 in) of near-instantaneous rise at 8.54 to 8.2 ka, in addition to 'normal' post-glacial sea-level rise. [26] Meltwater pulse sea-level rise was experienced fully at great distance from the release area. Gravity and rebound effects associated with the ...