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  2. British-Irish Ice Sheet - Wikipedia

    en.wikipedia.org/wiki/British-Irish_Ice_Sheet

    It probably reached its maximum extent during the Anglian Glaciation, and it was also extensive during the Late Devensian Glaciation (or Last Glacial Maximum). It was the only clearly defined major glacier in the Irish Sea and flowed about 700 km from its source areas to its southernmost margin. It is sometimes referred to as an “ice stream ...

  3. Last Glacial Maximum - Wikipedia

    en.wikipedia.org/wiki/Last_Glacial_Maximum

    A map showing the probable extent of land and water at the time of the last glacial maximum, 20,000 years ago and when the sea level was likely more than 110 metres lower than it is today. There were ice sheets in modern Tibet (although scientists continue to debate the extent to which the Tibetan Plateau was covered with ice) as well as in ...

  4. 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 ...

  5. Doggerland - Wikipedia

    en.wikipedia.org/wiki/Doggerland

    During the most recent glaciation of the Last Glacial Maximum, the North Sea and much of the British Isles were covered with glacial ice, and the sea level was about 120 m (390 ft) lower. The climate later became warmer, and around 12,000 BCE, Great Britain, as well as much of the North Sea and the English Channel, was an expanse of low-lying ...

  6. Climate: Long range Investigation, Mapping, and Prediction

    en.wikipedia.org/wiki/Climate:_Long_range...

    CLIMAP map of ice sheets, sea temperature changes, and changes in the outline of coastal regions during the last glacial. Climate: Long range Investigation, Mapping, and Prediction, known as CLIMAP, was a major research project of the 1970s and 80s to produce a map of climate conditions during the Last Glacial Maximum.

  7. File:Last Glacial Maximum Vegetation Map.svg - Wikipedia

    en.wikipedia.org/wiki/File:Last_Glacial_Maximum...

    Date: 22 August 2015: Source: Map generated from shapefile published by Ray, N. and J. M. Adams. 2001, “ A GIS-based Vegetation Map of the World at the Last Glacial Maximum (25,000-15,000 BP).

  8. Last Glacial Maximum refugia - Wikipedia

    en.wikipedia.org/wiki/Last_Glacial_Maximum_refugia

    The Last Glacial Maximum map with vegetation types. Last Glacial Maximum refugia were places in which humans and other species survived during the Last Glacial Period, around 25,000 to 18,000 years ago. [1] Glacial refugia are areas that climate changes were not as severe, and where species could recolonize after deglaciation. [2]

  9. Anglian stage - Wikipedia

    en.wikipedia.org/wiki/Anglian_Stage

    The Anglian was the most extreme glaciation during the last two million years. In Britain the ice sheet reached the Isles of Scilly and the Western Approaches, the furthest south the ice reached in any Pleistocene ice age. [ 7 ]