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  2. Holocene - Wikipedia

    en.wikipedia.org/wiki/Holocene

    The Holocene (/ ˈhɒl.əsiːn, - oʊ -, ˈhoʊ.lə -, - loʊ -/) [ 2 ][ 3 ] is the current geological epoch, beginning approximately 11,700 years ago. [ 4 ] It follows the Last Glacial Period, which concluded with the Holocene glacial retreat. [ 4 ] The Holocene and the preceding Pleistocene [ 5 ] together form the Quaternary period.

  3. Treaty of Versailles - Wikipedia

    en.wikipedia.org/wiki/Treaty_of_Versailles

    Map of territorial changes in Europe after World War I (as of 1923) The Treaty of Versailles resulted in the creation of several thousand miles of new boundaries, with maps playing a central role in the negotiations at Paris. [200] [201] The plebiscites initiated due to the treaty have drawn much comment. Historian Robert Peckham wrote that the ...

  4. Aftermath of World War I - Wikipedia

    en.wikipedia.org/wiki/Aftermath_of_World_War_I

    Revolutions of 1917–1923. The aftermath of World War I saw far-reaching and wide-ranging cultural, economic, and social change across Europe, Asia, Africa, and even in areas outside those that were directly involved. Four empires collapsed due to the war, old countries were abolished, new ones were formed, boundaries were redrawn ...

  5. Doggerland - Wikipedia

    en.wikipedia.org/wiki/Doggerland

    Appearance. Coordinates: 52.°N3°E52°N 3°E. Map of Doggerland at its near maximum extent c. 10,000 years Before Present (~ 8000 BCE) (top left) and its subsequent disintegration by 7000 BP (~5000 BCE) Doggerland was an area of land in Northern Europe, now submerged beneath the southern North Sea. This region was repeatedly exposed at various ...

  6. Holocene climatic optimum - Wikipedia

    en.wikipedia.org/wiki/Holocene_climatic_optimum

    The Holocene Climate Optimum (HCO) was a warm period in the first half of the Holocene epoch, that occurred in the interval roughly 9,500 to 5,500 years BP, [ 1 ] with a thermal maximum around 8000 years BP. It has also been known by many other names, such as Altithermal, Climatic Optimum, Holocene Megathermal, Holocene Optimum, Holocene ...

  7. Causes of World War I - Wikipedia

    en.wikipedia.org/wiki/Causes_of_World_War_I

    In 1900, the British had a 3.7:1 tonnage advantage over Germany; in 1910, the ratio was 2.3:1 and in 1914, it reached 2.1:1. Ferguson argues: "So decisive was the British victory in the naval arms race that it is hard to regard it as in any meaningful sense a cause of the First World War."

  8. World War I - Wikipedia

    en.wikipedia.org/wiki/World_War_I

    World War I[j] or the First World War (28 July 1914 – 11 November 1918), also known as the Great War, was a global conflict between two coalitions: the Allies (or Entente) and the Central Powers. Fighting took place mainly in Europe and the Middle East, as well as in parts of Africa and the Asia-Pacific, and in Europe was characterised by ...

  9. Timeline of World War I - Wikipedia

    en.wikipedia.org/wiki/Timeline_of_World_War_I

    The Great War. USA: Public Broadcasting System. "WWI Timeline". National Wwi Museum and Memorial. USA: National World War I Museum. "World War One Timeline". UK: BBC. "New Zealand and the First World War (timeline)". New Zealand Government. "Timeline: Australia in the First World War, 1914-1918". Australian War Memorial.