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  1. en.wikipedia.org › wiki › HoloceneHolocene - Wikipedia

    The Holocene is a geologic epoch that follows directly after the Pleistocene. Continental motions due to plate tectonics are less than a kilometre over a span of only 10,000 years. However, ice melt caused world sea levels to rise about 35 m (115 ft) in the early part of the Holocene and another 30 m in the later part of the Holocene.

  2. Holocen (stgr. ὅλος „wszystek” + καινός „nowy”), dawniej aluwium (łac. alluere „obmywać, oblewać”) – najmłodsza, trwająca współcześnie epoka geologiczna. Jako jej początek przyjmuje się rok 11 700 b2k (lub 11 650 BP; data radiowęglowa – 10,2 14. C tys. lat BP).

  3. 25 paź 2024 · Holocene Epoch, younger of the two formally recognized epochs that constitute the Quaternary Period and the latest interval of geologic time, covering approximately the last 11,700 years of Earth’s history.

  4. Holocene Epoch, formerly Recent Epoch, Latest interval of the Earth’s geologic history, dating from about 11,700 years ago to the present. The younger of the two epochs that constitute the Quaternary Period, the Holocene follows the last glacial stage of the Pleistocene Epoch.

  5. The Holocene Epoch. To observe a Holocene environment, simply look around you! The Holocene is the name given to the last 11,700 years* of the Earth's history — the time since the end of the last major glacial epoch, or "ice age."

  6. 27 mar 2013 · The Holocene Epoch began 12,000 to 11,500 years ago at the close of the Paleolithic Ice Age and continues through today. As Earth entered a warming trend, the glaciers of the late Paleolithic...

  7. 25 paź 2024 · The Viking-Norman Period. Approximately 1000–1250 ce the worldwide warm-up that culminated in the 10th century and has been called the early Medieval Warm Period or the “Little Climatic Optimum,” continued for two more centuries, although there was a brief drop in mean solar activity in the period about 1030–70.

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