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  1. The Younger Dryas, which occurred circa 12,900 to 11,700 years Before Present (BP), was a stadial (cooling) event which marked a return to glacial conditions, temporarily reversing the climatic warming of the preceding Bølling–Allerød Interstadial (also known as the Late Glacial Interstadial, which spanned from 14,670 to 12,900 BP.).

  2. El Dryas Reciente o Joven Dryas (c. 12.900 a 11.700 años AP) 2 fue un retorno a las condiciones glaciales que revirtieron temporalmente el calentamiento climático gradual después del Último Máximo Glacial (LGM, c. 27.000 a 20.000 años AP).

  3. Hace 4 días · Younger Dryas, cool period between roughly 12,900 and 11,600 years ago that disrupted the prevailing warming trend occurring in the Northern Hemisphere at the end of the Pleistocene Epoch (which lasted from 2.6 million to 11,700 years ago).

    • The Editors of Encyclopaedia Britannica
  4. 7 de feb. de 2024 · The Younger Dryas (YD; \ (\sim\) 12.9 to 11.7 kya) 1 was a rapid return to cold glacial conditions that occurred during the most recent deglaciation of the late Quaternary and marks the beginning...

  5. 20 de oct. de 2020 · El Dryas Reciente, o Younger Dryas, tuvo lugar hace 12.900 años y es un suceso de "gran importancia" porque supuso un retorno a condiciones casi glaciares en pocas décadas, cuando el planeta estaba saliendo de la última glaciación y el clima comenzaba a ser cálido y relativamente húmedo, han apuntado desde el IPE.

  6. This near-glacial period is called the Younger Dryas, named after a flower (Dryas octopetala) that grows in cold conditions and that became common in Europe during this time. The end of the Younger Dryas, about 11,500 years ago, was par-ticularly abrupt.

  7. The Younger Dryas (YD) is known as the best example of an abrupt climatic event recorded on land, in the oceans, and in ice cores (Alley et al., 2002, 2003). It was a cold event that occurred between 11,000 and 10,000 14 C years ago, (approximately 12,800 and 11,600 calendar years ago), and it lasted about 1,200 years.

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