Younger Dryas
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Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. The Younger Dryas stadial, named after the alpine/tundra wildflower Dryas octopetala, and also referred to as the Big Freeze, was a geologically brief (approximately 1,300 ± 70 years) cold climate period following the Bølling/Allerød interstadial at the end of the Pleistocene between approximately 12,800 to 11,500 years ago, and preceding the Preboreal of the early Holocene. In Ireland, the period has been known as the Nahanagan Stadial, while in the UK it has been…mehr

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Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. The Younger Dryas stadial, named after the alpine/tundra wildflower Dryas octopetala, and also referred to as the Big Freeze, was a geologically brief (approximately 1,300 ± 70 years) cold climate period following the Bølling/Allerød interstadial at the end of the Pleistocene between approximately 12,800 to 11,500 years ago, and preceding the Preboreal of the early Holocene. In Ireland, the period has been known as the Nahanagan Stadial, while in the UK it has been called the Loch Lomond Stadial and most recently Greenland Stadial 1 (GS1).