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Younger Dryas and Bond Events Explained by labppc105 is a document available to read on EtoBox.
The Younger Dryas, occurring 12.9–11.7 ka ago, was characterized by significant cooling and changes in oceanic and atmospheric conditions, likely triggered by freshwater influx from Lake Agassiz. This period is part of a broader deglacial sequence and is associated with various climate events, including Bond and Heinrich events, which document cycles of ice-rafting and climate fluctuations in the North Atlantic. These events highlight the complex interactions between ice sheets, ocean circulation, and clima
- Author
- labppc105
- Language
- EN