Ad
related to: younger dryas flood map search
Search results
Results from the WOW.Com Content Network
The Younger Dryas (YD, Greenland Stadial GS-1) [2] was a period in Earth's geologic history that occurred circa 12,900 to 11,700 years Before Present (BP). [3] It is primarily known for the sudden or "abrupt" cooling in the Northern Hemisphere, when the North Atlantic Ocean cooled and annual air temperatures decreased by ~3 °C (5.4 °F) over North America, 2–6 °C (3.6–10.8 °F) in Europe ...
The Younger Dryas impact hypothesis (YDIH) proposes that the onset of the Younger Dryas (YD) cool period at the end of the Last Glacial Period, around 12,900 years ago was the result of some kind of cosmic event with specific details varying between publications. [1]: Sec 1 The hypothesis is widely rejected by relevant experts.
Weiss, H. (2000). "Beyond the Younger Dryas: Collapse as Adaptation to Abrupt Climate Change in Ancient West Asia and the Eastern Mediterranean". In Bawden, G.; Reycraft, R. M. (eds.). Environmental Disaster and the Archaeology of Human Response. Albuquerque, New Mexico: Maxwell Museum of Anthropology. pp. 63– 74. ISBN 0-912535-14-8.
Postglacial Sea level Rise Curve and Meltwater Pulses (MWP) Meltwater pulse 1B (MWP1b) is the name used by Quaternary geologists, paleoclimatologists, and oceanographers for a period of either rapid or just accelerated post-glacial sea level rise that some hypothesize to have occurred between 11,500 and 11,200 years ago at the beginning of the Holocene and after the end of the Younger Dryas. [1]
It bursts and floods out through the Mackenzie River into the Arctic Ocean at 11,000 BC, possibly causing the Younger Dryas cold period. c. 12,000 BC c. 8,000 BC Göbekli Tepe, world's earliest known temple-like structure, is created. c. 10,800 BC Younger Dryas impact event is proposed to have occurred, causing the onset of the Younger Dryas.
Glacial melt-waters, at the end of the Younger Dryas Ice Age caused a dramatic rise in the sea level of the Caspian Sea. An earthquake caused a fracture, which allowed the Caspian Sea to flood across the fertile plains of Atlantis.
Image showing sea level change during the end of the last glacial period. Meltwater pulse 1A is indicated. Meltwater pulse 1A (MWP1a) is the name used by Quaternary geologists, paleoclimatologists, and oceanographers for a period of rapid post-glacial sea level rise, between 13,500 and 14,700 years ago, during which the global sea level rose between 16 meters (52 ft) and 25 meters (82 ft) in ...
The Younger Dryas was the last stage of the Pleistocene epoch that spanned from 2,580,000 to 11,700 years BP and it preceded the current, warmer Holocene epoch. The Younger Dryas was the most severe and longest lasting of several interruptions to the warming of the Earth's climate, and it was preceded by the Late Glacial Interstadial , an ...
Ad
related to: younger dryas flood map search