earth:geohammers:k_bce_events
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earth:geohammers:k_bce_events [2022/05/02 21:07] khavikanum |
earth:geohammers:k_bce_events [2022/05/20 22:46] (current) khavikanum |
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| Linked to a 1500 year climate cycle, the oscillation was first identified by Swiss botanist Heinrich Zoller. This was a pulse of freezing temperatures not quite as bad as the Younger Dryas event, but still significant, none-the-less. Most scientists apparently agree that the "6.2 kiloyear event" (as it's more commonly called) is linked to a meltwater pulse that threw off the thermohaline current. | Linked to a 1500 year climate cycle, the oscillation was first identified by Swiss botanist Heinrich Zoller. This was a pulse of freezing temperatures not quite as bad as the Younger Dryas event, but still significant, none-the-less. Most scientists apparently agree that the "6.2 kiloyear event" (as it's more commonly called) is linked to a meltwater pulse that threw off the thermohaline current. | ||
| - | [[http://en.wikipedia.org/wiki/8.2_kiloyear_event]] | + | [[http://en.wikipedia.org/wiki/8.2_kiloyear_event]]\\ |
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| + | ==== Storegga Slides, 6225-6170 BCE ==== | ||
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| + | Three different collapses of the Norwegian continental shelf cause tsunamis throughout Northern Europe, and likely swept Doggerland in devestating floods. | ||
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| + | [[https://en.wikipedia.org/wiki/Storegga_Slide]]\\ | ||
| ==== Mount Okmok, 6.3k BCE ==== | ==== Mount Okmok, 6.3k BCE ==== | ||
earth/geohammers/k_bce_events.txt · Last modified: 2022/05/20 22:46 by khavikanum
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