Pleistocene meteor crater on Greenland

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A newly discovered 31 km wide impact crater in Northern Greenland, hidden beneath a glacier, has been identified using advanced radar technology. The impact is estimated to have occurred during the Pleistocene epoch, approximately 2.6 million to 11,700 years ago, with the meteorite believed to be around 1 km wide. This discovery may have significant implications for understanding past climate changes, particularly its potential link to the Younger Dryas period of cooling, which could have disrupted North Atlantic water flow and affected North American megafauna and the Clovis culture. Researchers are also interested in a possible debris field associated with the impact, although this remains unproven. The conversation includes speculation about the crater's age and its relation to volcanic features, emphasizing the importance of distinguishing between impact and volcanic origins in geological studies.
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https://phys.org/news/2018-11-huge-crater-greenland-impact-northern.html
Paywall: advances.sciencemag.org/content/4/11/eaar8173

A 31 km wide crater in Northern Greenland has been hidden under a massive glacier, until now. Using new radar systems and older technologies, the authors document the existence of a newly found massive crater. Getting a date on the impact event is currently fuzzy. They estimate it occurred in the Pleistocene which is a lot of time. (circa 2,588,000 to 11,700 years ago, more than a 2 million year span) . They estimate the iron meteor was 1 km wide.

If you have an interest in punctual paleoclimate changes, then this research project - down the road - may be an interesting read as the subsequent planned research continues. There is a potential debris field, not proven yet, that is the next object of interest for the researchers.
 
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Genava said:

I was about to post on this.
The article explains much more about how the discovery came about as well as speculation about how the impact could have lead to the Younger Dryas period of cooling (fresh water from the impact melted ice disrupting the water flow in the N. Atlantic) which further speculation deals with how it might have affected North American mega fauna and the Clovis culture.
They did not want to put that in the original article because it was speculative and would raise lots of questions tangental to their crater discovery.
 
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Curious coincidence alert:
IIRC, if you look at the Iceland hot-spot back-track, it passes under that region at approx 80~100 MY.
Could this feature be much, much older than Pleistocene ??
I know there's a long and unfortunate history of impact craters being mistaken for odd volcanic features, could this be a rare example of the converse ?

FWIW, I'd be delighted if this feature is an impact crater of Pleistocene era, wholly or partly responsible for the very wide tektite 'strewn field'...
 
Nik_2213 said:
I know there's a long and unfortunate history of impact craters being mistaken for odd volcanic features, could this be a rare example of the converse ?

No, definitely not !
volcanic eruptions don't form shocked quartz
Nik_2213 said:
FWIW, I'd be delighted if this feature is an impact crater of Pleistocene era, wholly or partly responsible for the very wide tektite 'strewn field'...
which tektite strewn field are you referring to ?

I know of no known strewn field that isn't already related to a known impact

cheers
Dave
 
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Ah, the N. American tektites have been tied to the Chesapeake Bay feature ~34 MY.
My Bad.
 
Nik_2213 said:
Ah, the N. American tektites have been tied to the Chesapeake Bay feature ~34 MY.
yup
 
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There is a strewn field possibly related to the Hiawatha Crater Discovery. Its is the Younger Dryas . Boundary field and was documented in a paper I co-authored here, if you have any questions.: http://www.pnas.org/content/109/28/E1903
 
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