scientist believe they have evidence of the fastest - moving fling in an ice piece of paper ever recorded . The 10.5 - kilometer ( 6.5 - mile ) crack formed through an Antarctic chicken feed tack at a blistering speed of 35 beat ( 115 feet ) per second , or about 128.7 kilometers per time of day ( 80 naut mi per hour ) .

Researchers at the University of Washington observed the lightning - fast crack emerge in 2012 at the Pine Island Glacier Ice Shelf , the fastest thawing glacier inAntarctica , which accounts for around 25 percent of Antarctica ’s crank loss .

They made the observation using data from legal document placed on the ice ledge by other investigator and radar observation from satellites .

Satellite images taken May 8 (left) and May 11 (right), three days apart in 2012, show a new crack that forms a “Y” branching off to the left of the previous rift.

Satellite images taken May 8 (left) and May 11 (right), three days apart in 2012, show a new crack that forms a “Y” branching off to the left of the previous rift.Image credit: Olinger et al./AGU Advances

" This is to our knowledge the fastest breach - possibility event that ’s ever been keep , " lead subject author Stephanie Olinger , who persuade out the study as part of her doctoral research at the University of Washington and Harvard University and is now a postdoctoral research worker at Stanford University , tell in astatement .

A breach is a crack that passes right through an ice shelf . They are often the harbinger to shelf calving whenlarge lump of ice break off a glacierand gloam into the sea .

Other rifts in Antarctica can make over months or years . However , as this subject shows , they can also come about in mere moment , especially in the most vulnerable parts of Antarctica .

" This demo that under certain circumstances , an ice ledge can shatter . It tell apart us we want to depend out for this type of behaviour in the future tense , and it inform how we might go about describing these crack in large - shell ice canvass models , " explain Olinger .

Scientists are knifelike to realize the physics of how glaciers break aside , not least becauseclimate changeis localize to thaw Antarctic ice canvas and increase the relative frequency of falling out - opening outcome .

Glacier internal-combustion engine come out to act like a solid on short timescales , but it behaves like an oozing honey - like liquidity on long timescales . While this Modern study does suggest that ice can shatter like get around glass , the research worker believe the shot would have formed even faster if ice act like a dewy-eyed , brittle material .

" Is break formation more like glass breaking or like Silly Putty being deplume aside ? That was the question . Our computation for this event show that it ’s a lot more like spyglass breaking , " Olinger said

" Before we can improve the performance of large - plate ice sheet models and projections of future ocean - level rise , we have to have a good , cathartic - based understanding of the many dissimilar processes that influence ice ledge stability , " she summate .

The fresh study is published in the journalAGU Advances .