© Planet Observer/Universal Images Group via Getty ImagesThe rock was found within the Mistastin impact crater in Labrador, Canada, shown here in this satellite image.
It's confirmed: The hottest rock ever discovered in Earth's crust really was super-hot.
The rock, a fist-sized piece of black glass, was discovered in 2011 and first reported in 2017, when scientists wrote in the journal
Earth and Planetary Science Letters that it had been formed in temperatures reaching 4,298 degrees Fahrenheit (2,370 degrees Celsius), hotter than much of the Earth's mantle. Now, a new analysis of minerals from the same site reveals that this record-scorching heat was real.
The rocks melted and reformed in a meteorite impact about 36 million years ago in what is today Labrador, Canada. The impact formed the 17-mile-wide (28 kilometers) Mistastin crater, where Michael Zanetti, then a doctoral student at Washington University St. Louis, picked up the glassy rock during a Canadian Space Agency-funded study of how to coordinate astronauts and rovers working together to explore another planet or
moon. (Mistastin crater looks a lot like a moon crater and is often used as a stand-in for such research.)
The chance find turned out to be an important one. An analysis of the rock revealed that it contained zircons, extremely durable minerals that crystallize under high heat. The structure of zircons can show how hot it was when they formed.
But to confirm the initial findings, researchers needed to date more than one zircon. In the new study, lead author Gavin Tolometti, a postdoctoral researcher at Western University in Canada, and colleagues analyzed four more zircons in samples from the crater. These samples came from different types of rocks in different locations, giving a more comprehensive view of how the impact heated the ground. One was from a glassy rock formed in the impact, two others from rocks that melted and resolidified, and one from a sedimentary rock that held fragments of glass formed in the impact.
The results, published April 15 in the journal
Earth and Planetary Science Letters, showed that the impact-glass zircons were formed in at least 4,298 F heat, just as the 2017 research indicated. In addition, the glass-bearing sedimentary rock had been heated to 3,043 F (1,673 C). This broad range will help researchers narrow down places to look for the most super-heated rocks in other craters, Tolometti
said in a statement.
"We're starting to realize that if we're wanting to find evidence of temperatures this high, we need to look at specific regions instead of randomly selecting across an entire crater," he said.
The researchers also found a mineral called reidite within zircon grains from the crater. Reidites form when zircons undergo high temperatures and pressures, and their presence allows the researchers to calculate the pressures experienced by the rocks in the impact. They found that the impact introduced pressures of between 30 and 40 gigapascals. (Just one gigapascal is 145,038 pounds per square inch of pressure.) This would have been the pressure at the edges of the impact; at the zone where the
meteorite hit the crust directly, the rocks would have not just melted, but vaporized.
The findings can be used to extrapolate to other craters on
Earth - and elsewhere. The researchers hope to use similar methods to study rocks brought back from impact craters on the moon during the Apollo missions.
"It can be a step forward to try and understand how rocks have been modified by impact cratering across the entire solar system," Tolometti said.
Reader Comments
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Quebec was melted most probably within the last 20 million years, it's landscape is awash with impact creates, many of which are now lakes.
Most of the western side of America was swallowed up by volcanic activity that discharged humongous volumes of magma that covered the lands many miles deep.
hmmmmm, any info regarding Mont Tremblant, Québec??
initial observations suggest staged seismic activity that released magma to the West at a later date.
I noticed the 2 rivers, Devil's River and Riviere Rouge, they both meander, interesting, meandering is a slow process where water finds its route by cutting through softer terrain, something that would suggest that the area in question was not covered by later magma deposits and supports access to old geology records, as in rock formation.
Google earth also limits access to closer inspection of terrain, a tell tale sign that not all eyes are welcome.
A rule of thumb, if ancient ground supports evidence of previous civilisations, the authorities will either allow the land to be covered by wood lands or forest, or build a golf course.
Trees are a plenty and there's a rather large golf course by the river 😉
So after only a quick scan, the Area in question could possibly support evidence of earlier civilisations, whilst the land hasn't been covered by later magma flows any civilisation living there would have perished.
Mont Tremblant, Mont Carcan and several hills are composed of gneiss.
Gneisses result from the metamorphism of many igneous or sedimentary rocks, and are the most common types of rocks found in Precambrian regions. The Precambrian was the "Age of Early Life." During the Precambrian, continents formed and our modern atmosphere developed, while early life evolved and flourished.
So the area in question is a trembling relic of the past, some 4,600 millions old, I suspect the surrounding areas have much more recent magma deposits covering them, probably Jurassic in nature
So LM 😊 I hope that's useful.