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1.2 billion years ago, a 1-km asteroid smashed into Scotland

In 2008, scientists from Oxford and Aberdeen University made a startling discovery in the northwest of Scotland. Near the village of Ullapool, which sits on the coast opposite the Outer Hebrides, they found a debris deposit created by an ancient meteor impact dated to 1.2 billion years ago. The thickness and extent of the debris suggested that the meteor measured 1 km (0.62 mi) in diameter and took place near to the coast.

Image: Pixabay/RafaelMousob

Until recently, the precise location of the impact remained a mystery to scientists. But in a paper that recently appeared in the Journal of the Geological Society, a team of British researchers concluded that the crater is located about 15 to 20 km (mi) west of the Scottish coastline in the Minch Basin, where it is buried beneath both water and younger layers of rock.

The research team was led by Dr. Kenneth Amor, who was joined by multiple colleagues from the Department of Earth Sciences at the University of Oxford, and Stephen P. Hesselbo – a professor of geology at the Camborne School of Mines and Environment and Sustainability Institute at the University of Exeter.

Field photo of Stoer showing the laminar beds of sandstone in the bottom of the picture. Credit: University of Oxford

The Minch refers to the straight that sits between the Scottish Mainland and the Hebrides islands, which is part of the Inner Seas region just off the coast of western Scotland. The team determined that the meteor impact took place in this region based on multiple lines of evidence. These included field observations, analysis of broken rock fragments, and the alignment of magnetic particles.

“The material excavated during a giant meteorite impact is rarely preserved on Earth, because it is rapidly eroded, so this is a really exciting discovery. It was purely by chance this one landed in an ancient rift valley where fresh sediment quickly covered the debris to preserve it. The next step will be a detailed geophysical survey in our target area of the Minch Basin.

Based on their analysis, the team was able to determine where the meteorite sent material generated by the impact from several locations. From this, they backtracked the material to the most likely source of the crater, which led them to the “Minch meteor” site. The timing of this impact is especially significant given the state of the Earth at the time.

Roughly 1.2 billion years ago, during the Mesoproterozoic Era, the first complex life forms were emerging on Earth and the majority of life was still aquatic. In addition, the land mass that is Scotland today was located in the Laurentia craton (part of the supercontinent of Rodinia) and was closer to the equator at the time. This means that what the Minch meteor struck, the Scottish landscape was vastly different than it is today.

Close-up picture of spherules (“accretionary lapilli”) that form in the impact plume cloud, and found in the deposit. Credit: University of Oxford

In some ways, it would have looked similar to what scientists image Mars looked like billions of years ago, with semi-arid conditions and with some water on its surface. The study also provides insight into Earth’s ancient evolution and could even provide hints about future impacts. Roughly one billion years ago, Earth and the other planets of the Solar System experienced a higher rate of meteorite impact than they do today.

This was the result of collisions between asteroids and debris objects that were left over from the formation of the early Solar System. However, due to the number of asteroid and comet fragments that are still floating around in the Solar System today, it is possible a similar impact event will happen at some point in the not-so-distant future.

At present, impacts by smaller objects – measuring a few meters in diameter – are thought to be a relatively common occurrence, happening once every 25 years on average. On the other hand, objects measuring about 1 km (0.62 mi) in diameter are thought to collide with Earth once every 100,000 to one million years.

However, official estimates vary due to the fact that the terrestrial record of large impacts is poorly constrained. Unlike celestial bodies like Mars or the Moon, craters are regularly obliterated on Earth by erosion, burial, and tectonic activity. Knowing with confidence where and when past impacts took place, and what effects they had, is key to understanding what we might be facing someday.

In that sense, the identification of Minch meteor site could aid in the development of planetary defense as well as provide better insights into Earth’s geological history.

Further Reading: University of Oxford, Journal of the Geological Society

Source: Universe Today, by Matt Williams.


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