How Britain was formed: Mainland was created from the collision of not two but THREE ancient continental land masses
- Experts thought England, Wales and Scotland were created by two land masses
- Avalonia and Laurentia were thought to have collided 400 million years ago,
- A third land mass called Armorica was also involved geologists now believe
- The may have led to the abundance of tin and tungsten in England’s south west
Land from ancient France is now part of Devon and Cornwall, geologists studying how Britain was formed have revealed.
Their theory comes after studying the chemical profile of the west country counties’ rocks, which have more in common with France than the rest of the UK.
For centuries scientists thought England, Wales and Scotland were created by the merger of two land masses more than 400 million years ago.
Earth’s continents were on the move and Avalonia, which would become England and Wales, collided and fused with Laurentia, which would become Scotland.
Experts now now believe a third land mass – Armorica, which includes Brittany and Normandy – was also involved in the process.
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For centuries scientists thought England, Wales and Scotland were created by the merger of two land masses, Avalonia and Laurentia, more than 400 million years ago, but a third land mass called Armorica was involved in the process, geologists now say
It had been thought the border between Avalonia and Armorica lay beneath the English Channel.
Scientists based at the University of Plymouth have shown that the geological border in fact runs from the Exe estuary, on the south coast of Devon, in the East to the north Cornish town of Camelford, in the west.
The new way of thinking about the creation of Great Britain was based on an extensive study of mineral properties at exposed rock features across Devon and Cornwall.
They reveal a clear boundary running across the two counties, with areas north of it sharing their geological roots with the rest of England and Wales but everything south being geologically linked to France and mainland Europe.
This could explain the abundance of tin and tungsten in the far South West of England, metals also found in Brittany and other areas of mainland Europe, but not so evident in the rest of the UK.
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Lecturer in Igneous Petrology Dr Arjan Dijkstra, said: ‘This is a completely new way of thinking about how Britain was formed.
‘It has always been presumed that the border of Avalonia and Armorica was beneath what would seem to be the natural boundary of the English Channel.
‘But our findings suggest that although there is no physical line on the surface, there is a clear geological boundary which separates Cornwall and south Devon from the rest of the UK.’
Dr Dijkstra and Masters student Callum Hatch, who is now working at the Natural History Museum, visited 22 sites in Devon and Cornwall that were left exposed following geological events, such as underground volcanic eruptions.
These took place around 300 million years ago and brought magma from depths of 60 miles (100km) to the Earth’s surface.
Scientists have shown that the chemical profile of Cornwall and Devon have more in common with Brittany and Normandy than mainland Britain This image shows Porthcurno beach in Penwith, Cornwall.
The geological border runs from the Exe estuary in the East to Camelford in the west. This image shows the Pointe du Raz, one of the westernmost points of both Brittany and metropolitan France.
WHAT ARE TECTONIC PLATES?
Tectonic plates are composed of Earth’s crust and the uppermost portion of the mantle.
Below is the asthenosphere: the warm, viscous conveyor belt of rock on which tectonic plates ride.
The Earth has fifteen tectonic plates (pictured) that together have molded the shape of the landscape we see around us today
Earthquakes typically occur at the boundaries of tectonic plates, where one plate dips below another, thrusts another upward, or where plate edges scrape alongside each other.
Earthquakes rarely occur in the middle of plates, but they can happen when ancient faults or rifts far below the surface reactivate.
These areas are relatively weak compared to the surrounding plate, and can easily slip and cause an earthquake.
Rock samples from each site were collected and subjected to detailed chemical analysis in the lab using X-ray fluorescence (XRF) spectrometry.
The samples were also dissolved in acid in order to conduct a more intensive isotopic analysis, with scientists examining the levels of two elements – strontium and neodymium – to understand the full history of the rocks.
These findings were compared with previous studies elsewhere in the UK and mainland Europe.
Results showed the clear boundary running from the Exe estuary in the East to Camelford in the west.
Dr Dijkstra concluded: ‘We always knew that around 10,000 years ago you would have been able to walk from England to France.
‘But our findings show that millions of years before that, the bonds between the two countries would have been even stronger.
‘It explains the immense mineral wealth of South West England, which had previously been something of a mystery, and provides a fascinating new insight into the geological history of the UK.’
The study was published in Nature Communications.
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