Yahoo – AFP,
Richard INGHAM, April 4, 2017
Paris (AFP) - A giant waterfall tens of kilometres (miles) wide broke down a ridge which connected modern-day England to mainland Europe nearly half a million years ago, unleashing a mega-flood that gouged out the Channel and created the island of Britain, scientists said Tuesday.
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| Visitors walk on the cliff-top paths above the Fan Bay Deep Shelter, overlooking Dover, England, on July 23, 2015 (AFP Photo/LEON NEAL) |
Paris (AFP) - A giant waterfall tens of kilometres (miles) wide broke down a ridge which connected modern-day England to mainland Europe nearly half a million years ago, unleashing a mega-flood that gouged out the Channel and created the island of Britain, scientists said Tuesday.
In an
intricate piece of detective work, an international team of geologists said
they had answered a puzzle that has gripped their profession for more than a
century.
Their
sleuthing focuses on an ice age some 450,000 years ago, when much of the
northern hemisphere was covered by a thick glacial slab and sea levels were far
lower than they are today.
The
hypothetical picture of that epoch is of a Channel that was dry, cold and
tundra-like.
It rose to
a ridge of chalky rock that joined Britain and mainland Europe at what is now
the Strait of Dover.
The
scientists, writing in the journal Nature Communications, suggest that a mighty
lake, fed by continental rivers, built up in the southern North Sea between the
edge of the ice cap and this escarpment.
The lake
started to spill over the ridge, creating a waterfall some 32 kilometres (20
miles) wide and 100 metres (330 feet) high, and disgorging into a valley far
below.
The cascade
eroded the crest of the dam, and eventually the wall cracked and collapsed,
resulting in a tsunami that gouged out what is now the Channel.
Geological Brexit
The event
had a huge impact on history, shaping early human settlement in Britain and the
wars, trade, society and culture that followed.
"The
breaching of this land bridge between Dover and Calais was undeniably one of
the most important events in British history, helping to shape our island
nation's identity even today," said Sanjeev Gupta of Imperial College
London, who co-authored the paper.
"When
the ice age ended and sea levels rose, flooding the valley floor for good,
Britain lost its physical connection to the mainland," he said.
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The
geological Brexit (AFP Photo/Simon MALFATTO, Sabrina BLANCHARD)
|
"Without
this dramatic breaching, Britain would still be part of Europe. This is Brexit
1.0 -- the Brexit nobody voted for."
The idea
that a glacial lake made the Channel was first aired a century ago, but
struggled to make headway.
The new
study, though, finds fresh evidence to back the theory. In particular, it gives
the nod to a marine geologist named Alec Smith, who in 1985 suggested the
mega-flood was triggered by a waterfall -- an idea that was soon forgotten.
The big
clue comes from gigantic holes discovered in the bedrock of the Channel --
strange indentations up to several kilometres across and 100 metres (yards)
deep, and filled with gravel and soft sand sediment.
They were
found by accident in the 1960s and 1970s, when engineers drilled test holes in
the sea floor as part of exploratory work for the Channel Tunnel.
In fact,
the sediment was so loose that the engineers deemed that these holes were too
dangerous to tunnel, and as a result the route of the Channel Tunnel was
changed.
'Plunge
pools'
The
scientists believe that these holes are so-called plunge pools -- chambers that
are typically chiselled out in river beds beneath large waterfalls.
Eventually,
the holes can become so big that they cause the waterfall cliff to become
unstable and collapse.
Using new
sonar scanning of the sea floor and a technique called seismic reflection,
which uses pulses of energy to discern different rock formations, the team
found that seven of these giant holes form a remarkable straight line, running
from the ports of Calais to Dover -- the edge of the theorised ridge.
They also
saw evidence of an ancient giant valley on the Channel floor, the signs of a
massive outpouring.
The initial
breach of the dam was followed by a second big event, possibly caused by a spillover
of other, smaller lakes, the study suggests.
But the
timeline of the two events remains unclear, and they possibly occurred hundreds
of thousands of years apart.
Without
this stroke of geological fate, Britain would have remained attached to the
continent, rather like Denmark juts out into the sea from the European
mainland, the scientists say.


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