Atlantis was a myth, but real-life lost lands do exist.
Granite boulders dredged from the seafloor off the coast of
South America two years ago could be remnants of a long-vanished
continent, according to Roberto Ventura Santos, the geology director of
Brazil's Geology Service.
"This could be the Brazilian Atlantis," Santos told reporters,
adding that he was speaking metaphorically and not claiming to have
found the legendary sunken world. "Obviously, we don't expect to find a
lost city in the middle of the Atlantic," he said.
Santos and his team speculated that the granite—a relatively
low-density rock found in continental crust—belonged to a continent that
was submerged when Africa and South America drifted apart and formed
the Atlantic Ocean about 100 million years ago.
But Michael Wysession,
an Earth and planetary scientist at Washington University in St. Louis,
noted that granite can find its way onto the seafloor through other
means. "There are pieces of granite in the middle of the seafloor that
date to about 800 million years ago when we had a snowball Earth
scenario and there were large pieces of rock embedded in ice
rafts"—mobile glaciers, essentially—"all over the ocean," explained
Wysession, who was not part of the discovery. "As those ice rafts were
melting, large blocks of rock dropped down all over the seafloor."
Wysession thinks that because the ocean floor has been extensively
mapped with satellites, it is unlikely that evidence for any major lost
continent will be found. "There's nothing that big that's hidden down
there," he said.
The Atlantis-like lost, hidden, or fantastic world is a common theme in fiction. There are J. R. R. Tolkein's Middle Earth and James Hilton's Shangri-La, not to mention Lewis Carroll's Wonderland. The original lost land, Atlantis, was first mentioned by Plato
around 360 B.C. According to Plato, Atlantis sank into the earth and
drowned beneath the seas. Real continents rarely disappear in such
dramatic fashion. "Continents by definition are made of low-density rock
and cannot be subducted deep into the earth," explained Staci Loewy, a geologist at the University of Texas at Austin.
Nonetheless, there are real "lost lands" like the Brazilian
"Atlantis" that have disappeared from view because of rising seas or the
geological upheavals of plate tectonics and erosion. "Parts of
continents can be worn down by erosion, and fragments can be broken off
and isolated as microcontinents when larger continents break apart,"
Loewy said.
Here are some actual "lost lands" discovered by science.
Pangaea
A supercontinent believed to have formed around 300 million years ago, Pangaea was an enormous landmass that later broke up to eventually form the continents we know today.
Scientists now think several other supercontinents—such as Kenorland, Columbia, and Rodinia—existed before Pangaea, but the shapes of these ancient land masses are unclear.
Rodinia, for example, was a supercontinent thought to have been
formed about one billion years ago; it's believed that it subsequently
broke apart to form Pangaea.
"Those pieces are now part of the modern continents, but they have
been significantly altered by one billion years of plate tectonics and
erosion such that reconstructing the supercontinent of Rodinia is very
difficult," explained Loewy.
While they appear stationary, Earth's landmasses shift around over
geologic time, carried across the planet's surface by the slow, grinding
movement of enormous, shell-like plates.
"The surface of the earth is made up of a rigid layer called the
lithosphere; the lithosphere is broken into numerous pieces referred to
as tectonic plates," Loewy explained.
"These plates move around the surface of the Earth, colliding into
each other, creating mountains such as the Himalaya and Andes; pulling
apart from each other, creating volcanic ridges in the middle of oceans
like the mid-Atlantic Ridge; and sliding past each other, such as in the
San Andreas Fault in California."
Mauritia
Scientists earlier this year announced that they had found evidence of a drowned "microcontinent" off the coast of Africa, near the island of Mauritius.
Sand grains from Mauritius's beaches were found to contain fragments
of the mineral zircon that were between 660 and 2 billion years old—far
older than the island itself.
One theory is that the sand grains are remnants of Mauritia, a lost
microcontinent that once existed off the coast of Africa and which was
submerged when India broke apart from Madagascar about 85 million years
ago.
Microcontinents are shards of land broken off from continents and
supercontinents. The distinctions among the three aren't clear-cut,
however, and labeling a landmass a continent or microcontinent can be
arbitrary since there are no precise size requirements for each term.
New Zealand, for example, is actually part of a large continental structure that includes the Campbell Plateau.
"It's not all that different in size from Australia, but because most
of it is underwater, we call Australia a continent and New Zealand an
island," Wysession said.
Microcontinents can also merge into larger structures. For example, "the north African edge of the supercontinent Gondwana
broke up into slices like the pieces of an apple, and each of those
[microcontinents] moved north to form southern Europe," explained Louis Jacobs, a paleontologist at Southern Methodist University in Dallas, Texas.
Beringia
Though Asia and North America are now separated by a thin strait, it
is very shallow—about 150 feet (46 meters) deep—and when sea levels are
low, such as during ice ages, the two continents are connected by a land
bridge known as Beringia.
According to a controversial theory, humans heading east after
leaving Asia some 40,000 years ago found their way blocked by glaciers
and were forced to settle in Beringia for thousands of years until conditions thawed enough for them to continue to North America.
Less contentious is the theory "that the Clovis people came over from Siberia to North America about 14,000 years ago," Wysession said.
Scotland's Hidden Landscape
In 2011, geologists studying ocean-mapping data stumbled upon a
previously unknown landscape now buried beneath more than a mile of
marine sediment off the coast of Scotland.
The hidden landscape,
which had an estimated area of about 3,861 square miles (10,000 square
kilometers), had furrows cut by rivers and peaks that were once part of
mountains.
Scientists think it was briefly elevated above the waves by
geological processes about 55 million years ago but became submerged
again after about 2.5 million years.
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