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Earth, a 4.5- Billion-year-old planet,
still evolving.

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As continents shift and clash, volcanoes
erupt and glaciers grow and recede,

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the earth's crust is carved
in numerous and fascinating ways,

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leaving a trail
of geological mysteries behind.

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In this episode,

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the 450-million-year-old geological
history of New York City is explored.

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A metropolis pockmarked
with strange rocks,

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haunted by footprints
of ancient giant reptiles,

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and lined with a vast curtain
of solidified lava.

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Scientists investigate the evidence

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for fiery volcanoes,
massive floods and ice sheets

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four times as high
as the Empire State building.

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The clues to understanding New York
City's geological past provides a window

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into the formation of the earth itself.

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The investigation into New York City's
geological history begins here,

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with Manhattan's rocky outcrops.

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These rocks are clues
to how the land was made

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and how its geology helped it become
a dense, thriving, pulsating city.

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They're scattered all over Manhattan,

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poking through the surface of parks

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and through the concrete
between the buildings.

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Some, squashed between two apartment
blocks, are the size of a whale.

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They are the extraordinary
survivors of ancient times.

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Most importantly, they are
the surface tips of the bedrock

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in which Manhattan's buildings
are anchored.

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Gigantic skyscrapers stand in two
clusters, in downtown and midtown.

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In the section between,
the buildings are lower.

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The clues to the shape
of Manhattan's familiar skyline

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are the rocks beneath the surface.

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A leading expert on the rocks in New
York is geologist Charles Merguerian.

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The entire history of the
development of the earth's crust

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is emblazoned in the rocks beneath us.

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The rocks here in New York City
harbour an ancestry

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that dates back
over a billion years of time.

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Merguerian is searching for evidence to
show how the city's bedrock was made.

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At Inwood Hill Park in Upper Manhattan,
he's found an extremely hard piece

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of the bedrock
known as Manhattan schist.

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To the untrained eye,
it's just a piece of rock,

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but to Merguerian, this is his first clue.

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The rocks that we're looking at
right here

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are rocks of the Manhattan schist
formation

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and the... these rocks are very severely
deformed,

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and the structures here in this rock
is a structure that comes up like this,

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bends around and comes back down
on itself as such,

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and in three-dimensional view, it's a
structure that looks something like this.

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A very, very tight fold
with a plunge towards the south here.

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These are rocks that were
very, very strongly deformed

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over protracted periods of time.

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And it's the same bedrock that occurs
over much of New York City.

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This tight fold in the rock
suggests New York's bedrock

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was formed under great pressure.

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To confirm this hunch, Merguerian takes
a sample to the lab for detailed analysis.

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Radiometric dating proves this rock
is about 450 million years old.

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But the rock has even
greater secrets to tell.

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It contains a kaleidoscope
of minerals,

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which opens a window
into the ancient world.

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To me, minerals are like
the instrument cluster in your car,

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they tell you everything about
how your car is running.

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Merguerian uses a microscope with
polarised light to view the minerals.

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The examination tells us
the former depth regime,

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how deep the rocks were,
they tell you the age of the rocks,

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they tell you everything
you want to know

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about the development
of the earth's crust.

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What's striking about these samples is
that the minerals inside are elongated.

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It is a clue that these rocks must once
have been crushed by massive forces.

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And the colours support this theory.

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Under the polarised light, the sample
from Inwood Hill Park shows up blue.

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This comes from a mineral called
kyanite, which forms at great depths.

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It's conclusive evidence that this rock

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was compressed
deep under the surface.

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Rocks forged at these depths
are much harder,

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ideal for a city's foundations.

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But what gigantic weight was on top?

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Merguerian believes
there is only one answer.

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The rock was once buried
under the crushing weight

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of a chain of massive mountains.

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The minerals that we find
in the bedrock units of New York City

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tell us that the rocks of New York City
were formerly buried

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when they were formed,
under very high pressures,

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and that those high pressures indicate

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that these rocks formerly were
produced at depths of 20 to 25 miles,

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and probably the mountains were
as high as the Alps are today.

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But even the most impressive mountain
chains can't survive the ravages of time.

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The Rocky Mountains, for example.

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Millions of years ago, they soared
nearly six miles into the sky.

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Today, erosion has halved their size.

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The same process
happened in New York.

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Rain, wind and ice
wore the ancient mountains almost flat.

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But the microscopic crystals
found in the rock in Manhattan

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testify that they existed in the past.

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How did the mountains form?

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The answer lies in the way
the earth's crust moves.

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A network of interlocking individual
pieces makes up the Earth's surface.

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Geologists call them tectonic plates.

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Over millions of years, they collide and
break apart to form different continents.

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450 million years ago, the Earth's
surface looked completely different.

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North America was much further

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to the south.

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MERGUERIAN: North America
was tilted 90 degrees clockwise

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from its present orientation

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and it was straddling the equator.

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As such, the climate was tropical,

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the east coast of North America was
really experiencing Club Med conditions.

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The weather
may have been awesome,

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but the ancient East Coast
was heading for trouble.

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The plate beneath it was moving.

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The East Coast was on a collision
course with ancient West Africa.

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450 million years ago, they collided.

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The impact unleashed geological chaos.

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Under intense compression,
the land was forced upwards

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to form a soaring range of mountains.

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The collision that took place
is the most fundamental

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and impressive mountain-building event

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to affect the east coast
of North America.

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Today, all that remains
are their stumps,

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stumps that form the bedrock
of modern-day New York.

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The collision that built up the ancient
mountains also folded the bedrock

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into dips and rises.

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These folds are responsible for
the shape of Manhattan's skyline.

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The city boasts two clusters of
skyscrapers in downtown and midtown.

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Here, the hard bedrock that formed
deep underground was forced up.

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It is now close to the surface
and provides solid anchorage

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for the high-rise buildings.

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In the dip in the middle
the rock was folded down.

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The area is filled with loose sediments,
less suitable for skyscrapers.

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MERGUERIAN: When the bedrock
is at the Earth's surface

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where it's actually exposed,

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then it's pretty easy
to build tall buildings

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'cause you can root them
directly into solid rock.

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However, in areas where the bedrock
is deep and covered by glacial sediment,

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in those cases, it's very difficult
to build tall buildings

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because you need to root those
buildings either into solid rock

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or build concrete abutments called
caissons that can support tall buildings.

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New York's deep history
is beginning to take shape.

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Building up from tiny crystals
in the rock,

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scientists revealed how
New York's bedrock was formed

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under the crushing weight of
a massive ancient mountain range.

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The result was hard Manhattan schist,

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a perfect foundation
for the city's skyscrapers.

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But New York City
still had a long way to go.

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The colliding plates created
an enormous landmass -

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the last great supercontinent,
called Pangaea.

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New York was now trapped
in the centre...

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...but somehow it made it back
to the coast.

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Hidden beyond the city's streets is
evidence of huge volcanic eruptions,

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mass extinctions and continents
torn into pieces.

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Clues that could explain

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how New York became one of
the world's great maritime cities.

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Investigators are piecing together

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how New York City's unique geology
was formed.

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Much of its early success
as a trade and commerce centre

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is owed to its deep-water harbour
and its location at the coast.

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But 450 million years ago,
things were different.

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The area of New York City
was landlocked,

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embedded in the heart
of a huge supercontinent.

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How did it get to the coast?

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The investigation fast-forwards
250 million years.

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In a quarry in New Jersey,
25 miles northeast of Manhattan,

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paleontologist Paul Olson
unearths the first of a string of clues

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that could explain how
New York City reached the coast.

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A giant fossilised footprint.

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This is the footprint, actually
the mud that filled in the footprint,

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of a four-footed crocodile relative
that was the dominant carnivore

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during the late Triassic.

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You can see the toes here
have little pads on them

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and here's the handprint,
and these animals would have been,

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in this case, about the size
of a modest crocodile,

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but some of them became much,
much larger, the size even of a T. Rex.

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(ROARS)

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The footprints are from
a huge crocodile-like creature

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called Postosuchus.

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It first appeared on the Earth
around 230 million years ago.

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Then, some 30 million years later,
its footprints suddenly vanished.

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But Postosuchus wasn't alone.

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Half of all land animals
perished at the same time.

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The fossil evidence proves it to be

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one of the biggest mass extinctions
ever recorded.

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The evidence
for this mass extinction

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is that we have lots
and lots of fossils right in this area.

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And what you see is especially
in the... in the reptile footprints,

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you see one group of forms,

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the forms that are related
to crocodilians, disappear.

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00:13:00,714 --> 00:13:06,296
Whatever caused the mass extinction
must have been a catastrophic event.

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00:13:06,296 --> 00:13:10,296
Olsen had a hunch that the
mass extinction was somehow related

185
00:13:10,296 --> 00:13:13,463
to New York's return to the coast.

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The ancient area of New York
sat on a line of great weakness,

187
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the plate boundary
where two continents joined

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00:13:22,795 --> 00:13:25,627
to form the supercontinent Pangaea.

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And it was unstable,
prone to earthquakes and volcanoes.

190
00:13:30,835 --> 00:13:34,918
Olsen's quest - to find the evidence
for the natural disaster

191
00:13:34,918 --> 00:13:38,667
that finished off Postosuchus
200 million years ago.

192
00:13:41,001 --> 00:13:44,001
A band of dark rock
above the footprints

193
00:13:44,001 --> 00:13:46,875
in the New Jersey quarry caught his eye.

194
00:13:46,875 --> 00:13:52,541
It was basalt, the smoking gun
Olson was looking for.

195
00:13:54,291 --> 00:13:57,332
Basalt is a volcanic rock.

196
00:13:57,332 --> 00:14:03,248
It forms when hot lava erupts
onto the surface and cools.

197
00:14:03,248 --> 00:14:08,164
Did the volcanoes that forged
this basalt trigger the mass extinction

198
00:14:08,164 --> 00:14:11,830
and also rip Pangaea apart?

199
00:14:11,830 --> 00:14:16,080
On its own, the evidence
at the quarry was unconvincing.

200
00:14:16,080 --> 00:14:19,829
The layer of basalt
is only a few feet thick.

201
00:14:22,454 --> 00:14:26,287
To prove mass lava flows
caused this global catastrophe,

202
00:14:26,287 --> 00:14:29,870
scientists needed
corroborative evidence.

203
00:14:33,286 --> 00:14:34,994
High above the Hudson River,

204
00:14:34,994 --> 00:14:38,035
geologist Matt Gorring
follows another lead.

205
00:14:38,035 --> 00:14:40,951
He's studying the Palisades,

206
00:14:40,951 --> 00:14:44,577
a dramatic geologic feature
that hugs the Hudson River,

207
00:14:44,577 --> 00:14:50,825
beginning across mid Manhattan
and running into northeast New Jersey.

208
00:14:50,825 --> 00:14:53,659
They too are made of basaltic rock,

209
00:14:53,659 --> 00:14:58,408
the same rock implicated
in the mass extinction of land animals.

210
00:14:58,408 --> 00:15:03,116
But the Palisades are on
an altogether different scale.

211
00:15:03,116 --> 00:15:10,448
The Palisades are a sheet of basaltic
magma, about 1,000 feet thick,

212
00:15:10,448 --> 00:15:12,490
it's about 40 miles long,

213
00:15:12,490 --> 00:15:14,156
so it's a very prominent set of cliffs

214
00:15:14,156 --> 00:15:17,531
that run all the way up the west side
of the Hudson River.

215
00:15:19,281 --> 00:15:23,155
Here is proof of
massive volcanic activity.

216
00:15:24,613 --> 00:15:28,030
Hot lava flooded out of ruptures
in the Earth's crust

217
00:15:28,030 --> 00:15:32,279
and covered ancient North America
in a mile-deep sheet.

218
00:15:33,737 --> 00:15:36,195
The lava cracked as it cooled.

219
00:15:37,320 --> 00:15:41,653
The vertical ruptures formed
regular pencil-shaped columns.

220
00:15:43,194 --> 00:15:46,569
These distinctive rock formations
have been known to geologists

221
00:15:46,569 --> 00:15:48,736
since the 19th century.

222
00:15:51,485 --> 00:15:55,193
Intriguingly, they appear
on both sides of the Atlantic,

223
00:15:55,193 --> 00:16:00,734
in North and South America,
Europe and Africa.

224
00:16:00,734 --> 00:16:04,608
Geologists suspected that
their presence pointed to the spot

225
00:16:04,608 --> 00:16:09,566
where Africa and Europe
separated from America.

226
00:16:09,566 --> 00:16:14,649
But that was just an unproven
theory, until the 1950s,

227
00:16:14,649 --> 00:16:18,066
when scientists developed
a revolutionary technique

228
00:16:18,066 --> 00:16:20,315
called paleomagnetism.

229
00:16:20,315 --> 00:16:24,898
Now, they could study
the magnetic properties of rocks.

230
00:16:26,564 --> 00:16:31,438
Many rocks, including basalt,
have a distinctive magnetic signature,

231
00:16:31,438 --> 00:16:34,354
formed as the rock is born.

232
00:16:34,354 --> 00:16:37,980
Tiny crystals inside the rock
act like compass needles.

233
00:16:37,980 --> 00:16:41,270
When the magma that
forms the rock is fluid,

234
00:16:41,270 --> 00:16:45,603
the crystals align to the Earth's
magnetic field, pointing north.

235
00:16:48,145 --> 00:16:51,436
As the rock solidifies,
the crystals freeze,

236
00:16:51,436 --> 00:16:55,478
forever locked
in that fixed magnetic alignment.

237
00:16:55,478 --> 00:16:58,727
As continents move
and the rocks travel,

238
00:16:58,727 --> 00:17:03,393
the crystals end up pointing
in a different direction than north.

239
00:17:03,393 --> 00:17:08,976
Gorring and his team investigate the
magnetic signature of the Palisades.

240
00:17:12,392 --> 00:17:17,016
To get a sample, they bore
into the rock with a water-cooled drill.

241
00:17:21,516 --> 00:17:26,890
They measure the exact orientation
of the crystals today with a compass.

242
00:17:26,890 --> 00:17:29,765
When they offset this reading
with magnetic north,

243
00:17:29,765 --> 00:17:33,556
they can calculate
the original location of the rock.

244
00:17:33,556 --> 00:17:36,556
Uh... 14.

245
00:17:36,556 --> 00:17:39,347
One of the useful things
that you can do with this rock

246
00:17:39,347 --> 00:17:42,764
is you can take it back in the lab
and measure its magnetic orientation,

247
00:17:42,764 --> 00:17:46,555
and that magnetic orientation
will be when this rock crystallised

248
00:17:46,555 --> 00:17:48,512
or solidified 200 million years ago.

249
00:17:48,512 --> 00:17:51,429
So this rock would have minerals
that would be pointing

250
00:17:51,429 --> 00:17:54,596
in some other direction
other than north today.

251
00:17:57,386 --> 00:18:01,136
When scientists compared the
magnetic orientation of the Palisades

252
00:18:01,136 --> 00:18:04,094
with the other basalt outcrops
around the Atlantic,

253
00:18:04,094 --> 00:18:08,135
they discovered they formed at
approximately the same latitude.

254
00:18:08,135 --> 00:18:11,385
Not only did the rocks
have the same age,

255
00:18:11,385 --> 00:18:14,926
they were also born
at the same location.

256
00:18:14,926 --> 00:18:20,759
For example, 200 million years ago, New
York and Morocco were neighbours.

257
00:18:25,759 --> 00:18:29,174
The geologists had
all the proof they needed.

258
00:18:29,174 --> 00:18:32,840
They could now confidently
piece together what happened.

259
00:18:35,174 --> 00:18:39,840
It began with a global volcanic disaster.

260
00:18:39,840 --> 00:18:41,881
About 200
million years ago,

261
00:18:41,881 --> 00:18:44,923
North America and Africa
began to pull apart from each other.

262
00:18:46,423 --> 00:18:48,630
There were gigantic lava outpourings.

263
00:18:48,630 --> 00:18:54,004
These lava flows erupted along
very long cracks in the Earth's crust,

264
00:18:54,004 --> 00:18:55,963
that would have produced
fountains of lava

265
00:18:55,963 --> 00:19:00,337
extending thousands and thousands
of feet into the atmosphere.

266
00:19:02,254 --> 00:19:05,211
They covered an almost
inconceivably large area,

267
00:19:05,211 --> 00:19:08,628
roughly four million square miles,

268
00:19:08,628 --> 00:19:13,419
from southwestern France
to southwestern Brazil,

269
00:19:13,419 --> 00:19:16,252
from New York to central Mali in Africa.

270
00:19:16,252 --> 00:19:19,919
This area was covered
in ponded lava flows

271
00:19:19,919 --> 00:19:23,918
that in some places ended up
being nearly a mile thick.

272
00:19:27,501 --> 00:19:31,167
Volcanic eruptions led to
soaring temperatures.

273
00:19:31,167 --> 00:19:36,833
Half of the plants and animals died.
Postosuchus didn't stand a chance.

274
00:19:40,291 --> 00:19:43,457
As enormous forces tore Pangaea apart,

275
00:19:43,457 --> 00:19:47,332
a giant sea formed between
the separating land masses -

276
00:19:47,332 --> 00:19:50,081
the Atlantic Ocean.

277
00:19:50,081 --> 00:19:54,123
The city of New York
was now at the coast.

278
00:19:58,997 --> 00:20:02,955
200-million-year-old footprints
beneath a layer of basalt

279
00:20:02,955 --> 00:20:06,663
and the Palisades
towering above the Hudson

280
00:20:06,663 --> 00:20:08,954
provide evidence
that Pangaea split apart

281
00:20:08,954 --> 00:20:12,120
to create the east coast
of North America.

282
00:20:13,454 --> 00:20:17,120
But the story of New York City
was far from over.

283
00:20:17,120 --> 00:20:21,536
After being built by fire, the region
was about to be overcome

284
00:20:21,536 --> 00:20:24,869
by another destructive force.

285
00:20:29,493 --> 00:20:34,951
Scientists are piecing together the story
of New York's violent geological past.

286
00:20:36,867 --> 00:20:40,909
250 million years ago,
the Atlantic Ocean opened up,

287
00:20:40,909 --> 00:20:44,867
leaving the area of New York
on the coast.

288
00:20:44,867 --> 00:20:49,116
But the maritime city
still had a long way to go.

289
00:20:54,199 --> 00:20:57,073
There was no deep
Hudson River channel.

290
00:20:57,073 --> 00:21:00,906
It was nothing but a small stream.

291
00:21:02,531 --> 00:21:06,406
What forces transformed it
into the wide river

292
00:21:06,406 --> 00:21:09,739
capable of carrying heavy freighters
far inland?

293
00:21:13,322 --> 00:21:18,196
A clue to how the Hudson Valley
was created is the strange boulders

294
00:21:18,196 --> 00:21:21,862
that are scattered throughout
Manhattan's Central Park.

295
00:21:21,862 --> 00:21:24,987
Some of them weigh several tons.

296
00:21:24,987 --> 00:21:31,444
But they're strangers to these parts,
totally unlike the surrounding rocks.

297
00:21:33,569 --> 00:21:37,527
Geologist Charles Merguerian
investigates where they came from.

298
00:21:39,402 --> 00:21:42,276
This boulder is a boulder
from the Palisade sheet

299
00:21:42,276 --> 00:21:44,568
on the other side of the Hudson
in New Jersey.

300
00:21:44,568 --> 00:21:46,942
You can see it's very nicely polished.

301
00:21:46,942 --> 00:21:50,109
Compositionally, it's totally different
than the surrounding bedrock,

302
00:21:50,109 --> 00:21:51,650
which is Manhattan schist,

303
00:21:51,650 --> 00:21:54,233
and the Manhattan schist here
is very rich in mica.

304
00:21:54,233 --> 00:21:57,525
This rock has no light-coloured mica
in it whatsoever.

305
00:21:57,525 --> 00:22:02,024
The Palisade sheet is located
to the west and north of us.

306
00:22:05,816 --> 00:22:10,356
The Palisades run for 40 miles
along the Hudson River.

307
00:22:10,356 --> 00:22:14,564
Something immensely powerful
must have moved the boulders

308
00:22:14,564 --> 00:22:16,563
such a great distance.

309
00:22:18,522 --> 00:22:22,896
Merguerian knows the answer is ice.

310
00:22:25,646 --> 00:22:30,188
Scientists have noticed a similar
phenomenon 4,000 miles away

311
00:22:30,188 --> 00:22:32,145
in the Swiss Alps.

312
00:22:33,729 --> 00:22:37,395
As huge glaciers grind their way
across the landscape,

313
00:22:37,395 --> 00:22:42,186
they gouge out lumps of rock and
carry them along in the base of the ice.

314
00:22:43,228 --> 00:22:49,227
These rocks act like sandpaper
and carve out deep scratches.

315
00:22:49,227 --> 00:22:53,227
When the ice melts,
it leaves the boulders behind.

316
00:22:53,227 --> 00:22:59,434
Merguerian is convinced the same thing
happened in Central Park.

317
00:22:59,434 --> 00:23:01,892
Ice moved the Palisade boulders

318
00:23:01,892 --> 00:23:05,766
and carved out grooves
in the bedrock underneath.

319
00:23:05,766 --> 00:23:10,558
This bedrock exposure in Central Park
shows the profound effects of glaciation

320
00:23:10,558 --> 00:23:13,599
in the form of these
spectacular glacial grooves

321
00:23:13,599 --> 00:23:18,306
that move up the outcrop
and show this pattern

322
00:23:18,306 --> 00:23:20,722
where glaciers grabbed huge boulders

323
00:23:20,722 --> 00:23:25,222
and those huge boulders acted
like tools to produce these scratches.

324
00:23:28,139 --> 00:23:32,221
To Merguerian, the rocks in Central Park
are compelling evidence

325
00:23:32,221 --> 00:23:35,346
that New York once was covered in ice.

326
00:23:36,721 --> 00:23:40,262
Over millions of years,
growing and receding ice

327
00:23:40,262 --> 00:23:44,304
has repeatedly turned North America
into a frozen wilderness.

328
00:23:48,428 --> 00:23:53,219
But the grooves on the rocks
in New York don't tell the full story.

329
00:23:53,219 --> 00:23:58,926
The destruction caused by the ice
points to a gigantic glacial event

330
00:23:58,926 --> 00:24:02,218
that would dwarf the future metropolis.

331
00:24:04,676 --> 00:24:07,384
To find out the extent of the ice,

332
00:24:07,384 --> 00:24:09,092
Merguerian travelled to Bear Mountain,

333
00:24:09,092 --> 00:24:12,466
some 50 miles north of New York City.

334
00:24:15,508 --> 00:24:18,383
Once again, the clue was in the rocks.

335
00:24:19,424 --> 00:24:23,757
He found glacial marks
similar to those in Central Park.

336
00:24:25,299 --> 00:24:27,923
What we're looking at here
are chatter marks.

337
00:24:27,923 --> 00:24:32,131
Chatter marks are very
diagnostic features of glacial erosion,

338
00:24:32,131 --> 00:24:37,089
they're produced by boulders embedded
in the base of a thick sheet of glacial ice.

339
00:24:37,089 --> 00:24:40,380
Those boulders impinged on
this bedrock surface,

340
00:24:40,380 --> 00:24:45,088
polishing it, smoothing it off
and then plucking pieces of rock off

341
00:24:45,088 --> 00:24:50,045
as the glacial ice moved over with
the boulders embedded in the base.

342
00:24:51,671 --> 00:24:55,503
The gouges in the rocks
could mean just one thing.

343
00:24:55,503 --> 00:24:59,377
The glacier must have been
thousands of feet thick.

344
00:24:59,377 --> 00:25:01,794
In this case, although
we're standing at an elevation

345
00:25:01,794 --> 00:25:04,544
of about 1,280 feet above sea level,

346
00:25:04,544 --> 00:25:09,002
the glacial ice sheet covered Bear
Mountain as if it weren't even there.

347
00:25:11,376 --> 00:25:15,126
Scientists have found identical
chatter marks on nearby peaks

348
00:25:15,126 --> 00:25:17,709
up to a mile above sea level.

349
00:25:17,709 --> 00:25:20,376
It was unmistakable proof.

350
00:25:20,376 --> 00:25:26,249
A glacier at least one mile thick
ground its way across these mountains.

351
00:25:28,333 --> 00:25:32,873
Did this same ice sheet also
plough through Central Park?

352
00:25:32,873 --> 00:25:36,665
Another nearby rock face
provided the answer.

353
00:25:36,665 --> 00:25:38,790
The feature
that we're looking at here

354
00:25:38,790 --> 00:25:41,456
are a series of sub-parallel
glacial scratches and grooves

355
00:25:41,456 --> 00:25:45,873
and these are, again, are produced
by the glacial ice sheet

356
00:25:45,873 --> 00:25:49,413
dragging boulders across
this very durable granite surface,

357
00:25:49,413 --> 00:25:51,539
it's kind of polished the surface.

358
00:25:51,539 --> 00:25:55,621
And, in addition, it's produced these
rather subtle but... but... but obvious,

359
00:25:55,621 --> 00:25:59,329
when the lighting is right,
striae or grooves in the bedrock.

360
00:25:59,329 --> 00:26:01,995
Now if we measure
the orientation of these...

361
00:26:07,120 --> 00:26:13,535
...these... these come out about
north 20 degrees west,

362
00:26:13,535 --> 00:26:18,202
just about identical in orientation to the
striae that we measured at Central Park.

363
00:26:20,618 --> 00:26:24,784
It's significant evidence that the ice
sheet that covered Bear Mountain

364
00:26:24,784 --> 00:26:28,450
also flowed over the surface
of Central Park.

365
00:26:28,450 --> 00:26:33,200
Proof that New York City was covered
by a glacier four times higher

366
00:26:33,200 --> 00:26:35,949
than the Empire State Building.

367
00:26:35,949 --> 00:26:37,782
MERGUERIAN:
Just imagine glacial ice,

368
00:26:37,782 --> 00:26:40,865
a huge thick ice sheet over a mile thick,

369
00:26:40,865 --> 00:26:44,198
exerting tremendous pressure
on the surface

370
00:26:44,198 --> 00:26:48,031
and sculpting the surface into
the landscape that we see today.

371
00:26:50,406 --> 00:26:54,239
The ice sheet's crushing weight
bulldozed everything in its path

372
00:26:54,239 --> 00:26:58,280
and cut through the remains
of the ancient mountains.

373
00:26:58,280 --> 00:27:00,613
Before the ice arrived,

374
00:27:00,613 --> 00:27:04,238
the waters of the Hudson River had
gently cut down through the landscape

375
00:27:04,238 --> 00:27:06,154
to form a V-shaped valley.

376
00:27:07,612 --> 00:27:11,279
But a mile-thick glacier
takes no prisoners.

377
00:27:11,279 --> 00:27:15,528
It gouged out the sides
and the bottom of the river valley

378
00:27:15,528 --> 00:27:18,028
and turned it into a U-shaped riverbed.

379
00:27:20,194 --> 00:27:24,152
The Hudson River was now
navigable for big ships.

380
00:27:26,443 --> 00:27:30,568
The picture of modern-day
New York was almost complete.

381
00:27:32,609 --> 00:27:36,400
Long grooves in the rocks in
Central Park showed scientists

382
00:27:36,400 --> 00:27:41,150
that a vast ice sheet flowed over the
eroded remains of these mountains.

383
00:27:41,150 --> 00:27:45,066
And marks and glacial striations
on Bear Mountain

384
00:27:45,066 --> 00:27:48,232
proved this ice sheet was
at least four times higher

385
00:27:48,232 --> 00:27:49,899
than the Empire State Building.

386
00:27:53,024 --> 00:27:54,190
When the ice melted,

387
00:27:54,190 --> 00:27:58,939
it left a vast ridge of debris blocking
the Hudson River from the Atlantic.

388
00:28:00,147 --> 00:28:05,522
The final challenge for geologists was
to find out how the ridge was destroyed

389
00:28:05,522 --> 00:28:09,605
and how New York's harbour
opened to the oceans.

390
00:28:18,396 --> 00:28:23,270
New York today boasts one of
the largest natural harbours in the world.

391
00:28:23,270 --> 00:28:26,728
But it wasn't always that way.

392
00:28:26,728 --> 00:28:33,060
Towards the end of the last Ice Age,
the port's wide entrance was blocked.

393
00:28:33,060 --> 00:28:40,310
16,000 years ago, the melting glaciers
left behind a 220-foot-high wall of debris.

394
00:28:40,310 --> 00:28:43,142
The ridge stretched from Long Island
to Staten Island

395
00:28:43,142 --> 00:28:45,725
and forced the Hudson River
through a narrow,

396
00:28:45,725 --> 00:28:47,892
more westerly course to the ocean.

397
00:28:50,142 --> 00:28:53,808
What powerful forces
destroyed this rock jam?

398
00:28:53,808 --> 00:28:58,099
The prime suspect was a flash flood.

399
00:29:01,349 --> 00:29:06,306
But scientists needed evidence
to prove that such a flood had happened.

400
00:29:07,306 --> 00:29:11,055
In the 1960s, fishermen
made an unexpected find

401
00:29:11,055 --> 00:29:13,389
at the mouth of the Hudson River.

402
00:29:13,389 --> 00:29:19,555
They dredged up a giant mammoth tusk
from the depths of the sea floor.

403
00:29:19,555 --> 00:29:22,222
(TRUMPETS)

404
00:29:25,179 --> 00:29:29,304
Herds of these giant beasts
roamed the plains of North America

405
00:29:29,304 --> 00:29:34,136
before they became extinct
at the end of the last Ice Age.

406
00:29:38,636 --> 00:29:42,594
Finding the odd mammoth tusk here
and there is not so surprising.

407
00:29:42,594 --> 00:29:45,177
But since the initial discovery,

408
00:29:45,177 --> 00:29:48,385
scientists have found hundreds
more tusks and bones

409
00:29:48,385 --> 00:29:51,510
in the mouth of the Hudson River.

410
00:29:51,510 --> 00:29:55,676
It was as though a violent torrent
swept the mammoths away

411
00:29:55,676 --> 00:29:58,050
and dumped their remains off the coast.

412
00:29:58,050 --> 00:30:01,925
And there were more clues nearby.

413
00:30:04,592 --> 00:30:09,549
Huge boulders resting
on the sandy sea floor,

414
00:30:09,549 --> 00:30:13,174
some of them as big as cars.

415
00:30:13,174 --> 00:30:16,631
The boulders must have been part
of the ancient moraine

416
00:30:16,631 --> 00:30:20,255
that once ran
between Long Island and Staten Island.

417
00:30:22,006 --> 00:30:27,713
Geologist David Franzi knows that only
a raging torrent could have shifted them.

418
00:30:29,046 --> 00:30:31,504
Based on the size of the boulders
that we see here,

419
00:30:31,504 --> 00:30:34,296
we know that that flood
must have discharged

420
00:30:34,296 --> 00:30:38,378
on the order of 1.5 million cubic feet
per second.

421
00:30:39,712 --> 00:30:43,586
That's three times larger than the largest
Mississippi River flood ever recorded.

422
00:30:44,836 --> 00:30:48,461
And all that water had to
come from somewhere.

423
00:30:48,461 --> 00:30:51,544
Scientists began looking
for the source of this flood,

424
00:30:51,544 --> 00:30:57,876
a flood powerful enough to transport
huge boulders all the way to the sea.

425
00:30:57,876 --> 00:31:01,168
Rocks to a geologist are
like pages in a history book.

426
00:31:01,168 --> 00:31:05,750
For us, erosion oftentimes rips some
of the pages out of our history book,

427
00:31:05,750 --> 00:31:09,541
so it's the job of the geologist
to put together a fragmentary record

428
00:31:09,541 --> 00:31:12,916
into a coherent history of the events
that happened in the past.

429
00:31:14,708 --> 00:31:18,624
300 miles north of the city,
in upstate New York,

430
00:31:18,624 --> 00:31:20,915
Franzi tracked what might
have been the flood's path

431
00:31:20,915 --> 00:31:22,457
to an unusual grove of trees

432
00:31:22,457 --> 00:31:24,165
on Covey Hill

433
00:31:24,165 --> 00:31:25,998
in the Adirondack
Mountains.

434
00:31:28,706 --> 00:31:31,997
The trees are jack pines.

435
00:31:31,997 --> 00:31:36,288
They are rare in this area, where
the soil is usually fertile and deep.

436
00:31:38,330 --> 00:31:40,704
But on Covey Hill, their presence shows

437
00:31:40,704 --> 00:31:44,955
that there is no more than a few inches
of soil on top of the bedrock.

438
00:31:46,204 --> 00:31:48,079
The jack pine
is essentially rooted

439
00:31:48,079 --> 00:31:50,245
right on the top
of a rock's surface here.

440
00:31:50,245 --> 00:31:53,953
This is a bare sandstone surface,
very little mineral soil,

441
00:31:53,953 --> 00:31:58,244
and it's subject to prolonged periods
of dryness during the summertime.

442
00:31:58,244 --> 00:32:01,202
Jack pine's adaptations
make it able to survive here

443
00:32:01,202 --> 00:32:03,160
where no other tree species can.

444
00:32:05,118 --> 00:32:07,660
What happened to the soil?

445
00:32:10,118 --> 00:32:12,076
The jack pines continue to grow

446
00:32:12,076 --> 00:32:16,034
at the entrance of a long gorge
over 300 feet wide.

447
00:32:17,450 --> 00:32:21,575
Usually, gorges like this are cut down
over thousands of years,

448
00:32:21,575 --> 00:32:25,991
but in this case, the missing topsoil
points to a sudden flood event.

449
00:32:25,991 --> 00:32:31,407
A raging torrent must have ripped away
the soil and cut deep into the rock.

450
00:32:36,698 --> 00:32:40,198
In a helicopter,
Franzi follows the gorge west.

451
00:32:42,781 --> 00:32:45,613
Eventually, it opens
into a vast, empty basin

452
00:32:45,613 --> 00:32:50,863
located next to one of
the Great Lakes, Lake Ontario.

453
00:32:50,863 --> 00:32:54,362
It doesn't take much of a stretch
of the imagination here

454
00:32:54,362 --> 00:32:57,154
to imagine this valley filled with water

455
00:32:57,154 --> 00:33:00,945
and then with these hills
poking up through as islands.

456
00:33:02,570 --> 00:33:09,527
16,000 years ago, this basin was filled
with two billion cubic miles of water -

457
00:33:09,527 --> 00:33:12,777
a huge lake geologists
call Lake Iroquois.

458
00:33:12,777 --> 00:33:16,485
It formed at the end of the last Ice Age.

459
00:33:19,651 --> 00:33:24,693
As glaciers receded, the melt
waters slowly filled up the lake.

460
00:33:24,693 --> 00:33:27,900
The ice dams holding
the waters weakened.

461
00:33:27,900 --> 00:33:34,690
Eventually, the dams collapsed, causing
sudden and devastating flash floods.

462
00:33:34,690 --> 00:33:38,274
Lake level dropped
on the order of 70 feet

463
00:33:38,274 --> 00:33:41,315
and about 160 cubic miles of water

464
00:33:41,315 --> 00:33:44,273
were released into the
Champlain Valley, catastrophically.

465
00:33:44,273 --> 00:33:48,189
That floodwater would have
coursed down the Champlain Valley,

466
00:33:48,189 --> 00:33:51,647
through the Hudson Valley and
ultimately out into the Atlantic Ocean.

467
00:33:52,689 --> 00:33:57,480
The torrent raced towards
New York City, 300 miles to the south,

468
00:33:57,480 --> 00:34:00,479
then took the straightest course
to the sea.

469
00:34:00,479 --> 00:34:04,020
The floodwaters smashed into
the ancient moraine,

470
00:34:04,020 --> 00:34:08,896
the huge pile of debris blocking
the direct exit of the Hudson River.

471
00:34:13,561 --> 00:34:17,102
The bridge we see behind me
spans the channel that was cut

472
00:34:17,102 --> 00:34:18,644
by the flood event.

473
00:34:18,644 --> 00:34:21,602
When the flood wave came through,
it was of sufficient intensity

474
00:34:21,602 --> 00:34:25,851
to over-top the dam
and very rapidly cut the channel.

475
00:34:28,392 --> 00:34:31,642
The gap that was created
by the flood still exists.

476
00:34:31,642 --> 00:34:35,684
It's now a tidal strait called the Narrows.

477
00:34:37,183 --> 00:34:41,766
Today, the gap is spanned
by the Verrazano Bridge.

478
00:34:41,766 --> 00:34:45,641
The channel is deep enough
for even the biggest ocean-going ships.

479
00:34:45,641 --> 00:34:50,474
It's the most important entrance
to New York City's harbour.

480
00:34:54,265 --> 00:34:57,722
Mammoth tusks and huge boulders
at the mouth of the river

481
00:34:57,722 --> 00:35:01,347
showed scientists that there was
a torrent big enough to blast a hole

482
00:35:01,347 --> 00:35:03,555
through the ancient moraine.

483
00:35:03,555 --> 00:35:09,055
And a channel leading towards the Great
Lakes revealed the source of the flood.

484
00:35:09,055 --> 00:35:11,805
It was this flood that created
the Narrows

485
00:35:11,805 --> 00:35:16,303
and gave New York a wide entrance
to its port.

486
00:35:16,303 --> 00:35:21,095
A unique geology laid down
the foundations for New York City.

487
00:35:24,845 --> 00:35:28,594
But the same forces that constructed it
may also have sown the seeds

488
00:35:28,594 --> 00:35:30,927
for New York's destruction.

489
00:35:37,676 --> 00:35:44,342
Scientists have pieced together the
half-billion-year history of New York City.

490
00:35:44,342 --> 00:35:50,341
Huge mountains, volcanic eruptions
and glacial ice shaped the area.

491
00:35:50,341 --> 00:35:53,799
But New York's story doesn't end here.

492
00:35:56,091 --> 00:36:00,382
The geology that created one
of the greatest cities on Earth

493
00:36:00,382 --> 00:36:03,714
also has the potential to destroy it.

494
00:36:05,631 --> 00:36:09,131
Experts have been studying
the potential threat to the city.

495
00:36:09,131 --> 00:36:11,714
We're standing here
in Lower Manhattan

496
00:36:11,714 --> 00:36:13,047
on one of our major thoroughfares,

497
00:36:13,047 --> 00:36:14,089
Canal Street.

498
00:36:14,089 --> 00:36:16,547
And it's important, because in 1821,

499
00:36:16,547 --> 00:36:22,879
a Category 2 hurricane raised the water
level at the Battery 13 feet in one hour

500
00:36:22,879 --> 00:36:26,379
and, literally, the Hudson River
met the East River

501
00:36:26,379 --> 00:36:29,712
and Canal Street was covered by water

502
00:36:29,712 --> 00:36:34,877
and Manhattan was actually two islands
for three hours, until the water receded.

503
00:36:37,669 --> 00:36:42,085
New York City is vulnerable
because of its position on the coast.

504
00:36:44,710 --> 00:36:50,584
Long Island stretches northeast at a
right angle from the New Jersey shore.

505
00:36:50,584 --> 00:36:55,000
New York City is nestled behind
the western end of Long Island.

506
00:36:55,000 --> 00:36:56,833
Normally, the island protects the city

507
00:36:56,833 --> 00:36:58,333
from the sea,

508
00:36:58,333 --> 00:37:02,125
but when hurricanes threaten,
the opposite is true.

509
00:37:02,125 --> 00:37:05,998
Long Island becomes
a dangerous liability.

510
00:37:08,207 --> 00:37:12,331
Hurricanes racing north along
the beaches of the Atlantic coast

511
00:37:12,331 --> 00:37:15,498
pile up huge bulges of water
in front of them.

512
00:37:15,498 --> 00:37:17,956
They're called storm surges.

513
00:37:18,998 --> 00:37:21,580
Hitting the right-angled junction
at Long Island,

514
00:37:21,580 --> 00:37:24,830
the winds funnel the storm surge in
through the Narrows,

515
00:37:24,830 --> 00:37:28,330
the gap between Long Island
and New Jersey.

516
00:37:28,330 --> 00:37:32,496
This is the place, at the actual apex
of the right angle in New York

517
00:37:32,496 --> 00:37:37,328
where all the water being pushed
by a hurricane would be concentrated.

518
00:37:37,328 --> 00:37:39,870
And in the distance
is the Verrazano Bridge,

519
00:37:39,870 --> 00:37:43,828
and all that water is gonna go through
the passage we call the Narrows

520
00:37:43,828 --> 00:37:46,535
and it's gonna be accelerated
towards New York City,

521
00:37:46,535 --> 00:37:50,161
where it will rise to abnormal heights.

522
00:37:55,535 --> 00:37:58,409
Experts believe that in the United States,

523
00:37:58,409 --> 00:38:03,159
New York is the third most vulnerable
city after Miami and New Orleans

524
00:38:03,159 --> 00:38:05,200
to a hurricane disaster.

525
00:38:06,242 --> 00:38:10,491
If it was hit today, the consequences
would be serious.

526
00:38:10,491 --> 00:38:15,741
New York City is hit by hurricanes
only infrequently.

527
00:38:15,741 --> 00:38:21,324
Like, in 1821 and in 1893 and in 1938.

528
00:38:21,324 --> 00:38:24,156
However, the point is that the hurricane

529
00:38:24,156 --> 00:38:28,698
that will eventually hit New York City
again will be catastrophic,

530
00:38:28,698 --> 00:38:31,780
and what is going to happen
when the utilities are knocked out?

531
00:38:31,780 --> 00:38:35,655
What is going to happen when
salt water reaches into the subways

532
00:38:35,655 --> 00:38:38,446
and ruins the electrical system?

533
00:38:38,446 --> 00:38:40,737
We're talking about unbelievable
amounts of money

534
00:38:40,737 --> 00:38:42,904
to restore the infrastructure.

535
00:38:42,904 --> 00:38:46,279
We're talking about setbacks
and delays in commerce

536
00:38:46,279 --> 00:38:51,653
and banking and transportation,
a catastrophe that's never been seen.

537
00:38:54,320 --> 00:38:58,485
Storm surges are not the only threat
to New York's future.

538
00:39:00,569 --> 00:39:06,526
Earthquakes are also part of the vast
geological forces that shape this area.

539
00:39:06,526 --> 00:39:08,693
They are still at work today.

540
00:39:10,984 --> 00:39:14,817
Some could change the city
in an instant.

541
00:39:17,150 --> 00:39:20,525
November 4th 1884.

542
00:39:20,525 --> 00:39:25,232
New York City was shaken by an
earthquake that lasted ten seconds.

543
00:39:25,232 --> 00:39:29,190
The Brooklyn Bridge swayed
and people panicked.

544
00:39:29,190 --> 00:39:34,523
The earthquake showed 5.5
on the Richter scale.

545
00:39:35,523 --> 00:39:40,855
January 17th 2001,
New York City was struck again.

546
00:39:42,397 --> 00:39:46,854
This time the quake was
relatively small, only 2.4,

547
00:39:46,854 --> 00:39:51,563
but it struck right under 125th Street.

548
00:39:51,563 --> 00:39:55,479
The earthquake in 2001
is the first earthquake

549
00:39:55,479 --> 00:39:59,436
that we could confidently locate
in Manhattan,

550
00:39:59,436 --> 00:40:04,145
that's its claim to fame, it was felt widely.

551
00:40:14,393 --> 00:40:18,934
It's impossible to study
the cause of the quakes at the surface.

552
00:40:20,559 --> 00:40:23,892
The evidence is buried beneath the city.

553
00:40:26,642 --> 00:40:29,058
Deep within New York's bedrock,

554
00:40:29,058 --> 00:40:34,058
seismologist Leonardo Seeber
studies the cause of these quakes.

555
00:40:35,057 --> 00:40:36,599
(HORN BLARES)

556
00:40:38,932 --> 00:40:43,556
In a subway tunnel 100 feet beneath
the bedrock under the East River,

557
00:40:43,556 --> 00:40:45,764
there is a ready-made laboratory.

558
00:40:45,764 --> 00:40:50,222
Here, Seeber can study the rocks
up close and personal.

559
00:40:52,305 --> 00:40:56,054
It is the same bedrock
Manhattan is built on.

560
00:40:56,054 --> 00:41:00,179
But Seeber fears it isn't as
solid as once was thought.

561
00:41:01,304 --> 00:41:07,179
New York area is considered
a seismic zone,

562
00:41:07,179 --> 00:41:11,094
meaning there is a cluster
of known earthquakes

563
00:41:11,094 --> 00:41:12,886
that have occurred in this area.

564
00:41:12,886 --> 00:41:19,093
So we are, as geologists, very eager
to discover which faults are responsible

565
00:41:19,093 --> 00:41:20,593
for these earthquakes.

566
00:41:22,010 --> 00:41:24,717
The majority of earthquakes
occur at the boundaries

567
00:41:24,717 --> 00:41:27,842
between separate sections
of the Earth's crust,

568
00:41:27,842 --> 00:41:31,675
the tectonic plates
on which the continents sit.

569
00:41:31,675 --> 00:41:35,175
But New York's earthquakes
are different.

570
00:41:35,175 --> 00:41:38,382
The city is firmly in the middle
of a tectonic plate,

571
00:41:38,382 --> 00:41:41,466
halfway between the
mid-Atlantic ridge to the east

572
00:41:41,466 --> 00:41:44,341
and the San Andreas Fault
to the west.

573
00:41:47,091 --> 00:41:50,548
Seeber is anxious to discover
what's going on.

574
00:41:51,798 --> 00:41:56,423
As he examines the walls of the tunnel,
he comes across a possible clue.

575
00:41:57,797 --> 00:42:01,547
The long fractures in the rock
are fault lines that formed

576
00:42:01,547 --> 00:42:03,880
when pressure built up.

577
00:42:03,880 --> 00:42:08,046
As the tension was released,
the rock cracked and shifted.

578
00:42:08,046 --> 00:42:11,837
This is felt on the surface
as an earthquake.

579
00:42:11,837 --> 00:42:14,379
SEEBER: This is an example
of a very small fault,

580
00:42:14,379 --> 00:42:20,712
but it's a fault that probably did
generate some small earthquakes.

581
00:42:20,712 --> 00:42:22,836
When one of these faults
generates an earthquake,

582
00:42:22,836 --> 00:42:29,585
we think that perhaps other faults of the
same family can generate earthquakes.

583
00:42:31,501 --> 00:42:34,043
These faults in New York's bedrock
are evidence

584
00:42:34,043 --> 00:42:38,501
that the area was hit by earthquakes
in the past.

585
00:42:38,501 --> 00:42:44,667
But Seeber has no way of knowing if
the faults are still active and dangerous.

586
00:42:48,333 --> 00:42:51,124
If a large earthquake
hit New York today,

587
00:42:51,124 --> 00:42:54,457
the consequences
would be catastrophic.

588
00:42:55,582 --> 00:42:57,623
A large proportion
of New York City buildings

589
00:42:57,623 --> 00:43:00,582
are simply not built to withstand
earthquake shaking.

590
00:43:00,582 --> 00:43:03,665
We worry about transportation tunnels,

591
00:43:03,665 --> 00:43:06,456
in particular, tunnels that traverse rivers

592
00:43:06,456 --> 00:43:09,789
where parts of the tunnels
are rooted in solid rock

593
00:43:09,789 --> 00:43:12,080
and other parts
are resting on soft sediment.

594
00:43:12,080 --> 00:43:14,330
The oscillation of these
two different materials

595
00:43:14,330 --> 00:43:17,079
could cause severe
cracking and fracturing.

596
00:43:17,079 --> 00:43:20,413
The infrastructure
would be severely damaged,

597
00:43:20,413 --> 00:43:25,245
it would take tens of years to repair the
damage caused by such a large event.

598
00:43:26,829 --> 00:43:29,745
With the evidence geologists
have collected,

599
00:43:29,745 --> 00:43:34,119
the story of the creation of
New York City can now be told.

600
00:43:35,202 --> 00:43:40,494
The city's bedrock was formed under
a chain of mountains over a mile high.

601
00:43:40,494 --> 00:43:44,785
Volcanoes and lava fields
over millions of square miles

602
00:43:44,785 --> 00:43:50,617
split up the ancient supercontinent and
created the east coast of North America.

603
00:43:50,617 --> 00:43:54,366
Glacial ice, four times as high
as the Empire State building,

604
00:43:54,366 --> 00:43:56,991
carved out the deep Hudson River.

605
00:43:56,991 --> 00:44:00,324
A catastrophic flash flood
broke through the moraine

606
00:44:00,324 --> 00:44:05,532
to form the Narrows and opened up
New York City's harbour to the oceans.

607
00:44:09,864 --> 00:44:12,406
Looking ahead to the distant future,

608
00:44:12,406 --> 00:44:15,989
geologists see more
challenging times for the city.

609
00:44:17,031 --> 00:44:18,905
In 40,000 years,

610
00:44:18,905 --> 00:44:22,905
they predict this region will
be engulfed by another ice sheet.

611
00:44:23,905 --> 00:44:29,571
And in 250 million years,
the Atlantic will start to shrink again.

612
00:44:29,571 --> 00:44:34,654
Europe and Africa will eventually
crash back into the American coast.

613
00:44:34,654 --> 00:44:38,028
The fossilised remains of the
once great city of New York

614
00:44:38,028 --> 00:44:43,194
will become just another layer of rock
in a vast new mountain range.

615
00:44:43,194 --> 00:44:48,486
A footnote in the immense,
ever-changing story of planet Earth.


