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1
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Right across our planet, there is an
incredible variety of astonishing
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landscapes.
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00:00:16,309 --> 00:00:23,290
One of the most beautiful anywhere in
the world is Northern Ireland's Causeway
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Coast.
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00:00:32,720 --> 00:00:35,960
Piles of breathtaking cliffs arising
from the sea.
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00:00:38,000 --> 00:00:43,800
A coastline of wonders that has stood
here for millions of years before
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walked this coast.
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Two fragments of dinosaur bone have been
found here at the Gobbins in these
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Jurassic clades, and these are the only
dinosaurs known from anywhere in
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Ireland.
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00:01:01,710 --> 00:01:06,790
This coastline boasts some of the most
extraordinary natural phenomena
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These incredible stepping stones, which
they really almost don't look natural.
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They look like something man -made by a
giant with a hammer and a chisel.
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00:01:21,550 --> 00:01:25,470
And an abundant array of species have
blossomed here.
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When you look around, the scenery, the
people, the heritage, the glances are
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part of my DNA.
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We're going to take you on a journey
along the Irish Causeway Coast to
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admire its wonders and discover
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its secrets.
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Our journey begins at the great city of
Londonderry, or Derry, on the north
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coast of Northern Ireland.
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The city sits on the calm waters of Loch
Foyle, but seafarers have a route
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through a narrow passage straight out to
the wilds of the Atlantic Ocean.
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Viewed from space, The unusual shape of
the lock is striking.
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Almost fully encircled by land, it has a
tiny opening leading into the North
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Atlantic Sea at the top of the estuary.
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Our journey takes us east along one of
the most incredible coastlines anywhere.
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Rare birds relish this landscape, like
the black -tailed godwit and the
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cormorant, a diving bird who feeds off
these shores.
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From Loch Foyle, the earth rises steeply
upwards.
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It's our first sight of the great rock
formations that shape the whole
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of Northern Ireland.
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the aftermath of a series of great
volcanic eruptions that we know by the
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prosaic name of the Antrim Plateau.
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And the first great peak, rising 400
metres above the sea, is Mount Benevena.
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On a clear day, there are spectacular
panoramic views from here for miles.
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down to the peninsula of the McGilligan
Point and across to Donegal Beyond.
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Benevena is a special area of
conservation and has been recognised for
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coniferous juniper trees and a unique
assemblage of arctic alpine plants.
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The summit's hard impermeable rock is
perfect for retaining water and a lake
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formed, the ideal habitat for trout.
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From Benevena's lookout point, Downhill
House and Mussenden Temple stand out on
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the coast below.
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Built in 1780 for the Bishop of Derry,
the house and temple are perched on the
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edge of this exposed headland.
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But the estate suffered a devastating
fire in 1851, and the landscape here has
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almost engulfed it.
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The temple once served as a library for
the bishop's niece.
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But today it looks certain to tumble
down the cliffs and into the sea.
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What awaits us only a little further
east along the coast is a natural
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phenomenon that seems to come from a
vividly imagined dream.
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A place that has captured the
imagination of everyone who sees it.
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for many centuries past.
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We know it today by its mythological
name, the Giant's Causeway.
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The sheer strangeness of this place
defies belief.
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Writer Lolly Spence has found that an
interest in the Giant's Causeway has
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into more of an obsession.
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She finds herself returning here again
and again.
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I have grown up and lived and worked in
Northern Ireland all my life.
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My mother's family came across from
Scotland to live on the Antrim coast,
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over the water behind us here.
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And this Antrim coast road has really
been part of my upbringing.
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800 miles to the north, we have Iceland.
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00:07:05,080 --> 00:07:10,840
2 ,000 miles to the west, we have
Newfoundland. And under these cliffs, at
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edge of the world, we're looking at, on
the very north coast of Ireland, is the
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00:07:16,980 --> 00:07:23,640
Great Antrim Plateau, a huge basalt
landscape crashing into the North
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Atlantic Ocean here.
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00:07:34,990 --> 00:07:41,030
Giants collide, this massive volcanic
land mass hitting the mighty waters of
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00:07:41,030 --> 00:07:42,330
Atlantic Ocean.
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00:07:43,310 --> 00:07:49,590
And it almost slides away, this
honeycomb of rock, this basalt pavement
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under the waters of the Atlantic.
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This causeway never looks the same
twice.
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I have been the only person here. I have
been here with thousands of tourists.
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I've been here in the winter when the
rainwater had frozen in the cavities and
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the rocks when it was really cold.
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00:08:26,800 --> 00:08:29,280
And I have been here in glorious
sunshine.
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And of course on a day like this.
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Even the rain here feels fresher and
cleaner, certainly wetter.
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Viewed from above, the Giant's Causeway
is like a finger jutting straight out
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from the shoreline into the sea.
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It was formed by a volcanic eruption 60
million years ago.
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And a fascination around their formation
has brought tourists and scientists
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flocking to this area for generations.
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00:09:06,370 --> 00:09:11,570
It all began in the Palaeogene period
over 20 million years ago.
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00:09:12,830 --> 00:09:18,370
The molten lava rolls up through those
fissures and spread out to make an
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enormous lava lake.
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00:09:22,330 --> 00:09:25,910
Then over time, this slowed, it slowly
cooled.
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And as it cooled, you think of a puddle
at the side of the road, just a puddle
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of rainwater.
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00:09:31,250 --> 00:09:36,150
And as that dries out, you see the mud
in it beginning to crack itself. You
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the cracked mud in a puddle? Well, here
this happened on a larger, longer scale.
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The lava cooled over decades and
millennia. And as it cooled, it shrank.
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And because it cools so slowly and so
regularly, it formed these columns.
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00:09:57,560 --> 00:10:03,700
These incredible stepping stones, which
they really almost don't look natural.
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00:10:03,760 --> 00:10:07,960
They look like something man -made by a
giant with a hammer and a chisel.
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00:10:08,560 --> 00:10:13,980
Its wondrous hexagonal formations here
gave rise to a rich mythological
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explanation of its origins.
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Everything. about this place is colossal
in scale.
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00:10:21,020 --> 00:10:27,700
And as we walk into this giant
amphitheater with giant cliff tops and
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waves, it makes us, of course, wonder
about the old myth of who it was that
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actually built this.
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Ireland is full of myths and legends.
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00:10:42,120 --> 00:10:47,320
And one of our most famous giants is
Finn McCool, the mighty warrior.
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of the Celtic tail.
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Finn McCool had one enemy in all of the
world, the Scottish giant, Ben Andona,
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the Mountain of Thunder.
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These two giants, challenging each other
to a fight, couldn't get at each other
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because of the might you see.
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And so both giants set to, to make a
causeway.
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00:11:26,700 --> 00:11:32,040
The legend continues about how one day
Finn McCool was taking a rest from his
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labours. His wife Una, looking through
the window, spotted the Scottish giant
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drawing near. He had finished the
causeway. He was much bigger than her
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She knew for sure that he would defeat
Finn McCool in any combat.
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And so Una called Finn into the house.
She said, Finn.
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I want you to get into that cradle. I
want you to pretend to be a baby with
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thumb in your mouth.
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Our legend says when Ben and Donna
looked into that cradle and saw the size
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Finn McCool's baby, as he thought, with
its truly formed beard and its enormous
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size... He thought, I'm not staying
around to fight the father of a baby
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this. And carrying back to Scotland, he
was in such a hurry that he left his
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boot on the shore, where we can still
see the giant's boot over there.
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He tore up the causeway behind him for
fear that Finn McCool would follow.
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Everything about this place was just on
a giant scale.
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The giant honeycomb stepping stones, the
giant waves crashing.
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It was a place of inspiration to modern
writers, people like our own Seamus
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Heaney, who won the Nobel Prize for
Literature. He loved the giant causeway
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was very much inspired by this landscape
on the north of Antrim.
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For some Irish people, the Giant's
Causeway is simply the eighth wonder of
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world.
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00:13:18,080 --> 00:13:21,780
But it's only the first of the wonders
of the Causeway Coast.
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Its islands and seas have their own
fascinating stories to tell.
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From the Giant's Causeway, three miles
of cliffs and coves lead us to the mouth
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of the River Bush, whose tributary
provides
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an ideal sweet water supply for whiskey
-making on the Antrim coast.
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Just off this coast is Carrica Reed, a
tiny uninhabited island.
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There are no people, but from time
immemorial, there have been countless
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thousands of fish.
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Centuries ago, fishermen built a rope
bridge to reach the rich stocks of
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travelling from the Atlantic and
returning home here to the river's bush
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band to spawn.
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And the bridge, rebuilt and
strengthened, remains to this day, even
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salmon population, victims of
overfishing and pollution, has dwindled
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nothing.
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A larger island, big enough to be
inhabited, sits just north of the
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coast, only six miles from the
shoreline.
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Here, viewed from above the Mull of
Kintyre, the edge of Scotland seems to
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almost reach out and touch its near
neighbour.
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We're heading to the island shores, home
to 150 people and tens of
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thousands of creatures of the sea.
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One person who has made the journey
across this stretch of water all his
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life. He's Richard Lafferty.
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Richard ferries the island's residents
and curious visitors to and fro.
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For him, the seas around Rathlin Island
with their long history are like a
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second home.
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That's a fantastic place for the
wildlife.
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The islanders now survive on the island
by a bit of tourism, fishing.
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And also now they've got a kelp farm
where they harvest seaweed and people
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that now for food.
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And the island over the years has been
very famous for its smuggling.
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People over the years have travelled and
always have had to pass it. So the
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Vikings have been here, the English have
been here, obviously the Irish, the
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Scots. And many a battle has been fought
on the island.
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At this small stretch of water, which he
must cross, the force of the Atlantic
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Ocean is pressed through a sea passage
only six miles wide.
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And what we have is we have the whole
Irish Sea emptying and the Atlantic
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coming in when the tides change.
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That over the years has caused a lot of
problems for mariners.
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We've got wrecks from every era.
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And some of the most famous wrecks are
some of our war wrecks.
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In one day alone, a German U -boat sunk
three British warships in this Rathland
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Sound.
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We have two British warships just
sitting here now about half a mile to
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north of us.
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The most famous sea wreck happened
several hundred years earlier.
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Lagerona was dashed on the Causeway's
Rocks in 1588.
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The ship was part of the Spanish Armada,
who were fleeing the English fleet.
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Over 1 ,300 men lost their lives, making
it the biggest shipwreck disaster
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Ireland or Spain has ever seen.
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Just nine sailors survived and scrambled
ashore at Dunluce Castle.
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helped by the members of the ruling
MacDonald clan.
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Legend has it that they raided the
ship's washed -up booty using the
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rebuild their castle.
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La Llorona lay at the bottom of the
ocean for 400 years, but in 1967, the
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remainder of the ship's hoard of gold
was discovered by divers in these
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treacherous waters.
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Rattle -in -sounds waters may be
perilous for humans, but wildlife is
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at home here.
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The ocean currents, certain times of
year, the water's thick with plankton,
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that plankton is a food for marine
creatures.
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The island's wild, it's spectacular.
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The marine life on it's intense, bird
life, fish life, corals.
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00:18:55,230 --> 00:18:58,510
We're lucky enough that we will see the
bastion shark. They're feeding the
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plankton generally near the surface.
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It can be up to about seven, eight, nine
meters long and two or three meters
195
00:19:05,030 --> 00:19:08,950
wide. So not as big as this boat, but
not far off it. But a really impressive
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00:19:08,950 --> 00:19:10,830
creature to see in our water.
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00:19:14,190 --> 00:19:17,710
You never know what you're going to see.
There's some fantastic interactions
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00:19:17,710 --> 00:19:20,330
with the dolphins, whales and bird life.
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00:19:46,280 --> 00:19:51,300
Rathlin Island's 70 -metre -high basalt
cliffs are home to Northern Ireland's
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00:19:51,300 --> 00:19:58,020
biggest colony of breeding seabirds,
including the kittiwake, a
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00:19:58,020 --> 00:19:59,880
gull named after her bird call.
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00:20:03,720 --> 00:20:06,320
Because of their remote nesting areas,
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00:20:07,040 --> 00:20:12,360
their young are one of the few chicks
that are white at birth, as they don't
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00:20:12,360 --> 00:20:13,360
require camouflage.
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00:20:14,010 --> 00:20:16,310
like the chicks of more vulnerable
species.
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00:20:23,570 --> 00:20:28,770
Their young instinctively know to stay
still so they don't fall to certain
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00:20:28,770 --> 00:20:31,050
on the rocks below their cliffside nest.
208
00:20:34,790 --> 00:20:39,770
Among the thronging masses of birdlife
on Rathlin are the puffins.
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00:20:40,240 --> 00:20:44,100
who arrive like clockwork in March each
year for the breeding season.
210
00:20:49,940 --> 00:20:54,920
Puffins usually lay just one egg per
season, choosing the same mate.
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00:20:55,740 --> 00:20:59,500
The puffins' chatter on rattling
dominates the cliffs.
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00:20:59,760 --> 00:21:03,620
Whilst at sea, they remain perfectly
silent.
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00:21:09,390 --> 00:21:13,310
Also enjoying the coves of Ratlin at low
tide are the seals.
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00:21:13,890 --> 00:21:19,130
The island has a population of up to 1
,500 grey and harbour seals.
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00:21:20,970 --> 00:21:25,230
But they are not the only creatures to
take refuge on Ratlin.
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00:21:30,070 --> 00:21:36,030
In 1306, Robert the Bruce, King of
Scots, is said to have retreated to a
217
00:21:36,030 --> 00:21:38,490
Ratlin after being defeated by the
English.
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00:21:41,160 --> 00:21:46,820
Legend has it that observing an
industrious spider here inspired him to
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00:21:46,820 --> 00:21:49,420
to Scotland and fight for independence.
220
00:21:51,440 --> 00:21:56,740
And today these legends have been
replaced by fantasy through the famous
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00:21:56,740 --> 00:21:59,340
series filmed around the Causeway Coast.
222
00:22:01,980 --> 00:22:06,600
This whole area is famous for the Game
of Thrones scene. And we've got quite a
223
00:22:06,600 --> 00:22:08,840
few sites that have been made famous by
this series.
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00:22:09,440 --> 00:22:13,880
For example, behind us we've got
Dragonstone, where Jon Snow pitted the
225
00:22:13,880 --> 00:22:15,460
for the first time here at Fairhead.
226
00:22:27,840 --> 00:22:29,960
And we've got Slaver's Bay in Murloc
Bay.
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00:22:31,700 --> 00:22:35,140
Why does Game of Thrones come here?
Because they have such diverse geology,
228
00:22:35,520 --> 00:22:37,180
fantastic backdrops to the scenes.
229
00:22:39,690 --> 00:22:44,170
Other local places lend their atmosphere
and history to the filming.
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00:22:45,990 --> 00:22:52,690
Like the dark hedges of Amoy, a road
flanked by 150 beech
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00:22:52,690 --> 00:22:57,530
trees, planted to provide a grand
pathway to a local mansion.
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00:23:02,230 --> 00:23:06,910
Local legend has it that the hedges are
haunted by a grey lady.
233
00:23:17,230 --> 00:23:22,210
As we travel south along Northern
Ireland's causeway coast, we're going to
234
00:23:22,210 --> 00:23:27,710
tempted inland by the sight of a gentle
rise in the land known as Knockdew.
235
00:23:40,430 --> 00:23:43,510
But this is no naturally occurring hill.
236
00:23:47,340 --> 00:23:51,920
It's a Bronze Age fort, which dates to
around 2000 BC.
237
00:23:53,180 --> 00:23:59,120
A series of massive earthworks, three
banks, and dishes running for 300 meters
238
00:23:59,120 --> 00:24:01,100
and protecting the approaches.
239
00:24:03,420 --> 00:24:07,660
Excavations reveal the structures of
round houses inside the fort.
240
00:24:08,440 --> 00:24:13,640
A community must have lived here for
hundreds of years, up on the hills, even
241
00:24:13,640 --> 00:24:15,780
during the ravages of winter.
242
00:24:20,780 --> 00:24:26,020
4 ,000 years ago, the inhabitants would
have braved the fierce Atlantic winds
243
00:24:26,020 --> 00:24:29,900
from this lookout point, protecting
their homestead.
244
00:24:32,620 --> 00:24:39,160
We head inland on the wings of the
endangered Hen Harrier, whose population
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00:24:39,160 --> 00:24:45,920
in the Antrim Hills has dwindled by 80%.
He flies above the
246
00:24:45,920 --> 00:24:49,860
Antrim Plateau, an exposed and desolate
landscape.
247
00:24:50,590 --> 00:24:53,010
which has its own wild beauty.
248
00:25:05,310 --> 00:25:12,290
The male hen harrier, with its
distinctive white rump,
249
00:25:12,390 --> 00:25:14,430
provides food for the female.
250
00:25:15,230 --> 00:25:17,870
He settles at his stronghold.
251
00:25:18,250 --> 00:25:24,330
on the 800 metre long and 200 metre wide
Slemish Mountain, making his nest on
252
00:25:24,330 --> 00:25:26,670
the ground amongst the heather.
253
00:25:36,850 --> 00:25:41,870
Slemish is Northern Ireland's largest
volcanic plug, or lava neck,
254
00:25:42,130 --> 00:25:47,530
formed when magna hardened right at the
volcano's vent.
255
00:25:48,270 --> 00:25:52,910
the resulting dolerite rock is harder
than the rock that surrounds it, which
256
00:25:52,910 --> 00:25:55,790
why Flemish has not been eroded by
glaciers.
257
00:26:01,190 --> 00:26:07,130
According to legend, it was the first
known Irish home of St. Patrick, who was
258
00:26:07,130 --> 00:26:09,770
enslaved here as a boy working as a
shepherd.
259
00:26:12,430 --> 00:26:18,700
He is said to have found religious faith
on Flemish and the mountain, is now a
260
00:26:18,700 --> 00:26:19,820
place of pilgrimage.
261
00:26:29,640 --> 00:26:35,020
Seen from space, just south of Slemish,
another great landmark appears.
262
00:26:35,720 --> 00:26:42,000
Like a gigantic splat of ink, Loch Nei
sits in the center of the Antrim
263
00:26:42,880 --> 00:26:48,350
Formed 60 million years ago after
volcanic eruptions ceased, and the
264
00:26:48,350 --> 00:26:50,050
crust lowly sagged.
265
00:26:50,490 --> 00:26:56,710
Loch Ness' 115 square miles of fresh
water make it the biggest lake in the
266
00:26:56,710 --> 00:26:57,710
British Isles.
267
00:27:03,790 --> 00:27:09,630
Staying inland, we're heading north to
the Valley of Glenariff, known as the
268
00:27:09,630 --> 00:27:11,730
Queen of the Antrim Glens.
269
00:27:17,960 --> 00:27:22,460
It's just one of the nine valleys which
crisscross over the Anthem Plateau,
270
00:27:22,460 --> 00:27:26,260
leaving a blanket of green flanking the
causeway coast.
271
00:27:29,040 --> 00:27:34,160
Before the coast road was built here in
the 1830s, the glens were isolated from
272
00:27:34,160 --> 00:27:38,580
the rest of the country, and it was
easier to travel here by sea.
273
00:27:40,900 --> 00:27:45,200
So a strategically placed fort was
needed to protect the glen shores.
274
00:27:46,140 --> 00:27:49,860
and the fertile land surrounding it from
Scottish invaders.
275
00:27:55,500 --> 00:28:00,960
John Robin is a local historian and
direct descendant of the glensmen who
276
00:28:00,960 --> 00:28:04,480
ploughed this fertile land over 400
years ago.
277
00:28:05,800 --> 00:28:10,520
During the 16th and 17th centuries,
there was a heavy influx of Scottish
278
00:28:10,520 --> 00:28:14,340
settlers here due to this coast's
proximity to Scotland.
279
00:28:16,149 --> 00:28:21,030
resulting in an affinity between the two
countries that still felt today.
280
00:28:21,870 --> 00:28:26,870
I come from a long line of Glen's men,
and I am proud to call myself a Glen's
281
00:28:26,870 --> 00:28:27,870
man.
282
00:28:27,950 --> 00:28:33,510
And the first mention of my name in the
Glen's was in 1652.
283
00:28:34,950 --> 00:28:41,110
We are a mere 15 miles from the Scottish
coast. We can clearly see the Mullifcan
284
00:28:41,110 --> 00:28:43,650
Tyre and the Scottish mainland from
here.
285
00:28:44,120 --> 00:28:48,680
And it's basically so close that it's no
wonder that we were all part of the
286
00:28:48,680 --> 00:28:52,820
same kingdom for many, many hundreds of
years, the kingdom of Dalriada.
287
00:28:55,640 --> 00:29:00,300
This site of Red Bay Castle is said to
have been used by the 5th century
288
00:29:00,300 --> 00:29:04,840
kingdom, who ruled parts of early Celtic
Ireland from mainland Scotland.
289
00:29:07,680 --> 00:29:10,940
What's left of the castle today is 16th
century.
290
00:29:13,550 --> 00:29:18,550
The castle itself withstood many sieges
during its time. One of the most famous
291
00:29:18,550 --> 00:29:25,270
was in 1565 when Shane O 'Neill, a
warlord from Mid Ulster, at the
292
00:29:25,270 --> 00:29:30,150
behest of Queen Elizabeth I, decided
that he was going to oust the Macdonalds
293
00:29:30,150 --> 00:29:31,129
from the area.
294
00:29:31,130 --> 00:29:36,650
He came down through Glen Arras, he
burned everything, he sacked the castle,
295
00:29:36,650 --> 00:29:39,490
took two of the main Macdonalds
prisoners.
296
00:29:43,870 --> 00:29:48,270
The McDonalds won their castle back and
rebuilt it from the local stone.
297
00:29:51,290 --> 00:29:55,150
Well, you can see that there are two
types of stone here.
298
00:29:55,450 --> 00:30:00,330
One is the red sandstone. You can see
how red it actually is.
299
00:30:00,670 --> 00:30:02,590
And then you've got the basalt.
300
00:30:02,950 --> 00:30:04,670
The basalt will be harder.
301
00:30:05,430 --> 00:30:06,890
There's a good basalt there.
302
00:30:07,450 --> 00:30:11,950
But no matter how hard the stone was,
the castle couldn't withstand...
303
00:30:12,670 --> 00:30:18,330
the bombardment by Cromwellian forces in
the 1650s, which left us with the ruins
304
00:30:18,330 --> 00:30:19,330
that we have today.
305
00:30:21,630 --> 00:30:27,370
In retaliation against the 17th century
Catholic rebellion, Oliver Cromwell led
306
00:30:27,370 --> 00:30:32,170
a brutal conquest of Ireland, destroying
the native landowning classes and
307
00:30:32,170 --> 00:30:35,210
replacing them with colonists from the
mainland.
308
00:30:43,220 --> 00:30:48,600
Today's landscape has experienced layers
of geological history over millions of
309
00:30:48,600 --> 00:30:54,960
years. But it was just 20 ,000 years ago
that it was engulfed during the Ice
310
00:30:54,960 --> 00:30:55,960
Age.
311
00:30:56,620 --> 00:31:01,580
At the end of this period, the corries,
or V -shaped gaps between the hills,
312
00:31:01,800 --> 00:31:03,100
were smothered in ice.
313
00:31:03,340 --> 00:31:07,680
But as the glaciers thawed, they moved
towards the sea.
314
00:31:08,320 --> 00:31:14,040
taking land with them and flattening the
gaps to form a perfect U -shaped valley
315
00:31:14,040 --> 00:31:19,020
with an unspoilt sandy beach at the foot
of the glen.
316
00:31:21,340 --> 00:31:27,760
Glenarriff Beach is a conservation area,
backed by sand dunes, home to the
317
00:31:27,760 --> 00:31:33,580
yellow rattleflower, named after the
sound it makes as its seeds shake in the
318
00:31:33,580 --> 00:31:35,400
wind from the Irish Sea.
319
00:31:39,310 --> 00:31:44,930
Of the nine glens radiating off the
Antrim coast, Glen Arif is both the
320
00:31:44,930 --> 00:31:45,950
and deepest.
321
00:31:48,570 --> 00:31:51,930
And today, it's a haven for wildlife.
322
00:31:54,830 --> 00:31:59,650
Heron, kingfisher, and cormorant will
travel to the forest glen from their
323
00:31:59,650 --> 00:32:03,410
coastal roosts to fish on inland
waterways here.
324
00:32:17,230 --> 00:32:20,530
The buzzard has made a stunning comeback
to the glens too.
325
00:32:21,130 --> 00:32:27,470
Despite severe persecution and pesticide
poisoning, successful conservation at
326
00:32:27,470 --> 00:32:32,510
Glen Arif means he can flourish here on
the rich hunting ground of small mammals
327
00:32:32,510 --> 00:32:34,170
and amphibians.
328
00:32:37,910 --> 00:32:41,950
Also soaring above the glen is the
peregrine falcon.
329
00:32:42,570 --> 00:32:47,370
whose population is still recovering in
Ireland from devastating declines in the
330
00:32:47,370 --> 00:32:48,450
1960s.
331
00:32:50,350 --> 00:32:56,290
The peregrine falcon is the fastest bird
in the world and can strike his prey in
332
00:32:56,290 --> 00:33:00,850
a stoop dive at speeds of over 180 miles
per hour.
333
00:33:08,930 --> 00:33:11,410
Glenara means everything to me.
334
00:33:11,840 --> 00:33:17,500
When you look around, the scenery, the
people, the heritage, my ancestry,
335
00:33:17,700 --> 00:33:22,220
I just feel as if the glens are part of
my DNA.
336
00:33:33,600 --> 00:33:36,160
You'll probably notice the colour of the
water.
337
00:33:36,620 --> 00:33:38,180
Very dark black.
338
00:33:39,050 --> 00:33:44,470
That is because it is running off the
peak of the uplands and it turns it
339
00:33:44,690 --> 00:33:46,810
almost Coca -Cola colour.
340
00:33:49,930 --> 00:33:55,410
And that comes from the water running
off the peak which is in the uplands
341
00:33:55,410 --> 00:33:58,050
above, soaking through the blanket fog.
342
00:34:04,050 --> 00:34:09,000
Well, one of the best... Known animals
that would frequent the river here would
343
00:34:09,000 --> 00:34:10,000
be otters.
344
00:34:19,440 --> 00:34:25,659
We have quite a healthy population and
that is a sign that the water is of very
345
00:34:25,659 --> 00:34:26,659
pure quality.
346
00:34:31,280 --> 00:34:34,080
This is a hazy backwater.
347
00:34:34,540 --> 00:34:41,300
in the summertime sun beating through
the trees the water vapor cool
348
00:34:41,300 --> 00:34:44,040
at its heaven on earth
349
00:34:44,040 --> 00:34:57,700
we've
350
00:34:57,700 --> 00:35:02,420
journeyed from the city of londonderry
right around northern ireland's
351
00:35:02,970 --> 00:35:06,910
and find ourselves at the eastern side
of the Antrim Plateau.
352
00:35:08,710 --> 00:35:15,490
Looking down from space, we see the
strange shape of Island Magee, looking
353
00:35:15,490 --> 00:35:19,330
rather like an elephant's tail drooping
into the Irish Sea.
354
00:35:20,850 --> 00:35:25,590
And at the southern end of this
peninsula is a place where much of the
355
00:35:25,590 --> 00:35:29,670
extraordinary story of the geology of
this landscape was discovered.
356
00:35:31,880 --> 00:35:34,400
It's called The Gobbins.
357
00:35:40,380 --> 00:35:47,240
Its dramatic appearance is only half the
story, for The Gobbins has plenty else
358
00:35:47,240 --> 00:35:48,240
to tell us.
359
00:35:49,860 --> 00:35:53,900
Dr Mike Sims is a geologist based here
in Northern Ireland.
360
00:35:54,140 --> 00:36:00,160
For him, it's this place that holds the
key to the land he lives in.
361
00:36:02,280 --> 00:36:07,020
It's an amazing place to come and
actually look at some of the geology,
362
00:36:07,020 --> 00:36:10,660
the rocks that make up the landscape
along the Antrim coast.
363
00:36:15,900 --> 00:36:22,860
144 million years ago, the whole of
Ireland was submerged in a warm sea in
364
00:36:22,860 --> 00:36:27,580
white limestone was deposited and can be
seen in the cliffs of the Causeway
365
00:36:27,580 --> 00:36:28,580
Coast today.
366
00:36:33,260 --> 00:36:39,860
But at the Gobbins, that chalk was
overridden by huge fissures opening up
367
00:36:39,860 --> 00:36:40,860
Earth's surface.
368
00:36:43,420 --> 00:36:48,540
Go back 60 million years, which is how
old these rocks are, and in fact
369
00:36:48,540 --> 00:36:52,960
Ireland was more or less where Iceland
is now, and it's sitting on what we call
370
00:36:52,960 --> 00:36:53,960
a hot spot.
371
00:37:00,810 --> 00:37:05,910
Layer after layer of lava was erupted
onto this landscape 60 million years
372
00:37:09,390 --> 00:37:14,830
Those volcanic eruptions here during the
Paleocene epoch would look pretty much
373
00:37:14,830 --> 00:37:18,990
like the modern -day volcanic activity
on the islands of Hawaii.
374
00:37:22,570 --> 00:37:27,610
You've got all this great pile of lava
flows, probably four or five lava flows,
375
00:37:27,690 --> 00:37:29,870
with a red layer of ash at the base.
376
00:37:30,120 --> 00:37:31,120
of each one.
377
00:37:36,680 --> 00:37:41,940
These rocks now, they're very old and
cold. There's been no volcanic in
378
00:37:41,940 --> 00:37:43,960
Ireland for many, many millions of
years.
379
00:37:44,560 --> 00:37:48,280
And the reason for that is because we
have moved away from that hotspot. The
380
00:37:48,280 --> 00:37:52,760
Atlantic Ocean has been getting wider
and wider. It grows at about two and a
381
00:37:52,760 --> 00:37:54,480
half centimetres a year.
382
00:37:54,920 --> 00:37:59,810
And so, whereas we were once where the
volcanoes were, now we're... sort of a
383
00:37:59,810 --> 00:38:01,890
thousand miles away from them.
384
00:38:11,710 --> 00:38:14,990
Well, you would think that these bare
sort of rocky cliffs are pretty
385
00:38:14,990 --> 00:38:19,530
inhospitable places for anything to
live. And in fact, when you look at a
386
00:38:19,530 --> 00:38:23,310
these rocky cliffs, what you're seeing
is not the actual colour of the rock.
387
00:38:23,350 --> 00:38:25,830
You're seeing the colour of the lichens
that are growing on them.
388
00:38:28,840 --> 00:38:33,220
And a lichen is a partnership between an
alga and a fungus.
389
00:38:36,760 --> 00:38:40,800
And on coast, you actually see a very
distinct zoning.
390
00:38:41,540 --> 00:38:44,720
Low down on the shore, you'll see most
of the rocks look black.
391
00:38:45,040 --> 00:38:47,480
And a bit higher up, a lot of the rocks
look orange.
392
00:38:47,900 --> 00:38:51,060
And a bit above that, the rocks look a
sort of grey colour. And that's because
393
00:38:51,060 --> 00:38:52,540
of the lichens that grow on them.
394
00:38:58,160 --> 00:39:03,560
The dark, bathout rock found at the
entrance to the Gobbins holds its own
395
00:39:03,560 --> 00:39:04,600
secrets too.
396
00:39:06,300 --> 00:39:11,880
When the magma was deep beneath the
Earth's surface, actually within it, it
397
00:39:11,880 --> 00:39:13,200
actually contains a lot of gas.
398
00:39:13,520 --> 00:39:18,640
And when it comes towards the surface, a
lot of that gas is released as bubbles.
399
00:39:18,920 --> 00:39:22,800
And it's all to do with kind of hot
water percolating down through the lava
400
00:39:22,800 --> 00:39:24,060
after it's solidified.
401
00:39:24,340 --> 00:39:27,000
So all of these little white dots, these
were bubbles.
402
00:39:27,320 --> 00:39:31,560
It had lots and lots of gas dissolved in
it because it's full of all these
403
00:39:31,560 --> 00:39:37,280
little white specks here, which are
actually a white mineral called zeolite
404
00:39:37,280 --> 00:39:39,880
fills bubbles that was in the lava
originally.
405
00:39:40,120 --> 00:39:42,920
So this was fizzy lava. So as it came
out of the sepia, it probably would have
406
00:39:42,920 --> 00:39:45,280
fountained all over the place. Quite
spectacular.
407
00:39:49,540 --> 00:39:54,080
And the shoreline just south of the
Gobbins provides more clues to the
408
00:39:54,080 --> 00:39:58,230
creatures. who dwelled on this island
millions of years ago.
409
00:40:07,970 --> 00:40:10,530
You come to a beach which is covered
with...
410
00:40:10,830 --> 00:40:13,990
gray and white pebbles. And this gives
an idea of what rocks are actually
411
00:40:13,990 --> 00:40:17,370
underneath the basalt. It's a layer of
hard white limestone.
412
00:40:17,630 --> 00:40:21,970
And this was deposited beneath a sea, an
ancient sea 80 million years ago, far
413
00:40:21,970 --> 00:40:22,888
out to sea.
414
00:40:22,890 --> 00:40:27,990
And within this chalk, you sometimes
find fossils like this. It's a thing
415
00:40:27,990 --> 00:40:28,788
a belemnite.
416
00:40:28,790 --> 00:40:34,570
And underneath that layer of hard white
limestone, there is a layer of much
417
00:40:34,570 --> 00:40:39,270
softer Jurassic clay, which is about 200
million years old. And that Jurassic
418
00:40:39,270 --> 00:40:43,840
clay is actually full, of fossils and
i've got some here and you've got these
419
00:40:43,840 --> 00:40:48,580
little curly ones here this is a shell
of a fossil called an ammonite and there
420
00:40:48,580 --> 00:40:52,980
are other little sea shells in there as
well so this is evidence that 200
421
00:40:52,980 --> 00:40:57,420
million years ago this whole area was
covered by sea in which it was all sorts
422
00:40:57,420 --> 00:41:04,340
of creatures were living two fragments
of dinosaur
423
00:41:04,340 --> 00:41:09,190
bone have been found here at the gobbins
in these Jurassic clades, and these are
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00:41:09,190 --> 00:41:12,170
the only dinosaurs known from anywhere
in Ireland.
425
00:41:12,450 --> 00:41:17,410
So the Govan's is rightly famous for its
amazing cliff path, but it's also
426
00:41:17,410 --> 00:41:21,530
famous because it's the place where the
only dinosaurs known anywhere in Ireland
427
00:41:21,530 --> 00:41:22,530
were found.
428
00:41:26,250 --> 00:41:30,330
The cliff path is indeed something of a
wonder in its own right.
429
00:41:31,280 --> 00:41:36,220
At the end of the 19th century, a civil
engineer was so enthralled by the
430
00:41:36,220 --> 00:41:41,300
wonders of the Gobbins that he built a
chain of walkways for paying tourists.
431
00:41:42,880 --> 00:41:47,100
It was originally built by Barclay Dean
Wise, opened in 1902.
432
00:41:48,620 --> 00:41:52,480
But it's a difficult part of the world.
You're subject to storms and rock falls.
433
00:41:52,640 --> 00:41:56,200
So by the 1950s, it had fallen into
disrepair and was abandoned.
434
00:41:57,120 --> 00:41:58,320
But in the...
435
00:41:58,570 --> 00:42:03,170
Last couple of decades it's been
rejuvenated and rebuilt and now is a
436
00:42:03,170 --> 00:42:08,250
opened tourist attraction once more with
these amazingly engineered paths along
437
00:42:08,250 --> 00:42:10,430
this rather precipitous cliff.
438
00:42:34,540 --> 00:42:40,340
As we near the final stage of our
journey, the footprint of mankind
439
00:42:40,340 --> 00:42:41,340
and more visible.
440
00:42:44,540 --> 00:42:50,360
The next landmark is the Castle of
Carrickfergus, built by the Norman John
441
00:42:50,360 --> 00:42:54,660
Courcy in 1177, after he conquered
eastern Ulster.
442
00:42:55,660 --> 00:42:59,080
It had a strategic military role for
centuries afterwards.
443
00:43:01,320 --> 00:43:06,000
Three -quarters of the castle perimeter
is permanently surrounded by water.
444
00:43:08,020 --> 00:43:14,440
Around 55 million years ago, magma was
forced into the existing mudstone rock
445
00:43:14,440 --> 00:43:20,180
here, making it harder and more
resistant to erosion than the rest of
446
00:43:20,180 --> 00:43:21,180
shoreline.
447
00:43:21,720 --> 00:43:27,720
And this rock is perfect for building a
castle to last the onslaught of wind,
448
00:43:27,880 --> 00:43:29,520
waves, and water.
449
00:43:34,359 --> 00:43:40,480
368 metres above the sea level, the
rugged terrain of Cave Hill sits at the
450
00:43:40,480 --> 00:43:42,840
eastern point of the Antrim Plateau.
451
00:43:47,440 --> 00:43:54,320
Its giant profile is nicknamed
Napoleon's Nose, and from this natural
452
00:43:54,320 --> 00:43:58,200
point, the city of Belfast and its lock
revealed itself.
453
00:44:01,200 --> 00:44:06,880
A settlement here on the ford of the
rivers Farset and Lagen dates back to
454
00:44:06,880 --> 00:44:07,880
Iron Age.
455
00:44:10,100 --> 00:44:15,700
Like Londonderry's Loch Foyle 100 miles
away, Belfast Loch is perfectly
456
00:44:15,700 --> 00:44:16,700
sheltered.
457
00:44:19,440 --> 00:44:25,840
For centuries, this natural inlet has
offered seafarers 12 miles of virtually
458
00:44:25,840 --> 00:44:29,340
tide -free passage to the oceans of the
world.
459
00:44:30,600 --> 00:44:37,220
But its depth of 65 feet and 5 mile
width made it the ideal home for a
460
00:44:37,220 --> 00:44:38,360
shipbuilding industry.
461
00:44:40,620 --> 00:44:44,720
It was here that the most famous ship in
the world was constructed.
462
00:44:46,660 --> 00:44:47,980
RMF Titanic.
463
00:44:49,520 --> 00:44:53,960
Before it set off on its ill -fated
voyage in 1912.
464
00:44:57,680 --> 00:45:04,660
Today's ships still sail from Belfast
out to the open seas and away from
465
00:45:04,660 --> 00:45:07,200
the extraordinary Causeway Coast.
466
00:45:07,660 --> 00:45:12,460
Without doubt, one of the world's most
beautiful landscapes.
42724
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