All language subtitles for Undiscovered Vistas Series 1 12of14 Journey to Wales 1080p HDTV

Along the west coast
of Great Britain,

the world's longest
uninterrupted footpath

forges through more than 800
miles of breathtaking scenery.

And you've got this
wonderful sandwich.

On the left you keep the sea
your path in front of you

and to the right you've got
that undulating coastline.

From serene golden beaches

to towering limestone cliffs,

the wind and waves shape,
carve and chisel

this majestic landscape.

It's the power
of the ocean really

that does most of the work.

Waves around here can get
absolutely massive.

We're talking
15-, 20-meter swells.

A coast that reveals
geological mysteries,

framed by nature's
most beautiful sculptures

and chronicled by centuries
of rich human history.

This is the wild coast of Wales.

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On the first morning
of November, 1887,

strong gales whipped up around
the southern tip of Wales.

The roiling waters
of the Atlantic

flipped a cargo ship
heavily laden with timber.

Turbulent swells
carried the ship to shore.

The ship, the Helvetia,
came upon the sands

and got stuck in the sands

and gradually got buried
into the sands as well.

Time and tide wait for no man.

And over the many,
many decades,

the ship has turned
into a wreck.

I remember as a small child
coming here

and the Helvetia,
the ribs of the hull,

looking like an ancient dinosaur
coming from the depths of time.

Today, the remains
of the Helvetia

stand withered by the
restless waters of the bay.

The wreck continues to be buried
further in the sand

with every passing tide.

After all these decades,
it's just the prow standing,

making a last call,

before that too is buried
beneath the sands forever.

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The Helvetia's cargo,

more than 500 tons of timber,

was collected from the beach

and sold at auction
for a bargain price.

In fact it's said
there are very few houses

and barns left in the area
of the Gower

that don't have
some sort of wood or beams

from the wreck of the Helvetia.

More than 250 ships
have wrecked along this coast.

The treacherous winds
and hostile waters

that sealed the fate
of the Helvetia

also sculpted
the stunning scenery

along this wild coastline.

Wales is home to the world's
longest coastal footpath.

An 800-mile journey
that many begin here

on the Gower Peninsula.

The Gower projects westward
into the Bristol Channel,

a major inlet that separates
South Wales from England.

Rhossili Bay
stretches across three miles

of the Gower's
south-western tip.

Rimmed with sheer limestone,

topped with brilliant
green grass,

Rhossili Bay was designated

as the United Kingdom's
first area

of Outstanding Natural Beauty.

(Winds blowing
and waves crashing)

The sands of Rhossili Bay

lie between
two limestone outcrops.

These form a set of arms
that hug the bay.

Nestled between
these hard limestone arms

is softer sandstone.

Tides erode the sandstone
to form the hollow of the bay.

All the tides around
the Gower Peninsula

are influenced of course
by the Severn Estuary,

so it has a dramatic effect
on the landscape.

The River Severn is the
longest river in Great Britain.

Its estuary empties
into the Bristol Channel,

which opens
into the North Atlantic Ocean.

The tides in the Severn Estuary

rise and fall
by more than 45 feet.

It is the world's
second-highest tidal range,

exceeded only by Canada's
Bay of Fundy.

As the tidewaters
of the Atlantic

surge through
the Bristol Channel,

the sea pummels
the Gower Peninsula.

Over time, these tides
sculpt coves and bays -

rugged, yet beautiful.

In the 18th century,

the hidden coves and bays
of the Gower Peninsula

were ideal nooks
for smuggling goods.

Items like alcohol, tobacco
and tea

were snuck into Wales tax-free

and sold for bargain prices.

Smuggling was so widespread
along the Gower,

even the clergy
turned a blind eye.

Smuggled goods were stored

behind the Old Rectory
of Rhossili.

An operation that surely

could not have gone unnoticed
by the rector.

Now the solitary white house
you can see behind me

is the Old Rectory.

It was the house
where the priest

or the vicar of the parish
of Rhossili would live

and it was situated close by
to the church of Rhossili.

The old rectory,
you think stands alone.

But if you take yourself back
hundreds of years,

the village actually
was down there.

There were houses down there.

And they were brought up
on the top of the cliff

because of this
great sand inundation.

During the 13th century,
a change in tidal currents

unleashed wind and rain
so powerful

entire villages along
the southern coast of Wales

were buried under sand.

In Gower in particular,

we have this raised plateau
of limestone shelf

where the sand just packed in

and made these
wonderful beaches.

The old village of Rhossili
sat at the foothills

of this limestone shelf.

The Old Rectory
is the last surviving structure.

The rest of the village
of Rhossili is disappeared

underneath the sands.

Again, becoming a victim
of the tides

that are always sweeping against
the shores here at Rhossili.

The Old Rectory
has since been renovated.

Today, it is one of the region's
most sought-after lodgings

with a waiting list
longer than three years.

Now whenever
you come to Wales,

the one thing that you can't
help mentioning, of course,

are our woolly friends,
the sheep.

Down the Gower there's a lot of
what we call "Common Land",

where it's land that goes back
to medieval times

which is used communally
by all the people around here.

People always say,

well, how does a farmer know
which sheep is which?

The ownership of the sheep
are indicated

by little tags that the sheep
have on their ears.

Now you see the paint
on the sheep

but that indicates
whether the sheep have had

certain inoculations
or injections.

The sheep first came over
with those ancient Celtic people

about 500 years BC.

They are naturally
a Mediterranean animal

but we find that they live,
thrive, and survive

not only in the farmlands
but in the mountain regions,

the heathlands, the moorlands
and of course the coastal areas.

Now in Wales we've got a human
population of about 3.6 million

but we're vastly outnumbered
by the sheep.

At any time of year, there are
at least 15 million sheep

altogether in Wales.

So we've got about
five each for everybody.

On the southern tip
of Rhossili Bay,

a mile-long stretch of land
snakes out to sea

marking the most westerly tip
of the Gower.

The rocky bluff dips down
before rearing its head,

150 feet out of the water.

This is Worm's Head.

Now, legend surrounds
this Worm's Head.

The name Worm's Head
comes from "Wurm's head",

a wurm being a serpent
or a dragon

that used to look out
onto the horizon of the sea

to guard the shore
against any evil spirits

that might want to come in

and corrupt the people
that lived here.

Twice a day,
with the turn of the tide,

Worm's Head becomes an island

cut off
from Rhossili's coastline.

A causeway connects
the two landmasses

but it's only exposed
for just a few hours at a time.

If you are feeling
a bit intrepid,

you can actually walk yourself

out to the furthest-most tip
of Worm's Head.

You've only really got
a four-hour window

in which to get
through the causeway,

onto Worm's Head itself

and then back safely
to shore as well.

If you don't,
well, sit down and relax

because you'll have at least
a 6-hour wait

before you're able to return
back to the shore.

(Winds blowing
and waves crashing)

Further up the coast,
water packs a greater punch.

Waves around here
can get absolutely massive.

We're talking
15, 20-meter swells.

Out on the open ocean, they can
be reasonably frightening

but as they get
into shallow water

the wave height
builds up even more

and the front of the wave
topples over

and that's when
a lot of this erosion happens.

It's the sheer force
of those breaking waves

as they hit the cliffs.

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Along the south of Wales,

waves that have
powered their way

across the full expanse
of the North Atlantic Ocean,

come crashing
into the sheer cliffs

of the Pembrokeshire coast.

A coastline that twists
and turns west from the Gower

through 186 miles of West Wales.

A thick sheet of limestone
guards its western tip,

the Castlemartin Peninsula.

Here, the power of the waves

has carved one
of the Welsh coast's

most iconic natural sculptures.

A stone arch juts 65 feet
out to sea

and rises more than 60 feet
above the water,

clinging to the coast
of Castlemartin,

this is the
Green Bridge of Wales.

Natural arches like this
begin to take shape

when waves hitting both sides
of the limestone headland

carve small caves back to back.

Eventually, water breaks through
the dividing wall

and pierces through
the weaker rock

connecting the two caves.

Over time, this hole widens
through erosion.

The result is a natural arch,

one of nature's most beautifully
engineered structures.

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Someday the forces
that created this arch

will also destroy it.

These sea stacks
are the supporting pillars

of what was once an arch.

Each is taller
than a 10-storey building.

And represents the final stages
of maritime cliff erosion.

Over time, beating waves
isolate the rock

from the adjoining cliff.

Millions of years ago,

this scene would have
looked similar

to the Green Bridge of Wales.

Eventually, the sea will also
undermine these stacks

and the soaring pedestals
of stone

will become mere stumps.

As these striking features
wash away,

new ones take shape.

Farther up the coast is an abyss

nearly 150 feet deep,

more than 160 feet across.

Large enough to engulf
the White House.

This is the Devil's Cauldron.

An imposing crater formed by the
collapse of several blowholes.

A blowhole appears when water
erodes weaker sections of rock

to create a sea cave.

As waves move in and out,

water pressure builds
inside the cave

and wears away the rock.

Eventually, a narrow shaft forms

from the sea cave
up to the cliff top

releasing the surging water
through a jet spray.

Several of these blowholes
formed in this cliff.

As powerful waves continued to
erode weaker sections of rock,

the blowholes collapsed
creating a much wider shaft.

According to geologists,

the mass of rock that collapsed
to produce the Cauldron

is heavier
than the combined weight

of the three largest
ocean liners ever built.

Over time, the Cauldron cliffs
will also break apart

to form a series of stacks
and arches so imposing

they will dwarf the magnificent
Green Bridge of Wales.

The coast,
it's always changing.

But it's the power
of the ocean really

that does most of the work.

A walk along
the Pembrokeshire Coast Path,

for me, is always special.

You never know
what you're going to see.

It's always special
because of the geology.

These little guys down here,

they're 24 million years old.

So much, much, much younger
than anything else

in the whole of this area.

So it's a bit of a mystery
what on earth they're doing here

because they're
so out of context.

And what people think
is that limestone rocks,

which are the ones
we're surrounded by,

are very, very prone
to being eaten away by water.

You get lots of cracks,
lots of fissures.

And so when these rocks
were already quite old,

there were little streams
running down

through cracks in the limestone
through underwater caverns-

mini caves.

They brought material
down with them

and filled little caves
within the rock with this stuff,

water went on through,
left the stuff behind.

Now since then,
the limestone has eroded

and has left these rocks
at the surface

so way, way out of time
and way, way out of place.

Consequently,
rather interesting.

As the sun descends
on the Green Bridge of Wales

and the day comes to a close,

the restless waters
of the Atlantic

continue to undermine
the cliffs.

The morning sun illuminates
the wrinkled face

of the Pembrokeshire coast.

Every fault, crease and dimple

is exposed
to the wrath of the sea.

Water eats away
at these weaker pockets

as though taking a bite
out of the coastline.

There are so many layers
of the history,

literally in the rocks,
in the stories,

in the legends and the myths

and actually going
that mile further

and realizing there was
something extra special

around the corner somewhere.

Nestled in a hidden cove,

a small medieval church clings
to the rocks of a secluded bay.

An air of mystery
grips the stone structure.

This is St. Govan's Chapel.

St. Govan's chapel
has got lots and lots

of little myths and legends.

Many think the original,
simpler stone structure

was built as early
as the 6th Century

and restored
7 centuries later.

The entire building is smaller
than a one-car garage.

Little is known
about the man who built it.

Some people think
he might have been

one of King Arthur's knights.

Nobody's quite sure who he was.

Some legends say Govan
was an Irish monk

sent to educate the people
of this region.

St. Govan's chapel
is really interesting.

Many, many centuries ago,

you had this Christianity
developing on its own

but through old Celtic people's
history as well.

So you find a wonderful tapestry
of the history

of the Christian church
in particular

literally in the rocks.

Others say Govan was a coward

who took shelter in these rocks
to hide from pirates.

Further up the Welsh coast

on the south western tip
of the Dale Peninsula,

An isolated bay
called "Martin's Haven"

shelters a very
different inhabitant.

This time of year's pretty
special for the grey seal,

the Atlantic grey seal.

What these seals require
at this time of year

are safe, secluded beaches.

It's October, pupping season
on the coast of Wales.

The sheer Pembrokeshire cliffs
cradle the bay

providing the perfect
protected nursery

for these mothers
and their young.

Males patrol the water.

Females and their young
claim the beach.

It's a really lovely thing
to see,

these great little seal pups

and their mothers
looking after them.

A mother makes her way
up the shore

to feed her newborn.

The pup latches on to suckle.

At birth, most pups weigh
about 35 pounds.

They're easy to identify
by their soft and fluffy coat.

They're born with a rather
smart-looking white coat,

which is, you think slightly odd
for a seal

but a lot of the pebbles
on the beaches around here

are quite light-colored
so the camouflage is quite good.

This baby seal needs
to fatten up

before getting in the water.

It will spend the next two weeks
latched on to mom.

The mother's milk
is extremely rich

as much as 60 percent fat.

So the pup should have no
problem putting on the weight.

On average, a young seal will
gain about three pounds a day

and can quadruple in size
in just three weeks.

For this pup independence
is around the corner.

It remains on land living off
a reserve of blubber

while waiting for its baby coat
to moult.

The pup rubs against a rock
to speed up the process.

Once the new waterproof fur
grows in,

the young seal
will leave the beach

and learn to fend for itself
in the ocean.

Once the pup is weaned,

its mother is available
to mate again.

And there's no shortage
of suitors.

A persistent male
patrolling the waters

decides to make his advance.

He charges up the beach

to chase one of the females
down into the water.

Competition for mates is stiff.

Territorial fighting
is common among males

during breeding season.

Dominant males will mate
with as many as 10 females.

Larger males can grow
more than 7 feet long,

weighing in at nearly
800 pounds.

Females are smaller,
averaging five to six feet,

weighing up to 500 pounds.

It's quite easy to tell
a difference between the two.

The females,
they tend to be smaller,

lighter, with speckled fur

but their noses
are really different.

They have almost
a feminine head,

almost a cat-like head,
quite a narrow nose.

Whereas the male's darker
in appearance, larger animals,

with a much, much thicker nose,
rather more aristocratic nose.

The male's long, arched nose

earned the grey seal
its Latin name,

"Halichoerus Grypus",

"Hooked-nose sea pig".

Back on shore,
a playful mother and her young

lounge on the beach.

Others are busy nursing

or keeping a close eye
on their pups.

As autumn comes to an end,

the seals will leave
their breeding ground

and make their way home
to Skomer Island.

Less than a mile
from the Pembrokeshire Coast

off the south-western tip
of Wales,

Skomer rises more than 200 feet
above the Irish Sea.

From the mainland, Skomer looks
like two separate islands

connected by a narrow
strip of land.

The power of the sea eats away
at this weaker neck of rock

nearly slicing the island
in two.

The name Skomer originates
from "Skalmey",

a Norse word
that means "sliced" or "cut".

Skomer Island was once connected
to the mainland.

But as the sea broke through,

Skomer and the smaller
Midland Isle became isolated.

The surface area of Skomer
is only one square mile.

It takes just 20 minutes to
cross the entire island by foot.

Despite its small size,

Skomer has the largest
population of Manx shearwaters

in the world.

There's approximately
320,000 pairs of that bird

on this island.

But even if you came here in the
middle of the breeding season,

you wouldn't see them

because they're either
underground

or out to sea feeding.

The birds that have been feeding
only come back to the island

and swap over with their mate
in the burrow

under cover of darkness
to avoid seagull predation.

Manx shearwaters live
in underground burrows.

Rabbits and puffins
make similar homes.

As a result, the entire island

is covered in more than
one million burrows.

One misstep off the footpath
could collapse a home.

Skomer Island is a
National Nature Reserve,

a protected marine habitat

and an area of
Special Scientific Interest.

Beneath the burrows

and the bright green grasses
of the island

lies an important
geological story.

Distinct ribbons of rock
streak the coastline.

Each one represents
a different era

of a turbulent geological past.

Layer by layer
these rocks tell the story

of one of the last
major volcanic events

that formed much of south Wales.

More than 400 million years ago,
ancient plates shifted

causing volcanic eruptions
to pour lava and ash

3,000 feet thick

over more than 43 miles
of South Wales.

Over time,
the lava solidified to stone.

Skomer Island is made entirely
of this volcanic rock.

These rocks that we're
sitting on right now

are lava flows
from that volcanic episode

430 million years ago.

That makes Skomer special.

It's amazing to think
as you walk around this island

you're walking over products of
a 430-million-year-old volcano.

If you were to look at Skomer
from the mainland,

you would see a series of

what appear to be layers.

These layers are,
for the most part, lava flows.

Now all of those different types
cooled at different rates

to give you final products
that are subtly different.

But essentially, from the side
you have lava flows

that have been tilted
on their side

so they now dip 40°
to the south.

What caused that tilting?

Well, that's back
to the Caledonian mountains

being created.

When that mountain range
was created,

you had a tremendous bout
of orogenic activity,

that's mountain building
on the earth's surface.

The rocks of Skomer were folded
and tilted and buckled

and faulted.

And the Skomer lavas
that started out horizontally

were now tilted.

On the south side
of the island,

geologists have discovered
used artillery...

not from any manmade conflict

but from deep within
the earth's scalding core.

These are volcanic bombs
fired into the air

from the mouth
of an ancient volcano

more than 400 million years ago.

Occasionally a volcano will
get very excited and explosive.

It goes through
an explosive phase.

And now it jets out material
called "Pyroclastic bombs"

that get shot up
into the atmosphere

and then they're dumped
into the surrounding rocks.

Now if the surrounding rocks
are still soft,

as they would be
if they're new lava flows,

these spherical bombs of rock

get embedded
into a laval matrix

and you can see those
on the island,

which is quite an exciting thing
to be able to see.

You've got fantastic rock
formations just in front of you.

You look out
to the Atlantic Ocean.

So you have a big evasion
and a feeling of space.

And it's some of the
cleanest air on the planet.

Seeing how things
have changed over the time,

but how actually rather a lot
has stayed the same,

the beauty and the seclusion
and the peace and the quiet

has always been a constant
for Skomer.

Farther up the coast,
the stunning mountains

of the first designated
national park in Wales

stretch across more than
800 square miles.

This is Snowdonia.

A place built by fire
and sculpted by ice.

You could argue
that it's an area

steeped in the history
of fire and ice.

That being
it's the volcanic processes

that's formed the mountains
with tectonic movements

and associated volcanoes
folding the earth's surface

and then the glacial period

revealing all the wonders
of the geology.

What you'll see around you
is various peaks

of different sizes and heights

and some deep valleys--
river valleys

and some wide glacial valleys
as well.

The star of this landscape
is Snowdon,

the highest mountain in Wales.

Its peak rests in the clouds
nearly 4,000 feet high.

The sheer rock, unstable gravel

and tricky traverses
of Snowdon

make an ideal training ground
for professional climbers.

Edmund Hilary trained
at Snowdonia

before heading to Nepal.

And in May of 1953,

he and Sherpa, Tenzing Norgay,

became the first to successfully
summit Mount Everest.

Snowdonia's mountains
were born in a fiery collision

between tectonic plates.

About 400 million years ago,

the sediments were being laid
on the ocean floor

so you would have
the ash deposits,

you would have the sand
and silt, mud

being laid on top of each other.

And as the tectonic plates
were moving,

you would've had one
tectonic plate going
underneath another,

which created massive folds.

They would have
brought the layers

that would've been on the bottom
of the sea up to the tops.

That's why you got
the best place for fossils

on the tops of the mountains.

Cwm Idwal,
a picturesque glacial valley,

bears the evidence
of this tectonic shift.

Fossils of marine organisms,
once living on the sea floor,

lie embedded in the rocks
of Cwm Idwal.

We've got fossils
of these little sea creatures,

they're called "Brachiopods".

They would have been shelled
creatures with hard valves

and they would have been living
at the bottom of the sea

about 40 million years ago.

Nowadays they are being found
on the tops of the mountains

and that's due to the
tectonic forces that took place.

But these fossils,
once at the top,

now lie at the base
of Cwm Idwal.

How did some end up
at the bottom?

It was a puzzle
that perplexed Charles Darwin.

These boulders
laden with fossils,

provided some of the
earliest evidence

that this entire landscape
had been carved by ice.

Scientists like Darwin were only
just beginning to theorize

that there had once been
a period of immense glaciation.

Cwm Idwal is very important

in terms of its role
in the glacial theory

or the theory of glaciation.

One of its famous scholars
includes Charles Darwin

who visited the area.

The glacial theory relates to
how ice has formed landscapes.

And Cwm Idwal is a classic
cwm or cirque.

It's a bowl-shaped amphitheater,

formed when the glacier
moves down the mountain.

Darwin proposed
that as glaciers move,

they collect rubble
from the top of the mountain.

Then move the rocks
and dirt downhill

and deposit them at the base.

After helping Darwin
prove his theory of glaciation,

these rocks earned their name,

"Darwin's Boulders".

If it wasn't for the glaciers
scraping away the surface,

we would have never found
these fossils.

You can see the effect of ice
carving out the rock

all the way down
the valley there.

Today lakes fill
deep glacial hollows

and waterfalls
spill over rocks

perched high
above the valley floor.

(♪♪♪)

In Snowdonia, there's all
kinds of movements of water.

You've got your traditional
runoff which forms streams,

you've got glacial lakes,

you've got waterfalls where the
hard rock hasn't been eroded

and there's a cascade
of water there as well.

Cattle and sheep graze
in these mountain valleys,

as they have
for thousands of years.

(♪♪♪)

An ancient drover's crossing
constructed with loose stones

was once used to move livestock.

Now it is dwarfed
by a modern bridge.

The people have grown,

they've lived
in these mountains.

And the mountains themselves are
dominant peaks and landscapes

which help with navigation,
they provide shelter,

they provide different habitats
to graze upon.

But the important part

are the valleys
between those mountains.

It's where people come,
it's where cultures are shared,

it's where traditions
are shared.

There's thousands of years of
culture that I feel a part of.

I think I'm rooted
in these mountains.

And by standing by the root
of the mountains themselves

and looking at the majesty
of the mountains,

it just give you a sense of awe.

(♪♪♪)

Farther up the coastal path
at the northern tip of Wales,

a rocky headland,

2 miles long
and 1 mile across,

meets the Irish Sea.

This is the Great Orme.

The summit of Great Orme rises
nearly 700 feet above the water.

It's defended
by sheer cliffs,

which overlook the
surrounding countryside.

It is an ideal vantage point
to prepare for a coastal battle.

In 1940,
early in the Second World War,

the threat of a German invasion
put Great Britain on high alert.

The army relocated
its Coastal Gunnery School

from east coast Essex
to the west coast of Wales.

The view and the wide mouth
of the bay

made the Great Orme
an ideal training ground

for British gunners.

Boats were towed across the bay

and anchored in the distance
for target practice.

By 1942, the gunnery school

had trained more than
750 servicemen.

Today three
searchlight stations remain.

Very early on,
people had discovered

that it was a good
vantage point.

You could see what was happening
for miles around,

so I guess
that's one of the things

that attracted people to live
and to make their lives here.

By the 19th century, many had
settled on the Great Orme

to farm the headland.

In 1880, one landowner acquired
several Kashmir goats

from northern India
and set them free on his land.

Today these goats
still run wild

and now number in the hundreds.

I think the goats are
symbolic of the Great Orme.

There are feral goats elsewhere
in Wales, separate herds

but they're completely different
to the goats here.

This is a particular breed,
Kashmir.

Halfway down the headland,

steep slopes and narrow ledges

present an inhospitable
landscape for most.

(Goats bleating)

But for these feral goats,
this is home.

For the most part, the scene on
the slopes is quite peaceful.

Many goats rest
along rocky ledges.

Others
delicately nibble the grass

and pick
at the remaining berries.

The dominant males

have the largest curved horns
in the herd.

The horns are notched
with large ridges.

Each ridge represents
one year of growth,

making mature males
easy to spot.

These goats are best known
for their silky wool coat.

Soft cashmere wool
first gained popularity

during the reign
of Queen Victoria

and is still
in high demand today.

Human history on the
Great Orme goes back an
awful long way.

Over 500 sites
of historical interest

have been recorded
just on this small headland.

So it's really rich
in human history.

There are so many reasons
why the Great Orme is special.

It's hard to quantify, really.

You've got steep drops below you
straight down to the sea,

you've got the sound
of the seabirds,

that feeling of isolation.

It's--

Yeah, it's a magical place.

(♪♪♪)

From wide sandy beaches

to towering limestone cliffs,

a journey up the world's
longest coastal footpath

reveals spectacular landscapes

carved by the power of water.

Rich marine life
thriving amongst the cliffs.

And a Welsh culture rooted
in life overlooking the ocean.

The coast of Wales draws
this majesty with it.

It's this place where you just
repair and refresh and enjoy.

You'll see plenty of sheep,
you'll see these green hills.

You'll see really mysterious
peaks in the early morning mist.

And I think if anybody
was to come to Wales

and spend a majestic 3 months
walking around Wales,

they'll leave feeling
a little bit more Welsh

than when they arrived.

(♪♪♪)

(♪♪♪)