Transcript Antarctica The Last Continent Pictures by Alan Light, Drummond Small, Mike Usher, Paul Ward Text by Paul Ward / CoolAntarctica.com Copyright: Material on these.

Antarctica
The Last Continent
Pictures by Alan Light, Drummond Small, Mike Usher, Paul Ward
Text by Paul Ward / CoolAntarctica.com
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Antarctica covers the South Pole
Africa
South
America
South
Pole X
X
Australia and NZ
Midnight at the pole 21st December
The Living Earth, Inc. copyright 2006
Midday at the pole 21st June
The commonest way to get to Antarctica is still by ship. This means crossing
the “Drake’s Passage”, the narrow band of sea between Cape Horn and the
Antarctic Peninsula. It is the roughest sea on Earth.
As your ship approaches Antarctica, you will be followed by albatrosses.
This is a young Wandering Albatross – “The bird that made the wind to blow”.
Wandering Albatross have the greatest wingspan of any birds at up to 3.5m.
The first iceberg is like a doorway to
the South.
You don’t know where you will encounter it
and it will probably be a distant shape
made out through mist under a grey sky.
Once seen, it signifies your passage into
Antarctic waters and entry into a world
quite different to any you have seen
before.
Welcome to Antarctica.
Increasing numbers of people now arrive in Antarctica by air. Ice runways are
becoming more and more common and this is an increasingly common form of
transport for those on scientific bases. The passengers can be dropped off in South
America or Australia for onward transport rather than spending weeks on board ships
as was the case until relatively recently.
This ship is HMS Endurance, seen here it has pulled up against the edge of an ice
shelf in the Prince Gustav Channel between the Antarctic Peninsula and Prince
Gustav Island. This couldn’t happen today as the whole ice shelf broke up a
few years ago.
Ships are the ideal way to get around Antarctica. The continent and
surrounding islands are either very mountainous and rugged broken up rock, or
an endless unstable ice mass.
A Russian icebreaker leaves open water and starts to enter winter-formed
ice in the Antarctic spring. Not all ships that visit Antarctica are icebreakers,
but the great majority are ice strengthened. Coast-bound ice is common early
in the season and being able to break through it means that cargo can be
delivered without being so dependent on weather conditions.
The flat area between the near and the distant mountains is the sea. The
whiter region is consolidated pack-ice (last years sea-ice that formed elsewhere,
broke up and floated here). The darker region is “fast-ice” sea-ice that has formed
here in the last few weeks.
Sea-ice forming. At this stage it is maybe 1” / 2.5cm thick, but soft enough for
you to push a finger through. The shapes are caused as the tide rises and falls, so
pushing the edges of the plates over each other. The sea freezes quickly in calm
cold conditions, it is the movement of the surface that prevents it freezing earlier.
As the winter approaches, the only people left behind in Antarctica are
scientists and support staff on research stations. About 1000 people in an
area 1.5 times larger than the USA. Sea-ice doubles the area of Antarctica at this
time and flights are very rarely attempted due to the darkness and weather
conditions. This is Signy station (UK).
On the other side of Antarctica is the New Zealand Scott base. This is a fairly
typical size for an Antarctic base, there are about 10 winterers and up to 85 in the
summer months. The industrial-estate architecture is typical of Antarctic bases
unfortunately.
Antarctic bases old and new. In the foreground on Hut-Point McMurdo Sound
is Scott’s 1904 hut from the Discovery expedition that housed 25 men, in the
background is the modern McMurdo base that houses about 250 people in the
winter and around 1000 in the summer – it is far and away the largest Antarctic
Base.
The interior of Scott’s hut is preserved like a time capsule. A combination of
lack of visitors, cold temperatures and great respect shown by the few visitors
there have been means that many items are exactly as they were when left
over 100 years ago.
Amundsen-Scott Base at the South Pole. This base houses 75 over the
winter and 250 in the summer. It is the third base in this location, the previous
two were buried by accumulating snow and ice. Like other modern base
designs built on ice, this is elevated on legs and can be raised to stay clear
when the accumulation threatens to take over.
Science in Antarctica. Bases in Antarctica exist so that science can take
place, there are a great number of different projects from the small to the large.
This is a 10m telescope and laboratory at the South Pole.
A huge silence. As the temperature falls, so any water vapour in the air freezes and
falls out. You can see as far as there’s anything to see. From this point it is possible
to see over 100 miles (160km) in all directions. With no wind, the entire area is
motionless and totally silent.
Early exploration of Antarctica was by whalers and sealers seeking to exploit the
huge whale and seal populations – which they did to devastating effect. Seals
have since largely recovered, but the great whales haven’t. This plaque is painted
on a whale vertebra on an Antarctic base, it represents 118,159 whales killed
between 1911 and 1930 – in just one part of Antarctica.
Pack-ice is “glued” together by the sea freezing between the pieces to give
a solid surface. It is very rough and broken up however making a surface very
difficult to travel over. Vehicles or people on skis have to stop-start constantly and
change direction continually to find the best path.
Sea-ice freezes ice-bergs in place. In open sea they are free to move around.
When the sea freezes, they are fixed for the winter. Ice-bergs are made of freshwater, they formed as part of glaciers and ice-shelves and become a berg when
they reached the sea after hundreds or thousands of years and fell off the end.
It is possible to walk across the sea-ice to frozen-in ice bergs. The stripes in the
berg were formed when it was part of a glacier or ice-shelf and are a result of
different temperature and snow conditions as the berg was being formed. Whiter
bands have more air, they were formed in colder conditions. Bluer bands have less
air and were formed in warmer conditions.
Standing next to even a
small berg can be an unnerving experience.
If the sun is out, the
different colours warm up
at different rates, clear
regions can act like a lens
warming up the interior.
The result is all kinds of
creaks and bangs.
Add to this the sea-ice
around it creaking as the
tide rises or falls and it
becomes an uncomfortable
place to be.
There’s also the fact that
you’re on ice not very thick
and there’s 8-10 times
more ice below your feet
than you can see.
Fast-ice that forms in situ becomes hard and strong after many days of low
temperatures and forms an excellent travelling surface. The long pole carried by
one of these men is used to test the ice – more than 3 “thwacks” to get through and
it’s safe to walk on, less than 3 and it’s re-trace your steps carefully.
Field work in Antarctica. Some scientific work such as geological surveying in Antarctica
takes place away from bases in remote areas. This picture shows a more traditional camp
from the 1970’s when the field party consisted of two dog teams and sleds that can be
seen here arranged on either side of the tent.
Such scenes are still repeated today in the Antarctic summer with the difference that
instead of dog teams pulling the sleds, skidoos are used. Such field parties are supported
in the field by aircraft for re-provisioning allowing them to spend longer away from base
and go to more remote areas.
A field party in Antarctica has to be
the purest way of experiencing the
continent.
Little can match doing this with sleds
pulled by dogs. This is now a part of
history never to repeated as dogs were
banished from Antarctica under the
Antarctic Treaty in 1994.
It was some 20 years before that
however that dogs were used as a
matter of necessity. Far less romantic
internal combustion powered transport
has been used for many years now.
This Weddell seal is resting on the ice miles from anywhere on flat and
unbroken ice. It must have made a crack in the ice by ramming it from below and
then worked on the crack with its teeth to make a hole by which it could leave the
ice. Though the ice is strong, fortunately for the seal it was not too thick for it to get
through.
Ice bergs are endlessly varied and picturesque, just imagine how much ice
there is that you can’t see below the surface.
This is the same berg as in the previous picture, but from a different direction and
on a different day. Changing snow, ice and weather conditions can make
Antarctica an endlessly varied place.
Crossing glaciers and ice fields is hazardous as they are often riddled with
crevasses. These are cracks in the ice that form from top to bottom when the ice
sheet direction changes or when it goes over an obstacle. Roping-up is required,
so if one person goes down a crevasse, the others are able to rescue them.
A Pisten Bully tracked vehicle
with a crevasse probe.
The probe itself is electronic, it is
mounted on the end of the long
arm, the wooden platform and
inner tube allow it to ride ahead
of the vehicle on the snow or ice.
This vehicle will be the first one in
a convoy going ahead of all the
others and hopefully detecting
crevasses and stopping before
any vehicles are in danger.
Investigating a crevasse –
deliberately!
Crevasses are often covered
over by a bridge of blown snow.
Such bridges may be strong
enough to support a vehicle or
not strong enough to support a
single man.
Care is needed in approaching
them. Training to rescue
yourself or others who may fall
into a crevasse is a part of the
preparation needed to travel
around Antarctica overland and
away from bases.
There are many atmospheric
phenomena in Antarctica as a result of
the low temperatures.
Water vapour cannot form because the
freezing temperatures, so often there are
tiny ice crystals that float around in the air
leading to a wide variety of effects.
This picture shows a “Solar Pillar” caused
by the sun (behind the cloud at top)
reflecting from countless minute ice
plates suspended in the air.
The pillar is almost as bright as the sun
itself and because it is an optical
phenomena and not real (like a rainbow)
it moves with you when you walk around.
Here’s a fun thing to do on a cold day (-32°C here). Take out a flask of boiling
water and a plastic cup. Pour the water into the cup and throw it into the air. As
the +100°C water hits the cold air it instantly vapourises and drifts away. The
streaks towards the bottom left are small pieces of ice, the rest just becomes gas.
Diamond dust. Another atmospheric phenomena, shown here during a downhill
skiing break using skidoos as a ski-lift. The small white speckles are tiny ice
particles in the air that reflect the sun as if the air is full of glitter.
Antarctic land transport. Many vehicles are tracked including all that go away
from the bases, wheeled transport is used in and around bases where
conditions are predictable.
The first effective tracked vehicles in Antarctica. These are some of the
vehicles involved in the first successful overland journey to the South Pole in
the Trans Antarctic Expedition of 1955-58. The Massey Ferguson tractor was
the first tracked vehicle to reach the South Pole, a modified agricultural model.
The original form of transport in Antarctica was dog-sled pulled by
huskies. These animals helped to open up Antarctica and for many years were
the only reliable form of transport until vehicles became reliable and
trustworthy.
Strongly built, powerful and loyal until the end. The men who worked with huskies
never forget the connection of man, dog and landscape, being part of the pack and
working to a common goal in a challenging but ultimately hugely rewarding environment.
Dogs sleds became less important as a means of transport from the 1960’s
onwards. Initially they supported mechanical transport and then were taken over in
importance. Dogs were kept in Antarctica until February 22nd 1994 when the last team
was removed. Antarctic huskies became a breed apart being selected for Antarctic
conditions.
Antarctica is home to many millions of penguins, this one – an adélie is the
commonest species found in Antarctica and an animal of the deep south. Here
one is seen crossing the sea-ice to its nest site in early spring. As the season
goes on the ice breaks up and it doesn’t have to go so far. It is around 70cm tall
and about 5kg in weight.
A pair of adélies all clean and glistening after being freshly laundered by the
sea take a short break on their way to the breeding colony. These only had a few
miles to walk across the frozen sea. Sometimes if the ice persists, they can have
10’s of miles to go. Must be so much worse when you only have such little legs.
Early spring can still bring storms. These penguins are on their way to their
nesting grounds and have to face out the weather. They head into the wind so
their feathers are not ruffled to give the best insulation and pull themselves as
short and squat as they can to reduce surface area to reduce lose heat loss.
Nesting grounds start to fill up. This area has about half as many penguins as it
will have eventually. Early arrivals get the best places that are raised to some
degree, these are the least likely to get wet when it warms up and the snow melts.
Note the pack-ice in the distance, this will break up as the season goes on.
Like males the world over of
almost any species, this male
adélie penguin in the peak of
condition advertises for a mate
early in the breeding season.
Once a mate has been found, nest-building begins in earnest. Penguin
nests are amongst the least impressive of any birds nests consisting of just a
circle of stones on the ground. As the supply of stones is fixed, they spend much
of their time stealing them from each other over and over again.
The proud parents to be by their magnificent nest – that’s it I’m afraid. This
pair are in the process of a courting ritual. Starting low down they weave beaks
together, getting higher and higher, eventually throwing their flippers back with a
loud “awk, awk, awk” sound. It teaches them what their mate’s voice sounds like.
The large icy step is called
an “ice foot” it completely
surrounds coasts at the
end of winter. As the tide
rises and falls, so it leaves a
layer of ice each time which
builds up to be left as a
large step when the
attached sea-ice breaks up
and floats away.
These penguins are
returning from a fishing trip
to find the tide has gone out
and they can’t get back to
the shore, so they wander
up and down the bottom of
the ice foot until the tide
comes back in and can float
them back up to the right
level.
Maybe we can jump over the ice foot from here? Perhaps it’s just a game of
follow my leader to pass the time until the tide comes back in?
He seems to know where he’s going, lets follow him. Why are these guys
following me?
Snowfall at nesting time. It’s just around freezing point which can cause
problems for penguins with eggs or chicks if the snow melts and floods the nest
chilling the egg or chicks. Note the reddish colour under the flipper of the penguin
to the left, a way of losing excess heat by diverting blood through the flippers.
Eventually the eggs are hatched and the chicks born. Covered in fine down,
they are always protected by one of the parents until they are large enough to be
able to regulate their own temperature. Penguin chicks grow at a rapid rate
being supplied with food by parents who take it turn to baby-sit or catch food.
These chinstrap penguins are almost big enough to be left by the parents so
they can both go fishing to supply their every increasing need for food. When both
parents go, the chicks form loose “crèches” where they get better protection from
the cold and also from predators such as skuas.
Like youngsters
everywhere, penguin chicks
get dirty and into trouble
when their parents are
away.
As the season progresses, so
hygiene conditions deteriorate
– I won’t go into details.
Some chicks get dirtier than
others of course!
On a more serious note,
getting so dirty can be
dangerous as it decreases the
effectiveness of the down to
insulate the chick and unlike
the adults, the chicks can’t go
into the sea to wash
themselves off.
Adélie Chicks don’t go into the
sea until they have moulted
their juvenile down and gained
the adult feathers.
Penguin colonies are patrolled by predatory skuas looking out for unguarded
eggs and unguarded or weakened chicks every ready to pounce. Despite their
obvious presence and effect they have on the colony, they are only responsible for
a small part of the overall mortality (death rate) of chicks.
Hungry chicks chase a returning adult demanding to be fed. The adult runs
away as a means of getting rid of chicks that are not theirs, only their own chicks
will never give up until they are fed – they have no other alternative. These chicks
may both belong to this adult, or one may just be about to give up.
Gentoo penguin and chicks. One of the calmest and least aggressive of
Antarctic penguins, there are two sub-species, this is the southern sub-species
found down to the Antarctic Peninsula. The slightly larger northern sub-species
is found mainly on the sub-Antarctic island of South Georgia.
A King Penguin preening itself. These are the second largest of penguin species at
nearly 1m tall and around 15kg. They are not birds of the ice however breeding on subAntarctic islands.
Raspberry ripple snow. Found in polar and mountainous regions in the spring
as snow and ice begin to melt releasing stored nutrients, snow algae live in the
top 10 inches or so of recent (the last year’s) snowfalls. Treading on the snow
can release a faint smell of watermelon from the algae.
Blue eyed shag. A cormorant that nests in Antarctica down to the Peninsula. Blue
eyed shags will not go far from open water, a fact that early Antarctic explorers
soon learnt. When they are sighted by an entrapped ship it is a sign that an ice-free
region is not far away.
Blue eyed shags always seem to have a preference for the most dramatic of
nesting places. As they can fly – unlike penguins – they are able to nest in sites
very close to the sea but without needing a convenient beach or sloping rocks to
be able to leave the sea.
Blue eyed shag coming into land at its nest site. This can be a tricky
manoeuvre as shag nests are often pretty thick on the ground, so the birds need to
be careful of the neighbours as to where and how they land. They also often nest
on very steep or exposed ledges.
Cape Pigeons or Pintados are common small birds around Antarctic coasts.
They are a similar size to common pigeons though are not closely related, being
sea birds. They nest on ledges close to the sea.
Snow petrel courtship takes place largely in the air as the female leads the
males in an aerial ballet around the cliffs where they nest. The males task is to
keep up. Unwelcome attention is responded to by some accurately sicked-up krill,
the source of this males pink necklace.
Despite their small size and apparent fragility, snow petrels are quite capable
of toughing it out on the ice with no other shelter than putting their head under
their wing. Here at -20°C and 15-20 knot winds.
While snow petrels need some open water to fish for krill through, that water
can be as apparently restricted as a tide-crack. Tide cracks form when the tide
rises and makes the surface of the sea that little big bigger causing a crack that can
be several miles long, but no more than 1-2 feet wide at most. At low tide, it closes.
Krill are the engine that drives the
Antarctic ecosystem. They are shrimplike crustaceans about 4-5 cm (2
inches) long.
They feed on microscopic
phytoplankton, floating plants that
respond quickly to the rise in daylight in
the spring. As krill are so large, they are
available to nearly all Antarctic animals
that are bigger than they are.
In other oceans, the animals that feed
on phytoplankton tend to be smaller, so
the ability to “tap” the food chain so
close to the bottom is not available as it
is in Antarctica.
Krill outweigh the human population of
the earth by a factor of 2 or 3. Single
swarms have been estimated as
containing over 2 million tons of krill
spread over 450 square kilometres.
Antarctic fish are probably the best cold-adapted fish that the world has ever
seen. They have lived at between -2°C and +2°C for 20-30 million years with virtually
no transfer of species with any other seas. This ice fish has no red pigment in its
blood to carry oxygen hence its white gills, low temperatures and high blood volume
mean it is not required.
This small arthropod is found only around Signy Island in the South Orkneys
group. The Antarctic Ocean is unique in that it has no Decapod crustaceans –
crabs and lobsters – despite them being common elsewhere including the Arctic
Ocean. Other species take their roles instead.
Inshore fish may be caught by marine biologists using nets such as this, or by
hand while diving. Many Antarctic fish have special proteins in their blood that act
as an anti-freeze allowing them to become supercooled, but still go about their
lives as normal.
Diving during the Antarctic winter poses its own problems – a lack of water
being one of them! These divers are preparing to lay a line for a fishing net. 2
holes are made 100m apart, a line is attached to a diver who swims from one of
these holes to the next. The line is then used to set and recover fishing nets.
Dive holes can be made with a chainsaw with an especially long blade as
has happened here.
A square hole is cut and then the
floating ice cut into 4 pieces. These 4
pieces are then pushed down from the
surface under the ice where they float
up against the ice by their natural
buoyancy. These 4 pieces can be seen
around the diver.
Under-ice divers are always attached to
the surface by a rope held by a line-man
who lets the line out or pulls it in by a
series of commands. In emergency, he
can pull the divers manually back to the
surface through the hole.
Diving in the winter is a special treat. As the sea-ice calms the sea movement
down completely, any suspended sediment or particles just fall out of the water, so
the visibility increases to crystal clarity. Diving under ice can be an ethereal
experience. A fun thing you can do after a dive is to take your weight belt off and
push yourself back under the ice, stand up and walk about upside down.
The summer months means that boating is restored as an activity. Icebergs
such as this are usually given a reasonably wide berth as they may be unstable
and tip up. Sometimes though they’re just too fascinating to leave alone, and you
have to take it in turns to pose and take pictures.
Icebergs are shaped by many influences and as they age, they may become
unstable and break into smaller pieces or just tip up to a more stable position. They
are scarred with these processes and no two are identical, but some are prettier than
others.
An iceberg having undergone much erosion and melting above and at the
waterline. It’s not really that big, the ship is quite a long way behind.
This was a particularly fascinating place. We sat in a small high-powered
inflatable boat watching the waves rise and fall. As they rose, the gap in the berg
was flooded, as they fell it was just ice. We debated whether or not to try and rush
through on the rise. In the end discretion was probably the better part of valour.
Icebergs are endlessly varied in shape, but also in the way they appear in
different weather conditions. This specimen looks particularly spooky in the heavy
sea fog hanging at an altitude of 20-30 feet.
Mountains that emerge from an expanse of ice are called “Nunataks” they
are like islands that emerge from the ocean, except that in this case the ocean is
one of snow and ice. Surprisingly such sterile environments can attract birds that
nest on them despite being many miles from the sea and food.
Antarctica is very good at
dramatic scenery.
Perched atop this particular piece
is the former Soviet
Leningradskaya Station on a 1,000
foot nunatak in Oates Land. This
base operated between 1971 and
1992, but was closed as it was too
expensive and difficult to resupply.
More recently there have been
moves to possibly re-open it again.
A Föhn bank is formed by a Föhn wind - a warm contour-hugging wind that is
blowing across Coronation Island in the South Orkneys group here. As the warm
wind (relative to the ice and rock) blows across the land, it causes snow and ice to
sublime. That is to turn directly from a solid to a gas without passing through a liquid
phase, so causing the cloud layer that can be seen.
Ice bergs trapped in sea ice – these are one of the wonders of being able to visit
an Antarctic winter, going out to them is like being able to walk up to and touch a
cloud. You know they’re there, you know they’re huge, but most of the time, they’re
for looking at from a distance and not touching.
One of the finest animals in the world (IMHO) – an Antarctic fur seal. These
creatures can seem quite intimidating at first contact as they feign attacks and
growl at you. When you’re more familiar and comfortable with their presence
however, they can provide the best interactions possible with a truly wild animal.
Fur seals were brought very close to the edge of extinction by sealers n the
1800’s. They have recovered to a remarkable degree since however to the point
where their numbers are threatening some fragile habitats in sub-Antarctica
islands.
A young Weddell Seal pup with mother behind. Weddell seals are animals of
the ice. They live further south than any other mammal. Between the end of
August and early November in the southern hemisphere spring, the mother seals
to be haul themselves out of holes in the ice and give birth to their pups.
Newly born Weddell seal pups are officially some of the worlds cutest
creatures, they flop about the ice in the early days after their birth, not able to coordinate their over-sized flippers before they grow into them. The mother arrived
at the birth site some 10 days earlier pregnant and with enough resources of
blubber and protein to double the 25kg (55lb) birth weight of a pup in 10 days.
Weddell seal milk is one of the richest produced by any mammal. It contains
about 60% fat and is responsible for the rapid weight gain made by pups shortly
after birth. The pups are weaned at around 7 weeks when they weigh about 110kg
(242lb). Adults will weigh up to 400kg (880lb) and are up to 3m (10ft) long.
Keeping breathing holes open like this wears away the teeth of Weddell
seals and it is this that means that the Weddells only live to about 18 years old,
about half the life-span of another similar Antarctica seal the crabeater for
instance.
Weddell seal pups don't automatically realise that they can or should dive and
the early attempts are amusing to watch. The mother pushes the pup into the water
against its will. She then pushes its head under the water - again against its will.
There is much coughing, spluttering and panic before the pup realises that it can
hold its breath under the water and that this in fact does help!
Displaying skua. Display is to, or for a mate or other skuas to establish a
territory. Sometimes the birds do this as a pair, it is quite an impressive sight and
the squawking can be heard some considerable distance away. Skuas will also do
this if their nest is being approached by an unwanted visitor.
Sometimes the first sight you
get of a skua is a sudden
heart-stopping rush of air
through the wing feathers of
a bird flying at speed past
your head from behind, much
too close for comfort. If you're
particularly unlucky or if its very
unhappy at you being so close,
then rarely a whack at the back
of the head by the front of the
wing may result.
This is actually quite a good
way of finding skua chicks when the parents start getting
upset you know you're very
close to the excellently
camouflaged chick.
Here’s a parent letting this
researcher know he’s far too
close for comfort!
Antarctic terns nest on the Antarctic peninsula and islands. If an intruder gets
too close to the nest site, they will dive-bomb. This picture, this is exactly what it
seems like! The tern dives to great speed and lets out an ear-piercing call about 2
feet from your head that is perfectly timed to cause maximum panic!
A Giant Petrel, commonly known as a Geep, GP or to the old sealers as Stinkers This name came from their habit, quite common amongst sea-birds, of vomiting on
any one or thing that approached them and seemed to impose a threat. They build
the traditional Antarctic nest of small stones, but always seem to manage quite an
impressive pile of them in comparison to penguins for example.
Giant Petrel chick. The adults spend much of their time scavenging and are
always to be found where there is a dead seal or whale carcass. Sometimes eating
so much that after a couple of attempts at taking off due to excessive baggage, the
only remaining option is to be sick in order to lighten the load. They are large birds
the size of a turkey with a wing span of 2 metres or more.
An American sheathbill (also known as "Mutts") they're the garbage disposers
of the Antarctic. They will eat just about anything that they can lay their beaks on.
The only Antarctic bird species that don't have webbed feet and so are not able to
fish for food like the others. They usually stay out of the path of the sea-ice and
move north in the winter when the worst weather comes.
This sheathbill (Mutt) has been feeding on (in) a dead seal. They frequently
scavenge penguin colonies for eggs, dead chicks, even penguin faeces - there's
occasionally some not fully digested food there.
Southern Elephant Seals were one of the main targets for Antarctic sealers.
They were hunted for their blubber. Blubber is a “blanket” of fat just beneath the
skin. They need this as they are warm blooded mammals and need to keep a
normal body temperature despite hours in seas below freezing that would kill most
mammals within minutes.
Elephant seals have clear “sexual dimorphism”, there is a big difference
between males and females. Males, such as this individual can grow to be 8 times
heavier than the females. They bear the scars of many fights with other males to
gain supremacy over harems of females and become the “beachmaster”.
Clouds scurry past in Antarctica like no-where else on earth. The cold and
the wind make each day feel clean, new and fresh, especially when the sun
shines. It’s not a landscape to observe from the outside, but to be in and feel part
of, even if the part you feel is rather vulnerable and at the mercy of that cold, wind
and sun.
Sunsets can seem ethereal as snow and ice reflect the sky, so it’s not just a
case of the land silhouetted against the sky, but of the sky colouring the whole
world. Ice and snow become a canvas to be painted by the rays of sunset and
sunrise.
What is the biggest
threat facing
Antarctica?
To be ignored
For people not to know
about it.
If you don’t know about
something, how can you
care for or protect it?