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THE
FOCUS ON NATURE BIRDING AND NATURE TOUR IN ICELAND
June 2011
"Iceland and the Plight of the Atlantic Puffin"
Atlantic Puffins were among
the birds enjoyed
during the FONT tour in Iceland in June 2011
Links:
List
of Birds during our Iceland Tour - June 2011
Birds during previous FONT Iceland Tours
Complete
Iceland Bird-List
(383 species, including vagrants from mainland Europe, Asia, & North
America)
Wildflowers of Iceland (with some photos)
Upcoming FONT Birding & Nature Tours in Iceland
A following narrative was written by Armas Hill, leader of the tour:
Most of the many Atlantic Puffins in Iceland
are not along the northern coast of the country, but rather, they are locally
abundant along
the southern.
In the southernmost town on mainland Iceland, late in the evening, above the
Hotel Lundi in the heart of the town, I noticed a Puffin flying out from the
cliff. "Lundi" is the Icelandic word for "Puffin".
I watched the small bird fly with its little wings pitter-pattering rapidly. It
headed toward a distant swarm of birds that were all flying about in the twilit
sky by another cliff just above the ocean. I went closer.
That swarm, that at a distance appeared superficially as an evening mass of
insects or bats was of course, as I just noted, and knew at the time, of birds.
And all of them were Puffins with their little wings fluttering rapidly. There were at least a thousand in the sky. And many more than that were
out on the water. Others were standing out by their burrows on the cliff-tops.
It was going on midnight, but as it was mid-June, the lightness enabled me to
enjoy the spectacle.
The place in Iceland with the most Puffins was not far away: an offshore
group of 14 islands known as Vestmannaeyjar,
or the Westmann Islands.
We went there the next morning on the first ferry. What was more than a 3-hour
(and sometimes rough) ferry-ride to the islands is now less than half an hour,
from a new port.
From the ferry on the way to Heimaey, the
only one of the Westmann Islands that is inhabited by people, about 4,000 of
them, a flock of Manx Shearwaters was seen. In Iceland, that species only
nests in Vestmannaeyjar.
Also seen from the ferry were Northern Gannets, Northern Fulmars, Black-legged
Kittiwakes, and yes, Puffins.
Whereas there are people on only 1 of the 14 islands, there are birds inhabiting
all of them, on sheer rocky cliffs and otherwise. When we took a boat-ride
throughout the islands, we saw many.
There were 5 species of alcids. In addition to the Atlantic Puffin,
there were Razorbills, two kinds of Murres (mostly Common,
also some Thick-billed), and the Black Guillemot. We saw all of
these on and by those shear rocky cliffs along with the many Kittiwakes and
Gulls and Gannets.
On Heimaey Island, where we spent most of a
day, and a night, there's a place above a high seacliff that's said to be a
place for Puffins. At that spot, there is a wooden hide, or blind, with
openable windows, at a "Puffin spot". When we first went there,
during the day, there were Puffins in the area, but they were ALL below,
well below us, on the water of the sea. There were none on the nearby grassy
slopes above the cliffs.
When we returned later in the day, it was much the same.
But I remembered the previous evening's activity back by the mainland coastal
cliffs, so I returned to the hide at about 10pm. And, then, at that time, the
Puffins were coming in too!
So, I went back to the hotel to get the others, and soon, when we were inside
the hide, there were Puffins outside, sometimes nearly within
reach! There were well more than a thousand, for about 2 hours, before
they started to go, individually or in small groups, back down to the ocean
below.
What we learned, sadly, when we were in Iceland, and particularly when we were
in the Westmanns, is that the Atlantic Puffin has not been doing well,
for a few years now. It is becoming, and I must say sadly again, a species in
peril.
Yes, the same bird that in Iceland is depicted so many places, as on postcards
everywhere, on shirts and other garments, and on signs and in ads, is now in
trouble. The bird, clown-like in appearance, called the Puffin, or Lundi,
has been as common in Iceland as a caricature can be.
Referring to the "real thing", Iceland has had the largest number of Atlantic
Puffins anywhere, with over half of the total global population of the
species residing there in the summer.
An estimated 3 million pairs of Atlantic Puffins have been breeding in
Iceland each year - that is about 6 million birds. On average, 70 per cent of
the total Icelandic population of Atlantic Puffins are breeders, so the
total number in Iceland each summer has been from 8 to 10 million
birds.
And about half of the Atlantic Puffins in Iceland have been in the Westmann
Islands. As noted earlier, it has been the place in Iceland with the
most - but not just the most in Iceland.
The Westmann Islands has been the place with the most Atlantic Puffins on
Earth, with some 700,000 nesting pairs - that is 1,400,000 birds, with each pair
normally raising but one young bird per year.
So, it has been, on average, that about 20 per cent of the global population of Atlantic
Puffins (1 out of 5) has nested on the Westmann Islands.
And the birds even had a new island there on which to nest. It was noted that
there are 14 islands in the Westmann group. There were 13. That was until 1963
when a new island was created, as a volcano erupted in the ocean. On that
island, called Surtsey, afterwards,
Atlantic Puffins began making their
homes.
But during more recent years, the Atlantic Puffin population has fallen
so drastically that the species is being put on the Birdlife International
"watch list".
Overall, during the last decade, there has been a 20 per cent drop in the
species' population. And during the most recent years, the situation has
worsened yet.
In 2007, Maria Frostic, an employee of NASA in the US, took a leave in July and
August, and went to the Westmann Islands,
intending to make a documentary film about medieval sagas. Instead, learning
immediately upon her arrival how poorly the Puffins were doing during
that nesting season, she did instead a film entitled "Plight of the
Puffins" that aired the following year on television on PBS.
In 2009, it was in the news that on the Westmann Islands "very few Puffin
chicks hatched and survived the summer".
When we were in the Westmanns in June 2011, we were told that in the summer of 2010,
the Puffins on
the islands again did not successfully raise their young. And we were also told that the
current 2011 season did not yet seem to be any better.
A reason said for this, and also purported in that 2007 documentary
film, is the depletion of the Puffin's food-source, a fish called the Sand-eel.
From whatever cause, and maybe it's been said due to climatic change, that fish
is now scarce where it used to be abundant. And where it is now scarce is where
the Puffins are during their nesting season.
On the Westmann Islands during August, for years, there has been a
tradition. Puffins are weak flyers, even at best. They do best when they
take off into the air from the top of a cliff. Sometimes, young Puffins, after leaving their burrows, descend not to the water as they should, but
instead into the town on Heimaey.
They land on a moist road or street as it appears to be water. In the
evenings, when that happens, the children in the town go about and gather up the
forlorn Puffins, putting them in boxes to release them from cliff-tops in
the morning. The child, who doing so, saves the most becomes the "Puffin
Fledgling King" for a year. We were told that in 2010 there were no
young Puffins for the children to rescue.
After my return home from Iceland, I looked a bit more into the situation
regarding the Atlantic Puffins in Iceland. I found it written that the
decline of the species has been due in part to factors such as "human
persecution", pollution, and the reason that I had already been told,
"a shortage in the food supply resulting from oceanographic changes".
Due to the last of these, it's written that there has been ""poor
breeding success" and "a high mortality rate of young
birds".
I found it said that the fish consumed by Atlantic Puffins include, as
noted already, Sand-eel, Ammodytes sp., which is the majority of the diet
of the chicks, and some forage species including juvenile pelagic fishes such as
Herring, Clupea hareegus, and juvenile and adult Capelin, Maliotus
villosus.
I also found in a non-nature publication that in 2010, at least 38
Icelandic fishing vessels each caught fish worth more than 1 billion Icelandic
Kroner (or 8.6 million US dollars), which was a new record. As a comparison, 28
vessels reached that goal the previous year, in 2009.
Relating to the Capelin, the small cold-water fish eaten by Puffins,
after some years with meager catches, it is said that 390,000 tons will be
fished this year, providing a needed boost to the economy and a good increase in
exports. A starting quota of 200,000 tons was issued when the size of the stock
was first estimated. A further quota of 125,000 tons was later added. The quota is
decided on the basis of leaving 400,000 tons of spawning Capelin in the
waters to ensure sustainable stock.
A bit about Capelin biology: They come to the sandy shores of southern
Iceland to spawn between the ages of two and six. After spawning, most
die.
During the last 3 years, Capelin were scarce in Icelandic waters, with
about 100,000 tons caught each year.
Hopefully, an increase in one of the prey of the Puffin will help the bird.
And if that were to happen with the Sand-eel, the Puffin
would have better times ahead. Optimism certainly is not in order yet. Only time will tell.
Mention was made earlier of a new island that was created in 1963.
Another offshore Icelandic island disappeared back in the 1800s, and its doing
so was at least partly a factor in the disappearance forever of a bird,
referring to the extinction of the flightless alcid, the Great Auk.
The island of Geirfuglasker, where most of
the Icelandic Great Auks bred, disappeared under the sea in 1830 during a
volcanic cataclysm, resulting from an earthquake. Birds moved to Eldey
Rock when their former home sank. It was there, on Eldey
Rock, off the coast of the Reykjanes
Peninsula in southern Iceland, where the last of the world's Great
Auks, a pair, were clubbed to death on June 3, 1844. Unfortunately, Eldrey
was more accessible to men than Geirfuglasker
had been.
Now, Eldey Rock is the site of the largest
colony of Northern Gannets in Iceland.
During the FONT June 2011 Iceland Tour, we
were on the coast of the Reykjanes Peninsula, where we could see Eldey
Rock, and where there is now a larger-than-life statue of the Great
Auk. It's too bad that the bird is no longer "in
life".
One thing that there is now more of in Iceland than there has been in the recent
past is forest. Some good reforestation has been going on for
years.
Walking in an Icelandic coniferous forest, as we did during our June 2011
tour,
is a nice experience, even when the only birds are Redwings and Redpolls.
During our walks, a small white moth was seen. In all, 82 species of Lepidoptera
(butterflies and moths) have been recorded in Iceland, compared, interestingly,
with 76 in Norway and 77 in Britain.
Iceland is not a place to see butterflies. Only 4 species have ever been
found, all as vagrants: the Small Tortoiseshell, Red Admiral, Painted
Lady, and the Peacock.
Nor is Iceland a place for land mammals. Only the Arctic Fox is
native. Each year, lately, the odd Polar Bear has been coming ashore into
northern Iceland from the ocean. And some other mammals have been introduced by
man, including the Reindeer, American Mink, and a mouse or
two.
Of course, the most obvious of the mammals in Iceland today are the sheep
and the horse. They seem to be "everywhere", especially the sheep.
They occur even high up in the mountains and on small remote islands, on both at
times on precipitous slopes. The total winter stock of sheep in Iceland
is said to be about 900,000 animals.
Not many cattle are now seen as one travels around Iceland. But during
the first 800 years of human settlement in Iceland, until the 17th century,
there were many, peaking with about as many as 120,000 head. It was due to the
overgrazing by cattle that sheep later became the principal
livestock in Iceland.
Horses came with the first settlers to Iceland, the "most useful
servants", being tough, strong animals, They bore the brunt of long,
arduous working days. They brought home hay from distant fields. They helped
round up sheep in the mountains in the autumn. They took part in festivals. And
they were the only means of transport for both people and goods.
There were no bridges in Iceland until the early 20th Century, and all of the
large and dangerous rivers had to be crossed on horseback, a tricky affair that
could be fatal for both horse and man.
These are just some of the reasons why it's been said that without the horse,
Icelanders in all probability would not have survived in their barren,
mountainous, and remote land.
Today, the Icelandic Horse is one of the most picturesque aspects of the
Icelandic countryside, being attractive animals, with a notable characteristic
being their "fifth gait", a running walk that is not found in many
other breeds of horse.
It must be said that even though Iceland does not have
many wild land
mammals, butterflies, or any reptiles and amphibians, there is a considerable
amount of nature in the country, and much of it is quite interesting.
In the waters, there are sizable populations of marine mammals and large numbers of
fish.
There are, from spring through fall, large numbers of birds, with some of the
species in especially large numbers. The norm for species, at any given time, is
not large, with just over 70 species nesting annually. But it is
quite interesting that over 350 varieties of birds have been noted as
occurring in Iceland, as the island can act as a migrant for vagrants
from the Americas, elsewhere in Europe, and even as far as Asian Siberia.
And the geology of Iceland is, simply put, fascinating, or to use a word
of the day, "awesome".
The nature of Iceland includes glaciers, glacial rivers
with black sand, volcanoes and newly-formed lava fields,
extensive heaths and wind-blasted deserts, untouched wilderness,
areas of geothermal activity, crystal clear mountain streams, waterfalls,
sea cliffs, and the midnight sun.
An interplay of fire and ice occurs that can be found nearly nowhere else
on Earth.
Much of what was just noted in the previous paragraph was what we saw and
experienced during our June 2011 FONT
Tour in Iceland.
The oldest parts of Iceland were formed about 15 million years ago. But the
country is relatively young, with half of it less than 2 million years old, and
as much as 80 per cent less than 8 million years old.
There are almost 100 volcanoes in Iceland, of which about 30 are active.
Many eruptions have been recorded since the settlement of the country,
especially in four areas: Reykjanes, Hekla, Katla, and under the Varnajokull
Glacier. Other devastating eruptions have occurred outside those areas in the
Myvatn district, Lakagigar, Askja, and in the Westmann Islands in 1973.
The biggest of these were the Fires of Skafta. In 1783-84, lava and ash were
emitted from a fissure, 25 kilometers long, resulting in a row of craters called
Lakagigar. The lava covered 580 square kilometers and flowed up to 55 kilometers
from the craters.
Huge quantities of ash were discharged into the atmosphere forming a cloud that
spread around much of the Northern Hemisphere, influencing the climate of
northern and western Europe for several years.
More recently, in 1973, a powerful volcanic eruption shook the island of Heimaey,
in the Westmann Islands, causing extensive
damage to property. The population of about 5,000 escaped to the mainland. About
one-third of the houses and buildings on Heimaey
were destroyed in the eruption.
During the day and night that we were on Heimaey Island during our June 2011,
I'm glad to say that there was no volcanic activity whatsoever.
The famous volcanic eruption in Iceland in 2010, spewing ash and closing
European airports, was that of Eyjafjallajokull.
There are a number of areas in Iceland where geothermal heat reaches the
surface. Warm sources exist all over the country, but high temperature areas
reaching 200 degrees Centigrade are restricted to the active volcanic regions.
Warm pools and boiling fumaroles are characteristic of Iceland, especially geysers, although they are few in number. The most well-known geothermal
phenomenon is undoubtedly Geysir, from which the English word
"geyser" is derived.
The plume of steam going at intervals high into the air that we saw during our
June 2011 tour was the geyser known as Strokkur,
very close to where Geysir is now quiet.
The place, where during the tour, we experienced the most hot springs and pools was
the town of Hveragerdi.
Earthquakes occur regularly in Iceland, but most are weak, as is usually the
case where the continental plates are separating. Tremors occur mostly in
volcanically active areas, mainly in southern Iceland. A powerful earthquake
hits the southern region every 100 years or so. The most recent was in the
summer of 2000.
There were no earthquakes during our Iceland tour in June 2011.
The Mid-Atlantic Ridge, separating the European and American continental plates,
is nearly all under the waters of the ocean. But it is above sea level in
Iceland. In the southwestern part of the island, it is quite apparent. At a
bridge over the ravine in that area, one can walk "from America to Europe
and back again". We crossed that bridge during our June 2001
tour.
Iceland also lies at the meeting point of two great ocean currents. The warm
water of the Gulf Stream come from the south and meet the cold water streaming
down from the Arctic. Northern Iceland touches the Arctic Circle, at 66 degrees
north of the equator.
From the distant Caribbean Sea, the Gulf Stream carries carries warm water,
passing to the south of Iceland, and also to the west where it meets the icy
East Greenland Current.
Sea temperatures are on average 5 to 10 degrees
Centigrade of the south coast of Iceland, but 1 to 8 degrees Centigrade in the
north.
Iceland's climate is categorized as "temperate". It can be wet and
rather cold. Statistics indicate the average temperature to be 5 degrees
Centigrade, which is above that normally expected as such a northern latitude.
Glacial rivers in Iceland have their sources under icecaps, of which the
Varnajokull Glacier is the largest with 8,300 square kilometers. It is the
largest glacier in Europe. Other glaciers in Iceland, Langjokull and Hofsjokull,
are with about 1,000 square kilometers. Myrdasjokull Glacier is just under 600
square kilometers. That glacier could be seen in the distance from where we were
in southern Iceland during our June 2011 tour.
Glaciers are well-known features of the Icelandic landscape, covering about 11
per cent of the country. Their area has fluctuated since the human settlement of
Iceland.
The first human settlement in Iceland was back, way back, around the year 870,
during the Viking Age (from 800 to about 1050 AD). During that time,
bands of Norseman (that is, from Norway), known as Vikings, searched for new
territories, for pillaging, profit, and in which to settle.
The Swedes went east to Kiev in 862 and south to Byzantium. The Danes went south
to Normandy and England. The Norwegian Vikings made their way to Scotland,
Ireland, and then sailed further on the Atlantic Ocean to settling the
uninhabited Faroe Islands and Iceland. From Iceland, they went to Greenland, and
then on to the east coast of North America. Around the year 1000, maybe the most
famous of the Vikinfgs, Leif Eiriksson sailed from Greenland to what is
now eastern Canada off Newfoundland and maybe further south.
During our tour in June 2011, when we were in Reykjavik,
we saw a large statue of Leif Eiriksson in front of the famous landmark church
in the city, Hallgrimskirkja.
It is interesting that Christopher Columbus is said to have visited Iceland. He
visited Bristol, in England, in 1477, where he certainly heard of lands in the
west from English sailors. According to an account in his biography written by
his son, Columbus traveled from Bristol to Iceland, his first ocean
voyage.
A parliamentary assembly first functioned in Iceland back in the year 930,
established at a place called Thingvellir,
about an hour from Reykjavik by the shore of Iceland's largest lake, Thingvallavain,
and along the Mid-Atlantic Rift. That
assembly, called the Althing, has continued to function annually.
When we visited Thingvellir, now in a national park, during our June 2011 tour,
an "Icelandic Wren" was singing in the rocks along the rift.
It was at Thingvellir that the modern Icelandic Republic was born in 1944. That
was when Iceland separated from Denmark. it was a result of World War II when
Denmark came under the control of Germany, and Iceland was declared by Germany
to be in the "war zone". Britain and the United States then came to
the defense of Iceland.
Independence for Iceland in 1944, at Thingvellir,
came on June 17, now known as Iceland's "National Day". That
holiday was our last full day in Iceland.
We were, that day, in Rekjavik. as were many
Icelandic people celebrating with parades, speeches, and performances, mostly in
front of the Parliament Building in the city.
Traditionally, on that day, some woman wear a special dress called the Fjalkonan.
When wearing such a dress, as a "Mountain Woman", a poem is
read. The Fjalkonan represents the Icelandic spirit and nature and it
became a symbolic figure in Iceland's struggle over the years for independence.
That dress is normally worn only on National Day. It may be less so, on some
other holidays, and when people are dancing national dances.
We were fortunate on National Day to meet a lady wearing the Fjalkonan as
we were about to have lunch in a restaurant in Reykjavik, where we also saw some
young girls in pretty holiday garb.
Our lunch on that National Day was really quite Icelandic, as it was with lamb
and salmon, both specialties of the country, along with an array of Icelandic
salads and vegetables.
A traditional Iceland lunch was also enjoyed, earlier during the tour, in a
small fishing village in the remote northwestern fjord region of the
island.
It was with various types of fish, breads, vegetables, fruit, and yogurt. A nice thing in
any country is to enjoy during a tour a "typical country meal".
Mention should be made, as I nearly end this narrative, of the most famous of
the geothermal hot pools in Iceland, the Blue Lagoon. It was formed when
a local energy company was drilling for hot water. Minerals crystallize as the
water cools, and thus the pool takes on a vivid blue hue.
Bathing there, as done during the last full day of our tour, is both an
enjoyable and healthy experience.
Late that night, as I walking at just about midnight, I couldn't help but notice
that the sky overhead was beautiful with that same vivid blue hue as earlier
that day at the lagoon, with a smathering of beautiful pink-red clouds.
As it was just a few days before the longest day of the year, the Sun was
sitting low on the horizon, a Midnight Sun. It was the last if many fine
experiences during our June 2011 FONT tour in Iceland.
A traditional Icelandic
lunch
in the northwestern fjords region
during the June 2011 FONT Iceland Tour.
(photo by tour participant, Susan Lin)