Blue icebergs and glaciers of Iceland. Iceland glaciers Petra mineral museum

Volcano Hekla, also called the "gate to hell", is an active stratovolcano.

The oldest recorded eruption of Hekla occurred in 1104, but scientists know for certain that it has been active for at least 6,600 years.

The length of the mountain range, which includes the Hekla volcano, is 40 kilometers. And the most active part of the volcano is a crack in the rock 5.5 kilometers long. The volcano got its name - Hekla - because its top is almost always covered with clouds - like a cloak, because the literal translation of Hekla is a short cloak with a hood.

Her second name - "Gateway to Hell" - Hekla received from the monks. So, in the poem of the monk Benedit from 1120 about the adventures of Saint Brendan, the volcano is referred to as the prison of Judas. And in the 16th century, Caspar Peucer wrote that the gates of hell could be found in the bottomless chambers of the volcano Hekla, and the belief that Hekla was the gate to hell persisted until 1800. There is another story that says that witches gather here every Easter.

Over the past 900 years, there have been over 20 violent eruptions of the Hekla volcano. The last volcanic eruption was recorded on February 28, 2000.

Coordinates: 63.98757600,-19.67355900

Vatnajökull glacier

Icelandic blue glaciers are the hallmark of this extraordinary northern country. Well, the Vatnajökull glacier is one of the largest not only in Iceland, but also in Europe. The unusual local relief is due to the action of underground volcanoes that erupted right under the surface of the ice.

The glacier landscapes are truly stunningly beautiful and are fertile ground for amateur photographers. In addition, the line of sight on the glacier is one of the largest and is even listed in the Guinness Book of Records. Open spaces up to 550 meters open to the sight.

Coordinates: 64.54844000,-16.78710900

What sights of East Iceland do you like? There are icons next to the photo, by clicking on which you can rate this or that place.

Valley of Tjorsardalur

The valley of Tjorsardalur impresses with a variety of landscapes and rich colors.

One has only to see this picturesque painting once to fall in love with it forever. Against the background of sandy lava fields, the green of dwarf birches looks contrasting, and local rivers and waterfalls add all shades of blue to this natural idyll, which makes the Tjorsardalur valley unimaginably beautiful.

The longest river in Iceland, Tjorsau, also flows here, it is the most important source of electricity in the country.

In addition, it is from the Tjorsardalur valley that you can see the most active volcano in Iceland - Hekla. By the way, in 1104, after the end of the period of settlement of the island, the volcano woke up without warning and wiped out 20 farms in the Tjorsardalur valley.

Coordinates: 64.13390300,-19.85026100

The Leigardalur Valley is everyone's favorite park for family recreation and entertainment.

There is a large outdoor pool on the territory of Leigardalur, you can swim in it all year round thanks to the thermal springs. In addition, the park houses Reykjavik's main sports stadium and the Laugarsholla sports and exhibition center. Here everyone will find something to their liking: walking and jogging tracks, outdoor football fields and an indoor skating rink. A botanical park, a zoo and an amusement park will delight young travelers.

Coordinates: 64.14184000,-21.86711000

Hofsjökull glacier

Hofsjökull is the third largest glacier in Iceland (after Vatnajökull and Laundökull). It covers 996 km & sup2 and has a volume of 208 km & sup3, and is also the largest active volcano on the island. The highest point of the glacier is located at an altitude of 1765 meters above sea level.

From this glacier, the rivers Tjorsau (the longest river in Iceland), Blandau and Hvitau (a tributary of the Yolfusa river), rich in hydropower resources, originate.

The Hofsjökull glacier dome has a diameter of almost 40 kilometers! Its largest basin is 7x11 kilometers in size, but besides it, the glacier has a number of volcanic outcrops. The fumarole activity, concentrated in the middle of the complex, is the strongest on the island, in other words, while the volcano is dormant, it releases the largest amount of water vapor and other gases into the atmosphere of any existing glacier in Iceland.

Coordinates: 64.84426800,-18.81024200

Petra Mineral Museum

Petra's house in Stødvarfjordur has been home to her collection of minerals since 1946. Petra began collecting minerals as a child. Fortunately, this area is very rich in them, some of the stones from the collection of Petra are 10 thousand years old. From year to year, she replenished her museum with more and more stones, and now all these lovingly collected minerals can be seen in Stödvarfjordur.

The minerals collected by Petra constitute one of the finest and largest private collections in the world.

The Petra Museum is visited by about 20 thousand tourists annually, and Petra herself has not lived in her house for a long time, but comes here once a week to chat with visitors.

Coordinates: 64.83361200,-13.87428600

Hafragilsfoss waterfall

Hafragilsfoss is one of the largest waterfalls in the mountain ice river Jö kuls Fjö llum. The falls falls with a huge crash from a height of 27 meters (89 feet) and is about 90 meters (300 feet) wide.

The waterfall can be seen from both sides of the river, but the eastern side is more accessible and has a better view. To see the falls from the west side of the river, you must first go through a little adventure and climb steep climbs using several rope ladders.

The view from here is very picturesque, so if travelers are close to this place, they will definitely visit this waterfall either on their own or as part of excursions.

Coordinates: 64.66482300,-16.85483000

The most popular attractions in East Iceland with descriptions and photos for all tastes. Choose the best places to visit famous places in East Iceland on our website.

60 km ².

Due to geothermal activity, melt water accumulates under the glaciers, which can lead to a sudden flood of glacial lakes, called isl. jökullhlaup "jökullhlaup".

The likelihood of "jokullhloops" increases significantly when volcanic activity begins under the glacier. An explosion (rapid vaporization) of sub-ice water caught in a hot zone, in turn, can provoke a volcanic eruption.

Location of Iceland's 13 largest glaciers
Glacier Area, km² Volume, km³ Height above sea level, m Coordinates
1 Vatnajökull 8,300 3,100 2109,6 64 ° 24 ′ N NS. 16 ° 48 ′ W etc. /  64.400 ° N NS. 16.800 ° W etc. / 64.400; -16.800 (Vatnajökull)(G) (I)
2 Lungjökull 953 195 1360 64 ° 45 ′ N NS. 19 ° 59 ′ W etc. /  64.750 ° N NS. 19.983 ° W etc. / 64.750; -19.983 (Lungjökull)(G) (I)
3 Hofsjökull 925 208 1765 64 ° 49 ′ N NS. 18 ° 49 ′ W etc. /  64.817 ° N NS. 18.817 ° W etc. / 64.817; -18.817 (Hofsjökull)(G) (I)
4 Mirdalsjökull 596 140 1493 63 ° 40 ′ N NS. 19 ° 06 ′ W etc. /  63.667 ° N NS. 19.100 ° W etc. / 63.667; -19.100  ( Mirdalsjökull) (G) (I)
5 Drangayökull 160 925 66 ° 09 ′ N NS. 22 ° 15 ′ W etc. /  66.150 ° N NS. 22.250 ° W etc. / 66.150; -22.250 (Drangayökull)(G) (I)
6 Eyjafjallajökull 78 1666 63 ° 38 ′ N NS. 19 ° 36 ′ W etc. /  63.633 ° N NS. 19.600 ° W etc. / 63.633; -19.600  ( Eyjafjallajökull) (G) (I)
7 Tungnafellsjökull 48 1535 64 ° 45 ′ N NS. 17 ° 55 ′ W etc. /  64.750 ° N NS. 17.917 ° W etc. / 64.750; -17.917  ( Tungnafellsjökull) (G) (I)
8 Turisjökull 32 1350 64 ° 32'31 "s. NS. 20 ° 42'56 ″ W etc. /  64.54194 ° N NS. 20.71556 ° W etc./ 64.54194; -20.71556(Turisjökull)(G) (I)
9 Eiriksjökull 22 1672 64 ° 46′24 ″ s. NS. 20 ° 24'34 ″ W etc. /  64.77333 ° N NS. 20.40944 ° W etc./ 64.77333; -20.40944(Eiriksjökull)(G) (I)
10 Traudarökull 22 1236 64 ° 42′08 ″ s. NS. 14 ° 54′09 ″ W etc. /  64.70222 ° N NS. 14.90250 ° W etc./ 64.70222; -14.90250(Traudarökull)(G) (I)
11 Tindfjallajökull 19 1462 63 ° 48 ′ N NS. 19 ° 35 ′ W etc. /  63.800 ° N NS. 19.583 ° W etc. / 63.800; -19.583  ( Tindfjallajökull) (G) (I)
12 Torfayökull 15 1190 63 ° 53'39 ″ s. NS. 19 ° 07'37 ″ W etc. /  63.89417 ° N NS. 19.12694 ° W etc./ 63.89417; -19.12694(Torfayökull)(G) (I)
13 Snйfellsjökull 11 1446 64 ° 48′32 ″ s. NS. 23 ° 46′16 ″ W etc. /  64.80889 ° N NS. 23.77111 ° W etc./ 64.80889; -23.77111 ( Snйfellsjökull) (G) (I)

Write a review on Iceland's Glaciers

Links

Excerpt from Iceland's Glaciers

- My mother. My mother, my angel, my adored angel, mother, - and Dolokhov wept, squeezing Rostov's hand. When he calmed down somewhat, he explained to Rostov that he was living with his mother, that if his mother saw him dying, she would not bear it. He begged Rostov to go to her and prepare her.
Rostov went ahead to carry out the assignment, and to his great surprise he learned that Dolokhov, this brawler, Dolokhov, lived in Moscow with an old mother and a hunchbacked sister, and was the most tender son and brother.

Pierre has rarely seen his wife face to face lately. Both in St. Petersburg and in Moscow, their house was constantly full of guests. The next night after the duel, as he often did, he did not go to his bedroom, but remained in his huge, father's office, in the same one in which Count Bezukhiy died.
He lay down on the sofa and wanted to fall asleep in order to forget everything that happened to him, but he could not do it. Such a storm of feelings, thoughts, memories suddenly arose in his soul that he not only could not sleep, but could not sit still and had to jump off the couch and walk briskly across the room. Then he imagined her at first after marriage, with open shoulders and a tired, passionate gaze, and immediately next to her appeared Dolokhov's beautiful, arrogant and firmly mocking face, as it was at dinner, and the same Dolokhov's face, pale, trembling and suffering as it was when he turned and fell into the snow.
“What was it? He asked himself. “I killed my lover, yes, I killed my wife’s lover. Yes, it was. From what? How did I get to this point? “Because you married her,” an inner voice answered.
“But what am I to blame? He asked. “The fact that you married without loving her, that you deceived yourself and her,” and he vividly imagined that minute after dinner at Prince Vasily's, when he said these words that did not come out of him: “Je vous aime”. [I love you.] All of this! I felt even then, he thought, I felt then that it was not that I had no right to it. And so it happened. " He remembered the honeymoon, and blushed at the recollection. Particularly vivid, insulting and shameful for him was the recollection of how one day, shortly after his marriage, at 12 o'clock in the afternoon, in a silk robe, he came from the bedroom to the office, and in the office he found the general manager, who respectfully bowed, looked at Pierre's face, on his robe and smiled slightly, as if expressing with this smile respectful sympathy for the happiness of his principal.
“And how many times have I been proud of her, proud of her stately beauty, of her secular tact,” he thought; he was proud of his home, in which she hosted the whole of Petersburg, was proud of her inaccessibility and beauty. So that's what I was proud of ?! I thought then that I did not understand her. How often, pondering her character, I told myself that I was to blame, that I did not understand her, I did not understand this everlasting calmness, satisfaction and the absence of any attachments and desires, and the whole answer was in that terrible word that she was a depraved woman: he said to myself this terrible word, and everything became clear!
“Anatole went to her to borrow money from her and kissed her bare shoulders. She didn’t give him money, but she let him kiss her. Her father, jokingly, aroused her jealousy; She said with a calm smile that she was not so stupid as to be jealous: let her do what she wants, she said about me. I asked her once if she felt any signs of pregnancy. She laughed contemptuously and said that she was not a fool to want to have children, and that she would not have children from me. "
Then he remembered the rudeness, clarity of her thoughts and the vulgarity of expressions characteristic of her, despite her upbringing in the highest aristocratic circle. “I'm not some kind of fool… go and try it yourself… allez vous promener,” [get out,] she said. Often, looking at her success in the eyes of old and young men and women, Pierre could not understand why he did not love her. Yes, I never loved her, Pierre told himself; I knew she was a depraved woman, he repeated to himself, but did not dare to admit it.

Early in the morning, we drove along Route 1 along the southern coast of Iceland in order to reach the largest glacier in Europe in a day and have time to return back to Reykjavik. The distance to the Vatnajökull glacier is 450 km. With a favorable combination of circumstances, you can have time to make this trip during daylight hours.

We are repeating the path we traveled yesterday, leaving behind the famous Icelandic waterfalls and rocky outcrops, moving further and further to the east of the island. The landscapes undergo significant changes: after the village of Vik, where rocky outliers protrude far into the ocean, a real glacial desert begins, created by ancient glaciers, which, erasing everything in their path, slowly slide from high mountain plateaus into the valley, towards the Atlantic Ocean. We rush along a completely straight section of the road, and an absolutely flat plain of black color stretches around us, a strong cold rain adds to the severity of the landscape, the sky is completely covered with leaden clouds. Everything around is gray and black, such a picture can be pretty scary if you do not remember that here the weather can change quickly during the day. Indeed, as we move, we observe a gradual change, both landscapes and weather conditions.

The periglacial desert looks menacing, it seems that life has stopped here forever, but this is only the first impression, which is far from reality - in places on frozen lavas in the rain dense thickets of mosses and lichens turn green, in some areas, in deep dips formed along cracks, they manage to grow bushes and even tiny Christmas trees. But as we approach the huge glacier, which occupies more than 20 percent of Iceland's territory, its cold breath is felt, streams of icy air descend along the intermontane valleys to the ocean, and here we meet a completely flat, lifeless desert, the road cuts it, a perfectly straight section of the route is surrounded by gravel fields on which nothing grows at all. Black, lifeless desert, cold and inhospitable ... Having stopped the car, we go out onto this flat surface, and we feel like on another planet. If it were not for the mountains and glaciers looming on the horizon, one can imagine the infinity of the desert landscape. It is very cold here, a piercing wind is blowing, and in just a few minutes you freeze so much that returning to the warm interior of the car is a great pleasure.

The track approaches the rocks, they become much higher, piercing the clouds with their sharp teeth, hiding behind each other, from time to time presenting to our gaze deep gorges hiding between them with cascades of waterfalls flowing along them. Finally, in the misty haze, tongues of glacier sliding down from the mountain plateau appear, resembling frozen rivers from afar, millions of tons of eternal ice formed 5,000 years ago slowly flow into the valley.

We see the first tongue of a glacier falling from a high-mountainous plateau towards the ocean, the length of this icy river is several kilometers, then the glacier reminds of itself more and more often, and now, finally, we approach it close.

Ice blocks float along the bay, their color is bluish, which is typical for firn ice formed many thousands of years ago. Iceland produces the most popular drinking water in the world, which is 5,000 years old, since then it has been preserved in its original form, being the cleanest water on the planet, both physically and energetically. In those days, there was no technogenic civilization, so the water retained the memory of a clean ecological environment.

Ducks swim along the ice hummocks, suddenly two seals playing with each other emerge from under the water. Here, near the eternal ice, it is much colder, and the fauna is very different from that which we met in the western part of the island. From vegetation only mosses and cold-resistant flowering plants. No trees, no bushes - a real tundra.

For some time we observe the seals, which are exclusively occupied with each other, and we see an unusual vehicle rushing at full speed towards the water.

An amphibious vessel on large wheels carries tourists to ride on a glacier, wearing bright red life jackets. Here it rushes into the water with acceleration, the propeller starts up, and now it is a boat, rushing towards the eternal ice.

Unfortunately, due to lack of time we cannot take advantage of this miracle of technology, we move towards the coast, where we find all the same black sands covered with light gray pebbles, along the surf line - blocks of ice picturesquely cut by sea water, having the most bizarre forms, they ride the waves of the Atlantic, crashing down onto the coast.

But time is relentless in its run, and we still have a long way back to Reykjavik. On the way, we still call in to another branch of the glacier, here we manage to come close to it, seeing giant blocks of ice breaking off from the main massif and floating in a large glacial lake formed just below.

Iceland's glaciers cover 11.1% of the country's total land area and have a significant impact on the island's landscape. There are 13 large glaciers, among which the Vatnajökull glacier, the largest glacier in the country, occupies the first place in popularity among tourists. On the map below, you can see Iceland's glaciers in the form of white spots, a huge white spot is Vatnajökull:

Photo of the glacier tongues, taken from above:

The Vatnajökull glacier in all its glory:

Huge blocks of ice are in constant motion, imperceptible to the eye. The glacier slowly slides down and melts - this is clearly evidenced by the cracks on the ice of the thawed lake:

At the foot of the southern tongue of the Vatnajökull glacier, between the Skaftafell National Park and the city of Höbn, there is a unique glacier lagoon, Jokulsarlon, whose depth reaches 200 m. The lake appeared in 1934-1935. and as a result of the melting of the glacier, today it has grown to 18 sq.m.

The coast of the Jokulsarlon glacial lake, formed by solidified lava:

A block of ice in the rays of sunset:

It is noteworthy that there are two more glacial lakes near Lake Jokulsarlon.

The wonders of nature associated with the glacier do not end there. In the Vatnajökull glacier, the Kverkfjöll cave was formed due to hot springs under the ice. In the 1980s, this cave was measured: it turned out to be 2.8 km long and 525 meters wide.

Iceland Landscapes

Summing up the sights of Iceland, I bring to your attention a variety of landscape photos of this country, in order to make sure once again that Iceland is extraordinary, and its landscapes sometimes resemble the terrain of other planets from science fiction films.

Young lava fields on which a new ecosystem is being formed:

Torsmirk Valley:

Mount Valakhniukur in the Torsmork Valley:

Flocks of fulmars nest in the Torsmirk Valley in the Stackholt Gorge at an altitude of 100 meters above sea level.

Fool in flight:

Speaking of birds, it is impossible not to mention the bird called "dead end", of which there are quite a few in Iceland. This bird with an original color is interesting because, when chasing a fish, it dives and swims under water, using both its wings and legs.

Dead end caught a fish:

Let's continue the contemplation of the volcanic landscapes:

Atlantic coast near Vic village, from where the Three Trolls cliffs can be seen:

Rocks "Three Trolls":

Vik Village (South Iceland):

In the villages of Iceland, these well-fed sheep are raised:

Separately, it should be said about horses: in Iceland, all horses are very miniature, this is a special breed of "Icelandic pony", originating from the mixing of Northern European forest ponies with Celtic ponies brought by settlers to the island in the 9th century.

These small, but very hardy horses for a long time in Iceland were the only means of transportation, transporting goods and even crossing water bodies (Icelandic ponies swim well), and with their help, field work was carried out.

Icelandic ponies unmistakably find their way home, no matter how far they go, so after the annual drives of the sheep, the farmers who are busy sorting them often release the horses, and they themselves return to their native valleys.

Coast near the town of Husavik:

The town of Husavik is located in a sea bay ideal for whale watching and fishing. Ships with tourists ply along the bay in search of whales. It happens that during the whole day it is not possible to see a single whale, and on another day you can find a variety of animals performing unimaginable tricks.

Shallow water of the Khvita river flowing through the gorge:

And finally, another feature of Iceland is the northern lights:

If you decide to travel around Iceland by your car, then the optimal route is as follows: St. Petersburg - Vyborg - Turku - ferry - Stockholm - Oslo - Bergen - ferry - Lerwik (Shetland Islands) - Torshavn (Faroe Islands) - Seydisfjordur (Iceland). It should be noted that the variability of the weather in Iceland is a common thing. It may happen that at the end of May there will still be snow, and in December there will be long thaws. Therefore, at any time of the year, equip yourself "with a margin" for unstable climatic conditions, and do not forget to buy winter tires. And in order not to be hostage to earthquakes in mountainous areas, to avoid being hit by an avalanche or falling into a mud pit, stick to the marked hiking trails.

The Vatnajökull glacier, which is the largest in Iceland, demonstrates in its full size that not everything is so neglected in Icelandic society, and some words can be pronounced even by a non-Icelandic. And a well-pronounced word cannot carry something bad in itself.

So it happened with Vatnajökull. Translated from Icelandic, it means "giving water". And with this precision, characteristic of the Icelandic language, it is difficult to argue, especially in the summer.


Starting in spring, the glacier begins to turn limp and give out tons of water, which rushes through numerous tunnels to the sea-ocean in order to dilute at least a little the excessively salty water of it.

It happens, of course, that some piece of ice falls from the shore into the sea water, not having time to melt. But all this only decorates the coastal landscape. In addition, hard workers wind and currents, quickly pick up and carry the piece of ice into the sea, where it gets a beautiful name: an iceberg.



By summer, the sun begins to bake more and more and this affects the shape of the ice. In some places it forms impassable hummocks, and in some places it forms a bizarre figure. By the way, due to the strong waviness of the surface of Vatnajökull, excursions around it did not gain wide popularity.

And without an experienced guide, walking along it is out of the question. Because to fall somewhere in the direction of the earth's core, it is possible with a high probability.



The most beautiful thing that you can see here is undoubtedly the caves. For years, the water has sharpened numerous passages under the enormous mass of ice. Numerous tunnels on a sunny day are a fabulous sight. Due to the different thickness and structure of the ice, the colors of blue and light blue shimmer like the Northern Lights.



The caverns come in different heights and widths, but they all serve the same purpose: to let melted water flow out. In some places, overhead you can see ice that is a thousand years old.

It is particularly blue and clean. Visiting such caves usually takes place from December to March, since in summer it is dangerous to be not only under the glacier, but also next to it.



The Vatnajökull glacier covers an area of ​​over 8,000 square kilometers. The average thickness of its ice sheet is 400-600 meters.

The maximum thickness is over 1000 meters. According to the latter indicator, the glacier ranks first in Europe. And in terms of total area, he also ended up in the top three, triumphantly closing it.





The glacier itself, in support of its name, is the source of water for many glacial lakes, the most famous of which is the Yokulsarlon glacial lagoon.

It was formed on the coast in the first half of the 19th century, and due to the rapid melting of the glacier, it has grown by now to 18 square kilometers, with a depth of 200 meters. Search for cheap hotels.


How to get there.

There are several ways to get to Vatnajökull National Park. But initially you need to choose the place from which you will begin to explore the park.

The main point for receiving tourists heading towards the glacier is the city of Höbn. It can be reached by plane, bus and sea from Reykjavik. The distance between cities is 326 kilometers.

It is better to move around the park as part of excursions or in a rented car. These services are available in Höbn.