Iceland glaciers. Glacier Vatnayekyudl

The Watnaiyudle glacier, which is the largest in Iceland, demonstrates to all its size, which is not so launched in Icelandic society, and some words can repulse and nonyslandes. And a well-acrusted word cannot bear something bad.

It happened with Vatnayekyudlem. Translated from Icelandic, it means "giving water". And with this accuracy characteristic of the Icelandic, it is difficult to argue especially in summer.

Since the spring, the glacier begins to risen and extradite tons of water, which, through numerous tunnels, rushes to the sea-ocean, so that it is too long to dilute salty water ongoing.

It happens of course that some kind of ice will fall from the shore in sea water, not having time to melt. But all this only adorns the coastal landscape. In addition, workers wind and flow, quickly pick up and include iceclock in the sea where it acquires beautiful name: Iceberg.

By the summer, the sun begins to spit more and more and it affects the shape of ice. In places it forms impassable torosa, and in places of the bizarre form of the figure. By the way, due to the strong waviness of the surface of the Vatnaiyukudla, the excursions on it were not widely popular.

And without an experienced self, walk around it cannot be speech. Because to fall somewhere in the direction of the earth's kernel, it is likely to be likely.

The most beautiful thing is that you can see the cave unconditionally. For years, the water sharpened numerous passages under the huge mass of ice. Numerous tunnels on a sunny day are committed to a fabulous spectacle. Due to the different thickness and structure of ice, paints of blue and blue shades are transfused like the northern light.

Cave-passages have different heights and widths, but they all serve as one goal: let me push the wounded water. In some places, it is possible to see the ice with a led one.

It is distinguished by a special blue and purity. A visit to such caves is usually from December to March, as in the summer it is dangerous to be not only under the glacier, but also next to him.

The Watnaiyukyudl glacier occupies an area exceeding 8000 square kilometers. The average thickness of its glacial cover is 400-600 meters.

The maximum thickness exceeds 1000 meters. According to the latter, the glacier ranks first in Europe. And according to the total area, he also found himself in a prize tripler, triumpharally closed her.

The glacier himself, in confirmation of his name, is a source of water for a variety of glacial lakes, the most famous of which Glacier Laguna Okulsurloon.

It was formed on the coast in the first half of the 19th century, and at the expense of the rapid melt of the glacier grew to date up to 18 square kilometers, with a depth of 200 meters. Search for cheap hotels.

How to get.

Getting to national Park Vatnayekyudl can be in several ways. But initially you need to choose the place from which you will start to inspect the park.

The main point of receiving tourists following the Glacier is the city of Hubn. Before it can be reached by plane, bus and sea from Reykjavik. Distance between cities 326 kilometers.

On the park itself, moving better in the composition of excursions or on a rented car. These services are available in Hubne.

Vatnayyukyudl is the most big Glacier In Europe, which is located on the territory of the National Park of the National Park in Iceland. The total area of \u200b\u200bthe glacier is 8.1 km², which is about 8% of the total territory of Iceland. Ice thickness on average is 400 meters, and in some places it reaches 1,100 meters. According to the calculations of scientists, this block contains 3.5 thousand km3 ice.

This place boasts unique glacial landscapes with snow-covered valleys and gorges. Ice Cover rises 1400-1800 meters above sea level. No glacier in Iceland was so carefully studied as Vatnaya. Study began in 1934, when an eruption occurred in the area of \u200b\u200bthe glacier and since then a glaciological society (founded in 1950) a year after year continues to explore the glacier. Last large eruption happened in 1996 and 1998. The first documented journey to the top of the glacier on the south side and back took place in 1875. An Englishman and several Icelanders participated in the rise. They were the first to see Askiai's eruption, in the same year they reported this to people living on Miwatn Lake.

The name of the Glacier Watnaiyukudle is translated as "giving water", and all because it nourishes with a lot of Icelandic rivers and lakes. For example, it forms the Yoekulsau-Au Witch river, which is famous for gives life powerful waterfall In Europe - Dettifoss.

From a close distance, the glacier looks like an endlessly snow-covered field, and if you rise to its highest point, you can see ocean spaces and mountain peaks In the depths of the island.

Under the thick layer of ice there are several volcanoes, which sometimes make themselves to know. When the hot lava spills out from the volcano vulcan, it leads to a rapid melting large Square Glacier. Magnifying ice frees the land for grazing livestock. In 2004, a significant eruption of one of the volcanoes was griming.

In addition to volcanoes, hot springs lying in the area of \u200b\u200bthe Kverfydl mountain range are adversely affected by the ice cover. Hot water and steam cut out from the thickness of ice whole labyrinths of ice caves.

Watnaiyukyudl National Park was founded on June 7, 2008 and its area includes the territory of the glacier and the other two yoekulsurgluvur reserves and Skafatoothle. To date, the glacier is one of the most visited attractions of Iceland. Here travelers can stroll through its surroundings, as well as skiing and snowboarding.

Vatnayekyudl National Park covers 13% of the entire Square of Iceland. The park demonstrates the stunning variety of landscape, formed by the powerful forces of nature.

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Among all European glaciers, Vatniaküdl has the biggest sizes. However, only Antarctic and Greenland glaciers exceed it all over the world. Vatnanayudl Square over 8300 square meters. km, which is almost 1/12 of Iceland. Vertical Glacier has an average size about half a kilometer, but there are places in which its thickness exceeds 1000 m.

(20 photos of ice caves in Iceland)

Because of the enormous value of Vatnaya, even his branch ("Languages") are named by their names as separate glaciers.

Usually the glacier is formed due to the fact that a large amount of snow is dried and compacted, but Vatnanayuda has a slightly different story leaving for a distant past.

The very name of the glacier is translated as "giving water". And, however, Vatniakudl gave rise to a set of Icelandic lakes and rivers. With close examination of the glacier, it looks like an endless snowfield, and, having risen to his high point, you can see at the same time the ocean, and the mountains in the country's depth.

Under the thick layer of ice there are several volcanoes, some of them still act. When eruption, the lava stretches from Zherel leads to the melting of the large area of \u200b\u200bthe glacier. When ice melts, new fields are formed, where you can graze cattle.

In 2004, a rather significant eruption occurred of one of these "finished" volcanoes, grimspeat.

Not far from Vatniakudlo is the Dettifoss - the most powerful European waterfall, as well as Ykaulsurloon - Ice Laguna with icebergs.

The glacier and the lagoon are very popular when filming movies. So, for example, there were several moments from the film about Laru Croft and about James Bond.

In addition, a few distinguished distance from Vatniaukyudle is located national Park Skafatofetle, in whose territory, visitors can see the local landmark of the Svartifoss, the name of which can be translated and as a "black waterfall", and as a "dark drop".

So the waterfall was called due to columns from the black volcanic lava, which surround it. Created such a miracle slowly cooling lava flow, part of which was crystallized.

Having traveled to southern part Vatniaukyudl, you can see amazing beautiful cavesformed in the thickness of the glacier for hundreds of years.

Their halls and tunnels are flowing water, which was obtained by melting ice.

Due to the fact that there are very few air bubbles in old glaciers and icebergs, their ice has high strength and blue color.

When melting, the water is washes off the surface of the glacier - it gives the caves in it an amazing bluish radiance, similar to the shine of precious stones.

The sedimentary rocks from the lower part of the Vatniakudl can somewhat dilute the color range of more dark shades.