Summer season comes late
to the area and leaves it early. The month of May still sees snow storms
howling in the tundra and the mountains, and it is only in June that
warm days come. The snow mainly melts only by mid-June, while in deeper
gorges it remains until next winter. And the local winter returns
quickly. In early September the tops of the crests are covered with
white snow. Only two months are left for summer: July and August. But it
may also snow within this period.
If, in the midst of summer,
you come to realize one day that you can no
longer stand the dusty heat and the stuffy air of Moscow; if you
suddenly have the feeling that those huge masses of buildings threaten
to overwhelm you from above, and the burning hot asphalt is swallowing
you up from below; if you strongly feel like taking a good deep breath
of cool fresh air somewhere and changing the scene altogether, then
don't waste time.
Just make your way to
Moscow's Yaroslavsky Railway Station and buy a ticket from Moscow to
Labytnangi — the trains set off late in the evening. You may find your
first night in a stuffy carriage not much different from previous ones.
But you will not even see your second night. By then, in effect, you
will have gone far into the North, where in summer the nights are 'white
nights'. The following day in the afternoon, you will have crossed the
Arctic Circle — with the range of the Urals gradually approaching on the
horizon. Soon you will find yourself amidst the mountains. The
European-Asian borderline sign will then flash by — saying you are no
longer in Europe, but in Asia.
In
principle, you have already reached the destination. You have now only
to choose where to get off. My advice would be Polyarnaya (Polar)
station, immediately after crossing the European-Asian border. There is
a good earth road leading from the station to the north along the valley
of the Big Paipudyna River. Having walked a few hours along the road,
you will already find yourself in a wild nature preserve.
You are now in the Urals,
in the far northern part of the range, which is referred to as the
Arctic Urals in geography. Being one of the most mountainous areas
within the range, its summits are from 1,100 to 1,300 meters above sea
level. It is general knowledge that the Ural Mountains are rounded —
owing to their great age. In the Arctic Urals, however, you may come to
doubt this. The surrounding landscape reminds one of the Alps.
The plants and animals
hurry feverishly to use the short summertime. As soon as the snow melts,
the ground is covered with a multicolored carpet of herbs and
flowers.
The
local inhabitants, however, do not like the period very much. The reason
for this is the innumerable masses of mosquitoes and blood-sucking flies
that come up trying to snatch their own share of the natural bloom. The
period is not very good in terms of shooting or fishing either. The
shooting season opens towards the end of August. By that time there
ripen wild-growing berries, and mushrooms grow as well. They say, one
needs many pails to gather bog and red whortleberries, cranberries, and
cloudberries in the local forests.
But nonetheless summer is
summer any-way. The local summer is incomparable to its counterpart in
central Russia. Everything appears to be so different that you often
feel as if you were on another planet. It is not only the sun that never
sets: you just lose the usual sense of time, as if you were in a new
dimension. Gradually you fall out of your normal daily routine: you feel
sleepy in the daytime, and become restless during the night. It is at
night, too, incidentally, that blood-sucking flies are a little less
active.
The bluish radiance of ice
buildups will not disappoint
anyone!
You
come
across
this
in
many northern
rivers.
They form in places
where a river is shallow, and a river channel is comparatively wide. At
the beginning of winter a river gets frozen first of all in such places,
making a kind of hanging dam that blocks the river's flow. But flowing
water is the kind of force that will always find its way. Forcing its
way through to the surface of the dam, it turns immediately into ice. A
large multilayer accumulation of ice is thus formed over a winter. The
summer is too short to give the sun an opportunity to melt the entire
ice formation, which is strengthened from below by numerous cold springs
and permafrost. The sunshine and rains perform the work of a sculptor,
the shapes of the ice buildups changing daily, strikingly unusual in
form. On a clear sunny day, a kind of cold bluish luminescence emanates
from them. And as soon as the sun sets closer to the horizon, there
appears a thin haze creeping along the valley.
As you proceed further to
the north along the ridges, there appear more wonders: numerous rivers,
beautiful lakes, and even glaciers. There is, by the way, the Urals'
deepest tectonic lake, Bolshoye Shchuchye, 136 metres (446 feet) deep.
Humans
have inhabited the region since ancient times. For centuries, the Nenets
people have pastured their rein-deer there. Nowadays you can also come
across the reindeer-breeders' houses, chooms, and reindeer herds roaming
from place to place. And in the days of old, the enterprising
inhabitants of Novgorod were attracted to the land insofar as it
abounded in fur-bearing animals and fish. As early as in the 11th
century, they would travel along the Pechora and its tributaries, doing
trade with the lands behind the Urals. They would go up to the Pechora's
tributaries, and then portaged towards rivers within the basin of the
Ob. But the absence of direct waterways made the opening and
colonization of the region a slow process.
With the unification of the
Russian lands around Moscow in the 16th century, the exploration of the
region was intensified. At that time the state became involved in the
process. In 1552 Tsar Ivan IV gave the order "to survey the land and
make a draught of the whole state of Muscovy." Within the next 30 or 40
years, large cartographic and descriptive material was accumulated. The
Draught of the Whole State of Muscovy, which later was lost, was created
on the basis of this material. Such rivers as the Usa, the Pechora's
tributary, and the Sob, the Ob's tributary, were already plotted on
those maps.
The first consistent
geographic description and the first map of the Arctic Urals were made
after its territory had been explored by the Geographic Society's
expedition between 1847 and 1850. The geographic explorations of the
time were rather one-sided as their object was to search for waterways
connecting the Pechora River and the Ob River across passes in the
Arctic Urals.
The truly intensive
exploration of the region began, alas, at the time known as a gloomy
period in Russia's history. In the 1930s, they discovered a very rich
deposit of coal at the Vorkuta River. Thousands of Stalin's labor camp
political prisoners were forced to build towns and railways in the
region. It was they who built the railway between Seida and Labytnangi.
They went on building a railway still further, too. Following the death
of Stalin, however, the railway construction was discontinued. Nowadays,
many kilometers of rusting rails are a reminder of the times.
The times now are
different, fortunate-ly, and thanks to the railway the Arctic Urals is
just a beautiful region of the Russian North, easily accessible, having
preserved all the features of a wild nature preserve free from the
corruption of civilization.
By Sergey Arpukbin
(“Moscow today and
tomorrow” September. 2002)
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