23.08.2015

Mount People is the highest point of the Ural Mountains. Its height is 1895 meters. This geographical fact was set relatively recently. Due to the inaccessibility of the indoor region to Mount People, some scientific expeditions were committed.

At different times, the highest peaks of the stone belt Eurasia called the mountains: a saber (1497 meters), Telpos-from (1617 meters), Manaragu (1660 meters). In 1924-1928, the Severoural Complex Expedition under the leadership of B.N. worked here. Gorodkov. One of her detachments, which was led by A.N. Alyoshkov, in 1927 for the first time passed to the ridge of the River Národ. After examining the height of the mountain with the help of the scientific ways already in those times, they determined its height of 1870 meters (it is currently measured more precisely - 1895 meters).

It was Alyoshkov who gave her a name, and on what syllable should fall in him the emphasis did not specify anywhere. Disputes on the stress continued until the textbook's publication for pedagogical universities F.N. Malkova and N.A. Gvozhetsky in 1963, in which the emphasis was done on the first syllable. Since then, this option is considered correct formed from the name of the river beginning at the foot of the vertex. Although, according to Gorodkov, who spoke already after the death of Alyoshkov, she was named after the Russian people, as was customary at the time.

The Ural ridges were formed in the Paleozoic era during the period of the Hercino folding, later they experienced an update, and their crystalline breeds went to the surface. They are composed with metamorphic, sedimentary and volcanic rocks, very rich in various minerals and rocks. They form flat-terrain ridges with gentle stepped western and steeply swung oriental slopes.

The Narian (Mansiysk "People-from") on the Ural map is located as part of the research ridge of the Supolar Urals, on the border of the Khanty-Mansiysk Autonomous Okrug and the Republic of Komi, its coordinates of 65 ° S.Sh., 60 ° C. It consists of metamorphic shale and ancient quartzites. Its peak is rounded and double-headed, and the mountain slopes are covered with natural recesses - crashes, filled with water, glaciers, snowflakes, rock remains, mountain tundra, stone collaps.

Since the people became the place of pilgrimage of tourists, there were objects such as "here Vasya" - Bust Lenin, signs, memorable signs, the pyramid, in which those who arrived leave their notes, a worship of the cross with the words "save and save" written on it Mounted on a saddle between two vertices of the mountain in 1998. The eastern slope of the vertices, like the whole of the Urals, is breaking and impassing for tourists. The rise is carried out on the western slope, which is complicated by Karas, and on a more convenient Northern.

From the peaks there is a view of the surrounding top peaks of the Sabero, Manaragu, and others. The stern climate of the indoorry, who did not allow so long to get to these top peaks of the stone belt of Russia, forms a diverse and rich animal and vegetable world. Here you can meet coniferous and mixed forests, subalpine and alpine meadows, alpine and arctic tundra. In the warm season, there are numerous mosquitoes, wands, blind and smaller bloodsowing insects - Mocreas, midges.

Dwarf birks, blueberries, a richness, blueberries, a larch-shortness are replaced by herbs into the growth of a person who occasionally occasionally radiol. From animals there are many inhabitants of the tundra - sands, deer, partridges, wolves. There are badgers, bears, chipmunks. In mountain rivers there are only two types of Harius. In the lower reaches of the river fish slightly more.

Mount People [video]

The Ural Mountains are a mountain range on the border of Europe and Asia, stretching from north to south. In geography, it is customary to divide these mountains by the nature of the relief, natural conditions and other features on Pai-Hoy, Polar Urals, Polar, North, Middle, Southern Urals and Muurgary. The concepts of the Ural Mountains and the Urals should be distinguished: in a broader sense, the areas of the Urals are among the areas of the Urals - a Ural region, a priestle and a souralie.
The relief of the Ural Mountains is the main waterproof ridge and several side ridges separated by wide decrees. In the extreme north - glaciers and snowflies, in the middle part - the mountains with smoothed vertices, the Ural Mountains are old, they are about 300 million years old, they are noticeably processed erosion. The highest peak is a popul mountain - approximately a two-kilometer height.
The mountain range passes the watershed of large rivers: the Urals rivers belong to the main basin of the Caspian Sea (Kama with Chusovoy and Belaya, Urals). Pechora, Tobol, etc. refer to the system of one of the largest rivers Siberia - Ob. On the eastern slope of the Urals, many lakes.
The landscapes of the Ural Mountains are predominantly forest, noticeably the difference in the nature of vegetation on different sides of the mountains: on a western slope - mainly dark-haired, spruce-fir-fir forests (in the South Urals - mixed and broadcaming places), on the eastern slope - light-andquatic pine larch forests. In the south, the forest-steppe and steppe (for the most part of the plague).
The Ural Mountains have long been interested in geographers, including from the point of view of their unique location. In the era of ancient Rome, these mountains were submitted to scientists so far that they were seriously called Riphic, or Ripieski: literally with Latin - "coastal", and in an extended sense - "Mountains on the edge of the Earth". The name of the hyperborean (from the Greek "extreme northern") they received on behalf of the mythical country of hyperborei, it was used for a thousand years, until in 1459, the world map of Fra-Mauro appeared, on which the "edge of the world" was shifted already for the Urals.
It is believed that the mountains were discovered by Novgorod in 1096, during one of the campaigns to the Pechora and the Ugra, the publisy of Novgorod's hands, engaged in fur clan, trade and the collection of Yasaka. No name then the mountains did not receive. At the beginning of the XV century. Russian settlements appear on the upper chamber - the Anfalovsky Town and Sol-Kamen.
The first well-known name of these mountains is contained in the documents of the turn of the XV-XVI centuries, where they are called a stone: so in ancient Rus, called any large rock or rock. At the "Great Drawing" - the first map of the Russian state, compiled in the second half of the XVI century. - Ural is indicated as a big stone. In the XVI-XVIII centuries. The name is the name, reflecting the geographical position of the mountains between the two plains. There are such names such as a large stone, a large belt, a stone belt, a large belt stone.
The name "Ural" was originally used only for the territory of the Southern Urals and was taken from the Bashkir language, which meant "height" or "elevation". By the middle of the XVIII century. The name "Ural Mountains" is already applied to the entire mountain system.
The Ural Mountains - the ridge on the border of Europe and Asia, as well as the natural border within Russia, east of which - Siberia and the Far East, and to the West - the European part of the country.
It is resorted to such a figurative expression whenever you need to give a short and colorful description of the natural wealth of the Ural Mountains.
The antiquity of the Ural Mountains created unique conditions for the development of minerals: as a result of the long destruction of the erosion of the deposit, they literally were literally on the surface. The combination of sources of energy and raw materials predetermined the development of the Urals as a mining area.
It has produces iron, copper, chromium and nickel ores, potash salts, asbestos, coal, precious and semi-precious stones from the Ural gems. From the middle of the xx century. The development of oil and gas deposits is underway.
Russia has long been mastered the land adjacent to the Ural Mountains, occupying Komi-Permytsky Towns, connecting Udmurt and Bashkir territories: in the middle of the XVI century. After the defeat of Kazan Khanate, most of the Bashkiria and the Kama part of Udmurtia were voluntary. A special role in the consolidation of Russia in the Urals was played by the Ural Cossacks, which received the highest permission to engage here with free bakeries. The merchants of Stroganov marked the beginning of the purposeful development of the wealth of the Ural Mountains, receiving from the king of Ivan IV a humble diploma to the Ural land "and what lies in them."
At the beginning of the XVIII century. In the Urals, large-scale factory construction began, caused by the needs of both the economic development of the country and the needs of military departments. With Peter I, there were copper-smelting and cast iron plants here, and later large industrial centers were formed around them: Ekaterinburg, Chelyabinsk, Perm, Nizhny Tagil, Zlatoust. Gradually, the Ural Mountains were in the center of the largest mining area of \u200b\u200bRussia, along with Moscow and St. Petersburg.
In the era of the USSR, the Ural became one of the industrial centers of the country, the most famous enterprises - the Urals Plant of Heavy Machinery (Uralmash), the Chelyabinsk Tractor Plant (CHTZ), Magnitogorsk Metallurgical Plant ("Magnitka"), During the Great Patriotic War, industrial production was exported during the Great Patriotic War From the territories of the USSR occupied by the German territories.
In recent decades, the industrial significance of the Ural Mountains decreased markedly: many deposits are almost exhausted, the level of environmental pollution is quite large.
The bulk of the local population lives in the territory of the Ural Economic Area and in the Republic of Bashkortostan. In more northern areas belonging to the North-West and West Siberian economic areas, the population is extremely rare.
During the industrial development of the Ural Mountains, as well as the disassembling of their lands, hunting and cutting off the forests of the habitat of many animals were destroyed, and many species of animals and birds disappeared, among them - a wild horse, saiga, drought, strept. The flock of deer, previously among the Urals, was now discouraged into the tundra. However, the measures taken to protect and reproduce the fauna of the Urals managed to preserve in the reserves of the brown bear, Wolve, Wolverine, Fox, Sable, Earthside, Lynx. Where it has not yet managed to restore the populations of local species, acclimatization of the delivered individuals is successfully carried out: for example, in the Ilmensky Reserve - Spotted Deer, Beaver, Maral, Retal Dog, American Mink.

general information

Location: between the Eastern European and West Siberian Plains.

Geographical division: Ridge Pai-Hoi, Polar Ural (from Konstantinova Stone to the Hulger River Horrels), the Suporny Ural (cut between the rivers of Hulger and Schugol), the Northern Urals (howl) (from the Schugol River to the Kozvinsky Stone and Mountains Oslka), Middle Urals (Shore ) (From the mountain of Osh, to the Ufa River) and the South Urals (southern part of the mountains below Orsk), Muurgujara (Kazakhstan).

Economic regions: Ural, Volga, Northwest, West Siberian.
Administrative belonging: the Russian Federation (Perm, Sverdlovskaya, Chelyabinsk, Kurgan, Orenburg, Arkhangelsk and Tyumen region, Udmurt Republic, Republic of Bashkortostan, Republic of Komi), Kazakhstan (Aktobe region).

Large cities: - 1,428,262 people. (2015), - 1 182 221 people. (2015), Ufa - 1 096 702 people. (2014), - 1 036 476 people. (2015), Izhevsk - 642 024 people. (2015), Orenburg - 561 279 people. (2015), Magnitogorsk - 417 057 people. (2015), Nizhny Tagil - 356,744 people. (2015), Kurgan - 326,405 people. (2015).

Languages: Russian, Bashkir, Udmurtsky, Komi-Permytsky, Kazakh.
Ethnic composition: Russians, Bashkirs, Udmurts, Komi, Kazakhs.
Religions: Orthodoxy, Islam, traditional beliefs.

Currency unit: Ruble, tenge.
Rivers: Pool of the Caspian Sea (Kama with Chusovoy and Belaya, Urals), North Ocean Pool (Pechora with Usa; Tobol, Iset, Tour belong to the Ob system).

Lakes: Tavatui, Argazy, Wildlows, Tourgoyak, Big Shchuchye.

Numbers

Length: more than 2,600 km from north to south (with Pai Hoam and Mouthburg).

Width: from 40 to 150 km.

Geological age: from 250 to 350 million years.
The highest point: Mount People (1895 m).
Other vertices: Karpinsky (1878 m), Yamantau (1638 m), Manaraga (1662 m), Telposis (1617 m), Korzhakovsky Stone (1569 m), Payer (1499 m), Osl (994 m), Middle Baseg (994 m).

Climate and weather

Continental.
The average temperature of January: from -20 ° C (polar Ural) to -15 ° C (South Ural).

The average temperature of July: from + 9 ° C (Polar Ural) to + 20 ° C (South Urals).

The average annual amount of precipitation: Porpolar and Northern Urals - 1000 mm, South Urals - 650-750 mm.

Relative humidity: 60-70%.

Economy

Minerals: iron, copper, chrome, nickel, potash salts, asbestos, stone coal, oil.
Industry: mining, black and non-ferrous metallurgy, heavy engineering, chemical and petrochemical, fertilizer, electrical.

Hydroelectric Energy: Pavlovskaya, Yumaguzinskaya, Shirokovskaya, Iriklinskaya HPP.

Forestry.
Agriculture: Crop (wheat, rye, garden crops), animal husbandry (cattle, pig breeding).
Traditional crafts: Artistic processing of the Ural gems, knitting of Orenburg dying headscarves.

Field of services: tourist, transport, trading.

sights

Natural: Pechoro-Ilych, "Bashegi", "Shulgan-Tash", Steppe, Bashkir Reserves, Mineralogical Reserve, Caves of Divia, Arakaevskaya, Sugomakskaya, Kungur Ice and Capov, Rockies Seven Brothers, Cherto Gorodishche and Stone Tents, Bashkir National Park, National Park Yighda VA (Komi Republic), Gofman Glacier (Saber Ridge), Azov-Mountain, Alikaev Stone, Natural Park Oleni Brooki, Passing Blue Mountains, Threshold Rejun (River Ineset), Zhigalanskiy Waterfalls (River Zhigalan), Alexandrovskaya Sopka, National Taganai Park, Ustinovsky Canyon, Gmer Gorge, Spring Red Key, Sterlitamak Shikhana, Red Circle.

Curious facts

■ The peoples of the Urals still use the names of the Urals in their languages: Mansi - Ner, Khanty - Kev, Komi - from, Nenets - PE or Igarka PE. In all languages, this means the same thing - "stone". Among the Russians who have long lived in the north of the Urals, a tradition has also been preserved to call these mountains.
■ From the Ural Malachite and Jasma, the bowls of the St. Petersburg Hermitage are made, as well as the interior and altar of the St. Petersburg temple of the rescue.
■ Scientists have not yet found an explanation to the mysterious natural phenomenon: in the Ural lakes, they see, large kiskomach and turgoyak are unusually transparent water. In neighboring lakes, she is completely muddy.
■ The top of the Kachkanar Mountain is a bizarre-shaped scalation collection, many of which have their own names. The most famous of them is a cliff camel.
■ In the past, the richest deposits of high-quality iron ore of the mountains magnetic, high and grace, famous worldwide and entered into all textbooks on geology, are currently either broken, or turned into a career in a depth of hundreds of meters.
■ The ethnographic appearance of the Urals created three streams of immigrants: Russian Old Believers who fled here in the XVII-XVIII century, translated into the Ural plants peasants from the European part of Russia (mainly from modern Tula and Ryazan regions) and Ukrainians attracted as additional labor in the beginning XIX century
■ In 1996, Yighd Va National Park, together with the Pechoro-Ilychian Reserve, with whom the park borders in the south, was included in the UNESCO World Natural Heritage Objects under the name "Komi's virgin forests.
■ Alikaev Stone - 50-meter rock on the Ufa River. The second name of the cliff is Maryn Rock. Here they filmed a television movie "The shadows disappear at noon" - about life in the Uralsky outback. It is from Alikaev Stone, according to the film's plot, the Menusikov brothers dropped the chairman of the collective farm Mary Red. Since then, the stone has a second name - Maryn Rock.
■ Zhigalansk waterfalls on the Zigalan River, which is on the eastern slope of the Quarksh ridge, form a 550 m long cascade. With a river length of about 8 km, the height difference from the source to the mouth is almost 630 m.
■ Sugomak cave is the only cave of Ural Mountains with a length of 123 m, formed in the marble breed. On the territory of Russia there are only a few such caves.
■ Rodnik Red key is the most powerful water source in Russia and the second largest in the world after the source of Phonan de Vobluz in France. Spring water consumption Red key - 14.88 m3 / s. The attraction of Bashkiria in the status of the hydrological monument of the nature of the federal significance.

The Ural Mountains are a unique natural object for Russia. Why? It will become clear to everyone who thinks about this issue. First of all, because they are the only mountain chain crossing Russia from the south to the north, while performing the role of the border between the two parts of the world, as well as the large parts of our country - Asian and European.


Features of the relief of the Urals

Any geologist will agree that their structure is characterized by complexity. They include breed of different age and type. In the mountains, you can track the story of many Epoches of the Earth. There are not only depth faults, but also the sections of the oceanic bark. The base of the Ural ridge is a stone belt, a natural border that shares Europe and Asia, Sverdlovsk and Perm regions.
But the high Ural mountains can not be called. Mostly here are low and medium vertices. The highest point is the People's Mountain, located on the Supolar Urals. Its height reaches 1895 meters. But the mountain of Yamantau is the second in height of the Ural point - is located on the southern tip of the ridge.

According to the profile of the mountain remind of depression. In the north and south are the highest peaks, while in the middle part of their height rarely reaches 400-500 meters. Therefore, when intersection of the Middle Urals, only a careful tourist or traveler will notice the mountain.
The beginning of the formation of the Ural Mountains coincides with the Altai. But further fate has developed in different ways. Altai was often experiencing the strongest tectonic shifts. As a result of Beluha - the highest point of Altai - has a height of more than 4.5 kilometers. On the other hand, in the Urals, much safer for life - earthquakes, the stronger, occur here significantly less frequently.

Sights of the Ural Mountains

Mount Manaraga (Bear Lap) is not included in the list of the highest. But, definitely, is the most beautiful. The top of her is a series of sheer peaks, because of what Mora was published really similar to the raised paw of the bear.

The highest point of the Urals is the People's Mountain, the vertex of which is located at an altitude of 1985 meters.

In general, lists all the attractions, what can boast the Urals, quite difficult. Although bringing some of the most interesting will be useful:

  • mount Korzhakovsky stone;
  • cliffs seven brothers;
  • national Parks Zyuratkul and Taganay;
  • nattenage reserve stone;
  • natural Park Oleni Brooki,
  • chusovaya River;
    Mountain clean paintings and caps.

And this is only a small part of the most beautiful places located in the Urals.





Rivers and Lakes of the Ural Mountains

Also, the Urals can boast many beautiful rivers with crystal clear water and rapid flow, dangerous thresholds and picturesque rivers. It is no coincidence that many routes are laid here for both family holidays and sports alloys.

On the banks of the rivers there are many beautiful stones and rocks, and the endless taiga will not leave a single lover of nature indifferent.

These rivers have seen a lot and store many secrets to this day.

The Rivers of the Ural Mountains belong to the three seas pools: Caspian, Karis and Barentsva. The total number of rivers flowing here exceeds 5 thousand! Only in the Sverdlovsk region of their about a thousand, and in the Perm region - more than two thousand. The approximate annual flow of these rivers exceeds 600 thousand cubic kilometers.

Alas, today many of these rivers suffer from waste discharged by industrial production. Because of this, the relevance of the purification of river waters and the protection is becoming increasingly important.

But the lakes here are a bit, and their size is small. The largest lake is Argazi (refers to the Miass River Basin). Its area is slightly more than 100 square kilometers.

The Ural Mountains are considered the most ancient on earth, they stretched from north to south, dividing Russia to the European and Asian parts. Mountains begin at the Arctic Ocean, cross the whole country and end in Kazakhstan.

If you look at the map, it can be visible.

The highest of these mountains - which is in the north and its height is almost 2 kilometers.

The width of the Ural Mountains in some areas reaches 150 km!

An antiquity was known about the existence of the Ural Mountains, in particular the Greeks, it was believed that, precisely, behind these mountains there is a legendary country of hyperborea.

Geology of the Urals

The Ural Mountains were not always so low. Their education began 350 million years ago and during his "youth" Ural Mountains reached the height of six kilometers. There was a time, in the populoval volcanoes, the strong earthquakes were shaking all living things, and Magma, pouring, formed new rocks.

Future mineral deposits were laid here. Millions of years have passed, no insane volcanoes are no longer, the mountains collapsed and became small, but sometimes the Ural Mountains remember the dawn of violent youth and the earthquakes occur. The last thing happened in the fall of 2015.

Nature Urals

Throughout the mountain, there are several natural zones from the tundra in the north, Taiga in the middle and ending in the south of the steppe.

It turns out that nature and animal world are different everywhere.

If you can find a deer in the north, then in the south of Groundhog or Suslik. When tulips bloom in the south in the steppe, there are still cracked frosts in the north.

The mountain slopes are not cool, but perfectly create interference with the winds, therefore the climate of the European part differs from the climate of the Asian part of the mountains, and that is why attracting tourists and skiers from around the world on their slopes, using great popularity.

Mountain breeds Urals

In the depths of the Urals there is a lot of minerals. Some of them are very rare and occur only in the depths of the Ural Range. Of the most famous can be allocated:

  • gold;
  • silver;
  • iron ore;
  • copper ore;
  • dIY STONES;
  • oil;

Everyone knows crafts and decorations from Malachite, a beautiful green Ural stone.

Products from it can be seen in St. Petersburg Hermitage.

Many folk tale about the extraction of fossil wealth has been processed by the tale of the Bazhov P. P.

Population of Urals

Most of the population live in large industrial cities. By national composition, this is basically Russian. Then the Tatars, Bashkira, Ukrainians, Kazakhs, Mansi, Khanty and other nationalities are followed.

Industry Urals

In the Ural region, in particular, and the most common industries are metallurgy and mechanical engineering. It is known that even before our era, a copper ore was mined here. The modern, the period of the development of metallurgy began under Peter I, with Demidov Plants and Muses.

All over the world are the industrial cities of Chelyabinsk, the capital of the Southern Urals with His ChTPZ, and, like the capital of the Urals, with his Uralmash.

Between all the cities of the region, the railway, automotive and aviation message.

The only negative is that the highly developed industry pollutes the atmosphere and adversely affects the health of people.

However, it does not stop those who know that the Ural Mountains are natural, and wish to plunge into this atmosphere.

Fascinating you travel and excursions to the Ural Mountains.

Posted Sun, 08/01/2017 - 10:13 by Cap

Part of the Ural Mountains from the Massif Kosvinsky Stone in the south to the shore of the Schugol River in the north is called the Northern Urals. In this place, the width of the Ural ridge is 50-60 kilometers. As a result of raising the ancient mountains and the impact of subsequent glaciation and modern frosting weathering on the territory of the middle-growing relief, with flat vertices.
Northern Urals is very popular with tourists. Of particular interest are the rocks and remains of arrays of Man-Pupin-Nierr, Torre-Porre-from, Muning-Tump. Aside with the waterproop, the main vertices of this part of the Urals are located: Konzhakovsky Stone (1569 meters), carbacked stone (1492 meters), clean paint (1292), separated (1182), skin-from (1195),

The northernmost top of the Mountain System of the Ural - Mount Telposis in Komi. Located an object in the republic. Mount Telposis in Komi is composed by quartzite sandstones, crystalline slates and conglomerates. On the slopes of the mountain, the Telposis in Komi grows the Taiga Forest, - Mountain Tundra. Translated from the language of the local population, ORONIM denotes the "" Nest of the Winds ".
Porpolar Urals is one of the most beautiful areas of our Motherland. His ridges from the sources of the Hulger River in the north to the mountain of Telposise in the south stretched by a wide arc. The area of \u200b\u200bthe mountain range is about 32,000 km2.
Unfalled harsh nature, an abundance of rivers and lakes of fish, in the taiga of berries and mushrooms entails travelers here. Good paths of communication on the northern railway, on the steamboats and boats along the Pechora, Mustache, Obi, Northern Soche and Lyapin, as well as the network of airlines allow you to develop water-water, hiking and ski routes with the intersection of the Ural Range or along Western and Eastern slopes.
A characteristic feature of the relief of the Supolar Urals is a large height of the ridges with alpine formas of relief, the asymmetry of its slopes, deep dismemberment of through transverse valleys and gorges, a significant height of passages. The highest peaks are located in the center of the Supolar Urals.
The absolute height of the pass through the main watershed, separating Europe from Asia, and through the ridges located to the west of it, from 600 to 1500 m above sea level. The relative heights of the vertices near the passes are 300-1000 m. Especially high and difficult-class Passages on the Sablinsky ridges and an impregnable, whose slopes are ends with steep-walled karas. The most advantageous passes through the research ridge (from 600 to 750 m above sea level) with relatively gentle minor lifts, allowing to easily carry out wolbs, are located in the southern part of the ridge between the tops of the Puviva (the right influx of cuishes) and the trade (the right influx of schugora), and also Between the tops of the crate, Manya (Lyapina pool) and a large patch (the right influx of schugora).
In the area of \u200b\u200bthe Mountain and People's Mountain Ridge, the height of Pozals 900-1200 m, but here through many of them pass trails, according to which a relatively light wolfs from the Hulgerps (Lyapina), Heimay, Grubbai, Halmere, Peoples in the head of the tributaries of Lemva , Skin and Balbanyo (mustache basin).

Porpolar Urals is one of the most beautiful areas of our Motherland. His ridges from the sources of the Hulger River in the north to the mountain of Telposise in the south stretched by a wide arc. The area of \u200b\u200bthe mountain range is about 32,000 km2.

North border
From the border of the Perm region to the east along the northern borders of quarters of 1-5 of the forestry of the state of state of the Metal Stone (Sverdlovsk region) to the northeast corner of the KV 5.

Eastern border
From the northeast corner of a square. 5 south on the eastern borders of quarters of 5, 19, 33 to the southeast corner of square. 33, further east along the northern border of square. 56 to its southeastern corner, further south on the eastern border of square. 56 to its southeast corner, further east along the northern border of square. 73 to its northeastern corner, further south along the eastern border of quarters 73, 88, 103 to the B. Kozviv River and then on the left bank of the river. B. Kosva before his sign on the River Schuch offs, further on the left bank of the river. Schuch offs to the eastern border of the sq. 172 And further south on the eastern borders of quarters of 172, 187 to the southeast corner of the KV. 187, further east along the northern border of square. 204 to its northeastern corner.
Further south on the eastern borders of the quarters of 204, 220, 237, 253, 270, 286, 303, 319 to the southeast corner of the KV. 319, further east along the northern border of quarters of 336, 337 to the northeast corner of the square. 337.
Further south on the eastern border of quarters 337, 349, 369, 381, 401, 414, 434, 446, 469, 491, 510 to the southeast corner of the square. 510.

South border
From the southwestern corner of square. 447 east at the southern borders of quarters 447, 470, 471, 492, 493 to the sugar river, then on the right bank of the river. Soche to the southeast corner of the square. 510.

Western border
From the southwestern corner of square. 447 to the north on the border of the Perm region to the northwestern corner of the square. 1 forestry of the gentlemen "Methast stone".

Geographical coordinates
Center: LAT - 60O30 "29,71", LON - 59O29 "35.60"
North: LAT - 60O47 "24,30", LON - 59O35 "0.10"
East: LAT - 60O26 "51.17", LON - 59O42 "32.68"
South: LAT - 60O19 "15.99", LON - 59O32 "45,14"
West: LAT - 60O22 "56,30", LON - 59O12 "6,02"

GEOLOGY
The Ilmenogorsk complex is located in the southern part of the Sysert-Ilmenogorsk anticlinor of the East-Ural raising, has a fold-block structure and is complex in various compositions in magmatic and metamorphic rocks. Numerous unique pegmaty veins are of greatest interest, in which Topaz, Aquamarine, Phenacite, Zircon, Sapphire, Tourmaline, Amazonitis, various rare-metal minerals are found. Here, for the first time in the world, 16 minerals were opened - Ilmenite, Ilmenorut, Kasyisadanagita (Kali'ferrisadanagitait), Kankrinitis, Macarochinitis, Monazit- (CE), Polyakovit- (CE), Samskite- (Y), will communicate, Ushkovit, Fergusonite beta ( ), fluoroomagnesiaarfvedasonitis, fluororichtherite, child, chivkinite- (CE), Eshinite- (CE).

Ilmensky Reserve

GEOGRAPHY
The relief of the western unit low. The average heights of the ridges (Ilmensky and Ishkulsky) 400-450 m above sea level, the maximum mark of 747 m. Eastern foothills are formed by low elevations. More than 80% of the area is occupied by forests, about 6% - meadows and steppes. The peaks of the mountains are covered with larch-pine forests. Pine forests predominate in the south, in the north - pine-birch and birch. An array of old pine forest is located on the Western slopes of Ilmen's mountains. There are areas of larchs, stony, cereal-divergent and shrub steppes, moss swamps with cranberries and a richness. Flore marked more than 1,200 species of plants, many endemic, relict and rare species. Eat ermine, forest chore, columns, wolf, lynx, protein-flying, hares - Belyak and Rusak, enters a brown bear. Elk and roeble are few. Acclimated spotted deer and beaver. From birds are usually aunty - degrahae, tetrayev-Kosach, Ryabchik, gray partridge. The reserve nest swan-clikun and a gray crane, rare birds are marked - Eagle Belochvost, Moghox, Sapsan, Skop, Baloban, Strept.

Since 1930, there is a mineralogical museum founded by A. E. Fersman, which presents more than 200 different minerals found in the Ilmensky ridge, including Topaz, Corunda, Amazonites, and others.

In 1991, a branch was organized - the historical landscape archaeological monument to Arkim 3.8 thousand million. Located in the steppe foothills of the Eastern Urals, in the Karagan Valley. More than 50 archaeological monuments are preserved here: Mesolithic and neolithic parking lots, burial grounds, Bronze Age settlements, other historical facilities. Of particular importance is the fortified settlement of Arkim XVII - XVI centuries. BC e.

Location:

Gremyachinsky district of the Perm region.

Monument type: geomorphological.

Brief description: Weathered remains in ninecalented quartztopesters.

Status: Landscape Monument of Nature of Regional Values.

The city facing stone.

The city is located on the main vertex of the Ridge Rudyansky SPIA, the absolute height of which is 526 m above sea level. It is a powerful rocky array folded by fine-grained quartz sandstones of the lower carbon, which are part of the coal strata formed in the Delta of a large river.

The array is cut into deep, up to 8-12 m, cracks with a width of 1 to 8 m in both the meridional and latitudinal directions, which creates the illusion of deep and narrow perpendicularly intersecting streets, streets and alleys of an ancient abandoned city.

Ural is a mountainous country that stretches from north to south from the shores of the Cara Sea of \u200b\u200bthe Cara Sea to the Central Asian steppes and semi-desert. The Ural Mountains are the natural border between Europe and Asia.
In the north of the Ural ends with a low ridge of Pai-Hoi, in the south - Mountain chain of Mugarjara. The total length of the Urals with Pai Hoam and Muurgas - more than 2500 km.

In the east of the Orenburg region, the Governors of the Mountains (southern part of the Ural Mountains) come out - one of the most beautiful places of Orenburg. The provincial mountains are located 30-40 kilometers to the west of Orsk at the right bank of the Urals, where the Guberen river flows into it.

The Gubernlysky Mountains are the blurred edge of the high-risk steppe, a strongly dissected and rugged Valley of the Gubereli River, the logs and the gorges of its tributaries. Therefore, the mountains are not towering over the steppe, and lie below it.

They occupy an unbreakable strip along the valley of the Urals River, north passing to a high ovary steppe, and to the West, on the right bank of the province, replaced with a variety of low-rope. The gentle eastern slope of the provincial mountains is imperceptible to the plain, on which the city of Novotroitsk is located.

The territory occupied by the Governile Mountains is about 400 square kilometers.

"From open cracks, the settlement is raised indiscriminately thin, trembling couples against the sun, to which it is not possible to touch the hand; An abandoned birch bark or dry chips in one minute with a flame sunk; In bad weather and in the dark nights it seems to be a red flame or a fiery ferry for several Arrins of Embroiderer, "wrote 200 more years ago about an unusual grief in Bashkiria Academician and traveler Peter Simon Pallas.

Long-time Mount Yangantau was called otherwise: Karagosh Tau or Berkutov Mountain. According to the old good tradition, "I see, I call." To the mountain renamed, a certain exceptional event was to happen. They say that this event has even exact date: 1758. Lightning hit the mountain, all trees and shrubs on the southern slope were torn. Since then, the Mountain has become known under the name Yangantau (Jangan-Tau), translated from Bashkir - "Burned Mountain". Russian names slightly reeddied: burned mountain. However, despite the wide fame and absolute uniqueness Yangantau, the locals still remember the old name, Karagosh Tau, and still use it.

Pedestrian trips to the jippel can be carried out from May to October from the village of Talyuk (Chelyabinsk region). Before it can be reached from the Railway Station Vizialaya (70 km).

The road to Tyutuk is covered with gravel, to the Meshades asphalt. Bus runs.


Tyutuk - view of Zigalga Range

The base camp can be broken as in a tula, there are special paid places for tents or houses to choose from and on the way to the ripe at the river Karagayka.

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Source of materials and photo:
The team is wetting.
The encyclopedia of the Urals
List of mountains and ridges of the Urals.
Mountains and vertices of the Urals.

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