Minerals GMA Ugra on the map. Presentation on the topic "Minerals KhMAO-Ugra"
Slide 2.
Natural wealth of Ugra
The territory of the district along with oil and gas is rich in others natural resourcesAs renewable and non-renewable. Some of them belong to the resources of world importance (forest, water), others are all-Russian (solid minerals, flora and fauna, peat) and regional.
Slide 3.
The reserves of hydrocarbon raw materials
- The Khanty-Mansiysk Autonomous District in the reserves of hydrocarbon raw materials occupies a leading place in the world (about 5% of world oil reserves). Due to the fact that this raw material will be the main source of energy over the next 15-20 years, the role of the district as a territory supplying such raw materials should be maintained for all this period.
- Now Khanty - the Mansi Autonomous District supplies hydrocarbon raw materials in different regions Russian Federation And beyond Russia, mainly in European countries and the states of the CIS.
Slide 4.
Solid mineral reserves
The Khanty-Mansiysk Autonomous District has great potential reserves of iron ore, stone and brown coal, bauxite, copper, zinc, lead, tungsten, molybdenum, chromium, barite, manganese, rare metals, phosphorites. All solid mineral deposits are suitable for open Development. The presence of such fossils allows the autonomous district to develop new sectors of the economy, so necessary industrial potential of the Ural region.
Slide 5.
Minerals by origin
Slide 6.
Magmatic breeds
- Formed directly from the magma (molten mass of predominantly silicate composition), as a result of its cooling and frozen. Depending on the conditions of frozen, the intrusive (deep) and the effusive (reputable) rock rocks are distinguished.
- There are found in the western part of the district in the foothills of the Urals. Include non-ferrous metals, rare metals, polymetallic ores (from "Poly ..." and "Metals" - complex ores, in which the main valuable components are lead and zinc, passing - copper, gold, silver, cadmium, sometimes bismuth, Tin, India and Gallium).
Slide 7.
- Rhinestone
- Gold
- Lead
- Stone gems
Slide 8.
Sedimentary rocks
The formation of sedimentary material occurs due to the action of various factors - the effects of temperature fluctuations, the effects of the atmosphere, water and organisms on rocks characteristic of the surface part earth crust and resulting as a result of transition products of weathering and destruction of various rocks, chemical and mechanical precipitation from water, the vital activity of organisms or all three processes at the same time. Are found throughout the territory of the Khanty-Mansiysk Autonomous Okrug (oil, gas, peat, clay adsorption, limestone, sands and gravel)
Slide 9.
- Limestone
- Oil
- Clay admission
- Sand and gravel
Field(useful minerals) - natural accumulation of minerals, which in quantitative and qualitative relations can be the subject of industrial development at a given state of technology and in these economic conditions (industrial deposit). Other clusters, which, according to their data, could be developed only with changed technical and economic conditions, belong to the fields of non-industrial, differing in this sense from oreroy. In the size of stocks it can be large, medium and small. By origin, endogenous, exogenous and metamorphogenic deposits are distinguished.
Geological body -these are different in shape, sizes and conditions for the formation of the formation of the earth's crust (layers, veins, lenses, rods, etc.), folded with a useful mineral substance or containing it in the scattered form. In a number of deposits, there are several geological bodies.
Rudoprote - Natural accumulation in rocks of useful minerals of small or unexplained sizes. Sometimes, as a result of intelligence and study, ore reflection can be translated into the field.
Ore - This is an aggregate minerals from which gross method is technologically possible and economically advisable to extract metal or metal compound.
Mineral resource - Natural mineral substancewhich is in high quality and quantitative relationship Suitable for use in the national economy.
Minerals. Minerals can be used either in natural condition (high-quality coal, quartz sand), or after pre-processing them by sorting, crushing, enrichment (most ores).
Minerals find the most diverse use in various sectors of the national economy. Currently, almost any rock formation of a certain quality and in certain economic conditions can be used for certain purposes, and therefore "useless fossils" almost does not exist. Here, under the word "any" mean rocks related to off-balanced ores.
There is a chemical and technological classification of minerals. Its main principle is the real composition of ore and their application.
According to this classification, minerals are separated on metal, non-metallic and combustible.
Useful fossils, their diversity, degree of study and development belongs to a primary role in the economic assessment of the power of any state. Mineral raw materials - the first priority of the material development of society. Currently there are about 200 different species Mineral raw materials used in industry agriculture and construction.
Solid minerals.According to the complex of minerals, which at present, the described area is identical to the industrialized territories of the Urals. The district is known for oreroy and the mineralization points of many minerals. The development zone of the platinum belt and its framing are timed to manifestations of black, colored, rare metals and other minerals (Appendix 3).
Within the districts of the district, lead, copper, silver, gold and other metals, asbestos, numerous manifestations and mountain crystal deposits are also known. In search and shooting works, in previous years, stovered manifestations of the gold of many valleys of the watercourse of the Berezovsky district of the district were revealed. The column deposits of Gold Yarota Shore, Nyarta-Yu, Halmere and Hobye are divorced. The territory is rich in stocks of building materials (sand-pebble-gravel mixture, crushed stone, facing stones).
The main fields and manifestations of solid minerals are focused within the release zone of the crystalline rocks of the Eastern Slope of the Urals, which has a width of 20-45 km and a length of up to 450 km within the Khanty-Mansiysk Autonomous District.
From ore of ferrous metals (Fe, Mn, Cr, Ti, V) within the county, its own deposits form iron and manganese. Iron ores are represented by the skarn-magnetite and apatito-sulphide-titanium-vanadium magnetite (Volkovsky type) formations (Chorace Rudnya Node, sleepy manifestation, etc.). Manganese ores in Paleozoic formations have not yet been established, but the most promising is a manganese mineralization in early-itogenic sediments (Yana-Nny-Loche-SOS (Yana-Nnyal-Loche-SOS) with resources 200 million tons of ore.
Rudes of light metals (AL) are represented by deposits and manifestations of bauxite. Within the counties, Boksit Perspective Areas are highlighted: North-Socivinsky, Yatrinsky, Hulginsky, as well as the Trubja and Lullean playgrounds.
From the ore of non-ferrous metals (CU, PB, Zn, Ni, Sb), the ores of the cocked-type copper-polymetallic formation (Tykotlovskaya and Yarodashorskaya courts, Malosymoyvinskoye, Magnish, Leplinskoye Ruery, etc.). The main components are copper, lead, zinc.
Rude metal ores (SN, W, MO, HG, BE, LI, TA, NB) are represented by deposits and oreroitations (Ta-Nb) by an alkaline rare-metal-metasomatic (Taruver playground) and a rare-metal-metamorphic (MAN-Hambo site), as well as W-Mo-Bi and W-BE (shopping deposit, small-conditioning plot) formations. Noble ores (AU, PT, AG) Metals are represented by indigenous fields and places of the Lyapinsky golden area, as well as the axes of the North-Sosvinsky ore district.
The search for an axle gold on the Supolar Urals is conducted with the Xih century. The most intense and purposefully - starting from the 60s century. Installed industrial gold relationship valleys of the yarotashor and river. Hobye. In the late 70s, the stovery of Yarotashor is explored by the thematic geological exploration on Uralzoloto. A number of industrial placers (Nyartay, the tributaries of the R. Halmeria) were identified by the search and evaluating works of the Northern Party of Uralzolotransports. Oarser gold is currently the second most important mineral type. As of 1.01.04, in the territory of the Khanty-Mansiysk Autonomous Okrug - Ugra, 14 placer gold deposits with reserves of 3306 kg of chemically pure gold took into account. Of these, in a distributed fund - 1882 kg. The estimated and approved predictive resources are 20 tons by category P1 + P2 + P3.
On the Polar Urals of the Khanty-Mansiysk Autonomous District - Ugra Currently, from noble metals is widely developed in the main field of placer gold. Revealed several ores for indigenous gold. The forecast resources of ore gold are 128 tons by category P1 + P2 + P3. In 2003, the GKZ of the Russian Federation approved the reserves of ore gold in the amount of 1156 kg by category C1 + C2.
The ores of scattered and rare-earth elements of independent fields do not form, but they can be removed along the development of igneous, pegmatite, carbonate, albitite, hydrothermal and marginal ore deposits of non-ferrous, rare and radioactive metals.
The RFN is the most studied and promising territories of the district. The area of \u200b\u200bpromising land lands outside the contours of the allocated licensed areas is 301.8 thousand km2. During 2004, 11 new deposits were open at the unallocated fund of the subsoil at the expense of the subsoil of the Offline District: Akeegen Piezochman deposits, residential quartz and mining crystal are now the most prepared and partially exploited. On the territory of the district there are about 40 manifestations of residential quartz and mining crystal, which makes the prospects for the Supolar Urals according to this type of raw materials even higher.
In 2003, a residential quartz mining was started at Polyarny Quartz OJSC at the Dodo Deposit. Socivipromgeology, OJSC, cleaned the Puiva deposit, on which a collection of raw materials (rhinestone) was mined in a small amount (about 3 tons). Since 1993, within the framework of research programs and geological studies of the subsoil, the district conducted studies of filtering and sorption properties of zeolite-containing rocks of the Supolar Urals. At the same time, work was carried out to prepare the reserves of these breeds at the Mysh section. To date, it is found that zeolite-montmorlonite rocks are excellent sorbents. The prepared reserves of the Myshovsky field - 44 thousand tons. It is possible to assert with sufficient confidence that the Supilar Urals is a new zeolitone province of Russia.
The reserves of brown coal in categories A + B + C1 are 464.5 million tons, according to C2 category - more than 1.5 billion tons. In the district with a different degree of detail, both fairly large bromanized deposits are Sberling, Tolinsky, Lullean and small - Nyayskoye, Lopsinskoye, etc. Within the lulin field, the Borisov site is prepared, suitable for working for local purposes. The reserves of the Borisov site by category B + C1 are 4.95 million tons. To date, promising areas on brown coal are allocated: Trubja, Oceslaimskaya, seven and others. Mastering deposits is constrained due to the lack of transport highways. Torf stocks by category A + B + C1 are 86.55 million tons, according to C2 - 1148.81 million tons (according to the state balance of mineral resources of the Russian Federation for January 1, 2002).
On the flat part of the district territory revealed a large number of Building Materials: Clay Brick and Crimsitone, Sands Construction and Glass, Sand-Gravel Mixtures, Silico Stone Raw Materials, Landmarks. The reserves found in the Soviet, Berezovsky and Khanty-Mansiysk regions of the silicon-opal rocks (opoks, diatomites, tremies) are calculated with tens of millions of cubic meters. A number of prepared deposits of brick-ceramzite clays are not used only because of the delay in the construction of brick factories. Weak development of sand-gravel mixtures deposits are due to their location in the floodplains of rivers. Construction sand reserves are practically not limited.
Sapropel deposits are divided near Khanty-Mansiysk, Surgut, Nizhnevartovsk, Urai. Prepared sapropel reserves are estimated by more than 10 million m3. It can be used as an organic fertilizer and vitamin additive to diet of pets. The trial development of individual deposits of Sapropel is conducted in the district of Surgut.
At the Supolar Urals, Boksit Perspective Areas are allocated - North-Soshivinsky, Volinsko-Yatrinsky and Hulginsky (Bowlsothiness in Paleozoic sediments) and the Tujalanyan and Lullean manifestations of Mesozoic Boxitites. The genetic relationship of the geological formations of the Supolar Urals with those in the Northern and Middle Urals allows us to approve a sufficiently high prospects for the territory of the district to bauxites.
Confirmation of the prospects identified on the eastern slope of the indoor urals of iron ore and metal-hydrogenic zones is the discovery of the Otlyamsk-Turguine ore assembly, the resources of which are estimated at 3.1 billion tons. Within its limits, two promising manifestations of skiard-magnetite ores - Oces-Okhtlyamsk and Yana-Trician, total forecast The reserves of which are about 1160 million tons, incl. Outly suitable ores are about 390 million tons. Preparation of iron ore reserves is constrained due to the lack of transport communications.
Forecast copper resources P3 category are 2500 thousand tons; zinc category P3 - 2300 thousand tons; manganese ore category P3 - 284.1 million tons; Boxitites category P1 - 15.0 million tons, categories P2 - 18.0 million tons, categories P3 - 45.0 million tons; Brown coal category P1 - 635 million tons, categories P2 - 7764 million tons, categories P3 - 4757 million tons; Stone coal category P3 - 162 million tons.
As of January 1, 2004, 175 fields of solid minerals were open at the county terraine territory, of which 7 quartz deposits, 6 deposits of brown coal, 1 mine gold deposit, 10 placers deposits, 1 deposit of Zeolites, 1 glass sand deposit, 1 Bentonite deposit field Glyn, 1 building stone deposit, 12 siliceous raw materials deposits, 73 brick-ceramzite clay deposits, 53 building sand deposits, 9 sand-gravel mixture deposits.
In total, there are 5 quartz deposits in the district foundation, 6 placer gold deposits, 1 deposit of Zeolites, 1 deposit of volcanogenic rocks for the production of light foam concrete.
In the northern sucking pool, separate platin signs were found during gold scattering. They also note that the Ural researcher Yu.A.Volcheko found that the chromite ores of the Tyumen Urals contain an increased amount of minerals of elements of the platinum group - Osmia, Iridia and Ruthenium. These minerals can be extracted by flotation using a collective copper-nickel product (concentrate). Further processing of this concentrate will allow you to extract copper, nickel and pass the above-mentioned metals of the platinum group.
Oil.Oil is called a combustible liquid mixture, consisting mainly of hydrocarbons of methane, naphthenic and aromatic rows with an admixture of sulfur, nitrous and oxygen compounds.
One of the main properties of crude (non-transparent) oil is its density, which depends on the content of heavy hydrocarbons (paraffins, resins, etc.).
In practice, there is the following classification of oil in density (g / cm 3):
very light (with very low density) - up to 0,800;
light (low density) - 0,800 - 0.839;
average (with an average density) - 0.840 - 0.879;
severe (with high density) - 0.880 - 0.920;
very severe (with very high density) - more than 0.920.
In addition, there is a classification of refinery in the content of light fractions: sulfur (S), asphalt-resin substances (AS) and solid hydrocarbons (paraffins - P). Main chemical composition Oil is as follows: Carbon - 79 - 88%, hydrogen - 11 - 14%, sulfur - 0.1 - 5%, nitrogen, oxygen, etc.
The territory of the Khanty-Mansiysk Autonomous Okrug accounts for about 80% of the initial potential oil resources of the West Siberian oil and gas province and practically half resource potential Oil of Russia. About 90% of the district area falls on the territory promising in oil and gas attitude.
The district is currently one of the main regions where the exploration and extraction of hydrocarbon raw materials are underway; His contribution to the annual production of Russian oil B is over 57%.
The main oil and gas fields of the Khanty-Mansiysk Autonomous District are located in a latitudinal acquisition in the northern subzones (the southern slope of Siberian Urals) and the middle taiga (Surgut Polesie). On the territory of the district as of January 1, 2003, 414 deposits were opened, of which 358 oil, 22 gas and gas condensate, 34 oil and gas, gas-and-oil and oil and gas condensate. At the beginning of 2005, 249 deposits were in operation, oil production exceeded 1 million tons per year. About 40% of oil reserves in the fields have already been mined. To the current, that is, the categories of categories A and B prepared for development (invested), respectively, 4 and 10% of the initial reserves of industrial categories of the district, the currently explored (unnecesssed) categories C1 - 31%, for pre-valued resources category C2 - 18 %.
Thus, the share of current economically favorable oil reserves (current stocks of categories ABC1) from the initial revealed in the district is 45%.
A significant part of resources in the subscribed subsoil fund (RFN) is timed to the territories of the largest mining oil companies, in which there are 71% of the initial potential oil resources of the RFN and 84% of the total initial revealed deposit funds found in the distributed fund.
The provision of identified resources at the existing levels of mining from companies is different. Some of them are already experiencing a lack of resources identified to maintain production levels in the coming years.
The RFN is the most studied and promising territories of the district. The area of \u200b\u200bperspective land of the district outside the contours of the allocated licensed areas is 301.8 thousand km 2. During 2004, 11 new deposits were open at the undolocked fund of the subsoil at the expense of the subsoil of the subsoil of the Offline District: Aykegan, South-Nitrical, South Mytakhi, Yuzhno-Lyaminsky (Surgut region); Tankansky (Nefteyugansky district); Novomostovskoe (Soviet District); Tanganskoye and West Simividovskoye (Kondinsky district); Toresh, Yuzhno-Moimskoye, Oktyabrskoe (October District). In 2003, 15 deposits were opened.
Currently, 11% of the initial oil potential of the area of \u200b\u200bthe undistonted subsoil fund (NFN) is translated into reserves of deposits, and 13% of it accounted for promising oil resources C3 + D0. Analysis of the resource base of the district shows that for further and effective development, providing oil production by the current stocks of the ABS1 categories, the resources of the C2 category, the deposit of local objects, evaluated by categories C3 and D0, an increase in the volume of seismic and drilling work on low-examined territories and horizons where a significant part of potential resources is not yet localized, i.e. We account for the forecast resources of categories D1 and D2.
Most oil deposits in the GMAO deposits are characterized by relatively low viscosity values \u200b\u200b(low-grade - up to 5 MPa × c) reservoir oils. This is a special group or class of oils, creating favorable prerequisites for solving technical and economic problems of oil resource development. Almost 99% of oil (Category A + B + C) of the district belongs to small. The prevailing part of the Russia deposits is characterized by a change in the viscosity of the oils in the range of 0.5 - 25 MPa × with (in reservoir conditions), less often up to 70 - 80 MPa × c and more. The main part of the Shaimsky deposits, Krasno-Ninsky districts is characterized by the viscosity of the oil in the range of 0.5 - 5.0 MPa × c (only in small areas, oil with viscosity 6 is 8.8 MPa × from). In the Surgut district, the share of oils with viscosity of 6 - 8.5 MPa × with somewhat increasing, but in the main part of stocks, viscosity values \u200b\u200bare characterized in the range of 0.5 - 5.0 MPa × from. The Nizhne-Vartovsky District oil occupies a special place. The predominant part of the deposits is characteristic of viscosity in the range of 12 - 20 MPa × c and more. High-viscous oil is revealed in the APT-Senomanian sediments of the area (PC layers 1 - PC 21). So, on the Van-Egansky field, the viscosity of oils in the formations of PC 1 - PC 21 reaches 95 MPa × c, in the layer AB 1 - 12.4 MPa × c, and somewhat deeper - in the formations of AV 3 and AB 4 - 7 - it decreases to normal values \u200b\u200bof 3.9 and 2.2 MPa × with respectively.
According to source data, Tyumen oil, along with a large content of gasoline and kerosene fractions, has a lot of sulfur that needs to be separated. According to the content of sulfur, the area of \u200b\u200bthe district is mainly a medium-term (0.51-2%), its reserves are approximately 72% of the total reserves. The reserves of minor oil (up to 0.5%) make up a little more than 27%. The stocks of high-herded oil (more than 2%) are 0.9%. The separation of the sulfur occurs by turning it into sulfuric acid (according to special technologies), on special oil refineries.
Natural gas - This is a mixture of gaseous hydrocarbons (methane, ethane, propane, butane and pentane). The share of methane in it is 85 - 99%. In addition, natural gas is contained in a particular amount of nitrogen, carbon dioxide, helium, argon, water vapor, hydrogen sulfide and mercury.
Large gas deposits are located on the territory of the Autonomous Okrug: Berezovskoye, Verkhne-Colik-Egansk, Colik-Egybian, Varieghanskoye, Lianstor, Federovskoye, Wang Egansk, Samotlor, Bystrino, Mammoth, Priobskoye, etc. In these fields, 85.5% of stocks are concentrated in these fields free gas district.
Natural gas on the scale of concentration and use for practical purposes is the most important.
The composition of free and oil-based gases there are differences that are especially noticeable in the distribution of hydrocarbon components. Free gases - methane to 85-98%, the sum of methane homologues in the range of 0.1-10%; oil-based gases - methane to 60-70%; The sum of methane homologs in the range of 1-25%. Restricted components are mainly represented by nitrogen and carbon dioxide; In the form of minor impurities there are hydrogen, hydrogen sulfide, helium, argon, mercury, vapors of volatile liquid acids, etc. However, there are cases where "minor impurities" become very noticeable components. So, the content of non-relocarbon components natural gasand is characterized by: carbon dioxide - from a percentage of percent up to 10-15%, sometimes higher (in the deposits of the Samneynel deposit in the Berezovsky district of Ugra up to 85%); Nitrogen - most often within 1-3%, but in some cases up to 4-60% or more, hydrogen sulfide - no more than 1-3%, but in some cases up to 10-23%.
Within the county, the largest clusters of PG are associated with deposits of coal and continental-subguygular formations with high content of humus type. In conditions Western Siberia. This class of formations include the deposits of Senoman and Pata, with which the largest and unique fields of PGG (Urengoy, Yamburg, Bovanienkovskoye, Harasawa, etc.) are associated with the largest and unique deposits. Within the region of large deposits, PGG is not established. Most of the KGG clusters identified here are timed to the Jurassic sediments and belongs to the size of the classes of small and medium. The territory of the district belongs to the lands of predominantly affiliatedness.
minerals GMAO, Natural Resources Ugra, Fossil HMAO
Natural wealth of Ugra. The territory of the district along with oil and gas is rich in other natural resources, both renewable and non-renewable. Some of them belong to the resources of world importance (forest, water), others are all-Russian (solid minerals, flora and fauna, peat) and regional.
The reserves of hydrocarbon raw materials. The Khanty-Mansiysk Autonomous District in the reserves of hydrocarbon raw materials occupies a leading place in the world (about 5% of world oil reserves). Due to the fact that this raw material will be the main source of energy over the coming years, the role of the county as the territory supplying such raw materials should be maintained for the whole period. Now Khanty - the Mansi Autonomous District supplies hydrocarbon raw materials in various regions of the Russian Federation and beyond Russia, mainly to European countries and the CIS countries.
Reserves of solid minerals. Khanty - the Mansi Autonomous District has great potential reserves of iron ore, stone and brown coals, bauxite, copper, zinc, lead, tungsten, molybdenum, chromium, barite, manganese, rare metals, phosphorites. All fields of solid minerals are suitable for open development. The presence of such fossils allows the autonomous district to develop new sectors of the economy, so necessary industrial potential of the Ural region.
Magmatic rocks were formed directly from the magma (molten mass of predominantly silicate composition), as a result of its cooling and frozen. Depending on the conditions of frozen, the intrusive (deep) and the effusive (reputable) rock rocks are distinguished. There are found in the western part of the district in the foothills of the Urals. Includes non-ferrous metals, rare metals, polymetallic ores (from "poly ..." and "metals" - complex ores, in which the main valuable components are lead and zinc, pass through copper, gold, silver, cadmium, sometimes bismuth, tin , India and Galli.)
Sedimentary rocks The formation of sedimentary material occurs due to the action of various factors - the effects of temperature fluctuations, impact of the atmosphere, water and organisms on rocks, characteristic of the surface part of the earth's crust and resulting from moving the weathering and destroying of various rocks, chemical and mechanical precipitation Of the water, the vital activity of organisms or all three processes at the same time. There are found throughout Khanty - Mansi Autonomous Outline (oil, gas, peat, adsorption clays, limestone, sand and gravel)
Oil and natural gas. The main oil and gas areas and largest oil fields are concentrated in the district. Between the Urals and the Osco-Yenisei watershed, there are 294 oil fields with total reserves of more than 16 billion tons. To date, more than 9 billion tons are extracted from the depths of the district. There are about 61 large oil and gas fields in the district.
This presentation Not intended for any commercial use. This presentation is not intended for any commercial use. Graphic and text materials used in the creation of this presentation were obtained from the Internet resources using the search engine and the textbook "Geography of the KhMAO 8-9 Class" of Orlova. TK and others. Graphic and text materials used in creating this presentation are obtained from Internet resources using the search engine and textbook "Geography of the KhMAO 8-9 Class" Orlova Bez, etc.
Khanty-Mansiysk is surprisingly lucky with the natural foundation of the urban environment: towering over the city nature Park "Samarovsky Chugas", opening with hills, views of Irtysh, city birch alleys and parks give the city a unique, a kind of face, it is a big rare among the rapidly growing Siberian cities.
Khanty-Mansiysk refers to the zone continental climate, equal to the districts of the Far North. Continental air dominates here throughout the year moderate breadth. Meridional circulation is enhanced, as a result of which the territory enters both arctic and tropical air. With Western transfer, the Atlantic air comes here, to a large extent transformed.
Air temperature and precipitation rate
· Average annual temperature - -0.8 ° C
· Average annual wind speed - 2.4 m / s
· Medium annual air humidity - 77%
Khanty-Mansiysk is located within one natural zone - Forest.
Water mode of rivers is characterized by a stretched spring-summer flood. Spring water, spilling over the wide floors of rivers, form extensive grades. In winter, the river freeze for a long period - up to 6 months.
The climate is characterized by a rapid change of weather conditions especially in transition periods - from autumn to winter and from spring by summer, as well as during the day. Winter is harsh and long-lasting with a steady snow cover, summer short and relatively warm, transition seasons (spring, autumn) with late spring and early autumn frosts.
The negative air temperature in the district lasts 7 months, from October to April. A period of sustainable snow cover continues 180-200 days - from the end of October to May. Before mid-June, frost is often freedom. Most warm month July, average temperature from +15.7 to +18.4 degrees Celsius.
The prevailing direction of the wind in the summer - Northern; Unlike winter, when more often is observed south wind. Annual rainfall in the district from 400 to 550 mm. The height of the snow cover from 50 to 80 cm. In July, the maximum precipitation falls out, about 15% of the annual number. IN winter time On the territory of the district, the atmospheric pressure is much lower than within the Asian Anticyclone. The invasion of air masses from the Atlantic is accompanied by warming, snowfall and thaws. Average values atmospheric pressure In July (754-756 mm), lower than in the Arctic, but higher than in Central Asia.
Land resources of the city with their appropriate training are used to expand the volume of housing construction, as well as for the placement of small industries.
Natural sand and clay reserves create conditions for the development of production of building materials, and in perspective - and ceramics.