Development of the lesson "Reservations of the Novosibirsk Region". Natural conditions of Suzunsky district of the Novosibirsk region Fragments from the presentation

27.04.2021

Suzunsky district. Suzinsky Zannik.
Protection of the reserve:
Leading Hyover - Pakhomov Mikhail Mikhailovich
Okoven 1 category - Degort Andrei Viktorovich

Head of the Administration of the Novosibirsk Region

Decision

On the formation of a specially protected natural territory

Regional importance - State Natural

Reserve "Suzinsky" of the Novosibirsk region

(as amended by the decision of the head of the administration of Novosibirsk

areas of 07.05.2001 N 408, Governor's Resolutions

Novosibirsk region from 07.06.2006 N 259,

from 11.08.2006 N 348, from 07.22.2011 N 189)

In accordance with the Federal Law of 14.03.95 N 33-FZ "On Specially Protected Natural Territories", the Law of the Novosibirsk Region of September 26, 2005 No. 325-OZ "On the specially protected natural territories in the Novosibirsk Region" Decree:

(Preamble as amended by the Resolution of the Governor of the Novosibirsk Region of 11.08.2006 N 348)

By the decision of the Governor of the Novosibirsk Region of July 22, 2011 No. 189, amended Appendix 1.

1. To form on the territory of the Suzun district of the Novosibirsk region a specially protected natural territory of regional importance - the State Natural Reserve "Suzinsky" Novosibirsk region with an area of \u200b\u200b128,500 hectares without seizing land plots from users, owners and owners within the boundaries according to Annexes 1 (not given), 2.

(as amended by the Resolution of the Governor of the Novosibirsk Region of July 22, 2011 No. 189)

2. It has lost strength. - Resolution of the Governor of the Novosibirsk Region of July 22, 2011 No. 189.

2.2 - 3. It was raised. - Resolution of the Governor of the Novosibirsk Region of 07.06.2006 N 259.

4. I lost strength. - Resolution of the Governor of the Novosibirsk Region of July 22, 2011 No. 189.

V.Tolokonsky

Governor of the Novosibirsk region

Decision

From 04/20/2017 № 80

novosibirsk city

On Amendments to the Resolution of the Head of Administration

Novosibirsk region dated January 17, 2001 № 68

In accordance with the Federal Law of March 14, 1995 No. 33-ФЗ "On Specially Protected Natural Territories", the Law of the Novosibirsk Region of September 26, 2005 No. 325-OZ "On specially protected natural territories in the Novosibirsk Region" p o s t a n o in liyu:

To make a decision of the head of the administration of the Novosibirsk region of January 17, 2001 No. 68 "On the formation of a specially protected - state natural reserve" Suzinsky "of the Novosibirsk Region" (hereinafter referred to - the decision) the following changes:

1. In the title, the word "education" is replaced by the word "creating".

2. Clause 1 shall be amended as follows:

"one. To create a specially protected natural territory of regional importance on the territory of the Suzunsky district of the Novosibirsk region - the State Natural Reserve "Suzinsky" Novosibirsk region of 136034.0 hectares without seizing land plots from users, owners and owners. "

3. Appendices number 1, 2 to the decision to be recognized by invalid.

V.F. Gorodetsky

Decision

from 04/26/2017 № 160-P

novosibirsk city

On approval of the borders of a specially protected natural territory
regional importance - the State Natural Reserve "Suzunsky"
Novosibirsk region

In accordance with the Federal Law of 14.03.1995 No. 33-FZ "On Specially Protected Natural Territories", the Law of the Novosibirsk Region dated September 26, 2005 No. 325-OZ "On the specially protected natural territories in the Novosibirsk Region" The Government of the Novosibirsk Region P O S T A N O V L I E T:
To approve the borders of the particularly protected natural territory of regional importance - the State Natural Reserve "Suzinsky" of the Novosibirsk Region according to Annexes No. 1, No. 2 to this Regulation.

Governor of the Novosibirsk region
V.F. Gorodetsky

Appendix No. 2.

to the Government Decree

Novosibirsk region

from 04/26/2017 № 160-P

Government of the Novosibirsk Region

Decision

On approval of the Regulations on the regime of special protection

Especially protected natural territory of the regional

Values \u200b\u200b- State Natural Reserve

Suzansky Novosibirsk region

from 04.09.2013 N 379-P)

In accordance with the Federal Law of 14.03.1995 N 33-FZ "On Specially Protected Natural Territories", the Law of the Novosibirsk Region dated September 26, 2005 No. 325-OZ "On Specially Protected Natural Territories in the Novosibirsk Region" The Government of the Novosibirsk Region decides:

Approve the attached provision on the regime of the special protection of the particularly protected natural territory of regional importance - the State Natural Reserve "Suzinsky" of the Novosibirsk region.

Governor of the Novosibirsk region

V. Yurchenko

Approved

resolution

Governments of the Novosibirsk region

from 09/05/2011 N 389-P

POSITION

On the mode of special protection of a particularly protected natural

Regional importance - state

Nature Reserve "Suzinsky" of the Novosibirsk region

(as amended by the Government Decree of the Novosibirsk Region

from 04.09.2013 N 379-P)

I. General provisions

1. This Regulation on the mode of special protection of the specially protected natural territory of regional importance - the State Natural Reserve "Suzinsky" of the Novosibirsk Region (hereinafter referred to as a particularly protected natural territory of regional importance) was developed in accordance with the Land Code of the Russian Federation, the Forest Code of the Russian Federation, the Water Code of the Russian Federation Federation, federal law of 14.03.1995 N 33-FZ "On specially protected natural territories", the law of the Novosibirsk region of September 26, 2005 No. 325-OZ "On specially protected natural territories in the Novosibirsk region".

2. The organization of a specially protected natural territory of regional significance does not entail withdrawn from the owners, owners and users of these sites.

3. A specially protected natural territory of regional importance is under the jurisdiction of the Department for the Protection of the Animal World of the Novosibirsk Region.

(p. 3 as amended. Decree of the Government of the Novosibirsk Region of 04.09.2013 N 379-P)

4. Forests located on specially protected natural territories belong to protective forests.

II. Justification of the organization specially protected

natural territory of regional importance

5. A specially protected natural territory of regional importance has a biological (zoological) profile and is intended to preserve biological diversity, the protection of rare and endangered species of animals, as well as animals included in the Red Books of the Russian Federation and the Novosibirsk Region, ensuring the protection of nesting-broken birds of birds, as well as the reproductive stations of hoofed species of beasts and boroys.

6. A specially protected natural territory of regional importance is organized for a permanent period in order to:

1) the preservation of natural complexes and objects of Priobsky Borsi of Western Siberia (hereinafter - natural complexes and objects) in the natural state and maintenance of the environmental balance;

2) preservation, reproduction and restoration of natural resources, enrichment of adjacent economic used land;

3) Protection of reproductive deposits of moose, roofing, boar, hares, river beobra, gray groundhog, black birds, badger settlements, other species of wild animals;

4) the protection of winter parking lots and roeblers;

5) the protection of habitats of rare and endangered species of animals and plants;

6) conducting scientific research;

7) implementation of environmental monitoring;

8) ensuring environmental education, education and education of the population.

III. Special Protection Mode Specially Protected

natural territory of regional importance

7. On the specially protected natural territory of regional importance are prohibited:

1) Fisheries, sports, amateur hunting and other uses of the animal world;

2) fisheries, except in the cases specified in paragraph 8 of these Regulations;

3) all types of logging of forest plantations (with the exception of sanitary logging) and skiing work on highly protective areas of forests established in accordance with forest legislation, and in the stations of rare and under threat of disappearance of wild animals marked on the ground in accordance with the organization's project and devices of the specially protected natural territory of regional significance;

4) all types of logging of forest plantations within a radius of 0.5 km from the Currents of Malchak;

5) Soldering works in areas of barnsuka;

6) Conducting continuous logging of forest plantations (with the exception of continuous sanitary logging, continuous logging associated with the construction, reconstruction and operation of linear objects carried out in accordance with this Regulation, as well as in cases where selective cuttings do not provide the replacement of forest plantations, losing their media, water protection, sanitary and hygienic, wellness and other useful functions, for forest plantations that ensure the preservation of the purpose of protective forests and the useful functions performed by them);

7) the destruction of forest rings by any kind of economic activities;

8) harvesting and collection of non-timber forest resources (with the exception of the billet and collecting of the branch feed and billets of firs and trees of other coniferous breeds for the New Year holidays);

9) the workpiece of food forest resources and the collection of medicinal plants (with the exception of the preparation by citizens of food forest resources and the collection of medicinal plants for their own needs);

10) the destruction and withdrawal from the natural environment of rare and under threat of the disappearance of plant species listed in the Red Books of the Russian Federation and the Novosibirsk Region;

11) Zavitsa harvesting;

12) the creation of forest plantations and their operation;

13) the cultivation of forest fruit, berry, ornamental plants, medicinal plants;

14) the use of forests for the purpose of processing wood and other forest resources;

15) the use of pesticides, mineral fertilizers, chemicals for plant protection and growth stimulants, except in cases specified in paragraph 10 of these Regulations, the use of toxic chemicals for the protection and protection of forests, including for scientific purposes;

16) sealing, grazing and drive run outside of specially dedicated areas marked with warning signs;

17) spent sealing (from the edge to the center);

18) Land disintegration (except for forestry activities related to the use, protection, protection and reproduction of forests, and land units already used by owners, land users, landowners and tenants for agricultural products);

19) the destruction of brood nor animals, except for species that cause damage to agriculture;

20) the ruin of the nests and the collection of eggs (except for verneous);

21) conducting hydro-elevative and irrigation works, geological and exploration research and development of minerals, except in cases specified in paragraph 9 of these Regulations;

22) raised power. - Decree of the Government of the Novosibirsk Region of 04.09.2013 N 379-P;

23) allowing pallets, burning vegetation;

24) explosive work;

25) alloy wood;

26) the construction of reservoirs and other artificial water objects, as well as hydraulic structures;

27) the creation of facilities for the placement of waste production and consumption, radioactive, chemical, explosive, toxic, poisoning and poisonous substances;

28) providing land plots for development, as well as for collective gardening and gardening;

29) the introduction of living organisms in order to acclimatize them;

30) collecting zoological, botanical, mineralogical collections and paleontological facilities (except for research activities in the manner prescribed by the legislation of the Russian Federation);

31) the implementation of recreational activities (organization of seats of recreation and breeding fires), as well as the device of privalov, parking and camps, other forms of rest of the population, outside the places specifically provided for these purposes marked by preventive signs;

32) destruction or damage to barriers, shocks, stands and other information signs and pointers, as well as equipped ecological trails and recreation places;

33) Washing of vehicles in water protection areas of water bodies;

34) Travel and parking outside the roads of public on the vehicle and snow farte technique of citizens, whose stay at the specially protected natural territory of regional significance is not related to production activities, and are not owners, owners, users, tenants of land and forest areas, which are located within the borders a particularly protected natural territory of regional importance, and non-persons specially authorized state bodies in the field of environmental protection;

35) Finding with gunshot, pneumatic and throwing weapons, trappers and other hunting tools, including with firearms in the assembled form, as well as with products of extracting the objects of the animal world of persons who are not representatives of specially authorized state bodies in the field of environmental protection;

8. Citizens who permanently residing in settlements located on a specially protected natural territory of regional importance are entitled to carry out amateur and sports fishing in public areas after the end of the day the ban on fisheries in accordance with the rules of fisheries for the West Siberian Fisheries, approved by order. Federal Agency for Fisheries dated November 13, 2008 N 319 "On approval of fisheries rules for the West Siberian Fisheries Basin".

9. In the specially protected natural territory of regional importance, groundwater mining at the subsoil areas provided for use in accordance with the legislation of the Russian Federation on subsoils are allowed, subject to the peculiarities of special protection regime to ensure the functioning of settlements and enterprises located within the borders of a specially protected natural territory. regional importance.

10. Conducting agricultural work with the use of pesticides, mineral fertilizers, chemicals of plant protection and growth stimulants on the territory of a specially protected natural area of \u200b\u200bregional importance should be carried out in compliance with the requirements for the prevention of the death of the animal objects in the implementation of production processes, as well as during the operation of road triggers, pipelines, lines of communication and power stations approved by the Decree of the Government of the Russian Federation of August 13, 1996 N 997 "On approval of requirements to prevent the death of the objects of the animal world in the implementation of production processes, as well as during the operation of the transport highways, pipelines, communication lines and power transmission".

In order to reduce the harmful effects on the animal world, the use of chemical preparations for protecting plants and other drugs should be combined with the implementation of agrotechnical, biological and other events.

The regulations for the use of chemical and biological preparations, as well as the list of these drugs are approved by the Sanitary and Epidemiological Supervision and Agrochemical Service of the Russian Federation, taking into account international standards.

11. In a specially protected natural area of \u200b\u200bregional importance, economic activities are carried out in compliance with these provisions and requirements to prevent the death of the animal world facilities in the implementation of production processes, as well as the operation of transport highways, pipelines, lines of communication and power stations approved by the Government of the Russian Federation of 13.08 .1996 N 997 "On approval of requirements to prevent the death of animal world facilities in the implementation of production processes, as well as during the operation of transport highways, pipelines, communication lines and power."

11.1. On the specially protected natural territory of regional importance, construction, reconstruction and overhaul of capital construction facilities, including linear structures, are allowed in coordination with the Department for the Protection of the Animal World of the Novosibirsk Region.

(p. 11.1 introduced by the Decree of the Government of the Novosibirsk Region of 04.09.2013 N 379-P)

12. Project documentation of facilities, construction, reconstruction or overhaul of which on a specially protected natural territory of regional importance are allowed by this Regulation, subject to state environmental impact.

13. In the particularly protected natural territory of the regional importance, measures for the protection, protection and reproduction of forests are carried out in accordance with forest legislation.

14. On the specially protected natural territory of regional significance within the boundaries of water protection zones and protective coastal bands, there are prohibitions and limitations established by water law.

15. The boundaries of a particularly protected natural territory of regional importance are indicated by the places of the Achlands, special information signs, are indicated in land management cards, forest maps.

16. In the event of a threat and distribution of wildlife diseases, damage to the health of citizens, the objects of the animal world and their habitat are regulated by their number on the basis of the decision of the Department for the Protection of the Animal World of the Novosibirsk Region in accordance with the legislation on the animal world.

(as amended by the Government Decree of the Novosibirsk Region of 04.09.2013 N 379-P)

17. The protection of the specially protected natural territory of regional importance is carried out by the Department for the Protection of the Animal World of the Novosibirsk Region in the manner prescribed by the legislation of the Russian Federation and the Novosibirsk region.

(paragraph 17 as amended. Decree of the Government of the Novosibirsk Region of 04.09.2013 N 379-P)

18. The security area for a particularly protected natural territory of regional significance is not established.

I.. Suzunsky district on the map of the Novosibirsk region: the geographical essay.

The area is located on the extreme southeast of the Novosibirsk region and occupies the territory 4746 Square kilometers, borders in the north-west with Ordansky, in the north with Iskitim, in the East with the Cherepanovsky districts of the Novosibirsk region, and in the south with the Altai Territory.

In Suzunsky district lives 33510 Man (as of January 1, 2010), of them in the district center - the village of Urban-type Suzun - 14716 Man (2010).

The village was founded in 1764. The status of the workers' village was assigned in 1939.

Suzun is one of the largest urban-type villages in Russia. In 2010, Suzun in the number of population was located on 68th place out of 1348 villages in Russia and in 4th place in the Novosibirsk region after Lingo, Krasnobsk and Kochno.

Population density - 7 people per 1 square kilometer .

Suzunsky district is one of the 30 districts of the Novosibirsk region, in whose territory there are 14 rural and 1 village council, 42 settlements.

The main industrial enterprises of the Area are: OJSC PKF "Effect", Suzunskaya PPO "Bakery", CJSC "Idea", CJSC PFC "Update", OJSC Suzu Repair and Technical Enterprise, ZAO Mascarrouse "Suzinsky", Boltovsky Mascording LLC.

Agricultural production is engaged in 13 joint-stock companies, 115 peasant farms and personal subsidiary farms of the population. In agriculture employs 32.5% of all working. The main specialization of agricultural enterprises is the production of grain, meat and milk.

The railway line "Karasuk-Altai" of the West Siberian railway is held throughout the district. The length of highways is 340.5 km, of which, with a solid coating - 309.6 km.

Many villages of Suzunsky district were founded by Russian settlers in the XVI-XVII centuries.

The area was formed in 1925 as part of the Kamensky district of the Siberian Territory, since 1930 as part of the West Siberian Territory. On March 2, 1932, Suzunsky and the Bitkovsky districts were combined into one Lushnikovsky district with the district center in the village of Lushniki, and already on December 10, the same year, the Suzinsky district was restored with the center in the village of Zavod-Suzun. In 1937, the area was included in the newly formed Novosibirsk region.

The territory of the district includes the right-bank part of the Priobsky plateau with a maximum height in the west of 298 meters. Nature is extremely diverse, especially along the shores and valleys of rivers, which at any time of the year attract their inaccurate Siberian beauty. There are many magnificent places to relax, swimming, hunting and fishing, harvesting berries and mushrooms.

The former landscape, although in the modified form, is still preserved. This is a soft smoothing of the relief, the abundance of lakes and swamps, sandy shores, a variety of vegetation. It is not by chance that 3 monuments of the nature of regional significance and the Biological Reserve "Suzinsky", 80,000 hectares, which occupies almost the entire territory of Suzunsky Bora, the largest forest massif south of the Novosibirsk region, was formed in the Suzunsky district. Here are adjacent to the sections of pure and high bonitet and sedimentary trees of various fine breeds with a traditional undergrowth. "Whole pine arrays have in the smbrella trunks in the form of lowered arrows. It produces valuable industrial raw materials - Zhivitsa (resinous substance used in medicine). For the extraction of this product, Suzunsky Bor is one of the most productive neighbors in Russia.

In order to preserve rare for the Novosibirsk region of types of steppe sites and related ecosystems, preserving populations of rare and in need of the protection of animal and plant species, including 3 state monuments of nature in the Suzunsky district and were created in the Red Book of the Russian Federation:

1. "Sharcinskaya steppe" (67.87 hectares, part of the Valley of the Upper Caracan river, west of the village of Sharcino).

2. "Obian sand step" (76.48 hectares, the territory between the Kamyshinka roads-measure, in the floodplain of the right bank of Ob).

3. "Lake Alloy" (100 hectares, in the south of Suzunsky Bora).

In the southwestern part of the district, the Ob River during almost 100 km occurs. The movement of its waters is powerful, but it looks smooth, calm, majestic. Here the border of the Suzunsky District of the Novosibirsk Region and the Shelabolikhinsky district of the Altai Territory passes through the complex direction. According to the river, Ob, as if someone scattered the mass of the islands and, indulging, painted many radiation of various configurations. But "Neither someone," and she, the river Ok, did it all the way, and to this day it reproves, does and rework, moves from place to the place of the island, and other and clean it. "Arts" Ob is visual and on the left-bank meadow, and on the right-bank raised side. There are so many old men and ducts that even Suzun land surveyors seem to be confused in their designs and names. What is the island that ducts! The village of Kamyshinka.

The Suzunsky District River, which flows into OB flows along loose sedimentary rocks and easily blurred, form deeply embedded beds with steep shores, resembling canyons in miniature (30-40 meters).

On the gracious Suzun land, people have already lived several millennia. So 1.5 km south-east of the village of Klotovo (River Pool) archaeologists found a settlement of the middle of the II millennium BC. e. Tigli, bronze shill, knives, suspension were found in the settlement. Scientists assume that during the Krotovsky culture in Western Siberia there was a large metallurgical center. Here, ores from the Sayano-Altai Highlands were used, of which there were peculiar objects, including weapons. In total, 66 archaeological sites and monuments of different eras were revealed in the district.

The territory of the Suzunsky district began to master Russian people from the XVII century. By this time, almost all of Siberia was conquered, it was possible to organize their own bread production, peaceful relations with aborigines were established, the economic development of the region was established by industrialists, artisans and merchants, ore recognition was sent to the mountainous regions of Salair and Altai.

II.. Suzansky copper plant and Suzansky mint.

Historical reference.

Among the historical and cultural heritage of the village of Urban-type Suzun, the surviving residues of the Suzunsky (Nhinoshausung) of the Coplavl Plant with the only one in Siberia were deserved. The history of the first industrial enterprise of non-ferrous metallurgy is quite simple.

First, the Russian Empire by the end of the XVIII century came to the Pacific Ocean, established trade relations with China (Qing Empire) and other Asian countries, and carrying copper money for thousands of Luisst was expensive.

Secondly, in West Altai, the Colapo-Voznesensky plants paid copper from the local ore, and there was an opportunity to minted coins behind the Urals, that is, in Siberia.

On November 7, 1763, the Empress All-Russian Catherine II issued a decree on the chasing of the Siberian coin.

Already on January 18, 1764, the head of the Kolyvan-Voznesensky factories in Altai A. I. Poroshin signed an order to determine the place for the construction of a copper-smelter plant and a mint during him on the River Nizhny Suzun, where there was enough water, forests and limestone.

The construction of the mining complex began in 1764. The most grandiose building was the dam on the Nizhny Suzun River, necessary for the functioning of water wheels, many other mechanisms of the copper smelter plant. It was an advanced hydraulic structure of the XVIII century.

Traveler P. S. Pallas (1741-1811), who visited Suzun, wrote: "... Surprised the thick pine forest, according to which it was pleasant ... I struck the dam 110 in the width and 12 seeding in a height ...".

The construction of the dam led, Master's deeds - Ryabikov and Latnikov. Nikita Bakharev, Nikita Baharev, was appointed by the main "caretaker and the organizer on the orders of the office (his name is one of the streets of the village of Urban-type Suzun). About a thousand people took part in the construction.

In the spring of 1964, the spring was blocked by the dam, and only in the fall of 2008, the reconstruction of this structure took place.

A stonetly building remained from the Suzun Copper Plant. This is one of the manufacturing workshops of the plant, where the limestone was interpreted from the local deposit required for the mirror of copper. Toll walls, 1 meter thick, taking into account cold Siberian winters, made of characteristic bricks with stamps of masters, window openings and entrance on the facade are beautifully laid out in the form of an archer and semi-colors. The building is waiting for its restoration.

The building of the executive apartment and the office for the controlling a copper-smelting plant and the mint was built in the last quarter of the 18th century. Then he was called the "commander's house." This is one of the first houses in the village, preserved to the present day. Since 1989, a historic building, which is included in the Unified State Register of Cultural Heritage Objects of the Peoples of the Russian Federation, occupies a Suzansky Local Lore Museum located on Lenin Street, 15.

Thanks to the copper-smelter plant and a monetary court, a large industrial enterprise of non-ferrous metallurgy existed in the territory of the modern Novosibirsk region. Here, for the first time, engineering technologies and regular planning in construction began to be implemented, mining workers and technical intelligentsia appeared, and the first in the territory of our region, hospital and handicraft school were built.

Let us return to the official history of the first plant of the Novosibirsk region. The Russian Empire by the middle of the XVIII century greatly increased in a territorial relation, and carrying copper money for thousands of Luzst was too expensive. In addition, Altai has already paid copper from local ore on the colony-ascension plants. However, there were other precious metals in copper ore, and the smelting technology was imperfect. The Office of the Mountain District reported the Cabinet of Ministers: "... There is a considerable number of silver in ore and even a noble gold particle." After the calculations produced, they decided to compose from each Pone of Kolyvan copper not 16 rubles of coins, both throughout the country, and 25 rubles at once. The Suzun coin of the same dignity as in Moscow, weighed much less, although the walking had only in Siberia.

The opening of the mint in Suzun pursued two goals: to stop the annual import of money from Yekaterinburg for the content of the plants of the Altai Mountain District (the total weight of the money was 120 tons!) And use copper on site, the sale of which is unprofitable. From 1766 to 1781, the Suzun has proved, according to various sources, 3.5-3.8 million rubles that went from the Urals to Kamchatka, as well as used for trade with China and Central Asia countries.

Siberian copper coin was a different dignity: half (quarter kopeck), money (commissioning), penny, two kopecks, five kopecks and ten kopecks.

On the one hand, the coin was depicted on the coin - two sables at the shield; There is a cost, year of production and a circular inscription: "Siberian coin". On the other side of the coin - Monatherine II monogram, crowned with crown and framed laurel and palm branches.

In total, during the years of its existence, the Suzan Mint has released a copper coin of more than 300 species. Few collectors can boast a complete collection of coins of the Suzunsky yard: it is quite fully presented in the Novosibirsk Regional Museum.

After 15 years of chasing of the Siberian coin (1766-1781), the Suzansky Mint began to produce the usual all-Russian coin.

On the night of December 7-18, 1847, the Suzane Mint burned down as a result of a strong fire. Here is a document of that time from the Altai Archive: "Mountain boss Colonel Sokolovsky. Sim is forced to notify high inflamed that on December 7, 1847, a fire opened in the casing of the coin court at 2 o'clock in the housing. The results of extinguishing results were not given. All compartments of the coin court, somehow: printed, plush, slit, germ, cut-out, turning, countable room, intertwining at the throughput gate hut and part of the fastener fence - burned to the base. The fight against the fire is kept relentless ... "

And already under Nicolae I, after the fire, the mint decided not to restore, and the chasing of money was transferred to Yekaterinburg. In 1876, the mint closed and there, leaving the right to produce money exclusively at the capital of Russia. In 1915, copper was discontinued in Suzun.

In the territory of an almost destroyed plant, the twelve (production room, where the limestone, which served as a catalyst for the smelting of copper) was well preserved. There is a restored dam, the foundation of the copper-smelter factory remained, the bridge was renovated, the pond is cleared. The wooden warehouse building remains with extensions, a major stall was discovered during the excavations, a memorial plaque was installed on the grinding building. There is a design of an industrial museum, an archaeological museum under the open-air and other infrastructure facilities of the tourist complex, designed for receiving 50,000 visitors per year.

III. Pride, honor and heritage of the Suzun land.

Selected biographies.

Frolov Peter Kozmich (1775-183 ...) Born in the Zmeinogorsk fortress, in the family of an outstanding inventor-hydraulic engineering K. D. Frolova. At the end of the St. Petersburg Mountain School (1793), P. K. Frolov served on the Zmeinogorsk and other Altai mines.

Since 1797, he worked at the Suzun copper smelter on the inspection of the factory "melting and supervisory" works, as well as "consisted of receiving" brought from the Rudniks "and other factory supplies". At this time, they were performed a graphic drawing of the pristine Suzun, when there were no photos (a copy of the drawing is stored in the Suzun Museum of Museum).

In 1811, P. K. Frolov was transferred to St. Petersburg by the head of the Dwarf Expedition of Mountain and Salt Affairs, and since 1817 he was appointed head of the Kolyvan-Voznesensky factories. With it, a significant work was carried out on the mechanization of a number of mines and factories, silver smelting stabilized, the lead production increased, the Copper coin coincision increased, the first paper mill in Western Siberia was built, a meteorological and magnetic station was found. At the initiative of P. K. Frolova in Barnaul began construction of hospitals, foddes with the church, a mountain college with the orphan department and obelisk in honor of the 100th anniversary of the mining in Altai. P. K. Frolov, together with Dr. F. V. Gebler, founded a museum, uniting the existing museum collections and placing them in the same building (1823).

In 1830, at the age of 55, he retired and left Altai. He died in St. Petersburg.

Streggkov Filipp Vasilyevich (1769-1811) Born in the Family of the Master Suzun Plant. The service began in 1784 by a waswerler at the Zmeinogorsk Mine. I also graduated from school and was determined by a student to Master-Kamnezu Baklanov on a grinding mill at the Local Plant. A talented and diligent student, having replaced him after the death of Baklanov (1791). In 1793, F. V. Streggkov invented the "drilling machine", a significantly reduced processing time of stone products.

In 1800-1802, the Kolyvan grinding factory was built on his project, which he led to the end of life. F. V. Streggkov equipped the factory with high-performance equipment, its own invention: machines for simultaneous grinding and polishing the inner and outer surface of stone products, to pull the figure of oval shape, replaced the bridal emery by local abrasive material. Factory products were known far beyond Russia.

Laulin Mikhail Sergeevich (1775-1835), Mining specialist, son of a soldier. He graduated from the Barnaul Mountain School (1790). Working at the Suzunsky Plant, built an original installation of copper spilling in the form (setup) from the furnaces with cranes.

M. S. Laulin built one of the first cast-iron-rail roads in Russia between the Zmeinogorsk Rudnikovsky Silper Silper Plant, designed by P. K. Frolov (1806-1808), designed and built the body of the melting factory (instead of the burnt) Barnaul Silper Malvil Plant (1809- 1811).

From 1811 to the end of the life of M. S. Laulin - the manager of the Kolyvan grinding factory. Under his leadership, Kolyvan masters were made by numerous highly articles - a series of medallions about the Patriotic War of 1812, jasmic bowls and columns.

With it began the processing of the huge monolith of green jams from the Reznaya Kamencino, which became the world famous "queen VAZ", weighing 19 tons.

M. S. Laulin is buried in the village of Kolyvan Altai Territory. His grave with a massive granite slab, squeezed by Kydivan Kamnezes, was preserved to this day.

Tistrov Vasily Ivanovich (1799 - after 1845), born in the family of "Master's Glass Affairs". After graduating from the mountainous building in St. Petersburg, V. I. Tistrov went to Altai. The service began in Barnaul, where he was appointed "bye the melting production of the Barnaul Plant."

In 1823, V. I. Tistrov direct to the Urals "for comments on the discovery and development of gold-containing sands in Yekaterinburg plants ..." V. I. Tistrov acquired in the Urals and experience did V. I. Tistrov.

Over the years of work in Barnaul, he was a caretaker of the Mining Museum, a teacher of a mountain school, headed with a paper factory. In the 1930s V. I. Tystrov - the plants and mines of the Salair district. Since 1840, V. I. Tystrov was appointed manager of the Suzun copper-smelting plant and a mint.

In connection with the disease, on November 17, 1845, V. I. Tystrov receives a resignation from the service in the rank of lieutenant colonel of the building of mining engineers.

Cherkasov Alexander Alexandrovich (1834-1895) - Mining Engineer, Managing the Suzun Copper Plant (1872-1883), Writer-Naturalist. Born in the family of a mining engineer. In 1855 he graduated from the St. Petersburg Institute of the Corps of Mining Engineers and was sent to Transbaikalia (Nerchinsky Mountain District), where he served until 1871. It was awarded three orders and in the rank of major translated into the Altai Mountain District as head of the Salair Mine. In 1872, A. A. Cherkasov was appointed to the manager of the Suzun copper smelter.

In 1883, A. A. Cherkasov resigned in the rank of lieutenant colonel and moved to Barnaul, where he lived seven years, of which five years was a city head.

Over the years of service in Transbaikalia, A. A. Cherkasov proceeded by the whole Dauria, where he was addicted to "writing." Debit A. A. Cherkasova as a writer took place under the patronage of N. A. Nekrasov. In 1886, the magazine "Contemporary", which was edited by N. A. Nekrasov, published the "Notes of the Hunter of Eastern Siberia". A separate book "Notes ..." was published in German (1886), twice in French (1886, 1899), and in Russia the book was published 6 times, and four times - in the Soviet period. Essays "Broken Cup", "Ugryum", "Cultum" were published in the Moscow magazine "Nature and Hunting", and in 1893 - Roman "In Altai".

Books A. A. Cherkasova not only about the beasts, birds and methods of hunting for them. The works contain rich information about the past Transbaikalia, Altai, about culture, life and custom of the local population.

Petrodes Peter Filippovich (1908-1979), Suzansky chroniclel - local history, naturalist. Born in the village of Zorino Suzunsky district. For more than half a century of his life, Peter Filippovich dedicated to local history. He was interested in everything: history, culture, economy, wildlife, fate of people. All the years he did not part with a notebook and a camera.

P. F. Pirogkov was ideological organizer of the Suzun Museum of Local Lore, actively participated in the district and regional press, led in the regional newspaper "New Life" heading "Local Lore Chronicle Suzun".

Peter Filippovich created "Siberian Old-timer's Dictionary", in which about 400 unique words. The West Siberian Book Publishing House produced his book "Suzunsk Multiwill."

The name P. F. Pirochkova called the street under construction of a southwestern residential array of Suzun.

Forest Bonitet (it. Bonität, from Lat. Bonitas - benign), indicator of forest productivity, depending on soil and climatic conditions (habitat). Determined by the average height of the trees of the dominant plant of plantations, taking into account its age. Under the bonitational scale of plantations are divided into 5 classes of Bonitte, denoted by Roman numbers. The class I refers to plantings the most productive, to V class - the least productive. Often the number of classes of forest bonitet increase, for example, the IA sign indicates plantations with the productivity above I class and the VA sign - below V class. For all tree breeds adopted a common bonimary scale. Special scales are installed for seed and threshing plantations.

"Prioksko - Terraced Reserve" - \u200b\u200bunconscious value of the reserves. The duration of the smokery period in the priocco-terrace reserve is more than 135 days. The priocy-terrace State Reserve is located on the square of 5 thousand hectares. Environmental (environmental, media) value of reserves. Reserves are the most famous and rigid form of territorial protection of nature.

"Ecology of Nature" - Methodical Objectives: Stages: Results. Participants: Grade 11 school number 45. The main question: why do you need to protect nature? The creative name of the project: soil, air and water - our best friends. The topic of the educational project: protection or environmental pollution. Didactic objectives: educational items: German, ecology, regions.

"Reservations of Novosibirsk" - Manulylovsky Reserve. The northern part of the reserve May morning is included in the borders of wetlands. On the territory of the reserve, the Main Migration Paths of many species of birds run on the territory of the reserve. The Square of the Kirzi Federal Reserve - 119 808 hectares. The State Landscape Biological Reserve "Chanovsky" is 77% consisting of wetlands.

"Nature management" is a reduction in waters and territories for full-fledged economic activities. An idea of \u200b\u200benvironmental management as a system. A sign of the systemic crisis (SC) and the characteristic of the condition subsystems. The exacerbation of the unsatisfactory demographic situation. Sign SC. Progressive worsening environment of habitat, including climate change.

"Warming of climate" - the fertile regions of the coast will be a victim of the sea and will be flooded. Possible consequences of global climate warming. Kyoto Protocol. Increase in temperature will increase the evaporation of moisture from the surface of the ocean. Science has repeatedly proven, but the facts confirmed that the temperature is growing rapidly. Glacier Portage in Alaska.

"Environmental sewn" - emissions of polluting atmospheric substances, thousands of tons. Social stability (9 indicators). Definitions. Efficiency of resource use (7 indicators). Purpose and direction. Environmental protection. Indicators of environmental statistics are being introduced in accordance with the Government Decree No. 848.

Total in the subject of 16 presentations

Published:19.08.2008

Suzansky district - the southernmost of the eastern regions of the Novosibirsk region. Distance to Novosibirsk - 191 kilometers. Message to the regional center-rail and motor vehicle.

The total area of \u200b\u200bthe area is 4.7 thousand square kilometers (2.7% of the territory of the region).

The surface of the district is a slightly wavy plain crossed by manems and ravines. In the south of the district there is an 80-kilometer plot of R.Ok. There are many small lakes in the area - sports hunting and fisheries.

Minerals: granite, quartzite, limestone, clay, peat, swamp phosphates, sapropel, construction sands, construction stones.

The area is located in the forest-steppe zone. This is one of the rich forest areas of the region. The Forest Fund of the District has high potential capabilities, is characterized by the predominance of forest areas. Wood reserves make up 32.2 million cubic meters. Pine tremors prevail in the Goslefond - 62%. Ribbon bors - part of the natural historical monument of nature - Siberian tapes. Pine bors are rich in berries and mushrooms, serve as a place of rest. The number of moose is the highest in the area. A wolf is found, there is a roe, hare-white, columns, squirrel-televka in Boru. In the littered areas of the forest, Lynx is found. From the birds you can celebrate Glukhary, Tetherieva, Ryabchik, Gorzlitsa, White Partridge. Suzansky Hunting Reserve is a specially protected area, an area of \u200b\u200b80 thousand hectares.

In the structure of the land foundation, the forest area is 50%, agricultural land - 44%.

Agricultural area. Natural conditions (Northern forest-steppins, most of the soils - gray forest and chernozem; sufficient moisture) allow you to grow the average wheat varieties, oats, barley, buckwheat, to develop a cattle breeding of meat-dairy.

As part of the district of 15 administrative units, of which 14 are rural.

The population of the district is 33,800 people.

The district center is a working village of Suzun. The village was founded in 1764. The status of the working village was assigned in 1939

Suzunsky district has deep historical roots. The presence of a rich pine forest, rivers, the proximity of the Altai mines created favorable conditions for the development of the industry: Decree of Empress Catherine II dated November 7, 1763, Suzun became the place of occurrence of a copper smelter, on whose monetary yard was minted by the Siberian coin. Together with the plant in 1764 the village of Suzun arose. He was designed in the city of St. Petersburg. A sample for the construction of the plant was the Kolyvan Medelval Plant and the Ekaterinburg Mint. The plan was based on regular development, the streets were designed perpendicular to the bank of the River Nizhny Suzun and were parallel, these streets are still the foundation of the master plan for the village.

The most grandiose facilities were: dam, a length of 110 meters, 12 soil width, which blown up the river; Ice containment bridges; coastal ruffles; Processes for passing water and a complex system of other hydraulic structures. In 1827, a mining school was founded to prepare factory personnel in Suzun, where 30 boys were trained.

In 1847, the mint burned down and Suzun workshops moved to the fulfillment of major orders for the entire mining industry Siberia: copper was paid here, silver, the bells were cast, a rifle production was established. Suzun can be proud of the world's first steam turbine made in his workshops.

Suzunsky district is one of the 30 districts of the Novosibirsk region, in whose territory there are 14 rural and 1 village council, 42 settlements.

During its existence, the Suzansky region has undergone various transformations, both external and internal. The settlements that are currently included in the Suzunsky District have also experienced various changes regarding the size, subordination, status and renaming.

The territory of the current Novosibirsk region, on which Suzunsky district is located, in administratively since 1708, it was part of the Siberian province with the center in Tobolsk, from 1764 to Tobolsk province (governance). In 1804, Tomsk province was formed, which included almost the entire territory of the future Novosibirsk region, including the Suzun district. In 1822-1882 Tomsk province was part of the West Siberian Globrian General with the center in Tobolsk, and then in Omsk.

About the site of the Suzunsky district in the scheme of the administrative device in the pre-revolutionary period, it is not necessary to speak, but many villages, now related to the area, existed evenly and were geographically organized accordingly.

Many of our villages have formed immigrants in 16-17 centuries. - from. Bobrovskoe - 1786, der. Upper Suzun - 1526, der. The settlement is 1625, Zorino - 1574, der. Kargapolovo - 1625, der. Little - Malyshovka - 1625, der. Malyshevo - 1778, p. Merit - 1625, p. Momothing - 1770g., Der. Nizhny Suzun - 1756, der. Fotnalovo - 1845, G., Der. Taradanovo - 1624g Artamonovo, der. Bear - 1708g., P. Bounds - 1696, p. Boltovo - 1576, der. Yerezna -1805g., P. Ershovo - 1676, p. Zakovo, p. Lushnikovo, der. Maiurovo - 1891, der. Flat - 1787, p. Christmas, der. Tatchikha, der.- Wrupin - 1705g, pos. Kharkovka - 1911, der. Cold - 1875, p. Sharcino - 1727, der., Shigaeva - 1877, p. Shipunovo - 1776.

The date of education of the Suzun district is considered to be September 12, 1924. It was during this period that the Suzun enlarged parish was transformed into a Suzansky district, which mainly occupied the Priobi settlements. It consisted of 4011 yards, 17616 people lived. The main territory of the present district united the Bitkovsky district formed from the enlarged volost of the same name. It consisted of 6368 yards, there were 33269 people.

By the decision of the Presidium of the West-Siberian Regional Executive Committee of March 5, 1932 No. 2369 in accordance with the Decree of the Central Executive Committee of March 2, 1932, the Bitkovsky and Suzansky districts in the full composition of the villagers were merged into one Lushnikovsky, establishing a district center in the village of Lushnikovo, leaving all regional institutions In the village of Plant - Suzun.

On December 10, 1932, the newly educated area was renamed Suzunsky, with the center in the village of Plant - Suzun, whose boundaries did not change until today.

Decree of the Central Executive Committee of June 7, 1933, the village of Zavod - Suzun was renamed to the village of Suzun, and decree of the Presidium of the Supreme Council of the RSFSR of February 7, 1939, it is classified as a working room.
In 2003, the District village of Suzun was listed in the list of historical inherited places in Russia.

Climatic characteristic

The climate of the Suzunsky district of the Novosibirsk region is continental with sharp changes in temperatures, both between the seasons and within a day. In agroclimatic zoning, the Territory of the Suzunsky District refers to moderately warm, not sufficiently moistened to agro-climatic subarea.

Winter is harsh and continuous with sustainable snow cover and strong winds and snowstorms. Possible short-term thaws. Due to the abundance of sunlight and warmth summer is roast, but relatively short. Transition seasons (spring and autumn) are short and distinguished by unstable weather - spring refunds of cold weather, late spring and early autumn frosts. The latest spring frosts are observed until May 26-29, and the first autumn frosts - September 5-7.

Table 2.1.1. Basic climatic characteristics

Characteristic	Value
The average annual air temperature	+ 1.5 ° C
Average long-term air temperature of the cold month (January)	-24.5 ° C.
The average long-term air temperature is warm (June)	+ 19,6 ° С
Duration of the growing season (T\u003e 5 ° C)	165 days
The average annual amount of precipitation	387 mm
The average number of days with precipitation for the year	111 days (55 with snow)
Medium long-term evaporation	About 60% of precipitation
The duration of the sustainable snow cover	160 days (October 30 - April 11)
Middle power of snow cover	51 cm
Regulatory Depth of Soil Version	180 cm
Maximum depth of soil freezing	286 cm
The predominant direction of the wind	Southwest
Average wind speed	4.1 m / s
Average of maximum wind speeds	25 m / s

Sharp weather changes and general climate instability are caused by the penetration of cold arctic, as well as warm dry mass of air from Kazakhstan and Central Asia.

Atmospheric droughts and Sukhov are most likely in May and July. Intensity of droughts, as a rule, weak or average, duration 5-6 days, in some years to 15 days. The amount of precipitation for the 4 winter months (December - March) is about 70mm, which in the snowdown ensures sufficient soil moisture reader.

During the year, the winds of the south-western direction prevail in the area of \u200b\u200bthe district, but in May and early June, the northeast winds that cause frosts are frequent. The average wind speed is low (4.1 m / s), however, in some years, winds are observed in the spring period, a speed of 30-35 m / s, which causes windsword and burlyas (in pinemas, oxygen).

Fogs are observed throughout the year, the average number of days per year with fog -26. More than half of the fogs are observed at the calm, one third - with a weak wind and 10% with wind speed 3-5 m / s.

A distinctive feature of the climate is the high repeatability of inversions, the greatest - 37-40% is observed in winter, in the summer - 30%, in transition periods - 19-25%. The average power of surface inversion in the cold period is 0.5-0.9 km, in warm - 0.3-0.4 km. Inversion temperature gradient during the year varies from 10.6 degrees / 100 m in December, up to 2.6 degrees / 100 m in July. At the calm, 27% of inversions are observed.

Hydrological and hydrogeological characteristics

Surface waters

The hydrographic network in the Suzun district is created by the Ob River, which passes through the southwestern border of the district, and its tributaries. Obi basin area is 2990 thousand km². According to this indicator, the river ranks first in Russia. Ob is also the third of the water content in Russia. The river flows into the Kara Sea, forming the bay of the Obba lip (about 800 km long). According to the nature of the river network, the power facilities and the formation of the water regime, the Ob is divided into 3 sections: upper, medium and lower. Suzunsky district is located in the upper course of Ob.

Power river mainly snow. During the period of spring-summer flooding the river brings the bulk part of the annual flow. In the upper course, the flood begins from the beginning of April. Raising levels begins while icebetas; At the opening of the river, intensive short-term lifting levels occur as a result of congestion. Because of this, some tributaries are possible to appeal the direction of the flow. The flood ends in July, the summer interstitial is unstable, the rain flood passes in September-October.

Table 2.2.1. Characteristics of the main water bodies of the Suzun district

Name of the water site	Place of river failure, km	Length in district, km	The area of \u200b\u200bthe reservoir, ha
R. Ob	Kara Sea
R. Upper Suzun
R. Nizhny Suzun
R. Kamenka
R. Top Karakan.
R. Nizhny Karakan.
R. Inya
Oz. Nuju
Oz. Kulikovo
Oz. Osinova
Oz. Dolgushevo
Oz. Nechunayevskoye
Oz. Carasevo
Oz. Small bear

Valley rivers flowing into r. Ob, expressed weakly. Rivers belong to the I Hydrological District. A characteristic feature of these rivers is a small flow rate, a slight slope (from 0.35%) and a large toastness. All rivers have an orstive bottom and in summer heavily overgrow herbal vegetation. The module of the middle annual flow is 3 l / s per km 2 (r. Inya). Water mode of rivers is characterized by spring floods and floods in a warm time. The summer-autumn interleave characteristic of July-October is violated annually by the passage of rain floods. The average modules of the flow of summer-autumn membranes are from 0.25 to 3.04 l / s per km 2. Winter interley is stable, low-water. Thale snow waters are in the nutrition of the rivers of the region of 79-87%, the rain stock - 3-4%, soil - 10-17%.

Most of the lakes are concentrated in the southern part of the area. The shores of the lakes are mainly peat and fuse, the water level is not constant. The area of \u200b\u200bthe lakes are reduced, which is associated with the intense logging of ripe trees with the greatest water-regulating properties in forest arrays adjacent to lakes. In the recreational goals of the lake are practically not used.

The wetlability of the territory is 9%. The area ranks second after Bolotnic, among the areas of the Eastern Zone of the Novosibirsk Region. Most of the manes are located between the manes, i.e. According to intergreathe decreases and within the left bank of Ob.

Protection of fish stocks in the area is carried out by the Suzunsky Pilot of Fisherman of the Upperobsky Territorial Department of the Federal Agency for Fisheries. Rivers and Lakes of the Area are habitat not only widespread species of fish, but also rare, such as sturgeon, sterling and non-notma. Every year, from mid-April to mid-May, a ban on fishing is announced, activities for the protection of water bioresources, explanatory work with the population through the media.

The groundwater

According to the hydrogeological regionalization, the territory of the Suzunsky district refers to the Sayano-Altai hydrogeological folded area.

At a significant area of \u200b\u200bthe Sayano-Altai hydrogeological folded area, the only perspective source for organizing drinking and household water supply is a fascinating zone of Paleozoic breeds. In the extreme southern part there is a horizon of the heartless suite.

To the Jurassic Education, filled with local depressions in the Paleozoic foundation, is also timed to be promising for water supply aquifer of Yura.

Engineering and building conditions and mineral resources

Geological and geomorphological characteristics

The geological structure of the territory of the Suzunsky district is characterized by considerable complexity due to the fact that the joint of the West Siberian Plate and the Altai-Sayan folding system passes in the southern part of the district. In the area from the north to the south, 3 large tectonic structures are replaced by each other, sharply differing in time and conditions of formation: Lategracin Kolyvan-Tomsk folded zone; Gorlovsky Caledonian-Gerinian intergranium deflection and the folded structure of the Salair anticlinorium, formed in the Salair and Caledonian cycles of tectogenesis. They constitute a Paleozoic foundation, which in the south is replaced by the deposits of the Cenozoic era of the Biysco Barnaul Vpadina.

The following lithological and stratigraphic divisions are involved in the geological structure of Paleozoic foundation:

Upper Devon is represented by the deposits of the Frank and Fomensk tier Kolyvan-Tomsk folded zone. These are monolithic gray color sandstones, aleurites, clay shale of the Inski series, uniting the Paccine and Jurgin Sweets. Natural outcrops are found in Obi, Ini valleys, sometimes in the valleys of small rivers, ravines, logs. The power of the deposits of the Paccine Sweet 600 m, and the Yurginsky - 1600 m.

Integrated formations in the area are represented by granitoids, luberites, porphyrites. Granitoids are gray, pinkish-gray are composed of wild spatts, quartz, horn toilet, biotitis.

Triassic rollerities and the funite porphyrites are breaking through the deposits of the Pacinsk and Yurginskaya Sweet and are divers of dark gray massive rocks from gray and black pyroxen.

Intensively deployed, places metamorphized sediments of the Inski series and breaking their intrusions with developed on them the weathered bark form a complex foundation of the territory. Its breed is broken by ancient tectonic disorders. The surface of the foundation has a rugged erosion-tectonic relief due to tectonic processes and intensive weathered in the Mesozoic era.

The formation of the ancient crust of the weathered of Paleozoic rocks of smallpaleogenic and non -ogenic ages occur on interfluries, slopes, the bottoms of the valleys. Weathered cortex are composed of colorful aleurito-clay rocks.

On the sublime areas of the Paleozoic foundation of the right bank. ON there are small fields folded with overded products of the weathered cortex - the aeuritic clay of the kaolinito-hydroelluded composition. Features of the structure of the foundation influenced the morphostructure elements of coating sediments.

Almost throughout the entire territory, the foundation is blocked by lower-medium-quantities subaeral and subkval deposits. The floodplains of rivers are blocked by alluvial sediments.

Alluvial deposits are formed by river streams. These are small polyminamic sands, pebbles, gravel. Subakvali was formed in aquatorium aquatorium, clay illuminated, loams. Subaeral sediments are common on interfluries, slopes, these are loams, squeezers having an aeuritic composition.

Fourth inapproving terrace r. OBI is francmed middle-hardest sediments. The lower part is the channel allyvium, the upper one - the floodplain facies, is composed of loams, sandwiches, overlapped by forest loam and sachese or enamel sands.

Upper-quirky deposits of the third superstar terrace of OBS are deeply embedded into a sedimentary case. The lower part is sands with gravel and pebbles, upper - sandy, sands. From the surface is blocked by forest-like loams, sandy. Power 3-5 m. The third terrace of Ini is composed of illuminated sublinks and sudaine with a capacity of up to 15 m, from the bottom of the channel sands. The total capacity of the sediment of the terrace is 25-30 m.

Deposits II terrace r. Ob is basically sandy. II terrace Ini is composed by floodplain loams with sudesses. Obi terrace power - 13-18 m, ini - 11 m.

Upper-fascinating deposits of the first OIS terrace are represented by rolling robberies with pebbles, boulders and floodplain sounglicas. Terrace r. Inya is composed by sublinkami, less often with sachemes, the darling of aluminum consists of fine sand with pebble and gravel with a capacity of 3 m. Alluvial preciputes of the terrace from the surface are blocked by barried loams or gumulated soil.

Most small rivers, high floodplains are expressed in the middle and lower current, flood waters are rarely flooded. The height over the cut is 3-7 m, is composed of suglinkami and sachemes with sinks, places are transferred to the swamp sublinous soil 3-8 m. The deployment of a low floodplain terrace is developed in the lower flow of rivers, according to the composition they are similar to high floors, with a capacity of 1-1.5 m.

Modern lake-marsh deposits are illuminated loams, sandy, sands, enriched with vegetable material, spacing breeds and peat layers with a capacity of up to 2 m.

According to the peculiarities of tectonics and geology, the area can be divided into latitude of the district center into two parts. Two thirds of the district north of the latitude of the district center are within the collapsed folded mountain zones that were part of the Altai-Sayan folded mining system. The modern relief consists of alternating the mane and intergreic slides - logs. The height of the mane and the depth of logs from 3 to 10 meters. They stretch from the north-east to the southwest. Magic length 250 - 300 meters. Their absolute height ranges from 150 to 317 meters. The thickness of sedimentary rocks is not large, therefore, solid crystalline rocks, the foundation, perform on the day surface in the highest points of the relief, on the slopes of the hives, logs, deeply embedded valleys of the rivers.

The south of the latitude of Suzun the territory of the district lies within the West Siberian Plate, in its southeastern part - Biysco Barnaul Wpadin. This territory is composed with powerful strata of Mesozoic and Cenozoic marine and continental sediments, from the pebble, sand, soup, clay and other loose rocks. In this part of the area, relief is flat and finely dumping. There are no exits of solid rocks on the day surface.

The latitude of Suzuna is the boundary of the West Siberian Plain and the Predesalair sublime plain. On this line at great depth, tectonic violations are hidden - the junction of the West Siberian Plate and the Altai-Sayan folded system. By virtue of this, Suzunsky district is located in the zone of probable earthquakes by force of up to 7 points.

Physico-geological processes

On the territory of the district there are various adverse natural processes complicating possible construction.

Karsto-suffosion processes. Completed in places where the power of quaternary deposits is insufficient to neutralize karst processes. Celebrating phenomena are characteristic of Limsoid Suglinkles and Slades, composite deposits. The power of the sedimentation with a load of 0.3 MPa ranges from 1 to 10 m, with the predominant capacity of 5-7 m. The greatest impliety - to a depth of 4-6 m.

Plane washing and linear erosion. Distributed on the slopes of the erosion network, plots covered with forest-like sublinks are particularly susceptible. When rebuilding or carrying out large solid-sized logging with heavy machinery, these processes are subject to these processes and the slopes of another mechanical composition, primarily with the predominance of heavy soils.

Walking. It takes place on the ancient elulvial plains, in the floodplains of rivers in intergreic decrees. Especially subject to Left Bank. Ob.

Earthquake. The high probability of earthquakes at the junction of the West Siberian Plate and the Altai-Sayan folding system.

Engineering and construction zoning

The territory of the district in engineering and construction conditions is conditionally divided into three areas: relatively favorable for construction, favorable for construction and unfavorable to build areas.

The main construction limiters are erosion, the fever, the probability of an earthquake.

Territory favorable for construction:

River terraces are quite well drained, isolated by sandy and sampling soils;

The territory of the Biysco Barnaul Wpadin.

However, the negative factor is the spread of local lap processes. When laying roads and conducting other infrastructure, the local fever factor must be considered.

Territories are relatively favorable for construction:

The territory of the Kolyvan-Tomsk folded zone. The relief is represented by alternating the mane and logs. Conditions are complicated by the inhomogeneity of the relief;

Territory with a high probability of earthquakes. Located on the border of the West Siberian Plain and the Predesalair sublime plain;

Territories complicated by karsto-suffosic processes. Catching and fevering processes may be observed;

Territories complicated by local latling. Territories are focused in the northern part of the area. The level of groundwater is at a small depth. When carrying out construction work, an arrangement of artificial drainage or water insulation of basement rooms is recommended.

Unfavorable territory for construction:

Erosion network. These are growing ravines. Modern erosion manifests itself mainly in the deepening of ravines and their lateral growth. Significant slopes and dismemberment of the territory prevents use in urban planning.

Swamps and peatlands. In the swamps, powerful deposits of the implanted peat are formed. Construction seems inexpedient.

The floodplains of large and valleys of small rivers. The territories in the floodplains of rivers can with different probability (depending on the level of floodplain) be susceptible to flooding during flood and floods. This makes the construction of premises here dangerous, and in the construction of infrastructure facilities it is necessary to apply appropriate measures. Crossed relief in the valleys of small rivers and the prevalence in them of the booming processes also prevent the development of these territories.

Mineral and raw materials and soil cover

The territory of the Suzun district has an average mineral resource potential. Mineral resources are mainly represented by mineral resources used as building materials and raw materials for the production of building materials. On the territory there are deposits of loams of bricks, sands of construction, construction stones, sapropeli.

The total number of balancing reserves of brick loams is 1723 thousand m 3, 2 fields are located on the territory of the district, of which 1 is in reserve (Lushnikovskoye, the balance sheet - 880 thousand m 3) and one is developed by the Idea CJSC (on average, annual mining It is 14 thousand m 3).

Construction sands are represented by the wind field with shared balance sheets of 5543 thousand m 3. The plot of subsoil "damn throat" of the brass deposit is in the use of CJSC "West Siberian River Shipping Company" (the volume of annual production is 52 thousand m 3).

In the borders of the Suzunsky district there are 2 fields of construction stones (Bobrovskoe and Schaydurovskoye) with a total reserve of 14178 thousand m 3, the Shaydurovskoye deposit is developed by OJSC Novosibirsk Career Management (the volume of annual production is 50-55 thousand m 3), the Bobrovsky deposit is in reserve .

There are 1 deposit of sapropel (aspen) with balance reserves of 2000 thousand tons. At the moment it is in reserve.

On the territory of the Suzunsky district, four main types of soil are distinguished: in the south - ferrous-weakly casual sandy (boron sands); In the central part - black soiled; In the north - the chernozems are opollen and along the north-western border - gray forests. Due to the high wetlability of the territory of the area and salvation of the soil-forming rocks, and the soil waters can be found soils of saline rows: meadow-black earth, meadow, marsh, salt marshes, solonges and soles.

Dernovo-weak-casual soils have an acidic reaction throughout the profile, high (20-70%) insaturation of the bases. The content of humus can reach 5-7%, but the drop in its content with a very sharp depth, and fulvironment is dominated as part of humus. The upper horizons of turf-podzolic soil are depleted by one and a half oxides and is enriched with silica.

The upper horizons of gray forest soils have a weakly acidic reaction (PhKCl 4.0-6.5). The degree of saturation of the bases is 70-80% in the upper horizons and 90-95% in the lower. The content of humus ranges from 4% to 7%.

Chernozem soils have high agrochemical indicators. The content of humus in the upper 10 cm is 6-10%, the drop down the profile is gradual. As part of humus, humic acids prevail over fulvocosloids. In the upper part of the humus horizon, the medium reaction is close to neutral or neutral and only to the lower border of the humus horizon occurs its weak acidification. The absorbing complex is almost completely saturated with the grounds. Chernozems have the optimal complex of water-physical properties, in particular the strong bufferity of the soil profile to the mooring. However, the spray and germination of the magnutructure of the arable layer determines their reduced water permeability. Therefore, when using arable land, irrigation erronces are often observed. Livestone loams, the basis of many soils of the region, weakly waterproof, which in combination with the dismembered relief contributes to water erosion.

Forest resources and animal world

In accordance with the "Forest Code of the Russian Federation" (ed. From 18.07.2011 №242-ФЗ), the main territorial units of management in the field of use, protection, protection, reproduction of forests are forestry and forest parks (Art. 23, clause 1).

The territory of the Suzunsky district refers to Suzunsky forestry, which is formed in accordance with the order of the Federal Forestry Agency dated December 23, 2008 No. 405 "On the determination of the number of forestry on the territory of the Novosibirsk region and the establishment of their borders."

Foresting forests refers to the plains and are located on the right bank of the upper part of the Ob River, the main forest massif is concentrated in the south of the district. The main soils on the territory of the forestry are dererno-weak-prolonged. These soils, as a rule, are confined pure pine fields of IA-II Bonitte classes.

The total area of \u200b\u200bthe territory of Suzunsky forestry as of 01.01.2010 is 218,674 hectares. Modern forest areas of forest area - 70%.

On the territory of the administrative area, in addition to the forests of Suzunsky Leskhoz, there are forests of the Ministry of Agriculture and Food of the Russian Federation with an area of \u200b\u200b19084 hectares and a total reserve of 2662.5 thousand m 3, collective farm forests with an area of \u200b\u200b30599 hectares and a total reserve of 4321.9 thousand m 3, and Forests of other ministries of departments with a total area of \u200b\u200b5334 hectares and a total reserve of 353 thousand m 3. These forests are presented, mainly small arrays with a predominance of birch plantings. The forest system of the Suzunsky district as a whole is about 35%.

In forestry zoning, the territory of the district is related to the West Siberian subtoper-forest-steppe area, the forest-steppe zone (order of the Ministry of Agriculture of Russia dated February 4, 2009 No. 37 "On approval of a list of forestry zones and forest areas of the Russian Federation").

Significant distribution in the area of \u200b\u200bthe district have pine forests - bors. On the western outskirts of the area on the border with the Ordan district, the strip of eastern part of the Kakanan boron stretched. In the East, the southeast is Suzunsky Bor. To the main forest-forming breed, pine, fir and larch mixed in a number of raw seats. In the second tier, birch and aspen grow. In the undergrowth - Kalina, rowan, cherry, willow, acacia, hawthorn, rosehip. Large squares are busy young pine.

There is a forest-steppe between Karakan and Suzun boras wedge. In the forest-steppe, plowed areas alternate with rarefied aspen-birch slices.

In accordance with the Forest Code of the Russian Federation dated December 4, 2006, No. 200-FZ, Federal Law of July 22, 2008 No. 143-FZ "On Amendments to the Forest Code of the Russian Federation", Federal Law of December 4, 2006 №201 -FZ "On the introduction of forest code of the Russian Federation" of the forest in Suzunsky forestry in its intended purpose is divided into protective and operational.

The total area of \u200b\u200bprotective forests is 149.9 thousand hectares. The protective forests include:

Forests that perform the protection functions of natural and other objects (protective stripes of forests located along the railway tracks of common use, federal road roads, general road roads who are owned by the subjects of the Russian Federation; Green zones);

Valuable forests (forests located in desert, semi-desert, forest-steppe, timber zones, steppes, mountains; forbidden strips located along the aqueous objects; irregular strips; ribbon bors).

The use of protective forests involves sustainable forest management, preservation of forest biological diversity, increase their potential, preservation of media, water protection, protective, sanitary and hygiene, wellness and other useful forest functions, while using forests while compatibility of this use with the targeted destination of forests and with useful features.

Operational forests occupy 68.7 thousand hectares. The use of operational forests provides wood and other forest resources. Types of allowed use of forests of Suzun forestry are regulated by Article 25 of the Forest Code of the Russian Federation.

Suzunsky district has a significant species composition of the animal world. Due to the widespread reduction and deterioration of habitats, poaching, predatory attitude towards animals and other anthropogenic activities, there is a significant decrease in the number of many species of animals: birds, useful insects pollinators, hoofs. Spring agricultural panels are negative, forest fires, in which bird masonry are dying, mammalian young people.

There are three oction-fish farms in the district: Kargapolovskoye, Suzunsk and Mermet.

The main fishing species are: elk, roe, fox, columns, ermine, lynx, wolverine, wolf, hare (rusak and white), chorus, caress, protein. From the birds are constantly inhabited by the deaf, Ryabchik, thermis, white and gray partridges, quail.

The migration pathways of birds are running through the area, so there are many ducks, geese, kelits on spring and autumn flights. Wheaves rest on the water bodies during flights. In summer, a lot of waterfowl game: Mallard, thicoch, shilohvost, black and other. There are birds listed in the Red Book in the Area: Black Stork (Suzinsky's reserve, Ob River floodplains), Orlan-Belochvost (Suzinsky's reserve).

Especially protected natural territories

According to the Federal Law of March 14, 1995 No. 33-ФЗ "On Specially Protected Natural Territories", specially protected natural territories (hereinafter referred to) - plots of land, water surface and airspace over them, where natural complexes and objects that have Special environmental, scientific, cultural, aesthetic, recreational and health importance, which seized with decisions of government bodies in whole or in part from economic use and for which the regime of special protection is established.

The issues of education and functioning of the PAs in the Novosibirsk Region at the regional level are regulated by the Federal Law of March 14, 1995 No. 33-FZ "On Specially Protected Natural Territories", the Law of the Novosibirsk Region of September 26, 2005 No. 325-OZ "On Specially Protected Natural Territories in the Novosibirsk region, "as well as regulatory legal acts of the governor and the administration of the Novosibirsk region.

The formation and improvement of the system of specially protected natural territories is carried out in accordance with the "Development and placement of a network of specially protected natural territories in the Novosibirsk Region", approved by the decision of the Novosibirsk Regional Council of Deputies in 1996.

Features of the use, protection, protection, reproduction of forests, located on the PAs are determined by the order of the IPR of the Russian Federation of July 16, 2007 No. 181 "Features of the use, protection, protection, reproduction of forests located on specially protected natural territories".

For each PAs, in accordance with its status and the species in regulatory documents on the creation of the PAs, a special regime of protection is established.

In order to preserve the unique natural complexes and individual natural monuments to provide scientific institutions with government regulations on the territory of the Suzunsky district, specially protected natural areas are allocated (Table 2.6.1.)

In addition to this scheme of territorial planning of the Novosibirsk region, it is recommended to create a network of PAs. It is planned to organize the Ordinsky Natural Park, which will include part of the territory of the Suzun district (along the Western border).

For all PAs located in the district, it is recommended to develop passports.

Table 2.6.1. List of specially protected natural territories (PAs) Suzunsky district of the Novosibirsk region

OPT name		Location		create		Legal basis functioning
"Lake Alloy"	monument	Suzansky district, 14 km northeastern with. Measure	Habitats and growth of valuable, relic, small rare and endangered species of animals and plants; Plots of scenic locality. Profile - complex.	1998	100
"Obskaya Sand Step"	monument nature of regional significance	Suzansky district, near with. Measure	Nature Monument category: Places of growing valuable, relic, small, rare and endangered plant species; Natural objects playing an important role in maintaining the hydrological regime; Unique relief forms and associated landscapes. Profile - complex.	1998	36,15	Educated by the decision of the Novosibirsk Regional Council of Deputies from 11.12.97 (first convocation, 37 session); Decree of the administration of the Novosibirsk Region dated November 16, 2007 №176-Pa "On approval of borders and regulations on the regime of special protection of the territory of the Monument of Nature"
"Sharcinskaya Steppe"	monument nature of regional significance	At 1300 m below the river Top Caucan from the village of Sharcino	Nature Monument category: Places of growing and habitat of valuable, relic, small, rare and disappearing species of plants and animals; Sections of the picturesque area; Natural objects playing an important role in maintaining the hydrological regime. Profile - complex.	1998	31,89	Educated by the decision of the Novosibirsk Regional Council of Deputies from 11.12.97 (first convocation, 37 session); Decree of the administration of the Novosibirsk Region dated November 16, 2007 №176-Pa "On approval of borders and regulations on the regime of special protection of the territory of the Monument of Nature"
"Suzunsky"	Biological Reserve Regional	Southeast Part of the Suzunsky District of the Novosibirsk Region	Profile - biological. Created for: preservation of natural complexes (objects) of the Priobi borsi of Western Siberia; preservation, reproduction and restoration of natural resources, enrichment of adjacent economic used land; protection of reproductive moose stations, roasted, hares, river beobra, gray groundhog, black birds, badger settlements and other species of wild animals; protection of winter parking lots and roeblers; protection of habitats of rare and endangered animal species; maintaining the necessary environmental balance and stability of the functioning of ecosystems.	1967	128 500	Educated by the decision of the Novosibirsk Regional Council of People's Deputies from 04.08.67 No. 508, decision of 27.08.79 No. 593 The validity period was extended until 1990.

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