Report about the river or. River trip or. Malaya Almatinka River

ILI, a river in China and Kazakhstan. It originates in the Eastern Tien Shan (see TIAN SHAN EASTERN) with two sources Tekes (see TEKES) and Kunges (see KUNGES), merging in Xinjiang (see XINJIANG UYGUR AUTONOMOUS REGION) (China). Flows into the lake... ... encyclopedic Dictionary

Or a river in the Semirechinsk region- a river in the Semirechinsk region, merges from 2 rivers: Tekes and Kunges, flowing within the Chinese Empire. Of these, the main source Tekes originates in the north. slope of the Tien Shan, in the Khan Tengri mountain group at absolute. altitude 11600 ft. and goes... ...

Or a river in the Transbaikal region- a river in the Transbaikal region, a left tributary of the Onon River, originates at the heights of the Alahan Mountains, covered with snow most of the year, flows through very mountainous terrain to the southeast and after the 130th century. The current flows into Onon near the village. Ust Ilyinsky. I. is different... ... Encyclopedic Dictionary F.A. Brockhaus and I.A. Efron

Or- river flows into Lake Balkhash; China, Kazakhstan. The etymology of the hydronym is controversial: Mong. or sparkling, brilliant; other Turkic fast or big river. A common explanation in the past from Russian. il modern the authors exclude. See also Alma Ata,... ... Geographical encyclopedia

OR- a river in China and Kazakhstan. 1001 km, basin area 140 thousand km². Formed by the confluence of the Tekes and Kunges rivers, it flows into lake. Balkhash. Average consumption water at the mouth 329 m³/s. Kapchagai hydroelectric power station and reservoir. Used for irrigation. Navigable... ... Big Encyclopedic Dictionary

River Don- Don Don's Voronezh region The source of the Urvanka stream flows through the territory of Russia near Novomoskovsk Ustye ... Wikipedia

Or- Wiktionary has an article “or” Or a word in the Russian language, a conjunction expressing an alternative... Wikipedia

Or- (colloquial) IL I. union. 1. (when comparing a sentence or individual parts of a sentence, excluding or replacing each other by sign). Indicates the need to choose between sentences or members of a sentence (statement or before each compared ... ... encyclopedic Dictionary

river- water flow is comparatively large sizes, as a rule, permanent (in some areas, in some areas, temporarily drying out or freezing), flowing in the channel it has developed, fed by runoff from its catchment area. To Ch. characteristics... ... Geographical encyclopedia

RIVER- An important mythological symbol, an element of sacred topography. In a number of mythologies, primarily of the shamanic type, as a kind of “core” of the universe, a world path penetrating the upper, middle and lower worlds, stands for the so-called space (or... ... Encyclopedia of Mythology

Books

• River of mystery, wave of love, Latyshko Olesya. A summer cruise may seem like a dream for anyone, but not for Lesya. And it’s not surprising: she’s been going on such a “dream” for the fifth summer in a row. And all because her grandfather is the owner of a two-decker... Buy for 364 rubles
• The River That Carries Us, Jose Luis Sampedro. German expressionist, rebellious truth-seeker and God-seeker, preacher of self-purification Franz Werfel and the Greek Nikos Kazanzakis, a humanist excommunicated from the church because of his free interpretation...

The Ili River is the largest river in Semirechye. The river, with a total length of 1439 km, originates in China. The name of the river comes from the Mongolian word “ilansu”, which translates as “sparkling”, “shimmering”. The river was formed by the confluence of two rivers - Tekes and Kunges, which originate in the mountains of the Northern Tien Shan. The bed of the Ili River has a huge number of channels, islands covered with bushes and reeds. The river, flowing into Lake Balkhash, forms a wide delta.

Not far from Almaty, Ili forms the artificial Kapchagai reservoir and then flows into Lake Balkhash. The Kapchagai Reservoir is often called the sea. The maximum depth of the reservoir is 45 m, width – 22 km. In the warm season, this is a favorite vacation spot for local residents. There are beaches, health resorts and boarding houses along the coast, and there is a water park in the city itself.

A few kilometers from the reservoir, on the right bank of the Ili, there is a place that takes us back to ancient times - this is a huge stone from which images of Buddha and bodhisattvas have been looking into the sky for many centuries. On the mysterious rocks you can see many preserved petroglyphs, late Buddhist inscriptions, images of deities, semantic meaning which still need to be unraveled - there are only about one thousand different rock carvings, which scientists date back to the late Middle Ages.

For novice tourists and lovers of active recreation, rafting on the Ili River is of great interest, when you can get acquainted with animals and natural world floodplains of the river. The thickets are home to many birds, including unique ones. This area also attracts fishing enthusiasts. Pike perch, catfish, carp, grass carp, asp, bream - all this can become an excellent catch for an angler.

Kurty is a river located in Almaty region, Kazakhstan. It is the last left tributary of the Ili River. Kurty originates on the northern slope of the Chu-Ili Mountains. It is very low-water and is used to irrigate the local fields. It feeds on rain, snow and groundwater. In the 90s, a dam was built on it, which formed the Kurtinskoe reservoir.

The length of the river is 125 km and the basin area is 12,500 km². Nowadays, it is the main waterway of southeastern Kazakhstan. The river received its name in honor of the Kurt dynasty, who ruled in this territory in 1245-1389.

Every year hundreds of tourists come here to go fishing or just have a good time. Please note that fishing requires purchasing a special license, this is strictly controlled by local security. Kurty is also a great place for swimming, although the water in the river is a little cold.

Chilik River

The Chilik River is one of the main water arteries Kazakhstan. Chilik, flowing through the Almaty region, is the largest river of the Trans-Ili Alatau, or Northern Tien Shan. The name of the river has Uyghur roots, and in translation from Kazakh the word “shelek” means “bucket”.

Chilik - typical mountain river with a large number of tributaries (about 50), with a rapid current and a fairly steep drop. In the upper reaches of the river, the width of the channel is 5-6 meters, expanding in the middle reaches to 10-15 meters, the greatest depth ranges from 1.5 to 2 meters. In the early 80s, Chilik was blocked with a 60-meter rock-fill dam with a length of 330 meters. This was the last large-scale project of the Soviet period, the “Big Almaty Canal” - this is how the Bartogay reservoir was formed, which was created to accumulate water and irrigate fields in summer time. It is included in the number most beautiful places Kazakhstan.

Two large faults stretch under Bartogay earth's crust, and along the entire gorge in the river and on its banks large stones and boulders are visible that have rolled down from the mountains - evidence of the numerous earthquakes that occurred in these parts. In ancient times, a glacier passed through these parts, the traces of which can still be read on the rocks. The Chilik River is very popular among lovers of water tourism.

Charyn River

The Charyn River, in the middle reaches - Kegen, in the upper reaches - Shalkudysu, is a huge water stream flowing in the Almaty region of Kazakhstan. This river has a stormy character, like most mountain rivers in Kazakhstan. It has a huge number of tributaries and also feeds precipitation, so the river is full. Closer to the lower reaches, the Charyn River subsides and becomes calm. It is here that the beautiful valley is located, picturesque and enchanting.

This aquatic beauty originates far in the mountains, on the southern slope of the Ketmen ridge; small tributaries feed it and make it powerful and full-flowing. In its lower reaches, its tributary Temirlik flows into it and it flows into the Ili River and total it travels a distance of 255 kilometers. Charyn forms several interesting valleys in the area of ​​the Kuluktau Mountains - this is a canyon 400 meters deep, in the area of ​​loose sediments of the Zhalanash depression - Aktogay, in the eastern part of the Toraigyr ridge - Kartogay Canyon and then Sartogay in the lower reaches.

Particularly attractive is the Kartogai valley, which means burial forest. This is a picturesque corner, amazing in its shapes and outlines, especially in daytime, when we can perceive all the play of colors surrounding us and truly appreciate the beauty of this magnificent place. The Charyn River is not only beautiful, but also useful, as it produces a huge amount of energy, which is why the Moinak hydroelectric power station was built on the river.

Turgen River

Turgen is a mountain river originating from glaciers high in the Trans-Ili Alatau mountains. The gorge through which the Turgen flows is considered one of the most picturesque in the Northern Tien Shan mountains.

In the floodplain of the river there is the Turgen Gorge. At an altitude of 1230 m, on the ninth kilometer along the Turgen Gorge, there is the Batan forestry. Clean and cold water from the Turgen River flows into the fisheries basins where trout are raised.

Today the Turgen River is one of the most visited tourist places. This is due to the fact that the gorge is located not far from Almaty and attracts tourists with a rich selection of entertainment. In the gorge you can visit a trout farm and an ostrich farm, take a photo with the huge figure of the Golden Man and the man frozen next to him snow leopard, visit an open-air museum.

Aksai River

Aksai is a river flowing in Kazakhstan. The right tributary of the Kaskelen River originates in the glaciers of the Trans-Ili Alatau. The length is 70 km. The width of the Aksai River valley is 8 meters, the average depth is 0.2 - 0.7 meters, the greatest is 1.2 m. The river and its tributaries are prone to mudflows. The largest mudflows were observed in 1921 and 1960.

Mount Akzhar rises between the valleys of the Aksai and Kargalinka rivers. As a result of the catastrophic earthquake on May 28, 1877, a huge collapse descended from the northwestern slope. Rock fragments - reaching 30 - 50 tons - formed a stone scree. Mount Akzhar is a watershed between the valleys of the Aksai and Kargalinka rivers.

Ili River

Ili is one of the largest rivers located in the Almaty region of Kazakhstan. It originates at an altitude of 3540 meters in the Tien Shan in China. Its source is located at the confluence of the Tekes and Kunges rivers. The length of the Ili is 1439 km, of which 815 km flows on the territory of Kazakhstan.

The river flows into the western part of Lake Balkhash and greatly desalinizes it. At its confluence, it forms a vast delta with permanent branches: Topar and Zideli, as well as many backwaters and small lakes. Ancient channels lie on the right side of the modern river, the largest of them is Zhanatas.

At the beginning of the 20th century, the river was a fairly busy route from western China. In 1729, a battle between the Dzungars and Kazakhs took place here. Today it is very popular among tourism lovers, especially rafting to Balkhash. On one of the banks of the Ili there is the Singing Dune - the famous sand mountain, and not far from it - the National natural Park Altyn-Emel, where the famous Przewalski's horse is bred in our time.

Chu River

The Chu River originates in Kyrgyzstan, but most of it is located in Kazakhstan. Part of the river, which is 150 kilometers long, serves as a kind of Kyrgyz-Kazakh border. The surrounding area of ​​the river delights the eyes of local residents and travelers every day with its unshakable beauty and uniqueness.

Chu River - natural wealth Republic of Kazakhstan. To say that there are a lot of fish in this river is to say nothing. It is literally teeming various types fish, which will undoubtedly appeal to any traveler keen on fishing. There are many species in the Chu River large fish, so if you are a lover of a rich catch, then leisure on this river is especially for you. Even if you are just a beginner angler, local fishermen are always ready to lend a helping hand and make you fishing fruitful and unforgettable. Every year, such a sport and active recreation as rafting is becoming more and more popular, and the Chu River has all the conditions for such rafting. The Chu River is an ideal vacation spot for both lovers of secluded fishing and fans of extreme sports.

Malaya Almatinka River

The Malaya Almatinka River is a large mountain river, originating among the ridges of the Trans-Ili Alatau. Flows through the city of Almaty, The largest city Kazakhstan.

The Malaya Almatinka River is more than 125 kilometers long - it is one of the largest rivers in the region. There are many attractions along the banks of Malaya Almatinka. In the upper reaches of the river there is a beautiful Tuyuk-Su glacier, very popular among lovers of mountain tourism. Alpingrad is also located there - a site for tent camps for climbers.

A separate attraction is the Mynzhilki dam, built to protect the city from mudflows. From the top of the dam there is a wonderful view of the river valley. Also in this area is an old hydrometeorological station, opened in 1936.

In addition, Malaya Almatinka is surrounded by magnificent wild nature and stunningly beautiful mountain landscapes. Along the river there are popular tourist routes, however, it should be remembered that this road is only for experienced travelers: the area here is picturesque, but completely uninhabited.

Big Almatinka River

The Bolshaya Almatinka is a river in Kazakhstan, flowing along the western outskirts of the city of Almaty. The river originates from two sources - powerful glaciers. The length of the river is 96 kilometers.

The river basin occupies several different natural areas: mountain, flat and foothill. The mountain zone forms the runoff, its upper part is made up of rocks, glaciers, and snow. Below are alpine meadows, conifers and deciduous forests. In the lower reaches, the Bolshaya Almatinka is divided into several channels. The river flows into Big Almaty Lake.

The annual melting of snow caps causes a large amount of runoff, which can cause mudflows. In 1980, a barrier against mudflows and floods was built in the river valley. The forty-meter dam has a huge mudflow reservoir.

To ensure the improvement of the river area, comprehensive measures are regularly taken to help reduce water pollution in Almatinka.

Topar River

Topar is a steppe river in the Almaty region, surrounded by several flood lakes. It is especially popular among fishermen and hunters, since these places are rich in game, and the river itself is rich in fish.

In order to fish or hunt in these places, you must purchase a license (a free biting calendar is attached to it). The rangers keep order in the area, check for licenses and are ready to help with advice if necessary. Carp, pike perch and crucian carp are especially good here. Under favorable circumstances, the catch size in one evening reaches fifteen kilograms.

The endless steppe stretches around, creating a feeling of solitude and detachment from the bustle of the city. Of course, before going fishing, it makes sense to stock up on repellent. Fishermen from all over the region come here along the Astana highway to enjoy the clean air, beautiful views and excellent bite.

Having a natural origin and characterized by a constant directional flow. It can start from a spring, a small pond, a lake, a swamp or a melting glacier. It usually ends by flowing into another larger body of water.

The source and mouth of a river are its essential components. The place where it ends its path is usually easy to see, and the beginning is often determined only conditionally. Depending on the terrain and the type of reservoirs into which rivers flow, their mouths may have differences and characteristic features.

Terminology

From source to mouth, the river flows in a channel - a depression in the earth's surface. It is washed away by a stream of water. The mouth of a river is its end, and the source is its beginning. The land surface along the flow has a downward slope. This area is defined as a river valley or basin. They are separated from each other by watersheds - hills. During floods, water spreads into depressions - floodplains.

All rivers are divided into lowland and mountain. The former are characterized by a wide channel with a slow flow, while the latter are characterized by a narrower channel with a fast water flow. In addition to the original source, rivers are fed by precipitation, underground and melt water and other smaller streams. They form tributaries. They are divided into right and left, determined along the flow. All streams that collect water in a valley from source to mouth form a river system.

In the riverbed there are deep places (reaches), holes in them (pools) and shoals (rifts). The banks (right and left) limit the water flow. If during floods the river finds a shorter path, then in the same place an oxbow lake or a secondary channel (branch) ending in a dead end is formed, which connects downstream with the main stream.

Mountain rivers often form waterfalls. These are ledges with a sharp difference in height of the earth's surface. In valleys near rivers with wide channels, islands can form - parts of land with or without vegetation.

Source

Finding the beginning of a river can sometimes be difficult. Especially if it flows in a swampy area and takes water from many of the same type of fickle streams or springs. In this case, the beginning should be taken as the area where the current forms a permanent channel.

It is easier to determine the origin of a river if it starts from a pond, lake or glacier. Sometimes two independent large water streams, which have their own names, join together and then have one channel throughout. The neoplasm has its own name, but the point of confluence cannot be considered the source.

The Katun River, for example, connects with the Biya, which is similar in size. For both, the point of confluence will be their mouths. From this place the river already bears a new name - Ob. However, its source will be considered to be the place where the longer of these two tributaries originates. The confluence of the Argun and Shilka rivers seems to give rise to the Amur, but to say that this is its source is incorrect. At this point, two rivers merge to form a new name (toponym).

Estuary

All rivers flow into a larger body of water. The places where they merge are easily determined. It could be more large river, lake, reservoir, sea or ocean. For each case, the mouth will have its own characteristics.

IN in rare cases the mouth of a river is the place where it ends, spreading over the surface without any new formation. Often earth's surface in such areas it has a minimal or reverse slope. In this case, the water slows down, seeps into the soil or evaporates (dry mouth). It also happens that its demand in certain regions is excessively high. Water is withdrawn for irrigation, drinking or other needs.

Given this, the mouth is the section of the river where it flows into another larger water body, ends up drying out naturally, or is spent on consumer needs.

In addition to the usual confluence of rivers, deltas and estuaries are distinguished separately. They differ in the degree of manifestation of sedimentary rocks at the junction of the riverbed and the reservoir. Deltas are characteristic of rivers flowing into lakes, reservoirs and closed seas of continental type. They are formed by several branches and ducts.

On the coasts of oceans and open seas, the river is affected by ebbs and flows. Streams of salt water prevent silt deposits from being deposited, the depth remains constant, and wide estuaries are formed.

At the mouths of rivers there is often a long bay - a lip. It is a continuation of the channel, stretches to the very point of confluence and has a large width. The estuary, unlike the bay, is also a bay, but shallower due to the deposited silt deposits. It is often separated from the sea by a narrow strip of land. Formed due to flooding of low-lying coastal areas.

Delta

The name comes from the time of the historian Herodotus. Seeing the branched mouth of the Nile River, he called it a delta, since the outline of the area resembled the letter of the same name. This type of river mouth is a triangular formation consisting of several branches branching from the main channel.

Formed in areas where river flow carries downstream a large number of sedimentary rocks. At the confluence, the flow slows down and particles of silt, sand, small gravel and other debris settle to the bottom of the riverbed. Gradually its level rises and islands form.

The water flow is looking for new passage ways. The river level rises, it overflows its banks, flooding and developing adjacent areas with the formation of new branches, channels and islands. The process of settling of transported particles continues in a new place - the mouth continues to expand.

There are active deltas characterized by abundant sedimentary processes. They are formed under the influence of counter flows of fresh and sea ​​water. Internal deltas, in fact, are not such and can be located far from the mouth upstream of the river. They also have branching branches and ducts, but they then merge into a single channel.

Estuary

If a river carries an insufficient amount of sediment into the sea or ocean, a delta does not form at its mouth. The influence of ebb and flow of tides also does not contribute to this. In the open seas and oceans where rivers flow, salty water, entering their mouths, forms a powerful stream and wave, which in some cases can go several kilometers deep, changing the direction of the main current. During low tides, the backflow of heavy seawater removes all sediment particles.

An estuary is a greatly expanded mouth of a river. Unlike the delta, it has an ever-increasing depth and a pronounced wedge-shaped shape. The stronger the impact of the tidal wave on the banks of the river, the more distinct the outlines of the estuary.

Lozva is the fifth longest with a length of 637 km and an area drainage basin 17 800 square kilometers. The channel passes through the swamps of the West Siberian Plain within the Garin and Ivdel districts and flows into the Tavda. Lozva is considered the most picturesque river in the Northern Urals and is of interest for fishing and water tourism.

The name of the river comes from the Mansi phrase "Lusum Ya", the etiology of which is unknown. This phrase indicates a large number of oxbow lakes and marshy meadows.

General characteristics of the river

The Lozva River flows from Lake Lunthusaptur, located on the eastern slope of Mount Ortoten. This place belongs to the Belt Stone ridge of the Northern Urals. The source is located at an altitude of 885.1 meters above sea level within coordinates 61°32" northern latitude and 59°20"E longitude.

Lozva is a left tributary of the Tavda and flows into it at its confluence with Sosva. The height of the mouth above sea level is 56 meters, and the coordinates are 59°34" north latitude and 63°4' east longitude.

The value is 1.25 m/km.

Geography of the river

The route of the Lozva River in the Sverdlovsk region affects both mountainous and flat areas. In the upper reaches, the water flows at the greatest slope until it reaches the foot of the ridge. Here the river changes direction from east to south.

Throughout Lozva, the speed of the water flow and the nature of the banks change, and therefore the river can be divided into several sections:

1. The first 3 kilometers from the source are treeless mountain tundra with dry banks, the current is fast.
2. Mountain taiga to the foot of the slope - slower current, dry banks with taiga forest /
3. A section with a calmer flow from the mouth of the Akhtyl tributary - the river acquires a flat character, the channel meanders with the formation of bays and oxbow lakes, damp banks and marshy areas are periodically encountered /
4. Area with mountain current - characterized by steep banks, which in some places form canyons/
5. The flat part of the river (from the village of Burmantovo to the mouth of Lozva itself) is characterized by a slow flow, the channel meanders among swamps and forests, forming a large number of oxbow lakes along the way.

Below the confluence of the Ivdel, the Lozva River passes through a narrow (about one and a half kilometers) valley with steep steep slopes, among which there are rocky slopes 30-80 m in height. With access to the West Siberian Plain, the floodplain expands to 2-4 km, and the width of the river valley reaches 4-10 km.

There are no lakes or reservoirs along the route of the Lozva River.

Settlements

The following settlements are located on the banks of the river:

• Horpia.
• Pershino.
• Lycia.
• Winter.
• Ivdel.
• Shaburovo.
• Mityaevo.
• Burmantovo.

Most of the river basin is located in uninhabited or sparsely populated areas, which creates a favorable environmental situation.

water pool

The Lozva River has 45 tributaries, among which the main ones are:

• Auspiya.
• Vizhay.
• Ivdel.
• I drank.
• Sulpa.
• Manya.
• Colpia.
• Harpy.
• Ushma.
• Big Eva.
• Pynovka.
• Northern Toshemka.

Tributaries flowing into the mountain and foothill parts of the river are characterized by very clean cold water and rich ichthyofauna. Some rafting routes pass not only along Lozva, but also along Vizhay, the bed of which passes through picturesque natural places.

Characteristics of the channel

Average depth the river is one and a half meters. On the rifts it is very small (0.3), and on the reaches it varies from 2 to 2.5 m. The deepest areas are the river holes (up to 6 m). The width of the channel is 30 meters in upper reaches, 60 - in the middle and 80 - in the bottom. The river bottom is predominantly rocky and pebble with occasional muddy or sandy areas.

In the mountainous section (from the upper reaches to the village of Burmantovo), the riverbed has many rifts, holes and rocky outcrops. It is in this part that the Vladimir rapids are located, which are especially difficult for rafting. The section of the river between Burmantovo and Ivdel is calmer. Riffles, pebble reaches and rocky outcrops are much less common here, but they still exist.

The flat part of the channel (from Ivdel to the mouth) is the longest and deepest (2-3 meters). Reaches and pits are more common here. In this section, the channel is very winding and washes away the banks at turns, forming barks and tree debris. Plain Lozva has many branches and oxbow lakes.

Hydrology

The Lozva River is characterized by mixed nutrition (the main source is snow). The average annual water flow measured 37 kilometers from the mouth is 135.3 m³/s. average speed currents excluding riffles vary from 0.5 to 1.2 m/s. The annual flow volume is 1,973 cubic kilometers.

The river freezes at the end of October. Ice drift begins in the second or third month of spring. Lozve fluctuates significantly throughout the year. The flood is extended and lasts from May to July. Floods occur due to rains in late summer and autumn. The difference between the maximum and minimum levels of the Lozva River in the upper reaches is 2-4 meters, and in the lower reaches - 7-8 m.

Nature

The nature of most of the floodplain of the Lozva River is represented by taiga forest typical of the Northern Urals with small inclusions of deciduous trees (cedar, linden, larch, aspen). In the upper reaches along the banks there are alpine meadows.

The river itself is quite beautiful, with a wide channel and very clean water. The coastal forests are full of game, berries and mushrooms, making Lozva suitable for periodic stops during rafting, which can be occupied by fishing, gathering or hunting.

Coastal fauna

The fauna of Lozva is typical of a taiga forest. Of the wild animals there are:

• Brown bear;
• marten;
• reindeer;
• elk;
• wolf;
• raccoon dog;
• hare;
• roe;
• boar;
• fox;
• flying squirrel (rare Red Book species).

The bird fauna is especially rich, the diversity of which includes more than 130 species.

Ecology

Currently, the ecosystem of the Lozva River is almost untouched economic activity person. There are very few located along the coast settlements, as a result of which the water is not subject to significant contamination.

Main ecological problem Lozva is a fishing pressure that has led to a significant decrease in ichthyofauna populations. In this regard, fish farms were organized in the upper reaches, and bans were introduced on catching taimen, sturgeon and whitefish from the Red Book.

Alloy

The nature of rafting on the Lozva River depends on the height of the launch. The latter can be done in three ways:

• on a motor boat;
• by helicopter (landing on the ridge);
• on foot (the most extreme option).

The minimum length of the route is 7 kilometers, and the maximum is 307. The most popular and longest rafting runs from the mouth of Ishma to the village of Burmantovo. If desired, it is possible to continue the route to the confluence of the Ivdel tributary and below, but here the river becomes flat and the flow is much slower. In the presence of a headwind, rafting in this part of the channel is difficult.

Multi-day routes are very common, interspersed with overnight stays on the shore and fishing. Water tourism in Lozva is very well developed.

The rafting route is classified as the first category of difficulty. Obstacles on the way can be rapids, rubble and “combs” (typical of the upper reaches). The most difficult to pass is the Vladimir roll.

Fishing

The Lozva River is very rich in ichthyofauna and therefore favorable for fishing. The following fish species live here:

• gudgeon;
• dace;
• roach;
• tugun;
• pike;
• burbot;
• nelma;
• taimen;
• Siberian sturgeon;
• sterlet;
• common perch;
• Siberian grayling;
• Demoiselle minnow.

The river has long established itself as a very fishing place, but for the same reason it became an object for mass fishing and poachers, which led to a significant decrease in the number of representatives of the ichthyofauna typical of Lozva. The restrictions introduced by the government have not yet corrected the situation. Currently, fishermen are noticing a significant decline in the size and quality of their catches.

Fishing Features

Depending on the location, there are three types of fishing on the Lozva River:

• on the upper mountain site;
• in the upper foothills;
• on the plain (in the middle and lower reaches).

These fishing spots differ in the types of fish and the size of some representatives. Thus, in the lowland part the pike is much larger (up to 20 kg) than in the upper reaches. Whitefish and sturgeon are found only in the lower reaches.

The first and second areas are inhabited by species that prefer cold mountain waters (grayling, taimen, etc.). Plain Lozva abounds in fish such as ide, dace, nelma, tugun, ruff and perch. IN summer period some species migrate upstream.

Currently, fishing on the Lozva River is only possible with vouchers, and fishing for taimen, grayling and whitefish is prohibited.

The main season begins at the end of June after spawning. At this time, there is a very good bite on the river.