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Sea of Azov. Sea of Azov: Corinth of power, walking and Glibin of the Sea of Azov

Sea of Azov (Ukrainian Sea of Azov, Greek Μαιῶτις λίμνη, Latin Palus Maeotis) is a semi-enclosed sea of the Atlantic Ocean at the descent of Europe. Found the sea in the light: the glybin does not change 13.5 meters, middle glybin close to 7.4 m (from 6.8 to 8 m).

The Sea of Azov is surrounded by the Atlantic Ocean by a small line and sea (Kerch channel - Chorne sea - Bosphorus channel - Marmurov sea - Dardanelli channel - Egeyske sea - Seredzemne sea - Gibraltarsku channel - Atlantic Ocean).

Two most rivers flow into the sea - and the river Kuban.

THE COAST OF THE SEA OF AZOV I DELTI RIVERS

uzberezhzha Sea of Azov mensh malovnicho і profitably, nіzh Chornomorske. Ale є і has its own unique beauty. Vrytul up to the sea steppe, and the thickets outlined flowing in small parts. Take care of the poor, the stench is either low and flat, with a perennial turtle beach, or poor, albeit ovist, stacked with still forest-like loams. The coastal line of the sea makes it possible to finish the smooth vigini, and only when the food is mowed to give the deyaku ruggedness. There is a great number of cis - one c characteristics shores of the Azov Sea.

Went Uzbek.
The western coast of the Azov Sea of performances with a long scythe - the Arabat Shore. Vona vyyagnula uzdovzh the coast of the sea for 112 km, all the way from the new watercourse Sivash. The width of the whole flat grass-turtle mows ranges from 270 m in the middle and middle parts to 7 km in the small mountains.
Arabatska strelka is a magnificent natural beach. At the same time, a row of dovgy milens was stretched. You can wonderfully see the walls of the old Genoese fortress, roztashano near the village of Arabat, or right from the deserted rocky coast. vuz'kim bіlim greedy. Roll on to the krill, skim low over the water of the seagulls. In the distance, on the spit, it glitters through the interchanges of the hot sun of the vidobut from the Sivash sil. Beautiful sea in a storm. If dme lyutii Nordost, it’s dark, we will suvorim.
With angry noise, boiling white pinoy, steep-walled khvili fall on the shores. We can spend many years running through the sea space, with a strong big and boisterous surf.

If you have a people who have seen the Sea of Azov, you may have lost a spogad about him with an uncomfortable, ale sickly soul of beauty.
on Arabatskiy striltsi see the hot mineral water behind your chemistry warehouse and political authorities overturn the matsestinian. On the basis of the flowing waters, a new resort - Azov Matsesta - is transferred.

Pivdenne Uzbek.
It is presented by the territory of the Kerch and Taman pvostrovs, and between the two grows to the Kerch channel, which is Chorne sea... Kerch pіvostrіv є the dark edge of the Crimea. The area of yogo is close to 3 yew. Sq. kilometers. At the nadra of the pіvostrov, there are great genera of zaliznyh ores, which help to live the metallurgy of Priazov, naphtha and natural gas.
Pivnichna і pіvnіchno-skidna parts of the Kerch pіvostrov stored with marls, clays, vapnyak; Most of the time, there are the trials of the third party.
Zakhidna chastina Kerch p_vostrov is rivninn, skhidna is a hunchback. At the border of the pіvostrov, the pivdenny shore of the Azov Sea is steeply shaved in the sea, and the beach is covered with smog. By means of the misery of the shores of the banks, folded with bryozoans, it is easy to repair the onslaught of seaweeds. Such, for example, is Ms. Kazantip, which is based on a bryozoan reef - atoll. At the end of the city - the Arabat inflow, on the road - Kazantipskiy. On the slope towards the Kazantip Misu, the low-lying alluvial delineation of the coast stretches. Yuzhneemisa Kazantip - Aktashske Solone Lake. Central lake. Vono is a surplus of Kazantipskogo inflow, prick far into the land.
In the middle of the Kerch p_vostrov, from the approach to the skid, there was a simple Parpach crest. Mіzh cim comb і by the coast of the Azov Sea. The valley is wider later. In the lower parts of the її salt lakes, and the withers are dominated by their dominant authorities, the Chokrakskoe Lake, as well as a number of mud volcanoes.
At the turn of the Kazantipsky inflow, near the Kerch-channel, the coast of the Azov Sea is more quiet, but here for a new characteristic mix, folded with solid bryozoans, for example, Misi Zyuk, Tarkhan and others.

The Kerch channel, which is close to the Chorne and the Sea of Azov, is not wide and sometimes not wide. Its width varies from 4 to 15 km. Dovzhin channel - 41 km. Glybin to become close to 4 m.
At the old Kerch channel, it was called Bospor Kimmeriyskiy. In the very name, it takes a stretch on the shallowness of the channel, since "Bospor" in the translation to Russian language means "scourge brid".
Krims'kyi shore of the channel with m_stsy obrivisty. Near the second part of the city, the misto-port of Kerch has sprung up.

The Caucasian coast of the Kerch channel is low, with food, mice and dunes. The fairway of the channel will seize the reefs, the mows and the coastal mile, which earlier accelerated the navigation. Now for the passage of ships with a great draft in the prototypes of the canal.
Previously through the channel between the Crimea and the Caucasus, it was transported by great steam floats, which transported vantages and passengers. Sheds 1955 to the rock bulo vіdkrito zalіznichna ferry. On the Crimean birch tree, on the winter skid from Kerch, the landscape station Krim was prompted, and on the Caucasian birch tree, on the braid Chushka, the out-of-the-way station Caucasus was built.

On the great diesel-electric passages, it is easy and fast to be transported across the Kerch canal. Zaliznichny shlyakh mіzh Krim and the Caucasus with the most significant speed.
Tamansky pіvostrіv, which is є part Krasnodar Territory, Borrowing an area of approximately 1900 sq. km. From them, trocha more than 900 sq. km, and the sieve of the territory is estuary and smooth.
Yogo's nature is wild. From the geological point of view, there are young birds, as it was formed in the quarter period. Even in the 1st century AD That is, on the last day there are five islands close to five, the re-incarnation of some of the islands in the city, Mabut, in the 5th century. That is, before the accumulating accumulative activity of the rivers of Kuban, mud volcanoes and tectonic growths. Tamansky p_vostrov trivaє.

The upper part of the pіvostrov is a humpbacked ryvnina with low dome-shaped temporal ridges, twisted at the viglyadі of the distant ridges from the beginning of the entry to the pіvnіchny skіd. There are mud volcanoes and ancient burial grounds - burial mounds everywhere. .Landscape is full of estuaries. Widely widened and flowing, overgrown with outlines and sedge.

Tamansky pyvostrіv revenge in its nadra such natural resources, such as naphtha, combustible gases, zaliznі ore, Sil, awesome materials in viglyadi vapnyak, clay and gravel.
Climat p_vostrov is also warm. The dream is generously supplied with warmth of its exchanges, ale fell off here, it is not big - only 436 mm on the rik - and that is a marriage of a vologue.
On the pіvostrovі - dear chernozem and chestnut soils, cover the dry steppe, and along the valley of the rivers of Kuban - flooded dew.
Be famous for its vineyards at once.
Take care of the Tamansky pivostrov to reach the versatile, but also to cross two types of banks: high, steep - abrasion, to be done as a result of the ruinous robots of sea needles, and low, flat - accumulative. The rest were formulated from the food-clayey contribution as a result of the activity of sea needles and leaks.

The coast of the Taman inflow, from the Tuzla Misu all the way to the village of Taman, along the slopes. In the middle height, it rises from 15 to 30 m here. shidny uzberezhzh inflows. Just shave it off with little mischief, and that is often for a rakhun of the cultural ball of the old-time Fanagoria.
The pivnichny coast of the inflow is also carried out and it is steeply shaved to the sea.
"Accumulation" in Latin means "accumulation". Tsim terms in geology mean the process of adding fluffy material to a growing environment.

Scythe Chushka, stored in the world of quartz sand and broken turtle, on the low coast.
The bank of the Tamansky Piostrov is far away in the skid (up to 50-60 m above the ditch of the Sea of Azov) and often has a subdued character. Wines are stored in the main forest-like clays and swampy sands on the beach, which can be stored in clay-clays, in small pieces with houses of turtles, pebbles and crushed stone.
Then, right up to the village of Golubitskaya, the coast of the Sea of Azov either goes down or starts to move, ala, repairing from the village, the wine becomes low, and in the area of the delta of the river Kuban the swampy character is swampy.

Quite simply, in the area of the Kuchuguri settlement on the low birch of the Sea of Azov, green trees are more likely to form a relief near the small (1-3 m) humpbacks - the dunes, which were made in the middle of the winter.

The visual memory of the Tamansky Piostrov is the mud of the volcano (salsi), which can be found up to 25. Bagato from them can be seen in small cones with steep peaks. Deyakі salzi team doesn’t work for hours. Reshta sees brood and gas, such as methane, nitrogen. carbon dioxide gas, Oxide in coal, sirvodden, water.
The lurch of mud volcanoes is the lingering of the spoky and the inaccurate, but some of the lingering of the volcanoes, the way it is super-vibrated, and the products of volcanic activity are thrown up and out of the way for hundreds of meters.
Velmi Tsikave is a manifestation of mud volcanoes at the bottom of the Sea of Azov near the shores of the Tamansky Piostrov. So, the intensive mud volcanic activity was spasmed not far from the village of Golubitskaya. One of the pinnacles is assigned to the 6th month of 1799 rock. Feeling the hum of the ground, then the thumping sound of the thunder over the sea, about 300 meters from the shore, a stop was made from the fire and the black dim. Nearly two years ago, the vyverzhennya was trivial, which led to the establishment of the island with a brood with a diameter of 100 m and a height of up to 2 m.
Some variations were repeated and for the last time - in 1862, 1906, 1924, 1950 and 1952 rock. In 1952, at the end of the village of Golubitskaya, 5 km away from the coast, also as a result of mud volcanic activity, after the establishment of muddy islands, it was raised with sea bites.

Skhidny coast of the Azov Sea
The skidny coast of the Sea of Azov, from Temryuk to Primorsko-Akhtarsk, on a stretch of about 100 km is a low-lying delta of the Kuban river with numerous estuaries, channels, great floodplains, overgrown with outlines and sedge. Richka Kuban, shores an ear of ice in the Elbrus mountains, one of the largest and most abundant rivers in the Pivnichny Caucasus. Dovzhina її - 870 km. The area of the water intake pool is 57,900 sq. km. Delta її established itself on the site of the Azov Sea, deeply into the land. Tens of thousands of rock in that tsyu inflow prostyagavsya until that time, de at a time to be found Krasnodar. The majestic Bula lagoon is rimmed by the slope towards the sea and is gradually filled with river sediments. Therefore, the role in the form of the western-western part of the delta was played out and the activity of mud volcanoes (salzi) of the Tamansky Pyostrov, which is often a view of the archipelago of other islands. Products from the mud volcanoes carried the channels along the islands and filled the stepwise lagoon.
The formation of the delta is trivial in our hour, moreover, it is seen that the warehouses at Achuyvo are 5-6 mm for the rik, and in the middle of the deltas - 3 mm for the rik.
Richka Kuban to wine well in the Azov Sea in the middle 11.4 billion cubic meters. meters of water, to avenge 3 million tonnes of disclosed rivers and massu muty. The water in rіchtsі is muddy tsiliy rik It is especially rich in deposits during the floods, which in the Kuban tend to be in the middle of 6-7 on the river. The initial number of the winners of the firm rychkoyu hard words (so the titles of the hard stick) become 8.7 million tons per rik. To transport such a vantage, it would take 52,000 freight wagons. For rakhunok tsikh nosіv іde growing delta Kubanі. Infected Kubanska delta, which will borrow an area of 4300 sq. km, repair at the so-called Raz-der, close to the place of Slov'yansk, de-Kuban go to the right (at the beginning) a branch of the Protok. The remainder takes nearly 40-50% of the Kuban water and flows into the Azov Sea near Achuyvo.
Nizhche Protoki, not far from the girla, Kuban is divided into a number of sleeves, with the most important ones - Petrushin sleeve and Kozachiy Urik. Petrushin sleeve, which represents a ship-floating route here, the river bed of the Kuban river, where it flows into the Sea of Azov.

The Kozachiy Urik is the left bank of the Kuban, which carries its way to the great Akhtanizovskaya estuary, which has a link to the Sea of Azov through the Peresipskoy girlo.
The current delta of the Kuban rivulets is a labyrinth of shallow lakes, or estuaries, which are located between the channels, or, in a local way, rykami, which create chimeric loops between dry lowlands of swamps.
At the delta of the Kuban, the majestic areas are occupied by floodplains, which stretch for tens of kilometers. The floating deltas of the Kuban, which adjoin to the Sea of Azov, are called Priazovsky. The stench is dismembered by the river Protoka into two massifs: on the water of the Azov floodplains in the backward part and Angelina-Cheburgolsky in the backward part.
Priazovskiy smooth - the chimeric labyrinthine pains and estuaries of growing size, with spicy, semi-salty and salty water, thickets of above-water and underwater dewline. Sered perevazhayut delineate, delineate, sedge, horny and izhachogolivnik. Pidvodna, or "myaka" the height of estuaries - the price of water growth, rdesti, kushir, latattya and ін.

Near the Azov estuaries, there are overgrowths of a wonderful roseline - a lotus. At the time of blooming, over the crisp emerald leaves, they are fed on the stalks of the great rush of divine beauty, as they develop a strong aroma. Tsey tropical newcomer, deliveries to us from Africa, - corisne Likarska and kharchova Roslin.
Limani delty Kuban bagati for riba. There are more than 70 species here, including battering ram, lash, pike perch, puss, sprat, carp up to 15 kg, catfish up to 100 kg.
Near the floodplains and estuaries of the delta, there are many birds, especially waterfowl: wild geese, jock. There are a number of colonies of cormorants and pelicans. Swans, chapli, and abundant hizhikh birds live here. There are numerous foxes, wild cats and wild boars can be seen in deaf floodplains. Muskrat has been acclimatized, which is even brownish.

Nadra delty bagati on korisny kopalini - natural gas, naphtha, mineral waters.
A large part of the delta of the river of Kuban has not yet been mastered in the Sylkopodarskiy vіdnoshennі, I want the soil here velmy rodyuchі.
Ale stephovo Priazov's landscape. In the floodplains, the old lines and rotten estuaries are replaced by a lot of kilometers, even to stretch the blaky squares of rice checks. In 1952, the rotsi bula was introduced into the Kubans'ka zroshuvalnaya system with an area of 23 yew. Hectares. In 1967, there were 62 yews occupied by rice. Hectares of land doubled by meliorators near the floodplains. As soon as Krasnodarskoe vodoskhovishche on the river Kuban grows, rice fields expand to 250-300 yew. Hectares and will give our Batkivshchyna a choric rate of up to 700 thousand. Tons of high-yield rice.

At the pivnich from Primorsko-Akhtarsk, right up to, smoothly, there are no more in the arms of the steppe Azov rivers - Beisug and Chelbas.
The shores of the Sea of Azov are presented at the end of the day with low and gentle sloping braids, the small coast here is fast, or it descends steeply to the sea. Deposits of wines, as it is on the coast of the plain, forests and forest-like loams and clays of the late ice hour. The forest is a breed, it is easy to grow up and down, and the coast of the sea here quickly falls apart. The average speed of the route along the entire Uzbek road is 3 m in the river. The maximum is up to 18 m. The runt of the central part of the Priazov region is represented by carbonate western Ciscaucasian fertile chernozems. Earlier, the whole region was covered with a coppice-grass steppe, herds of wild horses-tarpan and herds of pond-footed saigas grazed on yak. We were able to navigate the moose. There are no earths of roses, and a drop here [there is a green sea of hlibs, fields of corn and a dormouse.
In addition to the rivers of Kuban, in the Sea of Azov, such steppe rivers immediately flow into the Sea of Azov (rakhuyuchi from pivday to pivnich), yak Kirpa, pour their water into the Kirpilska estuary; Beysug, which flows into the Beysuzky estuary; Chelbasa, which flows into the Solodky estuary; Її, foolishly drive into the great Uysky estuary, і, nareshty, small rivulets Mokra Chuburka і Kagalnik, which flow into the Sea of Azov without a second.
Characteristic is the peculiarity of the landscape of the shady Uzbek coast of the Azov Sea, which has already meant a vishche - the appearance of numerous estuaries.

Delta Don.
At its own private-social part of the Azov Sea, there is a great, strong Taganrozka inflow, into which one of the largest rivulets of the European part of the SRCP - Don, falls. Dovzhin yogo to become 1870 km, and the water intake area is 422000 sq. km. Don is chorіchno to wine in the sea in the middle close to 28.6 cubic meters. km of water. Significant mass of river water strongly delineates the Taganrozka inflow, and pour the water with a small amount of water and lead up to, which occupies an area of 340 sq. km. The current Don delta is repaired 6 km downstream of Rostov-on-Don, there, across the river to the right, there is a non-floating arm of the Dead Donets.
Don’t make a great life on the river; up and down over the course of the flow of business and numbers to the court. Spokіynu smooth surface can rostinayut passenger ships, vantage ships and ribal boats.
The lower stanitsa of the lizavetinskoy Don began to wind heavily along the wide low-lying valleys, breaking down on the numerical arms and channels, which, in a local way, are called rikami. Tsikh sleeves and erikiv grow ever larger in the world closer to the Sea of Azov.
The landscape here is free. Everywhere you can see the island, weakly hanging over the water, with chimerically porous shores, in the thick thickets of the outline. Ostrіvtsi, close to the sea, are gradually flooded with sea water, and there is not even a small grain on them. 100 km up the hill over the course.
Shidnі vіtri, how to bleed downstream Don nadaut vorotnuyu dіu. The water is bustling, besides, it is very strong, but not only the sleeves of the rychka, but the Taganrozka inflow, which will ruin the normal navigation. The amplitude of the malignant manifestations should become +3, -2 m.

Don wine in the sea in the middle is close to 14 million tons of broth and close to 9.5 million tons of mineralized rivers. For the rakhunok drift in the depths of the Don Delta, step by step all the distance in the sea hangs out about 1 km on the capital.

Pivnichne uzberezhzha
Pivnichne of the Uzbek Sea of Azov stretched out from the hand of the Don to the place of Genicheska. A number of small rivers flow into the sea in the Azov Sea. Beruchs on the cob in the winds of the Donetsk ridge, carry their waters into the sea, the rivulets Mius and Kalmius. Rivers Berdya, Obitochna, Korsak and a number of other rivers flow in the Azov Sea, flowing in the Azov Sea, and a number of other rivers that cross the rivers. mow with your own fineness to zaginayutsya on the west, for example, Kriva, Bilosarayska (for the first time from the city of Zhdanov), Berdyansk (at the place of Berdyansk).

Between the braids and the root coast, there are inflows and estuaries, for example, Berdyanskiy and Obitochna. As soon as the mows are turned on, the whole northern coast of the Sea of Azov is a steppe, which goes down to the sea with a cliff. Kosi and vuzka coastal smuga are stored in the main quarter naval inserts. At first glance, the valley is stored by forests, forest-like loams and clays in the late ice hour. On the cich rocks, rody chornozems have grown. Still in the last century, there was a lot of green grass and fescue, and in the last half, there was a grass and fescue steppe. They grazed tarpani, wild camels, and even earlier they began to see noble deer and elks. There were beavers near the small dogs. At the time of the flowering of the steppe, beyond the Vistula of M.V. Gogol, they represented a green-golden ocean, which vibrated by a few million squares. However, these steppes have long been familiar, the stench will grow more roseorani. Oh, they changed the uninterrupted fields of wheat, corn, dormouse, fruit gardens and vineyards.

THE NATURE OF THE SEA OF AZOV
The Azov sea is a wonderful and miraculous one near the bagatokh in the water. Look, those who have chosen the Radiansky Union from all the seas, but for their significance in the people's statehood stand not for the last moment. Yogo square, bordered by parallels 45 ° 16 "s. Ш. I 47 ° 17" s. latitude and meridians 33 ° 36 "E і 39 ° 21" E Warehouse total 37800 sq. km (without Sivash and estuaries). I do not cross 14 m, and the average depth is close to 8 m. When the depth is up to 5 m, it occupies more than half of the Azov Sea. The amount of money is also small and becomes 320 cubic meters. km. For example, for example, the Aral Sea perevyshke Azov by 2 times in area. The Black Sea is 11 times larger than the Azov Sea in area, and 1678 times beyond the general area. And all the same, the Azov Sea is not so small, on the new one two states of Europe, like Netherlands and Luxembourg, have been spread out. Yogo nibil'sha is 380 km long, and the nibil'sha width is 200 km. The initial length of the coastline of the sea is 2686 km.
The water relief of the Azov Sea is even more simple, the depths of the sea in the main and smoothly grow into the world from the distance to the shores, and themselves great glibini located in the center of the sea. The bottom is flat. The Sea of Azov has established an inflow, with the largest ones being Taganrozky, Temryuk and strongly reminiscent of the Sivash, which is the best in the estuary. Great islands on the whole sea of the Germans. Є a number of miles, partly flooded with water and roasted near the shores. Such, for example, the islands of Biruchiy, Turtle and іnshі.

THE HISTORY OF THE SEA OF AZOV
Meotida
The long-standing Azov Sea did not wither, and the Don, flowing at the Chorne Sea into the region of the bitter Kerch channel. The theory of the Chornomorsk flood has been transferred, and the reserve of the Azov Sea water has become close to 5600 r. BC e.
In antiquity, the Sea of Azov was called by the Greeks Meotiyske lake (Greek Μαιῶτις), by the Romans Palus Maeotis ("Meotiyske swamp"), by the Scythians Kargaluk, by the Meots Temerinda (which means "mother of the sea"), among the Turks - Bahr-el-Assake or Bahr-i Assake (Dark Blue Sea; such tur. Azak Denizi) and also - Balisira, among the Genoese and Venetians - Mare delle Zabacche.
The sea has been renamed bagatorazovo (Samakush, Salakar, Mayutis, etc.). On the ear of the 13th century hardened the name of the Saksin Sea. The Tatar-Mongolian conquerors reopened the collection of the names of Azov: Balik-Dengiz (Ribne Sea) and Chabak-Dengiz (Chabachye, Lescheva Sea). For deyakim danimi Chabak-dengiz as a result of the transformation: Chabak - dzibakh - Zabak - azak - aziv - the name of the sea has been changed (summarily). For інshih danimi Azak - Türkic prikmetnik, which means low, lowland, for іnshi danimi, Azak (Türkic girli rychki), which was transformed into Azau, and then in Russian Azov. At the prominence of the Vishchevkazan, the name of the sea rimmed out as follows: Barel-Azov (Dark blue river); The Frankish Sea (before the francs came to the senses); Surozke sea (Surozhem calling himself a lucky place Pike perch in Krima); Kaffa Sea (Kaffa is an Italian colony at the place of Feodosia in Krima); Kimmeriyske Sea (from Kimmeriytsiv); Akdeniz (Turkish, which means Bile sea). Naybіlsh vіrogіdno, so the name of the sea is to resemble the place of Azov.

There are a number of hypotheses behind the etymology of the word "aziv": on the name of the Polovtsian prince Azum (Azuf), who was killed when the place was taken in 1067; for the name of the tribe of the Wasps (Asi), in their own devil, which became nibito from the Avestan, which means "shvidky"; I will name it in the Türkic word azan - "lower", and in the Circassian uzev - "neck". Turkic, the name of the place of Azov is Auzak. Ale shche in the I st. n. e. Plіnіy, pererahoyuchi in their ancestors Scythian tribes, zgadu tribe Asoka, similar to the word Azіv. Accepted respectfully, the name of the Sea of Azov has come to the Russian toponymy on the ear of the 17th century. Moreover, a collection of wonders only started behind the yogo part (Taganrozkiy zakokoyu, which was called Donskiy Liman before the place of Taganrog appeared). Only in the other half of the 18th century, the name "Sea of Azov" has closed behind all the water. The sea gave the name to the villages of Azov and Priazovskaya, and the towns of Azov (in the lower rivers Don, Rostov region), Novoazovsk, the village of Priazovske and other settlements.

In the history of the Azov Sea, there are three stages:
Ancient (geographic) - from the hours of Herodotus to the ear of the XIX century.
Geological and Geographical - XIX cent. - 40th rock XX century
Complex - mid XX century - Christmas.
I am reading the map of Pontus Evksinsky and Meotidi sklav Claudius Ptolemy, in the same name geographic coordinates for mіst, girla rychok, misіv and outflow of the Uzbek Sea of Azov.
In 1068, the Russian prince Glib Svyatoslavich, who ruled at that hour in Tmutarakan, moved across the ice to see Kerch and Taman. It was written on the Tmutarakanskiy stone, the distance from Tmutarakan to Korchev (the old name Kerch) became approximately 20 km (for 939 years it was 3 km higher). The Genoese and the Venetians have begun to store the portolans (pilots and sea maps) of the Black and Azov Seas.

GEOGRAPHY OF THE SEA OF AZOV
The extreme points of the Azov Sea lie between 45 ° 12'30 "and 47 ° 17'30" Mon. latitude і між 33 ° 38 '(Lake Sivash) і 39 ° 18' n. dovgo ti. Naybilsha yogo length 380 km, width 200 km; additional coastline 2686 km; surface area - 37,800 km² (the area does not include the islands and kosi, which occupy 107.9 km²).
For morphological signs, it is carried to flat seas and is a shallow water with low coastal grapples. Outside the ocean, the Azov Sea is the continental sea of the planet itself.
During the wintering period, it is more frequent, or outside freezing, when there is a lot of ice to wine in the Chorna Sea through the Kerch canal. As a rule, ice-making is typical for the snow, albeit in cold rock, maybe a month earlier.

Map of the Sea of Azov

The sub-water surface of the sea is somewhat simple. Near the world to the distance from the coast of the mountain, it grows gradually and smoothly, reaching 13 m in the central part of the sea. The main area of the bottom is characterized by 5-13 m. The growth of isobaths, close to symmetrical, will break down a small species of femininity on the winter descent towards the Taganroz inlet. The distance of 5 m grows approximately 2 km from the coast, from far away from the nearby Taganroz inflow and into the very place of the Don. At Taganrozkiy glibini, it grows towards the Don's hand (2-3 m) right up to the upper part of the sea, reaching 8-9 m on the cordon outlets from the sea. the backwater (banks of Morska and Arabatska) Uzbek, the glides above the yaks change from 8-9 to 3-5 m. pidvodniy grabbed up to 11-13 m glybin.
The water intake area of the Basin of the Azov Sea is 586,000 km.
sea coast in the main plane of food, only on the forest birch, there is a burgeoning of volcanic trekking, as in a few moments it passes into the steep front of the mountains.
sea flows to be found in the wilderness of the darkness here is even worse than the strong winter-dormant and early-western winds, and to that end it often changes directly. The main plane is the circular current of the shores of the Sea of Azov against the godinnikovo line.

salinity
The salinity of the Sea of Azov in the XX century
Hydrochemical peculiarities of the Azov Sea are formed in the Persha of Chergu under the inflow of ryas flood of river waters (up to 12% of the water supply) and difficult water exchange with the Black Sea.
The salinity of the sea before the regulation of the Don Bula is three times less than the average salinity of the ocean. The value of її on the surface varied from 1 ppm in the Don River to 10.5 ppm in the central part of the sea and 11.5 ppm near the Kerch Channel. As the stem of the Tsimlyansk hydroelectric node started, the salinity of the sea began to grow. BEFORE 1977 p average salinity the sea increased to 13.8 ppm, and in Taganrozkiy zatotsi - to 11.2. In the large water area of the sea, the water is saline up to 14-14.5 ‰. In the period of an altogether high salinity (1979-1982 rock), the salinity was reduced to 10.9 ‰, even up to 2000 ї, the value of the newly matured and stabilized at 11 ‰. The mid-season number of salinity values is very close to 1-2 hectares.
At the private part of the Sea of Azov, the water has much less salt. For this reason, the sea is easy to freeze, and before the appearance of the krigolami, there will be no boats from the chest until the middle of April. The small part of the sea does not freeze and doesn’t have a peaceful temperature.
Throughout the XX century, practically all big-mensh big rivers that flow into the Sea of Azov, bully barred by rowing for the stem of water reservoirs. Tse summoned up to a significant speed to skip the water and mule in the sea.
The main water storage in the open sea part grows out of the salt storage to the ocean as a common cell of ions in chlorine and sodium and moving in the place of re-transporting components of land waters - calcium and carbonates.

Visibility and color of water
The transparency of the waters of the Azov Sea is low. Vona is not the same in the rural areas and in the winter when the rock is going and it rises in the fringes from 0.5 to 8 m. Naymensha's vision is promoted in Taganrozkiy zatotsi (0.5-0.9 m, height up to 2 m). The color of the water here changes from greenish-yellow to brownish-yellow. In the remote and remote areas of the sea, there is a clear view of the sea - in the middle 1.5-2 m, or even up to 3-4 m. sea waters the penetration of the water is from 1.5-2.5 to 8 m. The water here is greenish-blakite. A bit of discernment grows everywhere, ale in some small seas, as a result of a tumultuous development in the upper balls of water, and found growing green and green organisms, it drops to zero and the water is filled up. This phenomenon is called "flowers" of the sea.

Flora and fauna
Phytoplankton and benthos. Phytoplankton accumulate (in%): s diatoms - 55, first - 41.2, and blue-green algae - 2.2. In the middle of biomasi benthos, mollusks occupy the dominant camp. Їх skeletal surpluses, represented by calcium carbonate, may signify a pitched wagon in the form of a daily bottom siege and accumulative surface bodies.
The Іхthiofauna of the Sea of \ u200b \ u200bAzov includes 103 species and species of ribs in the Danish hour, which can be found up to 76 genera, and is represented by passive, like prodigal, marine and primordial species.
Passing species of ribs feed in the sea until the state of maturity, and only go into the river for spawning. The period of breeding in small and medium-sized loans does not grow for 1-2 months. Among the Azov prodigal ribs є the most popular promises, such as biluga, stellate sturgeon, oseledtsi, ribets і shey.
For breeding, it is possible to go from the sea to the rivers. However, in the rychka stench, it can be overshadowed for a trivial hour, not so bad (to rock). When young people are hungry, they will go away from the spawning grounds even more often and often get lost in the country for the winter. Before the first time ribs are introduced, there are a lot of species, such as pike perch, lash, ram, chekhonya and deyaki inshi.
Morski vid and breed and feed in brackish waters. Among them, you can see, constantly lingering in the Sea of Azov - pelengas, Chornomorsky kalkan, flounder-glosa, tulka, percarina, trigolkov thorn, pipe-tube and all vidi bichkiv. І, nareshty, є there is a large group of sea ribs, to enter the Sea of Azov from the Black Sea, including the regular migrations: Azov and Chornomorska hamsa, Chornomorsky oseledets, red-barnacle, Singil, Chornomorskaya stavors ...
When you see water, you constantly linger in the same area, water and great migrations do not come. Tsі vidi dwell in the wake of the definition of the water of the sea. There are such ribs, yak sterlet, Siberian crucian carp, pike, ide, bleak and іn.

Morskі ssavtsі in the Sea of Azov is represented by one species - sea pig (іnshі name - Azovka, Azov dolphin, fir, boy). Morska pig is a herd way of life. Up to the group warehouse there are two up to ten individuals. The number of the population is not large, due to the day. Azovka - find a creature from a group of whale-like animals. And the representatives of the Azov-Chornomorsk population of the mice, are not the dolphins from the other parts of the range. Females of trochas are larger for males: 90-150 cm. At home, the maximum size of males reached 167 cm, and females - 180 cm. Life is trivial - 25-30 years.
For a number of growing and natural organisms of the Sea of Azov, there are no small ones near the sights. For riboproductivity, tobto some ribs on one area, the Sea of Azov is 6.5 times overturned in Caspian Sea, 40 times - Chorne and 160 times over in the Middle Earth Sea.

Sea of Azov, Misto Uysk

Geographical ob'єkti of the Azov Sea
Overextended great for presenting special interest geograficheskie ob'єkti in the order of їkh following the year of the year, uzberezhzha repairing from the Genichesky channel.

The inflows of the estuary:
In the territory of Ukraine:
on a private visit: Utlyuk estuary, Molochny estuary, Obitichna inflow, Berdyansk inflow.
On the territory of Russia:
at the pivnichny gathering: Taganrozka inflow, Mis'koi estuary, Uysky estuary;
at the gathering: Yasenskiy inflow, Beysuzkogo estuary, Akhtarskogo estuary;
on p_vdn_-sidi: Temryuksku inflow;
at first entry: Kazantipskiy Gulf, Arabatsku inflow;
at the entrance: the outflow of the Sivash (from 1 April 2014 to the de facto fate of the Ukrainian-Russian sovereign cordon).

Kosi, misi, most islands:

Main article: Kosi of the Azov Sea
In the territory of Ukraine:
on a private visit: Fedotova spit and spit Biryuchiy island (Utlyuchi estuary), Obitochna spit (Obitichna inflow), Berdyansk spit (Berdyansk inflow);
at the pivnichny gathering: Bilosarayska spit, Kriva spit.
On the territory of Russia:
at the personal meeting: Beglitskaya spit, Petrushina spit, Taganrozkiy mis;
at the descent: Mis Chumburskiy, Glafirovskaya spit, Dovga spit, Kamishevatska spit, Yasenska spit (Beysuz estuary), Achuevskaya spit (Akhtarsky estuary), Uyska spit, Sazalnik spit;
at the first meeting: Mis Achuevskiy and Mis Kamyaniy (Temryuksku inflow);
in Kerch prototypes: Chushka spit, Tuzlinska spit, Tuzla islands;
on the first call: Mis Chroni, Mis Zyuk, Mis Chagani and Mis Kazantip;
at entry: spit Arabatska Strelka.

Richkas that run into the sea:
In the territory of Ukraine:
on a private visit: Maliy Utlyuk, Molochna, Korsak, Lozovatka, Obitochna, Berda, Kalmius, Gruzkiy Elanchik;
On the territory of Russia:
at the personal meeting: Mokriy Elanchik, Mius, Sambek, Don, Kagalnik, Mokra Chuburka, Eya;
at the first meeting: Protoka, Kuban.

Legal status
The international legal status of the sea begins with a number of dzherel law, the most relevant ones - Agreement mij Russian Federationі Ukraine about spіvpratsyu by the viceroy of the Azov Sea and the Kerch channel (ratifications both by the parties in 2004). All documents of Azov have been made to the category of internal waters of Russia and Ukraine.

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DZHERELO PHOTO I MATERIALU:
team Kochuyut
Sea of Azov // Encyclopedic Dictionary of Brockhaus and Efron: In 86 volumes (82 volumes І 4 additional). - SPb., 1890-1907.
Neznamov P.A. іst. museum. - 1941. - VIP. 14. - S. 73-81, repr. picture.
Velokurova N.I. Hydrometeorological characteristics of the Sea of Azov / N.I. Velokurova, D.K. Starov. - Moscow-Leningrad: Gidrometeoizdat, 1947.
Tushin Y. P. Rosіyske seafaring on the Azov, Caspian and Black seas (XVII century) / Y. P. Tushin; Auth. foreword V. V. Mavrodin; Artist. D. Stankevich; Leningradsky Order of Lenin state university imeni O.O. Zhdanov. - M .: Nauka (Head of the editorial office of the skidnoi literature), 1978. - 184 p. - 10,000 approx. (Region)
Encyclopedia of Taganrog. - Rostov-on-Don: Rostizdat, 2003 .-- 512 p. - ISBN 5-7509-0662-0.
Brodyanoy A. V. Name the Sea of Azov. - Vradiyivka: Vidavnytvo Kovalenko A.G., 2008 .-- 48 p. - ISBN 978-966-2035-01-8.
http://club.foto.ru/
Vіkіpedіya website

The Azov Sea is an internal sea at the descent of Europe. The sea has been found in the light, the depth is not 13.5 meters. For morphological signs, it is carried to flat seas and is a shallow water with low coastal grapples. The sea shores in the main plane and food, only on the birch trees, there is a volcanic hike, as a few moments pass into the steep front of the mountains. Outside the ocean, the Azov Sea is the continental sea of the planet. The coastal line is covered with streams and spits, the territory of which is a western or resort and recreational zone. The shores of the Azov Sea are low-lying, stored with food-turtle attachments. In the Sea of Azov, the great rivers Don, Kuban and the number of small rivers Mius, Berda and others flow into the Sea.

salinity

The level of salinity of the Sea of Azov is formed into the Persha of Cherga before the inflow of ryas flood of rychkovy waters (up to 12% of the flow of water) and difficult water exchange with the Black Sea. The water is even less salty in the private part of the Azov Sea. For this reason, the sea is easy to freeze. During the wintering period, it is more frequent, or outside freezing, when there is a lot of ice to wine in the Chorna Sea through the Kerch canal.

Pidvodny relєf

leaks

The sea currents are found in the fallowness of the mud here even stronger than the strong wilderness and early waning times, and it often changes too much. The main plane is the circular current of the shores of the Sea of Azov against the godinnikovo line.

fauna

The Іхthiofauna of the Sea of \ u200b \ u200bAzov includes 103 species and species of ribs in the Danish hour, which can be found up to 76 genera, and is represented by passive, like prodigal, marine and primordial species.

Passing species of ribs feed in the sea until the state of maturity, and only go into the river for spawning. The period of breeding in small and medium-sized loans does not grow for 1-2 months. Among the Azov prodigal ribs є the most popular promislovs, such as biluga, sturgeon, stellate sturgeon, oseledtsi, ribets і shema.

For breeding, it is possible to go from the sea to the rivers. However, in the rychka stench, it can be overshadowed for a trivial hour, not so bad (to rock). When young people are hungry, they will go away from the spawning grounds even more often and often get lost in the country for the winter. Before the first time ribs are introduced, there are a lot of species, such as pike perch, lash, ram, chekhonya and deyaki inshi.

Morski vid and breed and feed in brackish waters. In front of them, you see, constantly lingering in the Sea of Azov. Tse - pilengas, flounder-kalkan, glosa, tulka, percarina, three-spined lump, rib-golki and all vidi whips. I, nareshty, є there is a large group of sea ribs, which can enter the Azov Sea from the Black Sea, including regular migrations. Before them are mentioned: Azov hamsa, Chornomorska hamsa, Chornomorsky oseledets, red mullet, singil, gostronis, lobanon, Chornomorsky kalkan, horse mackerel, mackerel and in.

When you see water, you constantly linger in the same area, water and great migrations do not come. Tsі vidi dwell in the wake of the definition of the water of the sea. There are such ribs, yak sterlet, common crucian carp, pike, ide, bleak that іn.

For a number of growing and natural organisms of the Sea of Azov, there are no small ones near the sights. For the productivity of the Azov Sea 6.5 times overturned Caspian Sea, 40 times - Chorne and 160 times the Middle Earth Sea. Along with the size it is 10 times less than Chornyi.

Korisny kopalini

Geologists stand alone on the point where the nadra of the Sea of Azov is douche bagati. Here zircon, rutile, ilmenite are found. Under the bottom of the sea, there is a mineral, so to take revenge in a good half of the Mendelian table. At the paved-skidny part of the sea є underwater mud volcanoes. The nadrah of the Sea of Azov knows industrial reserves of natural gas.

The Sea of Azov (Ukrainian Sea of Azov, Crime. Azaq deñizi) is a pivne-skidny bichny basin of the Black Sea, with which there is the Kerch channel (Bosphorus Kimmeriysky in a long time, width of 4.2 cm). The Azov Sea is carried to the seas of the Atlantic Ocean.

For a long time, the Greeks called it Meotiyske Lake (Greek Μαιῶτις), the Romans Palus Maeotis, Scythian Kargaluk, Meoti Temerinda (symbol Mater of the Sea); arabi Nitshlakh abo Baral-Azov, Turks Baryal-Assake abo Bahr-Assak (Dark blue sea; in the bitter Turkish Azakdenizi), Genoese and Venets Mare delle Zabacche (Mare Tane).

The extreme points of the Azov Sea lie between 45 ° 12'30 "and 47 ° 17'30" Mon. latitude і між 33 ° 38 '(Sivash) і 39 ° 18' n. dovgo ti. The most popular is 343 kilometers, the most wide is 231 kilometers; more coastal line of a thousand chotirista seventy two kilometers; surface area - 37605 square kilometers (the area does not include islands and spits, which occupy 107.9 square kilometers.).

For morphological signs, the Azov Sea rises to the flat seas and is a shallow water with low coastal grapples.

The largest amount of glybin does not change 14 meters, and the average glybin is close to 8 meters. With a total glybin up to 5 meters, it takes more than half of the Azov Sea. Osyag yogo is also small and become 320 cubic meters... For the sake of it, let’s say that the Aral Sea will change Azovske by 2 times over the area. The Black Sea is 11 times larger than the Azov Sea in terms of area, and 1678 times beyond the obsyag. And all the same, the Azov Sea is not so small, two such powers of Europe, such as Netherlands and Luxembourg, would be located on the new one. The last one is 380 kilometers, and the most wide is 200 kilometers. The initial length of the coastline of the sea is 2686 kilometers.

The water relief of the Azov Sea is even more simple, the mountains are mostly and smoothly grow in the world from the distance to the shores, and the most glibs are located in the center of the sea. The bottom is flat. The Sea of Azov has established an inflow, with the most abundant є Taganrozkiy, Temryukskiy and strongly evoked Sivash, which is correct to respect the estuary. Great Islands on the Sea of Azov. Є a number of miles, partly flooded with water and roasted near the shores. Such, for example, the islands of Biruchiy, Turtle and іnshі.

Azov Sea

In Russia, the Azov Sea became vidomo in the 1st century A.D., and they called it - the Blue Sea. The creation of the Tmutarakan principality by the Azov sea became known as Rus. In the fall of the principality, the sea of bagatoraz was changed (Samakush, Salakar, Mayutis, etc.). On the ear of the 13th century Bulo hardened I will name the Saksin Sea. The Tatar-Mongolian conquerors reopened the collection of the names of Azov: Balik-Dengiz (Ribne Sea) and Chabak-Dengiz (Chabachye, Lescheva Sea). For deyakim danimi Chabak-dengiz as a result of the transformation: Chabak - dzibakh - Zabak - azak - aziv - the name of the sea has been changed (summarily). For іnshih danimi Azak - Türkic prikmetnik, scho means "low, lowland", for іnshi danimi, "Azak" (Türkic "girlo rychki"), which was transformed into Azau, and then in Russian Azov. In the midst of the Vischevkazan, the name of the Azov Sea was denoted by the following: Barel-Azov ("Dark Blue Richka"); Frakіyske sea (from frakіytsy vozmіlіy genoesі and venezіantsі); Surozke sea (Surozhem calling himself a lucky Pike perch in Krima); Kaffa Sea (Kaffa is an Italian colony at the place of Feodosia in the Crimea); Kimmeriyske sea (from kimmeriytsiv); Akdengiz (Turkish, which means Bile sea).

Naybіlsh worthy trail of vvazati, but the current name of the sea resembles the name of the place of Azov. There are a number of hypotheses behind the etymology of the word "aziv": on the name of the Polovtsian prince Azum (Azuf), who was killed when the place was taken in 1067; for the name of the tribe of the Wasps (Asi), in their own devil, which became nibito from the Avestan, which means "shvidky"; I will name it in the Türkic word azan - "lower", and in the Circassian uzev - "neck". Türkske name r Azov - Auzak. Ale shche in the I st. not. Plіnіy, pererakhoyuchi in their ancestors Scythian tribes, zgadu tribe Asoka, similar to the word Azіv. Accepted vvazati, but the current name of the Sea of Azov has come to the Russian toponymy on the cob of the 17th century. the writers of Pimen's literature. Moreover, on the cob, only after that part (Taganrozka inflow), and only after an hour of the Azov campaigns of Peter I, the name of the Sea of Azov closed behind all the water. The sea gave the name to the villages of Azov and Azov and Azov (in the lower reaches of the Don River, Rostov region), the village of Azov and Azovka farm.

History of the sea of Azov

In the history of the Azov Sea, there are three stages:

1. Ancient (geographic) - from the hours of Herodotus to the ear of the XIX century.

2. Geological and geographic - XIX century. - 40th rock XX century

3. Complex - mid XX century. - Christmas.

I am reading the map of Pontus Evksinsky and Meotid Sklavs Klavdiy Ptolemy, but I have given the geographical coordinates for the places, girla rychok, misіv and the outflow of the Uzbek Sea of Azov.

In 1068, the Russian prince Glib vimiryav across the ice to see Kerch and Taman. It was written on the Tmutarakan stone, the ride from Tmutarakan to Korchev (the old name of Tamina and Kerch) was about 20 kilometers (for 939 years it was 3 kilometers long).

З XII-XIV Art. The Genoese and the Venetians started to stock up the portolans (pilots and marine pictures of the Black Sea and the Sea of Azov).

Sea of Azov - geological minule

The Sea of Azov, from the point of view of its geological wind, is a young basin. Obrisi, close to the day, came out in the Quarter period. Bagato mіlyonіv rockіv that Azov Sea entered the ocean before the warehouse, which geologists call Tetis. The unconnected smoothness of yogi was stretched out Central America across the Atlantic Ocean, a part of Europe, Seredzemne, Chorne, Caspian and Aral Seas and went on the route through India to the Pacific Ocean.

The history of the Azov Sea is closely related to the geological past of the Crimea, the Caucasus, the Black Sea and the Caspian Sea. Injected internal forces crust now it sank, now it went down at the sight of the giant lancers, as it was, by the robotic movement of flowing waters and vivitryuvannyam, transformed into the dish. As a result of a series of processes in the waters of the Svitovoy Ocean, they flooded the land around the sea, then they exposed them, or, as it seems, geologists, spared transgression (advance) and regression (retreat) of the sea.

At the same time, naturally, the skirts of the continents and seas changed. At the same hour, there was a change to the klimat, the rose and tea light on the land, and in the sea.

Lish in the Cenozoic era (the era of the new life), cut the continents and the surrounding seas, including the Azov Sea, become such, like my bachimo їkh on the cards.

The Cenozoic era is formed, like vidomo, from two periods - tretine and quarter, or anthropogenous. In the end, it’s the same lyudin. At the anthropogenesis, the shape of the Sea of Azov has ended, and even now, this dreadful viglyad is literally on the eyes of prehistoric people.

The sea basin stretched out to the anthropogenes, including the Chorne, Azov and Caspian seas, repeatedly changing its shape, area, depth, splitting into parts and again.

The development of the whole basin in the anthropogen was rejected by the following names: Chaudinsky, Drevneevksinskoe, Uzunlarske, Karangatskoe, Novoeuksinskoe seas.

The Chaudinsky lake-sea was on the ear of the era of the great glaciation - more than 500,000 years ago. Abandoned the sea is known on the Misi of Chaud Kerch Pivostrov (stars and the name of the sea), є the smell is also on the Uzbek side of Tamansky Pivostrov. fauna ( tvarinny svit) Strongly delineated by the Chaudin Sea, the bullet is very close to the fauna of the Baku Sea, entering at that hour to the warehouse of the Caspian Sea Basin. Tsia obstavina led them to visnovka, where the Chaudinsky and Baku basins were drawn along the valley of the Manich rivulet.

Having developed a poorly warm period, the Chaudin Sea entered the Old Euksian Sea as a misfortune. Tse bulo strongly opr_snene lake-sea. It should be used up to the first half of the quarter period. The introduction of the Ancient Eurasian Sea is seen on the Kerch Peninsula, in the Taganrog region, on the Caucasian Uzbek Sea, on the Manich River. There is a great choice of fauna to tell about those, that the sea is surrounded by ancient Caspian and Baku basins.

At the ancient euksian hour, the Black Sea comes from the Seredzemny through the Dardanelles channel. The so-called Uzunlarske came to the winter of the Ancient Euksian Sea. Water infiltration Midland Sea to see the deeds of salinity of the Uzunlar Sea and to raise the level of salinity. Ostann called to the flooding of the lower parts of the uzberezhya і girla richok. At the end of an hour, the estates of the Dnipro, Don and other rivers of the Azov-Chornomorsky basin will be illuminated. The Manichsky channel, which closed earlier the Ancient Euksian and Ancient Caspian seas, in a whole hour ceased to exist.

The Uzunlarskoe sea was changing by the solonim of the Karangatsk sea, which was confirmed by the great sinking in the region of the Azov Sea and the Krimu.

Tsi sinking wicked transgression of brackish waters and penetration into the Karangatsk basin of sea fauna, rich in species, not just Chornomorska.

Every hour of the last icy Karangatskoe sea is changing by the semi-fresh Novoevksinskoe lake-sea. In the middle of the Caspian region, the Khvalinsky sea was stretched out in an hour, yak, judging by the abundance of faunas of both seas, dying from the New Eurasian one. The Novoevksinsky regressive stage of the development of the sea is changing the ancient Black Sea and the New Black Sea stages of its expansion.

The remaining, Novochernomorsk, stage of the development of the Azov Sea will be brought up to a number of independent stages, and itself: the stage of the maximum development of the New Black Sea transgression, since the sea is 2.5-3 m large in the middle of a modern small and the Nimfey stage. At the Meotic stages of the Azov Sea, according to the description of the ancient Greeks, was a pristine and swampy lake. At the Nimfeysky stage, the formation of the current outlines of the coastline is taking place, and in the early hours of the day, the new picture of the Sea of \ u200b \ u200bAzov.

Azov Sea - geography

Bathymetry of the Azov Sea

The water relief of the Azov Sea is somewhat simple. Near the world, the distance from the coast of the mountain is increasing and smoothly growing, reaching 14.4 meters in the central part of the sea. The main area of the bottom of the Sea of Azov is characterized by a glybin of 5-13 meters. The area of the greatest depths is located in the center of the sea. The growth of isobaths, close to symmetrical, will break down a small species of femininity on the winter descent towards the Taganroz inlet. It takes about 5 meters to grow approximately 2 kilometers from the coast, from the distance from the nearby Taganroz inflow and into the very place where the donut goes. At Taganrozkiy, the glibinia grows across the Donu arm (2-3 meters) right up to the upper part of the sea, reaching 8-9 meters on the cordon outlets from the sea.

At the bottom of the Sea of Azov, there are systems of sub-water basins, the bridle of the skid (the Zhelezinskaya bank) and the western (Morska and Arabatska banks) uzberezh, glibini over yaky change from 8-9 to 3-5 meters. For the underwater coastal cliff of the pivnic Uzbek, wider water (20-30 kilometers) with 6-7 meters of depth is characteristic, for the underwater Uzbek - the slopes of the underwater slope up to 11-12 meters. The water intake area of the Basin of the Azov Sea will become 586,000 square kilometers.

The sea shores in the main plane and food, only on the birch trees, there is a volcanic hike, as a few moments pass into the steep front of the mountains.

Geographical ob'єkti of the Azov Sea

It is great to be overwhelmed, or to represent a special interest in geography in order to follow the year of the year in the Uzbek coast of the Azov Sea, repairing the Kerch channel.

Inlets and estuaries of the Azov Sea:

Ukraine:

At first entry: Kazantipskiy Gulf, Arabatsku inflow;

At entry: Sivash inflow;

On a private visit: Utlyuk estuary, Molochny estuary, Obitochna - inflow, Berdyansk inflow;

Russia:

At the pivnichny gathering: Taganrozka inflow, Mis'koi estuary, Uysky estuary;

At the gathering: Yasenskiy inflow, Beysuzkiy estuary, Akhtarskiy estuary;

On a private meeting: Temryuksku inflow.

Kosi and Misi of the Azov Sea:

Ukraine:

On a first visit: Mis Chroni, Mis Zyuk, Mis Chagani and Mis Kazantip (Kazantipskiy Zatoka);

At entry: spit Arabatska Strelka (inflow Sivash);

On a first visit: Fedotova spit and spit Biryuchiy island (Utlyuchi estuary), Obitochna spit (Obitichna inflow), Berdyansk spit (Berdyanska inflow);

At the pivnichny gathering: Bilosarayska spit, Kriva spit;

Kerch prototypes: Tuzla spit.

Russia:

At the dinner party: Beglitskaya spit;

At the descent: Mis Chumburskiy, Glafirovskaya spit, Dovga spit, Kamishevatska spit, Yasenska spit (Beysuzky estuary), Achuevskaya spit (Akhtarsky estuary);

At the first meeting: Mis Achuevskiy and Mis Kamyaniy (Temryuksku zatoku).

Kerch prototypes: Chushka spit.

Richki, which flow into the Azov Sea:

Ukraine:

On a private visit: Maliy Utlyuk, Molochna, Korsak, Lozovatka, Obitochna, Berda, Kalmius, Gruzkiy Elanchik;

Russia:

At the party meeting: Mokriy Elanchik, Mius, Sambek, Don, Kagalnik, Mokra Chuburka, Eya;

At the first meeting: Protoka, Kuban.

Take care of the sea of azov

Uzbek Sea of Azov Mensh malovnicho і profitably, nіzh Chornomorske. Ale є і has its own unique beauty. Vrytul up to the sea steppe, and the thickets outlined flowing in small parts. Take care of the poor, the stench is either low and flat, with a perennial turtle beach, or poor, albeit ovist, stacked with still forest-like loams. The coastal line of the sea makes it possible to finish the smooth vigini, and only when the food is mowed to give the deyaku ruggedness. There is a great number of kis - one of the characteristic features of the shores of the Azov Sea.

Wandering the Uzbek Sea of Azov

The western coast of the Azov Sea of performances with a long scythe - the Arabat Shore. The coastline of the sea was lifted by 112 kilometers, all the way from the river Sivash. The width of the whole flat grass-turtle mows rises from 270 meters in the middle and middle parts, and up to 7 kilometers in the small mountains. Arabatska strelka is a magnificent natural beach. At the same time, a row of dovgy milens was stretched. You can see wonderfully from the walls of the old Genoese fortress, roztashovaya near the village of Arabat, or right from the deserted bedrock shore. In a quiet, sleepy weather, the greenish-blakitny sea with a light noise m'yako come to the food-turtle beach and the light surf is soothing, like a high-pitched bilim. Roll on to the krill, skim low over the water of the seagulls. In the distance, on the spit, it glitters through the interchanges of the hot sun of the vidobut from the Sivash sil. The Sea of Azov is beautiful in a storm. If dme lyutii Nordost, it’s dark, we will suvorim. With angry noise, boiling white pinoy, steep-walled khvili fall on the shores. We can spend many years meeting with the sea space, the strong big and the boisterous surf of the Sea of Azov.

Any people who have seen the Sea of Azov, want to forget about him with an uncomfortable, ale sickly soul of beauty.

At the Arabian construction site, they see hot mineral water, behind their chemistry warehouse and political authorities, to turn the mathematicians upside down. On the basis of the flowing waters, a new resort - Azov Matsesta - is transferred.

Pivdenne Uzbek Sea of Azov

The northern coast of the Sea of Azov shows performances of the territory of the Kerch and Taman pvostrovs, between which they grow up to the Kerch channel, which is located in the Azov Sea and the Black Sea. Kerch pіvostrіv є skidnym edge of Crimea. Its area is close to 3 thousand square kilometers. At the nadra of the pіvostrov, there are great genera of zaliznyh ores, which lead to the metallurgy of Priazov, naphtha and natural gas. Pivnichna і pіvnіchno-skidna parts of the Kerch pіvostrov stored with marls, clays, vapnyak; Most of the time, there are the trials of the third party. The wandered part of the Kerch pіvostrov is rіvninn, skіdna - hunchbacked. At the border of the pіvostrov, the pivdenny shore of the Azov Sea is steeply shaved in the sea, and the beach is covered with smog. By means of the misery of the shores of the banks, folded with bryozoans, it is easy to repair the onslaught of seaweeds. Such, for example, is Ms. Kazantip, which is based on a bryozoan reef - atoll. At the end of the city - the Arabat inflow, on the road - Kazantipskiy. At the turn towards the Kazantip misu, the low-lying alluvial dilyanka of the uzberezhzha stretches. Take care of both the inflow with soft clayey rocks. On a weekday from Kazantip Misu - Aktashske Solon Lake. Central lake. Vono is a surplus of Kazantipskogo inflow, prick far into the land.

In the middle of the Kerch p_vostrov, from the approach to the skid, there was a simple Parpach crest. A wide later valley grows along the coast of the Azov Sea. In the lower parts of the її salt lakes, and the withers are dominated by their dominant authorities, the Chokrakskoe Lake, as well as a number of mud volcanoes.

At the turn of the Kazantipsky inflow, near the Kerch channel, the coast of the Azov Sea is more quiet, here for a new characteristic misi, folded with solid bryozoans, for example, Misi Zyuk, Tarkhan and іnshi.

The Kerch channel, which is close to the Chorne and the Sea of Azov, is not wide and sometimes not wide. Its width varies from 4 to 15 kilometers. Dovzhina ducts - 41 km Glibina become close to 4 meters.

At the old Kerch channel, it was called Bospor Kimmeriyskiy. In the very name, it takes a stretch on the shallowness of the channel, as "Bospor" in the translation to Russian language means "scourge brid".

Krims'kyi shore of the channel with m_stsy obrivisty. Near the second part of the city, the misto-port of Kerch has sprung up.

Tamansky pіvostrіv, which is є part of the Krasnodar Territory, occupies an area of approximately 1900 square kilometers. In them, trochas more than 900 square ones fall on land. kilometers, and the sieve of the territory - estuaries and smooth.

Yogo's nature is wild. From the geological point of view, there are young birds, as it was formed in the quarter period. Even in the 1st century n.e. On the last day there were five islands close to five, the transformation of which into the past were brought up, Mabut, in the V century A.D. on the basis of the accumulative activity of the rivers of Kuban, mud volcanoes and tectonic events. Forming of Tamansky p_vostrov triva dosi.

The upper part of the pіvostrov is a humpbacked ryvnina with low dome-shaped temporal ridges, twisted at the viglyadі of the distant ridges from the beginning of the entry to the pіvnіchny skіd. There are mud volcanoes and ancient burial grounds - burial mounds everywhere. The landscape is filled with numerous estuaries. Widely widened and flowing, overgrown with outlines and sedge.

Tamansky pyvostrіv revenge in its nadra such natural resources as naphtha, combustible gases, ore, silt, awakening materials in viglyadi vapnyak, clay and gravel.

Climat p_vostrov is also warm. The dream generously supplied its warmths, albeit fallen off here, it is not rich - a total of 436 millimeters per day - and this is a marriage of a vologue.

On the pіvostrovі - dear chernozem and chestnut soils, cover the dry steppe, and along the valley of the rivers of Kuban - flooded dew.

Take care of the Tamansky pivostrov to reach the versatile, but also to cross two types of banks: high, steep - abrasion, to be done as a result of the ruinous robots of sea needles, and low, flat - accumulative. The rest were formulated from the food-clayey contribution as a result of the activity of sea needles and leaks.

The coast of the Taman inflow, from the Tuzla Misu all the way to the village of Taman, along the slopes. In the middle of the height, the distance here goes from 15 to 30 meters. At the turn of the village of Taman, the coast goes down and becomes low on all the stretch of the ancient and skid Uzbek river inlets. Just shave it off with little mischief, and that is often for a rakhun of the cultural ball of the old-time Fanagoria.

The pivnichny coast of the inflow is also carried out and it is steeply shaved to the sea.

Scythe Chushka, stored in the world of quartz sand and broken turtle, on the low coast.

The distance to the skid coast of the Tamansky Piostrov is high (up to 50-60 meters above the Azov Sea) and often has a subdued character. Wines are stored in the main forest-like clays and swampy sands on the beach, which can be stored in clay-clays, in small pieces with houses of turtles, pebbles and crushed stone.

Then, right up to the village of Golubitskaya, the coast of the Sea of Azov either goes down or starts to move, ala, repairing from the village, the wine becomes low, and in the area of the delta of the river Kuban the swampy character is swampy.

Quite simply, in the area of the village of Kuchuguri on the low birch of the Sea of Azov, green trees are more likely to form a relief at the view of low (1-3 meters) humpbacks - dunes, which were made in the middle of the winter.

The lurch of mud volcanoes is the lingering of the spoky and the inaccurate, but some of the lingering of the volcanoes, the way it is super-vibrated, and the products of volcanic activity are thrown up and out of the way for hundreds of meters.

Velmi Tsikave is a manifestation of mud volcanoes at the bottom of the Sea of Azov near the shores of the Tamansky Piostrov. So, the intensive mud volcanic activity was spasmed not far from the village of Golubitskaya. One of the pinnacles is assigned to the 6th month of 1799 rock. Feeling the hum of the ground, then the thumping sound of the thunder over the sea, about 300 meters from the shore, a stop was made from the fire and the black dim. Close to two years it was a trivial vyverzhennya, which led to the establishment of the island with a brude with a diameter of 100 meters and up to 2 meters. Through a kіlka mіsyatsіv wіn znik, rozmitіy hviliy Azov Sea.

Some variations were repeated and for the last time - in 1862, 1906, 1924, 1950 and 1952 rock. In 1952, at the end of the village of Golubitskaya, 5 kilometers away from the coast, also as a result of mud volcanic activity, with the establishment of muddy islands, raised by the wicks of the Azov Sea.

Skhidny coast of the Azov Sea

The skidny coast of the Sea of Azov, from Temryuk to Primorsko-Akhtarsk, on the outskirts of nearly 100 kilometers є the low-lying delta of the Kuban rivulet with numerous estuaries, channels, great floodplains, overgrown outlines and sedge. Richka Kuban, shores an ear of ice in the Elbrus mountains, one of the largest and most abundant rivers in the Pivnichny Caucasus. Dovzhina її - 870 kilometers. The area of the water intake pool is 57,900 square kilometers. Delta її established itself on the site of the Azov Sea, deeply into the land. Tens of thousands of rock in that tsyu inflow prostyagavsya until that time, de at a time to be found Krasnodar. The majestic Bula lagoon is rimmed by the slope towards the sea and is gradually filled with river sediments. Therefore, the role in the form of the western-western part of the delta was played out and the activity of mud volcanoes (salzi) of the Tamansky Pyostrov, which is often a view of the archipelago of other islands. Products from the mud volcanoes carried the channels along the islands and filled the stepwise lagoon with rychkovy sediments.

The formation of the delta is very difficult at our time, and it’s obvious that there are warehouses at Achuyvo 5-6 millimeters in the river, and in the other mids of the delta - 3 millimeters in the river.

Richka Kuban is grapevine in the Sea of Azov in the middle of 11.4 billion cubic meters of water, which is worth 3 million tons of distilled rivers and mazu muty. The water in the river is kalamutna round, albeit especially rich in deposits during the floods, which in the Kuban tend to be in the middle of 6-7 on the river. The initial number of the winners of the firm rychkoyu hard words (so the titles of the hard stick) become 8.7 million tons per rik. To transport such a vantage, it would take 52,000 freight wagons. For rakhunok tsikh nosіv іde growing delta Kubanі. The infection of the Kuban delta, which occupies an area of 4300 square kilometers, can be repaired at the so-called Raz-der, near the place of Slov'yanska, from the Kuban to the right (at the beginning) the branch of the Protok. The remainder takes nearly 40-50% of the Kuban water and flows into the Azov Sea near Achuyvo.

Nizhche Protoki, not far from the girla, Kuban is divided into a number of sleeves, with the most important ones - Petrushin sleeve and Kozachiy Urik. Petrushin sleeve, which represents a ship-floating route here, the river bed of the Kuban river, where it flows into the Sea of Azov.

The Kozachiy Urik is the left bank of the Kuban, which carries its way to the great Akhtanizovskaya estuary, which has a link to the Sea of Azov through the Peresipskoy girlo.

The current delta of the Kuban rivulets is a labyrinth of shallow lakes, or estuaries, which are located between the channels, or, in a local way, rykami, which create chimeric loops between dry lowlands of swamps.

At the delta of the Kuban, the majestic areas are occupied by floodplains, which stretch for tens of kilometers. The floating deltas of the Kuban, which adjoin to the Sea of Azov, are called Priazovsky. The stench is dismembered by the river Protoka into two massifs: on the water of the Azov floodplains in the backward part and Angelina-Cheburgolsky in the backward part.

Priazovskoy smooth - the chimeric labyrinths hurt and estuaries of growing size with spicy, semi-salty and salty water, thickets of above-water and underwater dewline. Sered perevazhayut delineate, delineate, sedge, horny and izhachogolivnik. Pidvodna, or "myaka" the height of estuaries - the price of water growth, rdesti, kushir, latattya and ін.

Limani delty Kuban bagati for riba. There are more than 70 species of ribs here, including ram, lash, pike perch, pusanok, sprat, carp up to 15 kilograms, catfish up to 100 kilograms.

At the pivnich from Primorsko-Akhtarsk, right up to the Don delta, smoothly grow out in the throats of the steppe Azov rychok - Beisug and Chelbas.

The shores of the Sea of Azov are presented at the end of the day with low and gentle sloping braids, the small coast here is fast, or it descends steeply to the sea. Deposits of wines, as it is on the coast of the plain, forests and forest-like loams and clays of the late ice hour. The forest is a breed, it is easy to grow up and down, and the coast of the sea here quickly falls apart. The average speed of the route along the entire Uzbek road is 3 meters per river. Maximum up to 18 meters. The soils of the central part of the Azov region are represented by carbonate western Ciscaucasian fertile chernozems. Earlier, the whole region was covered with a coppice-grass steppe, herds of wild horses-tarpan and herds of pond-footed saigas grazed on yak. We were able to navigate the moose. There are no earths of roses, and there is a lush green sea of hlibs, fields of corn and a dormouse.

In addition to the rivers of Kuban, in the Sea of Azov, such steppe rivers immediately flow into the Sea of Azov (rakhuyuchi from pivday to pivnich), yak Kirpa, pour their water into the Kirpilska estuary; Beysug, which flows into the Beysuzky estuary; Chelbasa, which flows into the Solodky estuary; Її, foolishly drive into the great Uysky estuary, і, nareshty, small rivulets Mokra Chuburka і Kagalnik, which flow into the Sea of Azov without a second.

Characteristic is the peculiarity of the landscape of the shady Uzbek coast of the Azov Sea, which has already meant a species, the appearance of numerous estuaries.

Delta Don

At its own private-social part of the Azov Sea, there is a great, strong Taganrozka inflow, into which one of the largest rivulets of the European part of Russia - Don, falls. Dovzhin yogo to become 1870 kilometers, and the water intake area is 422,000 square kilometers. Don is choric to wine in the sea in the middle close to 28.6 cubic kilometers of water. Significant mass of river water strongly delineate Taganrozka inflow, and pour wine with water and lead to the growing Don delta, which borrows an area of 340 square kilometers. The current Don delta is repaired 6 kilometers downstream of Rostov-on-Don, there, across the river to the right, there is a non-floating arm of the Dead Donets.

Don’t make a great life on the river; up and down over the course of the flow of business and numbers to the court. Spokіynu smooth surface can rostinayut passenger ships, vantage ships and ribal boats.

The lower stanitsa of the lizavetinskoy Don began to wind heavily along the wide low-lying valleys, breaking down on the numerical arms and channels, which, in a local way, are called riks. Tsikh sleeves and erikiv grow ever larger in the world closer to the Sea of Azov.

The landscape here is free. Everywhere you can see the island, weakly hanging over the water, with chimerically porous shores, in the thick thickets of the outline. Ostrіvtsi, close to the sea, are gradually flooded with sea water; In case of strong backwaters of the Azov Sea, it is necessary to straighten up in the river Don, to drive rivers of water, to walk from the banks, not only the delta is flooded, but the flood is up to 100 kilometers up the hill for the current.

Shidnі vіtri, how to bleed downstream Don nadaut vorotnuyu dіu. The water is bustling, besides, it is very strong, but not only the sleeves of the rychka, but the Taganrozka inflow, which will ruin the normal navigation. The amplitude of the malignant appearances should be +3, -2 meters.

Don wine in the Sea of Azov in the middle is close to 14 million tons of river sediments and close to 9.5 million tons of mineral waters. For the rakhunok sedimentation around the Don delta, all the distance in the sea hangs out in a step-by-step manner, about 1 kilometer per century.

Pivnichne Uzbek Sea of Azov

Pivnichne of the Uzbek Sea of Azov stretched out from the hand of the Don to the place of Genicheska. A number of small rivers flow into the sea in the Azov Sea. Beruchs on the cob in the winds of the Donetsk ridge, carry their waters into the sea, the rivulets Mius and Kalmius. Beginning on the unseasonable Azovskoy sea, the rivers Berdya, Obitochna, Korsak flow in the Sea of Azov, and a number of others, which dry out the flow of the river. Uzbeks are characterized by the appearance of a whole series of children, who are in the main from the beginning of the week and during the first day of the weekend, whereby the mows are taken with their children,

Between the braids and the root coast of the Azov Sea, there are inflows and estuaries, for example, Berdyansky and Obitochna. As soon as the mows are turned on, the whole northern coast of the Sea of Azov is a steppe, which goes down to the sea with a cliff. Kosi and vuzka the coastal smog of the Azov Sea is stored in the main quarter naval inserts. At first glance, the valley is stored by forests, forest-like loams and clays in the late ice hour. On the cich rocks, rody chornozems have grown. Still in the last century, there was a lot of green grass and fescue, and in the last half, there was a grass and fescue steppe. They grazed tarpani, wild camels, and even earlier they began to see noble deer and elks. There were beavers near the small dogs. At the time of the flowering of the steppe, beyond the Vistula of N.V. Gogol, they represented a green-golden ocean, which vibrated as a result of millions of kits. However, these steppes have long been familiar, the stench will grow more roseorani. They changed the endless fields of wheat, corn, dormouse, fruit orchards and vineyards.

Azov Sea - water

Hydrochemical peculiarities of the Azov Sea are formed in the Persha of Chergu under the inflow of ryas flood of river waters (up to 12% of the water supply) and difficult water exchange with the Black Sea. The salinity of the Sea of Azov before the regulation of the Don Bula is three times less than the average salinity of the ocean. The value of її on the surface varied from 1 ppm in the Don River to 10.5 ppm in the central part of the sea and 11.5 ppm near the Kerch Channel. As the stem of the Tsimlyansk hydroelectric node starts, the salinity of the Sea of Azov has begun to grow (up to 13 ppm in the central part). The mid-season number of salinity values is very close to 1%.

Water to take revenge on little salt. For a reason, the Sea of Azov is easily frozen, and even before the krigolam appear, it will not float from the breast to the middle of April.

Throughout the XX century, practically all big-mensh big rivers that flow into the Sea of Azov, bully barred by rowing for the stem of water reservoirs. Tse called up to a significant speedy skidannya vodi and mule in the Azov Sea.

Water regime of the Azov Sea

The water regime of the Sea of Azov lies in the main tide of the fresh river waters, which falls over the sea of atmospheric fall and comes up in the new salty waters of the Black Sea, from one side, and from the water from the Sea of Azov to the vaping through the river sea - from іnshogo. The water balance of the Sea of Azov is the first step. Don, Kuban and іnshі rivers, which flow into the Sea of Azov, bring 38.8 cubic kilometers of water. The average volume of atmospheric fall on its surface becomes 13.8 cubic kilometers. Through the Kerch canal, 31.2 cubic kilometers of water of the Black Sea flow into the sea, in addition, through the Tonky canal from the Sivash, 0.3 cubic kilometers of water rises into the sea. The outbound arrival of the driver is all 84.1 cubic kilometers. Vitrata and water from the Sea of Azov are stored from the vaporization from the surface of 35.3 cubic kilometers, the flow through the Kerch canal in the Chorna Sea is 47.4 cubic kilometers and the drain through the Tonky canal in Sivash is 1.4 cubic kilometers. The back of the vitrata of the waters of the Sea of Azov is also 84.1 cubic kilometers. When the size of the Azov Sea is small, the sea will get rid of a lot of rich water, some of which become close to 12% of the amount of water. Staircase of the river runoff to the obsagu of the Azov Sea - the best from the more seas earthly coo... The change in the hopefulness of river and atmospheric waters over the vaporization from the surface of the sea led to an increase in the definition and increase of the level of water, as there was no water exchange from the Black Sea. As a result of the water exchange in the Sea of Azov, salinity arose, favorable for living in new valuable industrial ribs.

sour mode

As soon as the Azov Sea has a low water content, as it has already begun, call it good to change, so all the water has plenty of water. Instead of a razchinenny sisnyu reach of 7-8 cubic centimeters per liter. However, in last hour often discouraged from the lack of acidity. The price is explained by a number of factors. Great importance is the control of the vertical circulation of the waters with hot lithium during calmness, if the top, the ball of sea water becomes easier to lie more lighter, and the weather is better. Tse pereshkodzhaє aeration of the lower horizons. Nice to ask for a deficiency, but also to ask for a deficiency. organic speech... If the weather is very quiet, then the rocky parts of the mule spend three hours at the bottom of the ball and go to the bottom of the river, and it’s pretty sour to turn on oxidized organic speeches.

Nestacha kisnu wiklikє the phenomenon of the so-called "zamoru", so that the parts of the creatures of the sea have died, so they inhabit the bottom and the water.

Chemistry warehouse

The great flood of river waters in the Azov Sea and difficulties in water exchange from the Black Sea are generated at the chemical warehouse of the Azov water. Don, Kuban and інші rivers, which flow into the Sea of Azov, bring 15 million tons of salts into the new one, in the warehouses which they transship іoni НСО3, SO4 and Са. With atmospheric debris, 760 yews rise to the sea. Tons of salt with the same amount of salt as in the river waters. Then from the Black Sea comes water, a lot of іons Сl ", Na" і K. " salt water from Sivash to bring about 6 million tons of salts. As a result of the change of water from the Rice Warehouse and Wine from the Sea of Azov in Chorna and Sivash, 570 million tons of salts will form a modern chemical warehouse of the waters of the Azov Sea. In the middle, in the surface spheres of the waters in the open sea part, there is an offensive number of ions (in grams per 1 kilogram of water): sodium - 3.496, calium - 0.132, magnesium - 0.428, calcium - 0.172, chlorine - 6.521, bromate - 0.029 , Iona hydrocarbonate - 0.169, and all 11.885.

The shutter of the waters of the Sea of Azov and the ocean show the similarity of chemistry warehouse... Near the waters of the Sea of Azov, they transship, as in the ocean, chlorides. However, the salinity of the Sea of Azov is much lower in view of the ocean water and the deterioration is typical for the ocean, the steel of the main salt-forming elements. The withers, in the case of the ocean, are rich in calcium, carbonates and sulphates in the Azov water, and chlorine, sodium and calories are reduced.

In the Danish hour, salinity Azov waters rise to the offensive rank. On the depths of the Prikerchensky region of the Azov Sea, where there is more salt from the Chornomorsk water, the salinity reaches 17.5%. The entire central part of the sea is even less saline, it becomes 12-12.5%. The area here is insignificant, the salinity is 13 ° / oo. At Taganrozkiy, the salinity decreases to the girl's Don to 1.3%.

Sheds and on the cob of lithium during the flood of ice and the great tide of river waters the salinity decreases. The recovery and collection of money is the same from the surface to the bottom of the sea in a great country. The most salinity is spostering in the water-borne waters of the Sea of Azov, Sivash, and the naymensha - in the Taganrozsky waters. In addition to the mineral rivers, the waters of the Azov Sea, there are abundant biological elements (like elements of organic walking), brought to the sea in the main rivers. Phosphorus, nitrogen and silicon are added to these elements. Let us know that the rivers and waters of the Black Sea and the atmospheric fall bring 17139 tons of phosphorus, 75316 tons of nitrogen and 119694 tons of silicon to the Sea of Azov. A part of the cich rechovins is to wine in the Chorna Sea, a part of it is to be found from the sea at once from the sea, a little more part is to sink into the ground at the bottom of the Sea of Azov. So, phosphorus is deposited close to 13 thousand. Tons, nitrogen - about 31 thousand tons and silicon - about 82 thousand tons. Tons.

The wealth of the Sea of Azov with rich chapters opens up with a friendly mind for the development of life in the whole sea. The price is explained by the milky water, the high biological productivity. All of them are friendly to the main processes.

Sea of Azov - climate and temperature conditions

On the climate of the Sea of Azov, there is a significant inflow of the great steppe expanses of the Holy Ukraine, Peredkavkaz and the Crimea with a dry climate. At Priazov, the average temperature of lime trees fluctuates from +22 to + 24 °, the temperature is from 0 to + 6 °, and the average number of fallen leaves becomes 300-500 mm.

Zvychayno, і the Sea of Azov, a singing rank of positive inflow into the climate of the new territories, which in the bik are connected with the continental. However, after a small area of the Sea of Azov, the flow is not particularly large and is mainly recognized in the coastal areas, which do not extend far into the vast expanses of the land.

As for the great meteorological processes, the Sea of Azov is found in unfriendly minds, and itself: atmospheric vice(So called, "Vі Voєykov"), as far as the sea, the cold mainland wind will be straightened, and it will lead to the freezing of the Azov Sea.

Above the Sea of Azov, there is a charge of dimness of the mid-range and of the winter and of the ocean, of the winter, of the ancient and of the western end of the world, which are linked to the passing of subtropical Atlantic cyclones and the mid-ocean.

Vlіtka, if the mode is set barometric vise, Close to normal, or maybe even normal, and cyclones pass deeper, the sea develops mice circulations near the breezes, so that the wind blows from the sea to the land, and at night from the land to the sea.

For the Sea of Azov, it is usually bitterly cold, but winter is short, m'yake lito With an equal rise in temperatures, heat in early spring, and during the spring, the weather is very common. The average temperature on the Sea of Azov changes between +9 and + 11 °. In addition, the temperature for all areas is the same. Maximum temperature in linden +35 - + 40 °. Move from lit to winter steps. The first frost in Taganrozkiy, but on the wintery Uzbek coast, they advance in the winter, and in the first part of the sea - in the first half of the leaf fall. The temperature can drop to -25 - -30 ° and only in the Kerch region the frost will not overtake -8 ° (if in the vicinity of the rock it can be as low as -25 - -30 °). In the coldest month of rock, in the middle of the millennium, the temperature at sea becomes -1 ° on the northern Uzbek coast of the Azov Sea to -6 ° on the winter.

There is a big round rik on the Azov Sea. Navigate in the middle of the month at least 75-85%.

Parts of the three are made up of vapors, which are close to 1000 miles for the whole Azov Sea.

The most low temperature of the surface of the water ball is spared in the private and remote parts of the Sea of Azov. Winter temperatures - from 0 to + 1 ° for breast-lute, here it rises from 0 to + 1 °, summer - for linden-serpen - from +22 to + 25 °. The temperature of the surface ball of the Sea of \ u200b \ u200bAzov in the western and eastern coastal regions is greater than the temperature and varies from 0 to + 3 °, and gradually rises to + 26 °.

The average water temperature of the Azov Sea at winter is + 11 °, and at midnight it is close to + 12 °. As the sea warms up, the water temperature reaches +30 - + 32 °, and in the middle part +24 - + 25 °. A levy, if the water cools below zero, the Azov Sea will be shrunken. People in іnshі rocky trivaє 4-4.5 months, from the breast to the birch trees. Tovschina ice reaches 80-90 cm. For all ice, the first is to appear in Taganrozkiy zatotsi, then in Utlukskiy, Yeyskiy, Beysuzkiy and Akhtarsk estuaries.

The shores of the Azov Sea and the Taganrozka of the inflow are covered with a suction kryzhany cover. Near the central part of the Azov Sea and in the Kerch region, floating ice.

Azov sea - tvarinny svit

On the banks of the rivers and waters, on the spits of the Sea of Azov, there are abundant water birds - geese, jocks, steppe sandpipers, gulls, red goose, mute swans, curlews, black-headed gulls, gulls, gulls. Near the steppe waters live marsh turtle, lake toad, stavkova toad, deyaki mollusks - boletus, pond snail, Luzhanka, crayfish and about 30 species of ribs.

Vilov ribi, 80 kilograms per hectare of surface in the Sea of Azov, 2 kilograms in Chorny, and 0.5 kilograms in Seredzemny.

Azov Sea is called sea of molluscs... Tse more important dzherelo live ribby. The most popular representatives of molluscs - heart, sendesmia, music.

For biological productivity, the Sea of Azov is borrowed from the first place in the world. Naybіlsh rozvinnosti phytoplankton and benthos. Phytoplankton accumulate (in%): s diatoms - 55, first - 41.2, and blue-green algae - 2.2. In the middle of biomasi benthos, mollusks occupy the dominant camp. Їх skeletal surpluses, represented by calcium carbonate, may signify a pitched wagon in the form of a daily bottom siege and accumulative surface bodies.

Of particular interest is the ichthiofauna. In the Sea of Azov, there are more than 70 species of small ribs, middle ones: biluga, sturgeon, stellate sturgeon, flounder, mullet, tulka, anchovy, ram, ribets, shemaya, different species of bichki.

Tyulka is the most abundant riba in the Sea of Azov, the pitchfork in the vicinity of the rock reaching 120 thousand tons. As far as the growth of all Azov sprat mids is 6.5 billion. Inhabitants of the planet, then the skin gets 15 ribbons.

In the Sea of Azov and in the arms of the river, there are 114 species and species of ribs.

I see the next group ribs:

Ribey, spawning in the floats of rychok (prohidnі ribi) - sturgeon (biluga, sturgeon, stellate sturgeon, ribets, shemaya). Price of the best prices for promislovy ribs.

Ribs, spawning in the lower reaches of the rychok (napivprokhidnі ribi) - pike perch, lash, ram, carp.

Ribey, do not leave the sea (morski) - tulka, whip, flounder.

Ribi, scho playing in the Chorne more (morski) - hamsa, oseledets.

Among the Azov ribs there are hijacks - pike perch, sterlet, biluga. Ale is the main mass of ribs to grub plankton - tulka, anchovy, scourge, lash. In the late 60s and 70s, the salinity of the sea reached 14% due to the arrival of the Chornomorsk waters, at the same time jellyfish were consumed in the sea;

Quite a bit of quilting, as the number of mid-sea species of creatures and roslin before entering the skid. There are more than 6,000 species of organisms in the Middle-Earth Sea, in the Chorny Sea - 1,500, in the Azov Sea - 200, in the Caspian Sea - 28, in the Aral Sea there are 2 kinds of the Middle-Sea organisms. It’s not worth talking about those that the sea steadily passed through the Seredland Sea in the distant past.

Mullet, honeysuckle and hamsa (anchovy) canopies go from the Black Sea to Azovs'k for a year. When the water temperature drops to 6 °, the ribs turn back in the Chorne more. Sturgeon ribi toss іkra, in the rivers Don, Kuban, Dnipro.

flounder- flat ribs, often lying on the ground, seemingly quick and easy to pick up from the color of the stylish surface. At the school of flounder є okremi, the cells are grown, which are changing, changing and changing colors. At the same time, they put on the flounders of the color eyepieces, and the ribs were magicalized to copy their glasses. Tsіkavo, scho slіpі flounder will be the head of the Black Colorado. The stench of yak bi to bang in front of me is tempering and apparently changing the barn. Flounder chomus vvazhayut lonely. It’s unsettling, she has two eyes for good. Vaga flounder up to 15 kilograms, live up to 25 rocks. Tsіkavo, scho її fry may have the shape of a til, flattened at the vertical area; step by step, one side of the ribi started to develop more quickly for іnshu, and the flounder yak bi lyagє on the bik.

Bіlugi krіm great vіdrіznyayutsya still to golіttyam. Live the stench of 70 - 80 years. True, in the case of the pike, which lives up to 200 rocky, and the sea turtle, which is alive 400 - 500 rocky, it is not very big, but in the context of the trivial life of the sea ribs, everything is significant. But I don't know much about how the ribs start out by lusts and by the way of the keys. On the tsikh parts of the tila ribi є ricnі kіltsya, also, yak on the trees. Meta іkru bіluga in quiet little rivers, and in the middle of sturgeon. Іkra їх are highly valued.

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Sea of Azov roztashovane on the European part of Russia. Vono z'єnutsya vuzkoy (up to 4 km), and other (4-3 m) Kerch channel with.

The Sea of Azov is the mildest and one of the best seas in the world. Yogo area - 39 yew. Km2, water volume - 290 km3, average depth - 7 m, best glybin- 15 m.

The sea is quite simple to look at. The pivnichny coast is flamboyant, strong, surrounded by nourishing braids. At the entrance to the Kremlin from the sea, the outflow, which is located by the sea, the Genicheskoy channel. On the first descent, the delta of the Kuban rivulet with great floodplains and numerous channels stretches for 100 km. Richka Kuban flows into Temryukska inflow. At the winter descent, the largest inflow of the sea is Taganrozky, the top of the Don river delta, for 140 km.

Milin of the sea coast to cross into a flat bottom. Glibini smoothly grow from the distance to the shores. Naybіlshі glibini are located in the central part of the sea, glibini in Taganrozkіy zatotsі - from 2 to 9 m. Near the Temryukskiy watercourse there are mud volcanoes.

As far as the whole river stick in the sea (more than 90%) comes from the rivers Don and Kuban. The part of the runoff is important for the spring-summer season.

The main exchange of waters of the Sea of Azov goes through the Kerch channel with. According to the average long-term data, the surface runoff from the Azov Sea is close to 49 km3 of water. The resulting flow of water from the Sea of Azov in Chorna becomes close to 15 km3 / ric.

Klimat gliboko vdajutsya into the land of the Azov Sea is continental. Winter is cold, dry and specotno summer is typical for new. In the autumn-winter season, the weather begins to flow in the direction of the Siberian anticyclone with the crossings of winter and winter-winter periods of 4-7 m / s. Strengthening in the flow of a cold wind is strong in the third (up to 15 m / s) and supervised by intrusions of cold weather. The average monthly temperature is -1 ... -5 ° С, before the hour of winter-late storms, the temperature drops to -25 ... -27 ° С.

Sheds and a bit of heat, the weather is clear with weak winters. At the mid-1000s, the temperature across the entire sea is 23-25 ° C, and the maximum is at 30 ° C. During the season, especially overhangs, the mid-sea cyclones often pass over the sea. 6 m / s, and in some and in squalls.

The main types of bottom extensions in the waters of the Azov Sea are mules, aleurites, sands, shell rock and fall of the small type.
Mules accumulate in the most glibo-water parts, in hydrodynamically calm conditions and occupy the maximum area of the broader. Alevritis є with transient speeches, to replenish the central part with water and accumulate in insignificant parts of the coast and in the innermost part of the Taganroz inflow. Pisky and shell rocks can be maximally expanded on accumulative forms, food and turtle banks, as well as braids and beaches.

Small size and small depths of the sea take in a quick development of the vineyard. After a few years, a corncob has been hitting the ear of the steel, and it’s so fast when it’s back. Chvili are short, steep, in an open sea they reach a height of 1-2 m, sometimes up to 3 m.

Mіzhrіchnі kolivannya rіvnya of the sea, which viznachayutsya pre-construction changes in the storage water balance, becoming a few centimeters. seasonal changes rivnya, in the main, to lay down in the mode. Rіchnyi hіd rіvnya is characterized by its growth in spring and summer months and reduction in growth and charge, swing of the head in the middle 20 cm.

Perevazhayuchi over the sea three victories naganyan zganyannya kolivannya rivnya. The most significant values for the period were indicated in Taganroz - up to 6 m.

In case of sharp changes and weather in the Sea of Azov, there can be winicaties of seiches - vilny standing kolivannya rivnya. Seiches are destroyed on the waterways of ports from time to time.

Those in the sea zbuduzhuyutsya, head rank, vіtrom. Nakhil rivnya, how to turn out in the result of the day, to serve as the cause of compensatory leaks. Near the estuarine areas of the Don and Kuban rivers run-off flows.

From the day of the ancient and ancient-western winds in the sea, the circulation of the waters takes place behind the old winds. Cyclonic circulation breaks down during the winter and winter, which is stronger in the private part of the sea. With the same winds, a little more strong in the northern part of the sea, the current may have an anticlonic character. at weak vitra and still, there are minor leaks in the winter.

Oscillations over the sea overload the weak ones and the small ones, the greatest repetition of the current may occur with the liquidity up to 10 cm / s. With strong winds (15-20 m / s), the fluidity of leaks is equal to 60-70 cm / s.

At the Kerch prototypes, during the winter of winter straight, it is possible to stretch out from the Sea of Azov, and when it is outside the warehouse, it is safe in the sea of the Chornomorsk water. Overvoltage leaks in the prototypes grow from 10-20 to 30-40 cm / s in the most university part. With strong winds, compensation for the leak is developing.

On the Sea of Azov, ice is often set in ice, moreover, the ice cover is strongly accumulated due to the nature of winter. In winter, until the cob, the sternum is set in Taganrozkiy zatotsi. By stretching the chest fast ice rises to bridle the pivnichny coast of the sea, and the trochies piznish - on the other shores. The width of the fast ice swamp is from 1.5 km at winter to 6 km - at winter. At the central part of the sea, there is no more in the end of the day - there is a floating ice on the cob of fierceness; Most of the development of crying out of reach in the first half of the fierce one, if the warehouse size is 30-40 cm, in Taganrozkiy zatotsi - 60-80 cm.

Lodovi mind in the winter to grow unstable. When changing cold and warm povitryan masі of winter floods over the sea, it is not once taken to be evil, and drift of crooked fields, illumination of hummocks. In the middle of winter, the central part of the sea, as a rule, is free from the ice;

The cleansing of the sea from the ice in the midst of winter is seen in the birch trees with a handful in the northern regions and the girly rivers, sometimes at the winter and the most recent - in the Taganroz region. The average triviality of the ice period is 4.5 months.

The increase in water temperature on the surface is negative or close to zero, if the Kerch canal does not move up to 1-3 ° C. During the whole sea the temperature on the surface is the same - 24-25 ° C. The maximum value in lime - sickle the sea reaches 28 ° C, while the coastline can reach 30 ° C.
The shallowness of the sea with a wide widening of the wind and convective mixing to the bottom, so that the vertical temperature rise can be increased: the difference in large drops does not change 1 ° C.

The vast growth of salinity in the minds of the natural tide of river waters could be brought to one-sided, horizontal gradients were promoted only in Taganrozkiy zatotsi, on the outskirts of which the salinity was 6-8 ‰. In the waters of the open sea, the salinity of the water boils between 10-11 ‰. Along the vertical line, in all regions of the city, the cities were spontaneously, in the main, at the link with the high waters of the Chornomorsk waters. Seasonal changes did not outweigh 1, only in Taganroz, but the stench went down because of the inflow of the intra-annual increase in the runoff.

Genera in carbohydrates in the Azov Sea

In the Sea of Azov, there are two regions: the Naftogaz-Indolo-Kubanska, which is shown by one change in the structure of the foundation and the siege cesspool, and the gas-bearing Zakhidno-Ciscaucasian, which includes practically the entire sieve of the aquatorium, for the wine The rest is brought to the Central Peredkavkazkoy gas-bearing region.

The oil and gas content of the Sea of Azov is tied with a wide range of applications. The wine includes the pre-development (triassi) of the transitional (industrial) complex and the creed-Cenozoic comrades of the siege coke of the Skifskoy plate. Based on the data of the deep-sounding drilling and testing of the upper reaches, five oil-and-gas-bearing and promising complexes are seen in the aquatic area: Pre-Cretaceous, Lower Cretaceous, Upper Cretaceous-Eocene, Maykop and mid-Ocene-Pliocene. At the same time, productivity was established only in the Maykop series and in the middle-upper Myocene, in some cases of gases.

Near Zakhidno-Peredkavkazkoy region, in the zone of Azov shaft, Maikopskiy added productive capacity to Morskiy, Nevelikiy, Zakhidno-Beysuzkiy, Beysuzkiy and Streletskiy areas. The gas content of the mid-upper Ocene period was established on Obruchevskiy, Signalnoy, Zakhidno-Beysuzkiy and Zhovtnevoy areas. It means, that on the Beysugskaya area, that є like bi near-cordon and local children of the Azov and Kaniv-Berezansky valleys, the main reserves of gas are tied from the Eocene food-argillaceous settlements of the Tikhoretsk; productive є also low-grade deposits, if the gas reserves in them are insignificant.

In the marine part of the Indolo-Kuban region, the industrial gas content was established in the mid-Ocene clay-carbonate settlements on Pivnichno, Pivnichno-Bulganatskoy, Pivnichno and Shuvaldno-and seismic

All the piles of gasses have appeared in the water area in the interval of depths of 300-1500 m, the vise in them is close to hydrostatic, the cob debits of the drill holes are small and dozens of yews are stored. M3 / add.

A lot of predicted resources in carbohydrates in the Sea of Azov, estimated in 2002, are close to 1.5 billion tons of mine fire (UT), including 757.4 million tons of standard fuel in the Russian sector of the Azov Sea. They are in the Indolo-Kuban Progin - 35.7 million tons of standard fuel, at the Timashovskaya step - 372.8 million tons of standard fuel, on the Azov shaft - 342.1 million tons of standard fuel, and in the Pivnichno-Azov Progin - 6.9 million tons NS.

Until recently, the Sea of Azov was the most productive near the light ribopromislovim reservoir. The Danish hour of won includes 103 vidi and pidvidi ribs. Among them, there are 14 species of rare species, but they know and tough - 7. The number of marine species becomes 39, of freshwater species - 8, anadromous and catadromic migrants - 14, brackish water - 42. Average catches per one or 70-80 kg. In the other half of the 30s of the 20th century, the large catches of “white” and “chervonoi” ribs at the same time reached 140-170 yew. T.

The chief rank of the prince was the beginning of the extremely friendly physical and geographic and hydrometeorological minds, to which they are referred to:

inland growth of the Azov Sea in outside latitudes at the pivdenniy outskirts of the Russian Rivnini;
pomirno-continental climate;
a great surge of total sleepy radioactivity (from 4.9 to 5.3 thousand MJ / m2), positive for ric, which is reasonably high average and ichnu (11.5 ° C and 24-25 ° C for certain);
the nature of the viznacha zokrema intensively in the middle of the mixing of waters;
a great tide of the sea, the flood of river waters filled with biogenic rivers, which will summarize a positive balance;
lowered, approximately three-fold, in proportion to the ocean waters, salinity;
high concentrations in the waters of biogenic salts (extraterrestrial nitrogen in the middle 1000 mg / m3, including mineral - 120 mg / m3; transient phosphorus - 65 mg / m3, including mineral - 9 mg / m3; silica - 570 mg / m3).

By the significant world of the region, the riboproductivity of the Sea of Azov is linked with the appearance of great areas (a large part of which, as a result of hydraulic engineering, has been consumed at once), period і 29% per day) or spring-summer period.

Characteristically, there is a small energy and quick reaction to the smallness of the river flow and processes, but because of the great spaciousness of the hour, not only the hydrophysical parameters, but also the biological characteristics.

In a given hour, the promiscuous catch in the basin of the Azov Sea does not outweigh 40 yew. T, moreover, the basis of the catches is stocked only from small-value species of ribs: sprat, anchovy, whips, as well as aklimatization species - pilengas. Such prices are of sturgeon rib yak, oseledent, ribets, shemaya, lash, carp and іn.

Regulated in 1952, the river Don (the stem of the Tsimlyansk water reserve), a quick drain on 13-15 km3 in the river and the inheritance of the state's activity in the basin of the sea wicked serious negative changes in the ecosystem of the sea.

A decrease in the river flow of the Don River by 30%, the value of a quick turnover of the river has increased the decrease in spawning areas, ruined the production of freshwater species.

The number and the warehouse have changed a lot, coming up in the sea of biogenic rivers, which rose in a stretch of fate. There is a large part of the well-known rivers that were deposited in the Tsimlyansk water shelf; there has been a significant change in the number of sheds that can be introduced into the sea and on the cob of litas; The change in the appropriateness of the mineral forms of phosphorus and nitrogen, and the number of organic forms grew rapidly, it is more important to be absorbed by organisms. Reaching the sea is mostly biogennye speech in Taganrozkiy places and in the smallest number of wine to win at the edge of the sea.

There has been an increase in the concentration of river and sea waters with small, high-grade chemical rivers - phenols, in some areas of the sea - with naphtha products. The most difficult things to do in the adjoining regions of the Don and Kuban rivers and on the aquatic areas adjacent to great ports... Significant ecological changes have led to a sharp decline in the biological productivity of the sea. The forage base of the ribs has changed, the catches of the fish have quickened, in the main, the most valuable species of ribs.

Vodogospodarska situation in the basin of the sea velmi is loaded. In a given hour in the sea, in the middle, close to 28 km3 of river water in the river. With this kind of runoff, there is a possibility of saving salinity in the borderlands of 13-14 ‰. Further, the growth of water supply in the pool with unacceptable waters, the splinters of the vortex, the growth of salinity to the level of the Chornomorsk and the result of the loss of minds for the habitation of the most valuable marine organisms.

The Sea of Azov, especially this Russian part, is a zone welcoming for the accumulation of the young polyutants themselves, for everything that the bottom of the pool may be significantly covered by the silt of a different warehouse, so that you can accumulate versatile people. At the same time, in the Russian part of the given basin, there are a large number of main dzherels of significant problems. Price, persh for everything, great rivers Don and Kuban, as well as a number of small ports in the middle and such a great center, like Rostov-on-Don. Mayzhe all of these began to grow in Taganrozskiy zatotsi, moreover, Mariupol, which is one of the most basic problems, in the territory of which it is seen and in the Russian part of the inlet. In addition, Taganrozka inflow is the greatest on the Sea of Azov, the length of abrasive shores, a lot of delays, which are very strong until catastrophic growth. In such a rank, Taganrozka inflow і th coast є the most ecologically stable in the whole Azov Sea. More other zones and hardships, tied to the wines of pollutants from the land, are heading to the front of the Uzbek coast of the Kuban and at the throat of the channel, drooping, where the water comes from the rice checks.

The more important place in the Sea of Azov for the nature of the hardening of the loan is especially the smuga aquatoria - the route of passage of ships from the Kerch Channel to Taganrozka Zatoka. The area on the Russian Uzbek coast of the Azov Sea is especially special in the sense of ecology, the zone of the Kuban floods from Primorsko-Akhtarsk to Temryuk. Over the last 100 years, the entire region was experiencing catastrophic flooding before the hour of surges during storms from the beginning.

recreational resources

The vastness of the Azov Sea (in the boundaries of Russia) becomes close to 1000 km and there is a great territory in the boundaries of the Rostov region and the Krasnodar Territory. The coastal zone of the sea has become friendly with natural and climatic minds for the development of recreational government. Recreational resources of the rural territory and Skhidny Priazov, madly, play the popular resorts of Chornomor, albeit, with respectful consideration, would like to make singing additions in the first place active support population. In the past few years, it is possible to docilely vikoristovuvati for the establishment of completely recreational types of systems (tobto only for recovery), the organization of recreational-resort areas can be deprived of mineral waters and mud. friendly natural mind(Sleepiness, warmer sea, food on the beaches, the appearance of balneological dzherel) provide a convenient way for organizing the situation, tourism and, perhaps, people who are well-off. For the improvement of recreational facilities of the territory, it is necessary to update the robot on the basis of the regional programs of recreational nature rational victoriannya coastal zone.

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The Sea of Azov in Russia became visible in the 1st century. e. Our ancestors called it the Sinu more. For that reason, as the principality of Tmutarakanskoe was established, I will call it Rosyyske. In the fall of this principality Bagatorazovo changed the Azov Sea. Yogo was called Mayutis, Salakar, Samakush, etc. On the ear of the 13th century the Saksin Sea appeared. The list of Tatar-Mongol conquerors has been updated. The stench was called yogo Balik-dengiz (in the cross-section - "Ribne sea"), and also Chabak-dengiz (Leshcheva, chabachye sea). For some kind of views, as a result of the transformation, the word "Chabak" was transformed into "aziv", the sounds and sounds are the current name. However, it is not approved by any means.

Naybilsh is worthy to vvazhaєnja pokazhennya uchasnaya name from the place of Azov. Just an hour of the famous Azov hikes, which were visited by Peter I, called the tse zakrypilsya behind my water.

Salinity of the Sea of Azov before and after the regulation of the Don

In the first place, when the flood of water flows from the river (it can become up to 12% of the outgoing water supply), and also the foldability of the exchange with the Black Sea is formed by the hydrochemical features of such waters, like the Sea of Azov. The salinity of the yogo bul is three times less, below the average salinity of the ocean, to the regulation of the Don. From 1 ppm to 10.5 and 11.5 (apparently, in the Don Gulf, in the central part and near the Kerch channel), the value changed. However, because of the fact that the Tsimlyanskiy hydrovuzol was built, the salinity of the Sea of Azov began to grow rapidly, having been stored in the central part up to 13 minutes. Ridko reach at a whole 1% of the seasonal number of values.

Sea of Azov water

It is not enough salt to take revenge in your waters of the Azov Sea. Salinity is the main factor, through which it easily freezesє. Until the appearance of krigolami tsіkaviy for us water, the bula is unsuitable in the period from the chest to the middle of the week. Water resources Sea of Azov in Yakost Morskoy Way that vikoristovuvalis deprived in the heat of the time of fate.

Practical all the most significant rivers, which fall into the new, boules stretching the 20th century, barricaded rowing alongside the stem of the waterways. The whole fact was called up to the fact that the mule was thrown off and the good water was quickly quickened.

Water balance

Basically, due to the influx of the fresh waters of the small rivers, atmospheric falloffs, which fall over the sea, and also from the intruders of the waters of the Black Sea and vitrates on the stick and vaporization through the Kerch canal, to fill the water regime with such water, as the sea Coming in the rank of viglyadє yogo Kuban, Don and іnshі rivers, which flow into the whole sea, bring a total of 38.8 cubic kilometers of clear water. 13.8 warehouses on the surface of the middle of a large number of falls from the atmosphere. Shchorіchno through the pouring in of water approximately 31.2 cubic meters. km. Tse resources of the Black Sea. From the Sivash through the channel under the name Thin, in addition, to approach the sea for about 0.3 cubic kilometers. 84.1 km warehouse Vitrate is stored from a number of vipars from the surface (close to 35.5 cubic km) to the drain through the Kerch channel (47.4 cubic km), and also to the Sivash through the Tonky channel (1.4 cubic km). Tobto wine is also expensive 84.1.

Putting a rychkovy drain to a zahalny yogo obsyagu

At the same time, the river runoff becomes the best of the best seas on the planet. As the hopefulness of atmospheric and rychkovy waters overshadowed the vapors from the surface, it called for the growth of water and the growing definition, as the water exchange did not boil over the Chorny sea, as a result of which the rinse was raised.

Rospodil salinity of the Azov waters

Let's start with the rank of rozpodіlen in Danish hour in such water, like the Sea of Azov, salinity. Vaughn reachє 17.5% on the depths of the Prikerchensky district. Here you go to the best of the Black Sea. Here the salinity becomes 17.5%. The central part of the third parameter is unidirectional. The Danish indicator becomes 12-12.5% here. The territory of 13% is insignificant. The salinity of the water up to the mouth of the Don (the river, the yak in the Sea of Azov flows into the sea) decreases to 1.3%.

On the cob of lithium and overhang through the tannins of ice, as well as the flow of water in the sea of river waters, the salinity of the trocha decreases. The collection and recovery are approximately the same from the surface to the bottom. The most salinity of the Azov Sea water spontaneously in Sivash, in the

Glibina of the Azov Sea

The Sea of Azov is carried to flat. Vono is a man of the poor, they grabbed the Uzbeks with little water.

The most glibine of the Azov Sea does not vary by 15 meters, and the average is located at about 8 meters, while the area is up to 5 meters, while it occupies the territory in the size of more than half of this area. The length of the sea is also small, becoming 320 cubic meters. For example, for a person who can turn over the Aral Sea by a factor of 2 and beyond. Mayzhe is 11 times more than the Azov Chorne, and beyond the obsyag - as much as 1678 times.

Sea of Azov, prote, zovsim is not so small. For example, two such European powers, Yak Luxembourg and Netherlands. The maximum length of the sea is 380 kilometers, and the width is 200. 2686 kilometers is the long distance, as there is little coastal line.

Pidvodny relєf

Velma is simple on the sea. Basically, smoothly and more often the sea grows in the world from the distance to the shores. The characteristics of the Sea of Azov from the point of view of the relєfu are offensive. Near the center of it there are the most glibini. The bottom є is practically flat. The Sea of Azov is becoming a flood of water, the greatest of those є Temryuksky, Taganrozky, as well as Sivash, are very strong. The rest of the correct bulo used the estuary. There are practically no great islands on the Sea of Azov. There are a number of miles, which are often flooded with water. Roztashovanі stench bіlya shores. For example, the islands of Turtle, Biryuchiy and іnshі.

This is the main characteristic of the Sea of \ u200b \ u200bAzov from the point of view of salinity, glibin and relief.

Wellness by the sea

Oskilki, yak mi vzhe zgaduvali, Sea of Azov є druzhe dribnim, water stretching last month in the new get warm. Look for a bit of degrees warmer, lower, for example, in Chorny. M'yaky klimat and wonderful weather will be optimal for a resort, roztashovani on uzberezhzhi.

The water of the sea is vvazhaєtsya all over. Besides, it is also possible to take revenge on the lack of words, as they infuse it beneficially on human organism. Lead Volodya the great number of the Corinthians chemical elements During the bathing process, they seemingly penetrate into the body through the surface of the shkiri.

Bathing in the sea, in addition, is a priceless hydro massage. Pomirniy і steep mode of sleepy vipromynyuvans, which is characteristic of Priaz, allows you to take a course of sleepy baths on a regular basis. This is the best place for the whole - the beaches of the Azov Sea.

From us you can create a holiday, so that you can use water in a vidminny misem to improve your health. There are some reasons here for the prophylaxis of young heart-bladder ailments, as well as positively on the body, to improve its tone.

Sea of ​​Azov. Sea of ​​Azov: Corinth of power, walking and Glibin of the Sea of ​​Azov

Azov Sea

History of the sea of ​​Azov

Sea of ​​Azov - geological minule

Azov Sea - geography

Bathymetry of the Azov Sea

Geographical ob'єkti of the Azov Sea

Take care of the sea of ​​azov

Wandering the Uzbek Sea of ​​Azov

Pivdenne Uzbek Sea of ​​Azov

Skhidny coast of the Azov Sea

Delta Don

Pivnichne Uzbek Sea of ​​Azov

Azov Sea - water

Water regime of the Azov Sea

sour mode

Chemistry warehouse

Sea of ​​Azov - climate and temperature conditions

Azov sea - tvarinny svit

Genera in carbohydrates in the Azov Sea

recreational resources

Salinity of the Sea of ​​Azov before and after the regulation of the Don

Sea of ​​Azov water

Water balance

Putting a rychkovy drain to a zahalny yogo obsyagu

Rospodil salinity of the Azov waters

Glibina of the Azov Sea

Pidvodny relєf

Wellness by the sea

Sea of Azov. Sea of Azov: Corinth of power, walking and Glibin of the Sea of Azov

History of the sea of Azov

Sea of Azov - geological minule

Take care of the sea of azov

Wandering the Uzbek Sea of Azov

Pivdenne Uzbek Sea of Azov

Pivnichne Uzbek Sea of Azov

Sea of Azov - climate and temperature conditions

Salinity of the Sea of Azov before and after the regulation of the Don

Sea of Azov water