Introduced, general characteristics of the Chornomorsk uzberezhzh, physical and geographic position - rozrobot tourist tour

Geographic features of the Black Sea

Long ago the name of the sea - Pont Aksinsky(Πόντος ξενος, "The unworthy sea"). In "Geography" (7.3.6), it was transferred, so I call the sea through difficult navigation, as well as wild witchcraft tribes that inhabited its shores. Protestingly, for all the Greeks, they took the name of the sea, which represented the reflex * axšaina- "dark blue", "dark", which was referred to by its ninth name, and re-interpreted him for the "sound" word from the wickedness. Formerly, after the long-distance development of the shores by the walnut colonists, the sea became known as Pont Evksinsky (Πόντος Εξενος, "Hotel Sea"). However, Strabo (1.2.10) є clues about those who in antiquity called the Chorne the sea and simply “the sea” (pontos).

V Old Russia In the 10th-16th centuries, the name “Russian Sea” was introduced in the writings of the literature;

The occasional name "Black Sea" has been shown in large numbers: Μαύρη θάλασσα, black sea, Marea Neagră, Black sea, Karadeniz, Chorne sea, Amshin Eina that in. Naybilsh early dzherela, the name should be guessed, it should be mentioned before, the protest signs of the fact that it was victorious and earlier. There are a number of hypotheses for the reasons for the denunciation of the following:

Turks and іnshі conquerors, who became magical about the population of the coast of the sea, made fires from the side of the Adigis (Circassians), Abkhazians and other tribes, for which they called the sea Karadengiz - Chornim, innocent.

For some reason, on the thought of a number of glimpses, it may be the fact that before the hour of storm the water in the sea is very dark. In the meantime, storms in the Black Sea are not even more frequent, but dark water before the hour of storms in all seas of the earth.

Another hypothesis of a prodigy name is to be grounded on the fact that metal objects (for example,), dropped into the water of the sea more than 150 m for a trivial hour, were covered with a sludge of black color of zavdyaki diya.

Our hypothesis is tied to the "kolinny" known sides taken from a number of Asian regions, de "chorny" meaning the beginning, the Chorny sea is the ancient sea.

One of the most widespread hypotheses is about those that the name was tied up with a fortune about cutting out the Bosphorus 7500-5000 years ago, after all it was catastrophic to move the sea to a 100 meter high, so that it was filled with great ...

It’s a Turkish legend, the rich man sleeps in the waters of the Black Sea, like a buv of thundering thudi for the passage of the wandering charmer Ali. Through the whole sea, to swallow, magayuchis viplesnuti from their glybin deadly zombies, and to get into the black color.

Geography

The shores of the Black Sea are few and far between, mostly in the private part. єinium great p_vostr_v- Krimskiy. Most inflows: ,,,, і in Ukraine, і in Bulgaria, і - at the northern coast of the sea, in Turechchina. At a wine and a wine visit, when the rye falls, it is bottled. Zagalna coastline - 3400 km.

A number of dilyanoks of the Uzbek sea may be called powerfully: in Ukraine, in Russia, and in Turechchina. At the entrance and the initial entry of the coast, the coast is beautiful, with a little curvature; c - in the main lowlands, behind the vignette of the ancient mountainous shores and the east coast at sunset. On the sloping and ancient shores to the sea, there are a lot of roads and mountains.

There are few islands in the Black Sea. samiy great island, Yogo area 62 km². The Rashta of the island is nabagato less, the most - і (offending area less than 1 km).

The Chorne Sea has some of the most rivers flowing into it: ,,, as well as more waterfalls ,,,, (Kodor), (at the descent of the sea) ,,,, (at the beginning), (at night).

Geology

The Black Sea will keep the isolated depression, it will rise between the Pivdenno-Skhidnoy Europe and the Eastern Europe. The tsia depression was established in the era, in the process of active, that it divided the ancient ocean into splinters around the waters (in which, the edge of the Black Sea, was established, and the sea).

One of the hypotheses of the Black Sea (zokrema, visnovki participants in the international oceanographic expedition on a science ship "" in 1993) testifies that 7,500 years of that were the most important on the earth. After the end of the breakthrough, the Bosphorus is the isthmus of the breakthroughs. The boules were flooded in a total of 100 yew. Km² (nyrodyuchіshі earthі, alsoprobluvanі). The flooding of the cikh of vast lands, perhaps, became the prototype of the myth of Fr. Winning of the Black Sea is well known due to the great hypothesis of the huge bend of the whole freshwater living light of the lake, the product of which is distributed is the reach of high concentrations at the bottom of the sea.

The Chornomorska depression is stored in two parts - ancient and skidnoy, distributed to children, and by natural advancements. Pivnichno-western part of the sea is characterized by a remarkably wide smog (up to 190 km). Pivdenne uzberezhzha (how to lay out Turechchina) and skidne (Georgia) are more steep in nature, the smog of the shelf does not extend 20 km and is surrounded by a number of canyons and depressions. The depths of the coastline grow rapidly towards the edge, reaching up to 500 m above the coastline in decile kilometers. The maximum sea level (2210 m) is accessible to the sea in the central part, for a day off.

In the warehouse girskikh breeds, They store the bottom of the sea, in the coastal zone they reload the coarse detritus: ,,. From the distance from the shore, there is a drop in grain size. In the wilderness-western part of the Black Sea it is widely widened; for schilu and bed sea ​​trap Extra-fine pelitic mules.

In the middle of the main cinnamon copalins, lay them on the bottom of the sea: and on the wilderness-western (, Uzbek Caucasus).

Hydrology and Hydrochemistry

The Black Sea is the most meritorious in the world (with unmixed water) with my water. The upper ball of water (), so to lie down to a depth of 150 m, more cold, less salty and less salty, brooding, comes out of the lower, more warm, salty and thick, full of water ball.

A single out-of-the-box explanation of a walk in the Black Sea is still there. Є Dumka, in the Black Sea, to become a leading rank as a result of life, a sharp turn of water and a weak vertical exchange. It is also the theory that water has become established in the results of the freshwaters, which died when the salty waters of the Middle Sea were penetrated by the hour of education and science.

The deyaky of the last rocky years allow to talk about the Chorna Sea, as the giant reservoirs are not just sour water, but, as you see, it is better for everything, also in the process of microorganisms, as well as from the bottom of the sea.

The water balance of the Black Sea is composed of the offensive components:

The lower ball, inasmuch as we live in water, does not take revenge on living organisms, behind a vignette (a product of life and water). Salinity here grows up to 22-22.5 ppm, the average temperature becomes ~ 8.5 ° C.

In the circuit of the Black Sea flows, there are two magnificent closed circuits with a length of 350-400 km. In honor of the first to describe the scheme, they called it "Oculyari Knipovich."

climat

Climate of the Black Sea, in conjunction with the middle continental camp, in the main. and the winter coast of the Crimea is captured by the mountains from the cold winter winters and every summer, and on the winter road from Tuapse -.

Significant inflow on the weather over the Black Sea is over the Atlantic Ocean, over which a great part of cyclones will arise, which will bring bad weather and storms to the sea. On a winter-shady Uzbek seaside, especially in an area, there are no mountains for the cold weather povitryan mas, Yakі, perevaluyuchis through them, amumovlyuyut strong cold wind (), the inhabitants of the city call it Nord-Ost. During the winter and old days, invite you to the Chornomorsk region to bring warmth and supply to the Chornomorsk region. Yak pidsumok, a large part of the sea is characterized by the warmth of the winter and the more dry summer.

Sered ribs, which can be found in the Black Sea: small vids (scourge-golovach, scourge-batig, scourge-round, scourge-martovik, scourge-rotan), Azov hamsa, Chornomorska hamsa () ,,, five species ,, (hack) ,, (Zvychayna Chornomorska Sultanka) ,,, Chornomorsko-Azovska, Chornomorsko-Azovska ,, and ін. Zustrіchayutsya (biluga, stellate sturgeon, Chornomorsko-Azov (Russian) and Atlantic sturgeon).

In the middle of the not safe ribs of the Black Sea - (the best is not safe - the cut off spines of the dorsal fin and the chopsticks);

Deyaki vidi tvarin, as they do not live in the Black Sea, are often brought into the new one through the channels of the Bosphorus and the Dardanelli flow, or they flood independently.

Economics

transport value

Great transport significance of the Black Sea for the economy of powers, which is washed by the cim water. A hundred and a half of seafarers will be able to make flights, so that they will not be able to export from ports of Russia (in the first place) and ports of Georgia (). Witm, obsyagi vyvezennya is often streamed interconnected throughput channel Bosphorus and Dardanelli. The most important naphtoterminal with naphtha intake within the framework. It is also possible to find out about the projects of building naphtha pipelines and bypassing the Chornomorsk ducts. Naftothermіnali Novorossiysk zdatnі accept.

Krym naphtha and products and processing, from Russian and Ukrainian ports of the Black Sea, to transport metal, machinery and possession, lis, grain and іn. The main duties imported to the Chornomorsk port of Russia and Ukraine fall on friendly comrades, food products, a number of native goods and in.

The Chornomorsk Basin has a wide range of containers for transportation, and there are large container terminals. Transportation for assistance is being developed; pratsyuє zaliznichnі () - () і () - (). Rozvineni in the Black Sea and sea passengers transported (in the meantime, when there is a drop, they have significantly decreased).

An international transport corridor (Transport Corridor Europe - Caucasus - Asia, Europe - Caucasus - Asia) passes through the Chorne Sea. Chornomorsk Port є Kintsev points a number.

Promislove ribalism

In the Black Sea, promises are made of the following types of ribs: mullet, anchovy (hamsa), mackerel, horse mackerel, pike perch, lash, sturgeon, oseledts. Main Ribal ports: Odessa, Kerch, Novorossiysk and ін.

V the rest of the rock XX - the ear of the XXI century Ribnium promissed signifi- cantly speeding up the journey of the Perevilov Ribi and the destruction of the ecological camp of the sea. I mean the problem is also the harrowing of the bottom of the trawling, especially the sturgeon. So, only after another period 2005 by the fakhivtsi of the Chornomorsk State Basin Administration for the Protection of Water Living Resources of Ukraine ("Chernomorribvod") on the territory of Crimea bulo rozkrito 1909 collapses of the Ribbon Legislation, vilucheno 33

recreational value

friendly climatic mind in Prychornomor'i to summarize the development of an important resort region. To the largest resort areas on the Black Sea, there are: (,,,) in Ukraine, (,, in Abkhazia, in Georgia, and in Bulgaria, in Rumunia.

Chornomorske uzberezhzhya Caucasus є the main resort region Russian Federation... In 2005, the number of tourists was close to 9 million; In 2006, according to the forecasts of officials, the Danish region was not less than 11-11.5 million respondents. On the Russian Uzbek coast of the Black Sea there are over 1000 boarding houses, sanatoriums and hotels, and their number is gradually growing. The natural advancements of the Russian Chornomorsk uzberezhzhi є uzberezhzhi, the most popular resorts such as boules are popular in an hour. The development of the resort industry on the Chornomorsk Uzbek coast of the Caucasus is being streamed by an altogether short (for example, in times of the Middle Earth Sea) season, ecological, transport problems, and in Abkhazia it also caused a new status of Georgia.

Ecology and protection of nature

Uzberezhzha of the Black Sea and the pool of the river, which flows into the new one, є areas with a high anthropogenic inflow, which have been populated by people since ancient times. the Black Sea camp in the whole unwelcoming.

Among the main factors that destroy the level of the environment in the ecological system of the sea are the following:

Stronger obrudnennya flow into the sea rychok, especially with runoffs from the fields, to avenge the mineral goodness, especially i. The process of over-fertilization () of the sea waters is not easy for itself, and, as a heritage, - the growing growth of phytoplankton ("color" of the sea - intensive development), a change in the penetration of waters, the collapse of high-water weeds.

The obstruction of the waters of the sea by the entrances of human life - the discharge of unpurified or insufficiently purified, etc.

Masoviy Vilov Ribi.

Zaboronene, ale everywhere, the bottom of the trawl is victorious, where the bottom of the biocenosis is living.

Change of warehouse, change of number of individuals and mutation of water light due to the introduction of anthropogenic factors (including replacement of root species natural light exotic, scho z'yavayutsya as a result of the flow of people). So, for example, for the assessments of fahivts from Odessa PivdenNIRO, only for one ten years (from 1976 to 1987), the population of the Black Sea bottlenose dolphin passed from 56 thousand to seven thousand individuals.

On the thought of a number of fakhivtsiv ecological camp of the Black Sea over the last ten years, it has gone unimportant to the decrease in economic activity in a number of the Black Sea regions.

President of the Crimean Academy of Sciences Viktor Tarasenko, having caught the thought, the Chorne Sea is the most difficult sea in the world.

to guard dovkilla in the Black Sea region, it was accepted for pleasure ("Agreement on the Conservation of the Cetaceans of the Black Sea, Mediterranean Sea and Contiguous Atlantik Area"), one of the main food is protection і.

The main international document, which regulates food protection of the Black Sea, is written by the Black Sea regions - Bulgaria, Georgia, Russia, Rumunin, Turechchina and Ukraine in 1992 (Bucharest Convention). Also in 1994, representatives of Bulgaria ,,,,,, Rumunia ,,, Ukraine and Art. Yak the result of the values ​​\ u200b \ u200bwill, bully svoreni (), i (). Donate to organize the function of coordinating nature conservation programs, and to get together within the framework of the conventions.

The International Day of the Black Sea is celebrated in all the regions of the Chornomorsk region.

Chorne more (structure of water spheres)

The bottom of the Black Sea from the surf and up to 120-200 meters of water is, for a small blame, a gentle grab. Tse so ranks the shelf. We all have a drink in the most milky part of the shelf, de skeli and іsok. Glibshe at the bottom of the shelf zalyagaє mule.

The shelf is shaved off in the Caucasus region by steeply steep ledge 2.5-10 kilometers from the coast, some distance. The lower part of the ledge is buried for 500 meters. The ledge is much less sedimentary - the stench accumulates from the first person in a wide plume - and it is like a bi stin, heavily sprinkled under water canyons, start to grow against the great rickets.

Such concessions are spared not only in the Black Sea, but near all continents and large islands. Х glibini insignificantly grows one out of one, which gave me the idea of ​​the advancement of the Holy Ocean the geological hour will stop.

Geologists and oceanographers will tie the phenomenon to the tannins of the ice dweller Europi in the quarter period. Obsyag the ice of the ice-dweller behind the smallest pidrachunks, which will be sufficient, so that they can move the ocean by 75-100 meters. Yakby, for example, having roasted the ice cover of Antarctica, the ocean rim moved by 60 meters.

One hour, from the rising of the ocean, the river, the sinking coast near the Chornomorsk ugovina, fill the ice with the water and the rychok water. (The water of the Black Sea in antiquity was mostly dull, and it is less saline hour by hour.) The continuation of the river valleys on the bottom of the sea (underwater canyoni) to a depth of 500 meters is expected to rise.

Behind the ledge, 500 meters from the road, the bottom becomes flat and slopes towards the sea step by step. It is abysal, tobto glibokovna area is covered with a ball of a mule of old times.

At the sea level, it is close to 2 kilometers, approximately parallel to the Caucasian birch tree, under the bottom of the Black Sea, the continental skil ends up earth measles... Far from the mainland, it began to turn into a thinner basalt shell, which whistled the bottom of the oceans and was called an oceanic type crust.

Even in the old days, seafarers, plowing the waters of the Black Sea, marveled, why, from the great glibines, the metal yakir was found to be poured with black nalot. They were astonished, and could not explain the phenomenon.

In 1890 rotsi glibovodna expedition of the Russian hydrograph I. B. Shlindera carried out in the Black Sea prospect and vivchennya of sea glybin. The expedition set up, about 100-200 meters from the mountain, and to the very bottom of the Black Sea water is filled with water. It became zrozum_lim, why anchors from chorn_li metal. Having eaten in the middle of the water, the stench was covered with plavkoy sulphide of zaliza.

We have been respecting the Chorne Sea in a whole lot of different worlds at once. Ale now sirkovodneve infection has been established in the valleys of the Caspian Sea and in the central part of the Arabian Sea - the walled edge of the one named after it. A number of important allowances are made for the infection of large areas of the sea basins in the past geological era, which was widened wider.

The glibina of the upper boundary of the waterborne contamination of the Black Sea is unsettled. At the middle part of the sea, the wonders are 80-100 meters, the coastline of the Caucasus is 200 meters, and the coast of the Crimea is 150 meters. In such a rank, the surface of the razdilu will make a shape. Down there is water flowing up to the most glibin, tobto 2245 meters.

The Sirkovodneva area of ​​the Black Sea is uninhabited. In such, relieved sourness, water cannot live with organisms, except for some bacteria. The life of cich bacteria is based on the presence of inorganic spoluks of the seed, the salinity of those elements, which they call sulfur bacteria, iron bacteria and so far - in the fallowness of the one that smells like smell.

Comrades, the waters of the Black Sea are divided into three balls: upper, middle and lower - sirvodnevy.

The upper ball up to 40-60 meters in height, subdued up to the seasonal temperature of the surface: from 7 degrees Celsius up to 24 hours, and from the coast in the Caucasus up to 29-30 degrees. With the glibinous temperature, the temperature rises. At 40 meters, the temperature changes from 8 degrees to 11 degrees. The whole ball of water can lower salinity, and lie lower.

The middle ball is stretched from 40-60 to 100-150 meters. There is a permanent cold here. At our glance, it was sighted. For children of ribs, the temperature of the driving ball is suitable - 6-8 degrees tsiliy rik... Tsikavo, the lowest temperature of the water, and it starts to rise in the middle of the middle ball. Kisnyu here is half the size, lower in the near-surface part of the sea. The water is more warm - up to 9 degrees - and so it will be found in the sphere of the water.

Why does the temperature go down in the middle of the ice?

On the right, at a depth of 100 meters in the Black Sea, there is a breakdown of waters: the upper mens are salty, they are filled with boards, rychki, and big salty waters, which come here through the channels of the Dardanelli and the Bosphorus Midland Sea... Vertical circulation of water at a low temperature is lost in the boundaries of the upper ball, so yak mensh salt water, Navit herself is cold, she is lighter than salty. The axis of the won і piles up at the viglyadі cold prodigy like a salty ball of water. At a glybin of close to 100 meters of intensive mixing does not occur, and the interface between the upper and middle ball is very fast and it is easy to be analyzed as an analysis of water from low glybin in terms of temperature.

In such a rank, the cold water will be charged up to salty water, the water will be heated up to 9.5 degrees over the course of a year, and the cold water will melt, if it does not warm up to a quiet 9.5 degrees and will not wander into its deep cold, wintry.

In such a rank, the Black Sea is like a double-topped one with a thickened waterway, where the sea organisms descend upon arrival.

Top on top of the center of buds, warm in last hourі cold vybku, inflow to populate with ribs from the Seredland Sea.

Lower on top of the permanent colonization of cold-loving ribs - the so-called Boreal-Atlantic forms. The charge, if the temperature of the balls rises, the cold-loving ribs populate the upper top.

Cold-loving ribi є rulers of the Black Sea of ​​their own

In the first place, the one who lingers in the new tsiliy rik, in a different way, the one who was settled earlier, having arrived from Atlantic Ocean in the beginning of the tretine - the ear of the quarter era, sending water from the Sered-earth Sea through the Dardanelli and the Bosphorus.

Small salinity due to difficulties in water exchange with the Black Sea and the great tide of river waters. There is one more argument for the birch birch ...

Economic and transport significance of the Azov Sea

Inflow to the natural specialties and gospodarske vikoristannya. All the same, I will give great respect to ...
... 18% o), in Azov it is strongly discounted (11% o). Maximum glybin Black Sea - 2245 m, yogo mirror is 423 yew. Km2.

Geographical position of Russia

At the first entry of the Russian Federation, sea cordons pass through the waters of the Azov and Black Seas, which lead Russia to Ukraine, Georgia, Bulgaria, Turechchinoy, Rumuniyu.
Geographic features economical links are provided by transport options.

Entry

A tour of insurance for people with average and high incomes, such as cruises, one of the best looking for tourism. In every way, people are in any case, because they have no problems with their quality.

Type of road: route є kіltsevym, bagatodennym, ecologo-pictorial.

Find more expensive:

· Satisfy the needs of the child on the sea;

· Enjoy fun and colorful excursions.

The route is valid during the period from grass to zhovten, if the swimming season is three.

Road route: Sochi - Tuapse - Dzhubga - Gelendzhik - Novorosisk - Anapa - Sochi.

The triviality of the trip is 10 days / 9 nights.

> Zagalny characteristics of the Chornomorsk uzberezhzh

> Physical and geographical position

The route of the Prolyagaє vdovzh of the Chornomorsk uzberezhzh of the Krasnodar Territory. Route: Sochi - Tuapse - Dzhubga - Gelendzhik - Novorosisk - Anapa - Sochi.

Chornomorske uzberezhzhya Rossii (Chornomorske uzberezhzhya Rossiya (Chornomorske Riv'era, Russian subtropics) is a pristine smuga coast in the Krasnodar Territory of the Russian Federation and the Black Sea and the ridges of the Great Caucasus. Roztashovans in the subtropical zone and on a larger part of their length - the resort area.

The length of the Chornomorsk Uzbek coast of Russia from Tamansky p_vostrov to Adler (cordon of the Republic of Abkhazia) to become close to 400 km from the time of the coastline. There it is close to 145 km (36.3%) to enter the warehouse of Veliky Sochi, including the beach smog Sochi to become 118 km - this is the name of the Russian Riv'era. The Russian dilyanka of the Chornomorsk uzberezhzhya to the Caucasus of the rostrum at the extreme pivnіchnіy part of the subtropical belt. Smuga of Anapa-Tuapse of the Chornomorsk Uzbeks of Russia is one of two dry subtropical regions of Russia, the order of the Caspian Uzbeks of the Republic of Dagestan. Smuga Tuapse-Sochi is the only one in Russia and the most recent region in the world of subtropics.

At the extreme winter, the coastline of the Chornomorsk Uzbek coastline is zivist, lowland, є without pain (the Kuban delta), plain lakes and salty estuaries (Vitiazevsky estuary and іn.). Little food mows, milines, drifts, drifts, islands, pivostrovi (Taman). Pislya Anapi shores take on a girsky character, two great harbors (Novorosiska bay and Gelendzhik bay). The coastline of Gelendzhik has a natural character, digesting small rivulets and cones for small rivulets, which flow from the Caucasian ridge in the Chornya more. At a few moments the coast is rugged and skeletal, you can see Eagle's skeletons near the place of Sochi. The peculiarity of the Chornomorsk Uzbek coast of Russia is the presence of decile types of beaches on an altogether short 400-km distance. Here they are fine sand, rough large pebbles, bays and slopes. In the Anapi area there are beaches with quartz peaks. (Http://ru.wikipedia.org/)

The water resources of the Chornomorsk uzberezhzhya value, ale rozpodіlenі stench on the territory nerіvnomіrno. One part of the district is rich in richkov, іnsha water resources bіdna. The agro-industrial complex gives 50% of the production to the district. Central to the region of the country, develops subtropical cultures: tea, pomegranates, citrus fruits, persimmon, іngir. Friendly and versatile, soil-climatic, and allow you to grow in the territory of the region of rural agricultural culture, the head of which is winter wheat and corn. Among technical cultures, the main one is the sleepyhead ( Krasnodar Territory). Chornomorske uzberezhzha - a great region of viticulture; here you can find all the vineyards of Russia. The creation of a high level development. For the population of thinness and productivity, one of the advanced regions of the country.

Water resources are evaluated on a factor-based and integral basis. At the same time assessing the fallowness due to the nature of the recreational activity, in which vicories are: beach-bathing solutions (for health-improving purposes) and the growth of water tourism,

Short rivers of the Chornomorskiy district (Makopse, Shahu, Khosta, Sochi, Matsesta and іn.) That is why the main health-improving natural resource is the sea. The swimming season is three months from the middle of the grass to the middle of the end of the day from the temperature of the water from +18 to +24 degrees, in the vicinity of days to +29 degrees. The season for the implementation of the route depends on the swimming season.

The link with the heterogeneous landscape-geomorphological minds of the Uzbeks extends to a number of natural-recreational areas. From the western edge of the Tamansky Pivostrov to Novorossiysk Uzbek lowland, the shores of abrasive-sunshine and accumulative beaches with a width of 10-15 m, and in the surrounding areas up to 100 m and more (Anapa). The distance from Novorossiysk to Sukhum (about 450 km), the Uzbek coast is the abduction of a ravine of small width, which is connected to the front of the Great Caucasus. From Novorossiysk to Tuapse Uzbeks are wider (from 2-3 to 5 km), flat or slightly sloping. From Tuapse to Sukhum, it sounds intermittently up to hundreds of meters. On the bagatokh dilyankas, they are steep, in front of the gir'ya, the mayzhe vprytul go to the sea (Gagra). In the area of ​​Pitsundi of New Athos, Uzbeks expand up to 3 - 8 km. Such dishes of the Uzbek are timed to the cone to the wine, and hanging in the sea with misses. Throughout the stretch of the Uzbek coast from Novorossiysk to Sukhum, they reload the abrasive and abrasive-dry shores of the deep-water aquatic areas, where they can be equipped with accumulative dylyankas in the little ones. Uzdovzh uzberezhzha mayzhe the smog of boulders-pebble beaches stretches without interruption; Widely developed beaches with a width of more than 25 m. On the path of Pitsunda - Novy Afon, pebble beaches change gravelly. Uzbeks from the river KODAR to the river Kintrish nice, the coast of accumulative and abrasive-accumulative with wide food beaches.

Chornomorske Uzbeks in the borderlands of the Adjara Republic is similar to the beaches of Uzbeks in Tuapse - Sochi - Gagra: the foothill rivnina vuzka, stolen and divided, mountains close to the sea, the shores of abrasive and abrasives 25 m. The basic data on the resources of the beaches in the central part of the Chornomorsk Uzbek coastline with beaches is close to 480 km (68% of the Uzbek coast), of which the beaches are more than 25 m close to 290 km and a width of less than 25 m 190 km. as much as 200 km (28% of the Uzbek coast) occupy the skeletal banks, the possibilities of recreational development are surrounded. Nearly 60 km (8, 6%) of the Uzbek economy is occupied by state institutions, gardens, vineyards, and it cannot be lost in the quality of recreational resources.

They are indifferent to those in the Chornomorsk region of the Uzbek Caucasus - one of the oldest and most promising recreational areas of the country, while the development of Uzbeks is characteristic only for the small resorts - Great Sochi, Anapi, Gelendzhikhik, resort. Great and uniquely valuable natural and recreational resources of the region (warmer sea and beaches, unique subtropical landscapes) will be mastered in a meaningful world. Farther away is the resort and recreational development of the Chornomorske uzberezhzhya in the direct of the intensification of the resources of the beaches, all the smog in front of the village and in front of the town.

When assessing water facilities for a beach and bathing, the next step is to be seen:

· Mind you go to the water;

· Evidence of flat smog;

· The nature of the bottom;

· Shvidk_st current (rychki);

· Perevazhannya weak hvilyuvannya on the great waters;

· Temperature regime.

For an assessment of water facilities for a beach and bathing site of the Chornomorsk Uzbek coast, all pererakhovani umovi are looked at. The beaches of the Chornomorsk Uzbek coastline, gently sail into the sea, just across the coast without steep descents, suitable for mastering in a natural camp. The bottom of the sea pischane. The water temperature is 18-24 degrees - the most pleasant for a bathing trip. The sea beaches of the Chornomorsk Uzbek coast are of great importance. Їх exploitation is guilty of being carried out strictly according to the norms of permissible anthropogenic navantage, yak at a given hour of storage 5m2 per person, and in dispensaries for ailments for tuberculosis and with damaged support-ruch2 equipment per person - up to 12m2. Sochi resort zone on mіskih beaches і norms, unfortunately, do not touch. The ruinous inflow on the beaches is not just recreation, but only the abrasion of the sea (ruining the coast with wounds). At the same time, the Uzbek coastline of the Black Sea will change, there will be deterioration, but, however, to reduce the intensity of the change of water in the coastal zone and to a strong ecological hardship.

On the territory of the Chornomorsk Uzbek region, there are the most important areas of the sanitary-resort state and tourism. Here, 30% of the drainage mud and mineral waters of Russia are covered. Necessary mental development of recreational resources and development of tourism industry and tourism infrastructure. The peculiarity of the field in the one-hour service of the tourists and the local population, the development of the tourist development of the territory, will improve the mind of the inhabitants of the given area.

Economic-geographic assessment natural resources is one of the most important problems, since the number and the quality of natural resources are the natural resource potential of the territory, which is a great inflow to the state development of the regions, to the special development of the region, and to the special development of the world. 7 million people. The population density is not skid. Most populated villages and in front of the city's districts.

	Physical and geographical description of the Black Sea
	Temperature conditions and salinity
	Flora and fauna
	Promislovі vidi gіdrobіonіv
	Chornomorska horse mackerel
	Chornomorskiy sprat
	Chornomorska hamsa
	perspective by water
	List of vikoristanikh dzherel

1. Physical and geographical description of the Black Sea

The Black Sea is the inner sea. At the entrance of the river, I cross the western shores of the Balkan Peninsula, at the first time it is surrounded by the European Rivne, at the descent - the Caucasian Uzbeks and the Colchis lowlands, and in the past - the Uzbeks. Dovzhina coastline warehouse 4 100 km. Chorne Sea є Midland Sea of ​​the Atlantic Ocean. The Bosphorus canal is tied to the Sea of ​​Marmur, while the channel is to be bound by the Seredzemny. At the pivnichi Kerch channel, the Chorne more Sea of ​​Azov Azov Sea you can see the great negliboki inflow of the Black Sea. The Black Sea area becomes 420 325 sq. Km. to become 1,149 km, the most wide road is 611 km. Naimensha width - 263 km. Glibina of the Chornomorskoy ulogovini will increase on a weekday, the maximum reach is 2,245m. average glibin - 1 271 m, obsyag-537 yew. sq. km. Three main forms are clearly visible in the Chornomorsk bottom, the shelf, the mainland and the deep water. The shelf ends at depths of 9-110 meters, borrowing 24% of the bottom area. Near the last shelf, there was a rivninoy river, along which rivers flowed. The mainland fell to become 40% of the bottom area. Wine of steps. There are three main steps. The bottom of the settlement is occupied by 36% of the sea water. Vono rivne, my little nahil in a straight line. The coastline is loosely porous. The Chornomorskiy coast is b_dniy p_vostrovami. Among them is the best - Krimskiy pіvostrіv. Few islands. Three great islands: Snake, Berezan and Kefken. Rivers of two continents flow into the Chorne Sea - Europe and Asia: Danube, Dnister, Don, Dnipro, Kuban and іnshi.

1.1 Temperature conditions and salinity

Average temperature today in the private part of the Black Sea become approximately - 1 ... -3 ° C (in the area Odesa), Ale in the vicinity of rocky can go down to -10 ° C or more. On the territories adjacent to the Pivdenny coast of the Krimu and the Uzbek coast of the Caucasus, winter is on the way: the temperature drops slightly below + 5 ° C. The average temperature of lime trees at the winter sea becomes + 23 ... + 25 ° C. The maximum temperature is not so high for the water reservoir and does not overtake 37 ° C. Find a better place on the Uzbek coast of the Black Sea - the Uzbek coast of the Caucasus Gagra on the territory of the day Abkhazia(Average temperature + 17 ° C).

Even more salty relish of sea water and nadaє sodium chloride, and girky flavor - magnesium chloride and magnesium sulfate. There are 60 new items to enter the warehouse. Alle, it’s possible to take advantage of all the elements that appear on the Earth. Morska water I have a number of dominant authorities. Salinity of water is close to 19%.

Malunok 1 - Chorne more

1.2 Flora and fauna

The Roslinny light of the sea includes 270 species of greenery rich in greens, burikhs, and red-bottomed algae (cystose, ulva, enteromorph, etc.) At the phytoplankton warehouse of the Black Sea - not less than six hundred species. Among them are plaits, including dinoflagellates abo perіdinієvі water growth, різні diatoms of water, Kokkolitoforidi i in.

The Black Sea has 2,500 species of food (of which 500 species single-line, 160 views spine − ribі ssavtsiv, 500 views cancer-like, 200 views molluscs, Reshta - spineless new species). Among the main reasons for the vividness of the sea water: low salinity of water, long presence of water on the slopes of 200 m.

At the bottom of the sea hesitate мідії, oysters, And also the shellfish-hijak rapana, brought in by ships from the Distant Descent. In the gorges of the coastal skel and the middle of the stones, there are numbers krabi, є shrimps, See the rise, see jellyfish(Most extended cornerotі aurelіya), actinia, sponges.

mid rib, which can be found in the Black Sea: Rіznі vidi bichkiv, Azovska hamsa, Chornomorska hamsa ( anchovy), shark-katran, flounder-glosa, flounder-kalkan, mullet five species, bluefish, hake(Hake), marine HYPERLINK "https://ru.wikipedia.org/wiki/%D0%9C%D0%BE%D1%80%D1%81%D0%BA%D0%BE%D0%B9_%D1%91%D1%80 % D1% 88 " yorge, Barabulya (Zvichayna Chornomorska Sultanka), piksha, mackerel, horse mackerel, Chornomorsko-azovska stinker, Chornomorsko-azovska tulle, garfish, sea ​​conicі ін. To see sturgeon(Biluga, stellate sturgeon, Chornomorsko-Azov (Russian) і Atlantic sturgeon) і Chornomorsky salmon(Vinogradiv, 1958).

Kolishnu internal sea Russian Empire now, by the very shady volodinnyms of our state. Pivnichno-shidnі territories check their pіdkoryuvachіv. One z comor natural resources a part of the planet є the Bering Sea, geographic location What is not only a significant role in the development of the world's regions, but also the great prospects of expanding the economic activity of Russia in the Arctic latitudes.

Bering Sea. to describe

Pivnichna outskirts of the Pacific Basin - the vast majority of the seas, which wash over the shores of Russia. Yogo area 2 315 yew. Km 2. ​​For porvnyannya: the surface of the Black Sea in five and a half times less. The Bering Sea is the best in the middle of the coastal seas and one of the best in the waters. The most low elevation is located at the depth of 4,151 m, and the average depth is 1,640 m. Wonderful, with such indicators, close to half of the sea bottom is as far away from the surface of the sea as it is for a pivkilometer. With little water, it is possible to bring the sea to the continental oceanic type. Pivnichniy distant water to vmishuє 3.8 million km 3 of water. The majority of the Bering Sea voyages explain the views from this part of the ocean of the Commander-Aleutian Ridge, which has witnessed some of the global tectonic processes in the distant past.

History of visibility and development

A happy guide to walk like the name of the first European prelude to Vitus Bering. A Dane at the Russian service organizing two expeditions in 1723-1943 rock. By making it more expensive, I’ll get shocked to the cordon between Eurasian and America. I want the channel between the continents to be surveyed by topographers Fedorov, Gvozdov and Mashkov, and the names in honor of the hired seafarer. One hour of another expedition of the Bering Boulevard in the territory of the Pacific Ocean and in the city of Alaska. On old Russian maps, the pivnichne water space is named Bobrov, or the Kamchatka Sea. Uzberezhzha reached the level of Russian explorers from the ear of the 18th century. So, Timofiy Perevalov in the 30s sklav the map of the territories of Kamchatka and Chukotka. Through thirty years and a month, D. Cook has come. The Tsar's uryad was ruled by the expeditionary staff of Sarichev, Bellinzhausen and Kotzebue. Fortunately, the name of the bulo is proponated by the Frenchman Fliorier. We have a wide experience of the terms of the leaders of the Russian seafarer Admiral Golovnin.

Description of the geographical position of the Bering Sea

Geomorphological characteristics are based on the natural boundaries of the coastal line at the descent and entry, as a group of islands at winter and as a smart cordon at night. The pivnichna border is connected to the waters of the same channel, which is located at the bottom of the Chukchi Sea. The interconnection takes place from Misu Novosilskiy in Chukotz to Misu York on Pivostrovi Seward. From the start to the west, the sea stretches for 2,400 km, and in the afternoon for the next day - 1,600 km. The paved border is marked by the archipelagos of the Commander and Aleutian Islands. Klaptiki land in oceans okreslyuyut free giant arc. Beyond the boundaries of the Pacific Ocean. On the edge of the planet's greatest waters, the Bering Sea. Geometric aquatic babies are characterized by the sound of the water space up to the polar cola. The Bering channel is divided into two continents: Eurasia and Pivnichnu America- and two oceans: Pacific and Pivnichny-Lydovitiy. The winter-western waters of the seas wash the shores of Chukotka and the Koryatsky visochin, the winter-western waters of Alaska. The runoff of continental waters is minuscule maliy. On the side of Eurasia, Anadir flows into the sea, and on the shores of Alaska, the legendary Yukon has its arm. Richka Kuskokuim flows into the sea at the same time.

Uzbeks and islands

The number of bays, inflows and outlets of the river form the youngsters of the Uzbek coast, which are characteristic of the Bering Sea. Olyutorsky, Karaginsky and Anadirsky inflows are the most common on the Siberian shores. The great streams of Bristol, Norton and Kuskokim are located on the shores of Alaska. Non-numbered islands are known for their travels: mainland islands are not large land areas in the boundaries of continental plateaus, islands of volcanic trekking become internal, and of a folded type - the calling belt of the Commander-Aleutian arc. The ridge itself stretched for 2,260 km from Kamchatka to Alaska. The outlying area of ​​the islands is 37 840 km 2. The Commander Islands lie within Russia, all of the United States: Pribivalova, St. Larentia, St. Matvia, Karaginsky, Nunivak i, vividly, Aleuti.

climat

Significant numbers of average temperatures, which are faster for continental landlocks, flow through the Bering Sea. Geographic position is the primary factor in the formation of the climate in the region. To the largest part of the sea territory subarctic zone... The private side is to be carried out before arctic zone, A pivdenna to in the middle latitudes... The side is going to cool down stronger. And through those who adjoin the sea to the sea, the Siberian territory is weaker, the process of water development is much colder than the skid. Over the central part of the sea during the warm season, it warms up to + 10 ° C. The charge, without affecting the penetration of arctic winds, does not go below - 23 ° C.

hydrosphere

At the upper horizons, the temperature drops to the northern latitudes. Drive, as you wash the European Uzbeks, colder than the American American zone. At the coldest time of the rocky coast of Kamchatka, the sea temperature on the surface of the road is + 1 ... + 3 ° C. The sea temperature of the Uzbek coast of Alaska is one or two degrees higher. A bit of the upper ball is warmed up to +9 ° C. The value of the glybin of the Aleutian ridge channel (up to 4,500 m) for active water exchange is The Pacific Ocean on all horizons. The inflow of the waters of the Chukchi Sea is the smallest in the way of the small valley of the Bering Channel (42 m).

Beyond the step of the well-being, the persche of the middle of the seas of Russia is also the Bering Sea. A bright ocean is a kind of water, then it is based on the characteristics of the stage of boisterousness of the periphery. Values ​​of glybin and storm activity are negligible for strong deterioration. A large part of the rock is meant to be hvilyuvannya with the height of water combs up to 2 m. During the winter period there are a number of storms with a height of up to 8 m.

Lodova furnishings

Lodove pokrittya by the type of walking є mіstsevym: a lot to form and tane in the very aquatoria. The Bering Sea in the private part is covered with ice in the winter season. In the first currents of crying, the shell will shackle the closed bays, the inflows and the coastal zone, and the most widened area is accessible in the square. Tanennya will end only in the middle of the summer. In such a rank, the surface in the zone of high latitudes of the skut is more than nine months per river. At the place of St. Lavrentiya, bilya shores of Chukotka, until the seasons of the year and people are not tantalizing. The pivdennaya side, navpaki, does not freeze by stretching out the rock. Through the Aleutian ducts, warm masses come from the ocean, which bring the edge of the ice closer to winter. The sea channel between the continents is mostly filled with ice packs. Deyakі kryzhanі fields reach up to six meters. Bilya uzberezhzhja Kamchatka drift massiv and start navigating in the serpentine. Pilotage of sea vessels by sea route, Vimaghak participation krigolamiv.

Tvarinniy and roslinny light

On the coastal skeletons, they vlashtovuyut their colonies of gulls, guillemots, puffins and іnshі feathered bagans of polar latitudes. Along the gently sloping shores, it is possible to establish rookeries for walruses and sea lions. The real miracle of the Bering Sea can be reached for more than three meters. The great number of seaweeds are built. Morska flora is represented by dozens of coastal roslin. On the personal level Phyto-algae take the development of zooplankton, so, in their own circle, they bring free seafoods. For every year there are humpback whales, representatives of the gray and toothed species of whales - killer whales and sperm whales. The Bering Sea is rich in ribbons: the submarine fauna is represented in three hundreds of species. V beer waters bag and shark. Polarna trim on great depths And the hizchka - salmon is not safe - aggression to people who do not come. Without summing up, the sea glibini did not see all of their confessions.

Mіzh Asia and America

Non-numbered groups of animal industries have begun to conquer the wine-growing world from the 40s of the 18th century. The islands of the Aleutian archipelago, a majestic natural place, allowed merchants to travel to the shores of Alaska. The position of the Bering Sea, and the very part of the ice-free part, has welcomed the establishment of live shipfaring in Petropavlivskiy on Kamchatka, and once again prompted by strong points on the American continent. True, the Russian experience in America was not good enough, all close to ten rockies.

territorial super-links

In the era of M.S.Gorbachov's rule, it was laid down to please about the actions of the USA on a significant part of the sea and the continental shelf behind-the-scenes mayzhe 78 yew. km 2. At the heart of 1990, the Minister of Foreign Affairs of the SRSR, E. Shevardnadze, together with the State Secretary D. Baker, wrote in favor. The lasting trawling fleet has lost the power of the ribs in the middle of the sea. In addition, Russia has absorbed a hundred segment of the promising naphthonic province on the shelf. The bill has been bolstered by the American Congress in the same way. In Russia, it is pleasing to accept persistent criticism and has not yet been ratified by the parliament. Rozdilova line rejected the name Shevardnadze - Baker.

Gospodarska dіyalnіst

The economy of the region consists of two components: industrial government and sea transport. Unsurpassed ribbons of resources are receiving active activity of Russian ribopromisloviye companies. On the Uzbek coast of Kamchatka, there are no more processing plants. On a commercial scale, fishing for oseledaceous, salmon tricky and flounder species is great. On a small scale, mainly in the interests of the indigenous population, it is allowed to fall on sea creatures and whales. In the rest of the rock, there is a scientific interest in the whole distant region. In the main tsiklikano pochukov genera in carbohydrates on the shelf. Bilya uzberezhzhya Chukotka is seen three small naphthonic basin.

Klondike at the bottom of the ocean

On the sea slopes, there have not been any complex advances yet, except for some buv bi shots of corianne copalins or collection of geological data for more promising noises. At the boundaries of the aquatoria, there is a load of brown copalins. And on the coastal dilyankas, there are genera of tin and filler stones. At Anadirskaya ulovinі there was a family in carbohydrates. And the axis on the protylezhny uzberezhzhі is already a splinter of rockіv will overrule the bottom in tricks of the same metal. A hundred years ago, until the development of the region, gold was used, as was known on the banks of the Yukon and a feisty woman was carried out for a lot of gold. The Bering Sea on the cob of the XXI century is a gift of new hopes. The greed for profit is a breed of cunning technical attachments. An extravagant excavator is installed on the old barge, a gurkit for procuring inert materials and improvised primitiveness, as a wake-up wagon, in which an electric generator is displaced. Additional technical "monstrosity" of the Bering Sea is growing more and more wider.

Original project for Discovery channel

The axis of the season has already begun for the popular science-based American television channel Discovery to pursue a share of the easy-earning scammers. As soon as the water rides through the ice, on the Uzbek coast of Alaska, prospectors are scrambling from the sea, and in the northern latitudes there will be a new fever of gold. The Bering Sea has a small surface area. Tse allow koristuvatisya by hand. The improvised fleet of kidak wiklik poems. The sea is undergoing a transformation of the skin into strength and manhood, and the sea bottom is reluctant to share its belongings. Only the most blessed happy ones zbagatila gold is a feverish woman. The ice of the Bering Sea allows the businessmen to feed their robots during the winter period. With a sweep of a series of gray documentary films, you can sponsor three teams of goldsmiths, who use their lives for the love of the precious metal.

Roztashovans in the continent, the Chorne Sea is the best part of the Svitovoy Ocean. At the first entry, you get to the Marmur Sea through the Bosphorus channel, between the seas to pass along the line of Mis Rumelimis Anadolu. Kerch channel to the Chorne and Azov Sea. The area of ​​the Black Sea is home to 422 yew. Km2, ob'єm - 555 yew. Km3, average depth - 1315 [...]

The Black Sea can reach great dimensions along the width and the ring sounds in the middle. The sea is deeply embedded in the land. Practically from each side, surrounded by the mainland. The Bosporus and Dardanelli canals cross between the Marmur and the Middle-Earth seas. Lead the Black Sea from the Azov Sea through the Kerch Channel. In such a rank, the Chorne Sea has links with the waters [...]

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 from the Black Sea. 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, maximum depth - 15 [...]

The Azov Sea is located in the paved part of the Russian Rivnin. It is practical from the sides of the mainland cordon. There is only a small channel at the bottom of the river from the waters of the Black Sea. The route between the sea and the sea passes through the Kerch prototypes along the line, from the end of the river to the city of Takil and of the Panagia. Sea of ​​Azov, there is a desire for connections from the Holy Ocean, є internal. Azovske [...]

Roztashuvannya of the Middle-Earth Sea: between Europe and Africa. The area of ​​the Seredland Sea is 2 500 thousand km2 Average Glybin The middle ground sea is 1 541 m. best glybin Sered-earth sea 5 121 m. Bottom relief of the Sered-earth sea: Algerian-Provence basin with depths of depth 2 800 m, Central basin with depths close to 5 100 m, Levantin basin (4 380 m); sinks of the sea [...]

Pislya Russian-Turkish war 1768-1774 rr. Territory of Crimean bully was from the Ottoman rule, and Kerch and the fortress of Oni-Kale became the power of the Russian Empire (the last of the Crimean lands went to the warehouse in 1783). The Russian team has been deployed in the Kerch prototypical battery. Pіznіshe Paris Peace Treaty, signatures in kіntsі Krimskoyi vіyni 1853-1856 rr., Oholosiv Chorne sea with a neutral zone, and the construction of the change was continued in the area of ​​inflow - vin [...]

Fortetsya Oni-Kale (which is translated from Turkish as “nova fortetsya”) was inspired by the sinking of Kerch by the Ottoman Empire. For the establishment of the Kerch channel, there was a place on which there was a majestic significance - the cruise ships of the Russian Empire could eat from the Azov Sea in the Chorna Sea. The Turks did not bach the Russian ships in their waters, so on the ear of the 18th century. they sounded the fort Ani-Kale. The walls of the її stood on the ryvnyi rіvnya across the mountainous relief. V [...]

Ayu-Dag, or Vedmid Mountain, is divided into two municipal districts - Yalta and Alushta. There is a legendary legend, a majestic witch has turned up the mountain, like a namagavsya vipiti Chorne sea. At the start of the day, it looks like a skylight with characteristic outlines - it’s not the volcano that rises, the magma that didn’t whirl through the name, but caught at the dome of the viglyad. Going to Vedmid Mountain, call me to fix it in the village of Partenit - here you can poach an ancient tomb Bishop Ioann Gotsky, religious [...]

The Vishukan Altanka with vitonized stone columns, we will take a dome with a spire and stand on the very edge of the Shagan-Kai skeleton. The name of the last one is changed from the Crimean Tatar yak "falcon gnіzdo". The original name of the goitre altar is tied to the penetrating winds, like panting on the tops of the skeleton. On the mosaic podlozi the image of the trojan horse is displayed. In our days, the Altanka was awarded no less romantic name - "Zorepad spogadiv". When the weather is clear, the wonders are seen: Partenit and [...]

First day. To dedicate the first day of moving to Krima to the knowledge of the resort capital of Yalta. Zdіysnіt vrance, we propose a walk along the embankments and small areas, go to the beaches or see the crocodile. In the evening go to the cafe chi, if you will also go to the nightclub "Orange". Another day. Knowing about the Pivdennyi Shore Krim to find it from the road to Alupka, look around [...]

From Balaklavi the coastline of the Black Sea turned to the early stage, and on a stretch of 10 km є the tsikavi mission. First for all the beaches, otocheni with skeletons, to which you can go only by the sea. At 2 km from the bay є Srіbny, or Blizkiy, beach, and 3 km, Trokhi dalі, - Golden, or Dalekiy, beach. Above the beach on the skyla of the Asketi mountains, you can bachiti unwittingly in the 1920s for a long time [...]

The 35th coastal artillery battery (won at Fort Maxim Gorky II), founded in 1913-1929 rocks, is the very fortification of sporud on the territory of the SRSR. Approximately the style of concrete, the image of the future of the Zaporizhzhya GES went to the future. Immediately after the end of the operation, the battery is specially drawn into the Stalin. A great part of the complex has grown up from the earth, and here, during 1942, the results of staying for the sake of [...]

First day. To dedicate the first day to look around the place of Russian glory of Sevastopol. We propose a walk along the embankments of Artbuhta and Grafskiy pier. Having reached a couple of zupinka to the Ushakov square, make a small convergence on the pagorb, the panorama of the defense of Sevastopol is destroyed. Take a bite to eat with Panoramas in one of the cafes and viruses in Chersonesos. After spending a couple of years there, turn to the center of the place. Pid evening [...]

The panorama of the Pivdenny coast of Krimu, a unique natural landscape, is seen at the Angarsk pass. The head ridge of the Krymsky mountains, surrounded by the land from the winter winds, and the warmer Chorne sea was opened natural mind, Bagato in what is close to the Mediterranean: with a soft, non-trivial charge and a specotny sleepy lith. The Pivdenny Coast is a wide smoga (up to 9 km), laid between the mountains and the Black Sea, stretching towards the [...]

Yalta - heart resort Krimu... Yogo alpha and omega. Not vaguely, as much as Bulgakov wrote the following lines, assigned to the place: “Yalta is good and good, and power in them is constantly changing.” The axis of what, the boundary line of the Radiansky hulk, was a simple formula: "I will make a suit with an eye-catching one - and to Yalta!" Who does NOT have [...]

The pike perch is small, and even more beautiful is the perlin of the Krymsky Uzbek, roasted in the Malovnich_y valley. Not far from Sudak there is a beautiful little creek of Russia, which is called Novy Svit. It is good for Sudak and the New World to rotate grapes and ferment wine, the glory of which has crossed far beyond the boundaries of the wine. It is even warm here, there are no more boards, and there are plenty of [...]

The Kaluzka region is roztashovana in the center of the European-European region, approximately on the rural area (800-850 km) from the Bily, Baltic, Azov and Black seas. Її territory become 29.9 yew. Km2. Tse is one of the most popular areas of the European part of the country. At the entrance of Kaluzka, the region is between Smolensk, at the entrance - with Bryansk and Orlov, at the descent - with [...]

Basic Figures of Physical Geography Skhidnoi Europe A part of the European continent is a majestic territory, where the development of the minds of natural geography is growing. The largest part of the loan is Skhidno-European or Russian Rivnina, the area of ​​which will become close to 4 million km? At winter time, it will be washed by the waters of the Pivnichny The icy ocean[...]

Features of the transport complex The transport complex includes a net of transport lines, transport universities and technical facilities for transportation, as well as a robot for transporting vantages and passengers. The main types of transport are zaliznichny and rychkovy, the role of which is gradually decreasing, as well as automobile, pipeline, sea and aviation, which are significant in transported adults. The length of transport lines is characterized by their length - in yew. Km [...]