A little more about the festival
The Creative Intelligent Club "Climbing" is the organizer of the Festival of the author's song "Yasenskaya Spit" Khutor Morozovsky on the Yasenskie Spit.
1995, August month. The first authentic song and poetry festival, which organized and held participants of the club "Climbing" in the Yasenski Spit. The enthusiast group took up a difficult thing.
Objectives and objectives: Propaganda of tourism as a healthy lifestyle, strengthening and developing cultural and creative ties between the Krasnodar Territory, regions of Russia, the CIS, promotion of the author's song and poetry, identifying new giving, the involvement of young people in the SP and AP.
Conditions of residence: three days of living in conditions tent camp on the shore Azov Sea On the Yasenskie Spit. Food reserves with me. You can cook on fires, gas stoves. Products can be bought in the farm or in the city that are not so close.
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City Primorsko-Akhtarsk Located on the coast of the Sea of \u200b\u200bAzov, in the Krasnodar Territory, near Akhtar Limana (Russia). The city is the district center - Primorsko-Akhtar district. Nearby is located Baseugian LimanIn general, Primorsko-Akhtarsk is located among the many Limanov, there are deposits of therapeutic mud. Until the 18th century on the territory of Primorsko-Akhtarsk there was a Turkish fortress Akhtar-Bakhtverwhich Russian troops captured in 1774. This is quite famous in Russia azov resortHere is a good sea and beaches, many pensions and recreation sites. In that resort town You can find accommodation in price cheap, prices are affordable, there are rooms with amenities. Rest in Primorsko-Akhtarsk can be quite diverse, there are private pensions, hotels, hotels, a well-developed rest infrastructure.
Some recreation centers and boarding houses in Primorsko-Akhtarsk: recreation center "Azak", "Breeze", "Wave", Turbaza "Lotus", "Meotida", "Venice", "Bricks", There is a camping and a tent town. Not far from Primorsko-Akhtarska also on the shores of the Azov Sea khutor Morozovsky. Morozovsky is not very famous yet resort villagebut there you can also find accommodation and stay on summer rest. Especially good for semi-wild rest lovers.
Satellite map of Primorsko-Akhtarsk - Wikimapia.org (Sea of \u200b\u200bAzov, Primorsko-Akhtarsk)
Weather forecast and current weather in Primorsko-Akhtarsk -
The shores of the Azov Sea within Krasnodar Region part 2
Primorsko-Akhtarsk - Yasenskaya Spit
The shore between Pyrimorsko-Akhtarsk and the root of the Yasenski Kosh Abrasion all over. The average height of the coastal cliffs is 4 m, the maximum - 8 m. The coast has a fibrous structure, the capes are formed by the most dense differences of Suglink. The average velocity of the abrasion for the perennial period is 1.0-3.6 m / year, the maximum - up to 6.0 m / year. Coastal ledges are composed of forest loads and clays and practically do not give the beach-forming material.
Therefore, the abrasion terrace is only covered with a low-power cover of the sand, and by the missing abroad. The terboard work in Primorsko-Akhtarsk was performed in 1956-1970. In the form of a concrete discharge wall with a stubborn tooth in the base and parapet at the top, which protect the embankment. The total length of the fortified area of \u200b\u200bthe shore is 3.8 km. Bows are built of iron plates with a thickness of 0.15 m mounted between rows of piles and interconnected in a single design by a monolithic cap bar.
A total of 14 bun were built. Currently, the coast of Primorsko-Akhtarsk protects the wave-duty wall and bun. In the central part, the beach is a gravel and sandy beach with a width of up to 35 m. Part of the bun is destroyed, west of the city center, the wave-duty wall is broken directly into the water. Also in Primorsko-Akhtarsk, the wall and the embankment restored, an artificial pebble beach (3.8 km) was created from the Lotos pension to shipyard (Fig. 6). FROM eastern The beach protect three bows with a length of 30, 35 and 50 m. The space between the riots is filled with brought by pebbles in diameter 4-6 cm. Head parts of the bun have minor damage, in the root part of the buna are blocked by a layer of pebbles.
Figure 6 - Wave-woven wall and artificial pebbling beach "Lotos" Tourbase
The shore of the Khutor of Morozovsky south of the root of the Yassen Spit is strengthened by a sloping wall with Berma on the basis and parapet at the top of the wall. The length of the fortified shore is 450 m. Construction was conducted in 1985-1986. The south of this site begins an abrasion cliff with a height of 1.5-2 m with a winding contour in the plan (Fig. 7). Next, there is a second fragment of the berertaging structure (about 400 m), from concrete beam, a sloping wall and a massive parapet with a wave-reflective visor. The crest of the parapet towers above the middle level of the sea at 3.5-4.0 m (Fig. 8). End parts of the sloping wall are designed. 
Figure 7 - Abraded shore north of Primorsko-Akhta Lighthouse 
Figure 8- Berusting Khutor Morozovsky
Yasenskaya Spit - Baysuga Limana
On the coast between the root of the Yassen Spit and Art. Yasenskaya has two accumulative forms with general genetic devils - Yasenskaya Spit and Perepozing Oz. Khansky. The YaseN space of 18 km long is focused in the northeast direction and is formed mainly from biogenic material. The width of the beaches here does not exceed 5 m. In the middle part of the braid, the width of the beaches increases to 15-20 m, on distille - 50 m. The biogenic material comes from the bottom. The root of the Yasesen Spit is strengthened by stone berm from a 10-50 cm material in diameter. Berm width is 6 m, height is 1-1.5 m (Fig. 9). Pozing of Lake Khansky has a length of 25 km and a width of 1-2 km. The body of the sleeper by 80-90% is composed of a shell-free detrituit with a small admixture of sand, gravel and pebbles from the breeds of the blurred shore. The width of the beaches in the Yasensky crossing exceeds 30 m. 
Figure 9 - Fortified Shore at the root of the Yasenskie Spit
Shore in the village. them. Tamarovsky is a redefined plateau with a height of 2-2.5 m. Not far from the cut, the same height cliff. Clean beach, width from 1 to 10 m. In the center of the village of Shore, he is strengthened by inclined concrete slabs. To the north-west of 1-1.5 km from the village begins the breakdown, the rigorous-abrasive coast. The height of almost vertical, folded leafy lines of cliffs reaches 15 m. The coast has a pronounced festral structure. The beach is practically absent. The southeast coast of Limana is relatively stable, the shores threw the cane.
Yasenskaya Crossing - Kosa Kamyshevatskaya
In the vicinity of the village. Yasenskaya crossing the shore is low, accumulative. The beach is predominantly a shell, 5-20 m wide. For 15 km north-west of Art. Shirovka shores are folded by forest loam. They are subject to active ribbing-abrasion processes, frequent scratching and collaps. The height of the coastal cliff hesitates from 18 m on the southern outskirts of Art. Kamyshevatskaya to 7-8 m at art. Shilovka. Beaches are narrow (5-10 m) with slopes 0.11-0.12. Folded from sand, sink material, small pebbles and gravel.
Kosa Kamyshevatskaya - Spit Long
The coast between Art. Kamyskhevatskaya and Art. Dolzhanskaya includes an abrasive coast (art. Kamyshevatskaya - Dolzhanskaya) and two accumulative forms - Koshi Kamyshevatskaya and long. Kamyshevatskaya Spit is located on the southeastern tip of the Yeisk Peninsula. This is a flat surface with an ancient coastal and lowering system oriented from the northeast to the south-west. Its length is about 6 km, and the width in the root part is 4 .0 km. Rakusha and shell dedrit is 80-95% of the composition of the material. The mineral part is represented by quartz sand, gravel and a small amount of pebbles. IN last years The western coast of the spit is eroded (Fig. 10), and the distal end increases and at the same time turns to the shore. 
Figure 10 - West Coast of Kamyshevatskaya Spit
Between Art. Kamyskhevatskaya and the root of the muster braid (30 km) of the indigenous coast refers to the abrasion-collapse type. Coastal cliffs are stacked by lesident loams, which are littered with Scythian clays, and have a height of 7-15 m. The beaches are leaky, width from 10-25 m, the slopes - 0.07-0.11, and the bottom slope - 0.10-0.17. The composition of the beach material is fine-grained sands with an admixture of rocus. Spit is long located at the entrance to the Taganrog Bay. Her length is 12 km. Opposite the distal end is the island separated from the braid of the industrial. The body of the braid is composed mainly with a shell material. Width of the beaches from the side open sea up to 25-40 m (Fig. 11), the coastline is stable. 
Figure 11- The beach of the Admiral Wharf North-East Coast of Spit retreats at a speed of 6-8 m / year.
The width of sand-andracked beaches is only 1-4 m (Fig. 12). The shore in the area of \u200b\u200bthe "Cossack smoky" and the former fish region is blurred at a speed of up to 10 m per year, part of the buildings turned out to be on the riva line and collapsed (Fig. 13). Protection of the shore of the holiday home "Azov" at Art. Dolzhanskaya was performed without design and survey work. Initially, the regeneration was a sloping wall made of reinforced concrete slabs and about 20 short spurs with 6 m long of the same plates set on the edge at a distance of 5 m from each other. Currently, the slope wall and spurs are practically destroyed (Fig. 14). 
Figure 12 - Blurred Northeast Coast of Long Spit 
Figure 13- Dedicated on the edge as a result of the coast erosion and partially envelled building 
Figure 14- Remains of the wavepool wall at the holiday home "Azov"
Stanitsa Dolzhanskaya - Skita Yeisk
On the plot between Art. Dolzhanskaya and G. Yeisk is an abrasive coast (Fig. 15). The cliffs are composed of forest-like sublinks, the height of which in Jeysk up to 20-26 m and 3-6 m at the station Dolzhansky rate of the recession of the shore on the site of Yeisk - Vorontsovka is estimated 2.2 m / year, but in some years up to 4.0 m / year increase in some years. Beaches are narrow - 5 m, the biases of them are 0.08-0.09. From Voronetsovka to the station Dolzhanskaya Abrazion Coast retreats at an average rate of 1.9 m / year, maximum - up to 5.0 m / year. In the village of Vorontsivka, the height of the cliff decreases, the width of the beach changes from 3 to 25 m, but the shore continues to be actively blurred, and the remains of the berererous structures on the shore. In Yeisk, southwest of the root Yeisk braid Strengthened shore in length 3.5 km (Fig. 16).
The start of this site was held in 1988-1996 as an anti-emergency event. The dumping of Berma from the pebble-curled material at a distance of 20-40 m from the cliff sole of a height of 19-21 m. The construction reliably covers the shore from the erosion not only from ordinary storms, but also at high hugging levels. Yeisk Spit is composed by quartz sand, shell material and detritus with admixture of pebbles and gravel. The surface of the braid is built up. The width of the beaches in the distal part from Limana is 13-15 m, from the side of the Taganrog bay - 20-30m. Strengthening Yeisk Spit on the part of the Taganrog Bay is made between the port and its distal end at a length of 1.8 km. At the tip of braid, the shore in length 0.5 km was reinforced in the pre-war time with a wooden tongue wall with a bite stone. 
Figure 15- Abrasion-shared bank on the plot of Art. Dolzhanskaya - Vorontsovka 
Figure 16 - BEGORREPULATION within the city of Yeisk
Shore of Yeisk Limana
The coastal cliffs of Yeisk Liman are composed of forest loads and belong to the abrasion-collapse type with a height of 5 to 19 m. Cliffs are dissected with ravines and beams. The width of the beaches 4-6 m, the slopes of them - 0.10-0.26. On the Yeisk Protection, the bank is an abrasion-rod, intensely exposed erosion, weathelation and erosion. Bench from Scythian clays is almost ubiquitous. On the coastal occasions of small height develops and scraping, at higher (above 18 m) - collaps and landslides. The blurry of the coast is celebrated on south Bank Limana, where the Yeisk-Krasnodar railway passes.
West of p. Sverogank and in the city of Jeysk shore along the mound railway For 7 km strengthened. The strengthening of the coast was made of an ECD to protect the railway canvas along the shore of the estuary and is a berr with a torn stone (3.0 km) and a rustling of a height of up to 1.5 m (5.5 km). In several places, the retaining wall is damaged, and beach strip At a considerable distance there is no or has a width of 1-5 m. For this reason, the strengthening of the shore is not reliable enough. However, in this form, the coastal structures ensure the stability of the coastline for 30 years.
The coastal slope is currently mortgaged, while on the neighboring unprotected section, the broccoping of the abrasion ledge retreated 20 m. The artificial pebble beach of 1 km long was built on the southern shore of the Yeisk Bay from the village. Alexandrovka). Strengthening the coast in the early 1990s to stabilize the coastline and create a recreational beach. The beach is steady, has a width of 15 m and protects the shore from the abrasion. In the eastern part and the northeastern part of the Limana of the shore relatively neutral. Suglitinous cliffs are separated from cutting with reed thickets (Fig. 17). 
Figure 17 - A characteristic view of the shore in the area of \u200b\u200bthe village.
Nikolaevka Glafirovskaya Spit - Sazalnitskaya Spit
The Glakhrovskaya Spit has a length of about 7 km. The distal end will be rented in Yeisk Liman. The beach is an average 12-20 m wide. Ancient shafts are noticeable on the spit surface, which are stretched in parallel to the West Bank. It should be noted that the West Territory of the Glakhrovskaya Spit retreats at the same rate as the adjacent portion of the abrasion coast, and the distal end increases. The coast adjacent to the spider - the riveted, are composed of loams (Fig. 18). The average height of the coastal cliffs is 10-15 m, the maximum is marked at the village. Shabelskoe - 26 m. The average speed of erosion is 1.4 m per year. Type of shore abrasion-landslide. To the foot of the abrasion cliff, a sand-sewing beach was led by a width of 7-22 m. In the area of \u200b\u200bthe village of Shabelskoye beach, more than 20 m protects against the effects of excitement (more than 15 m), an exposure of the cliff, folded by sublinks (Fig. 19). 
Figure 18- Root of the Glakhirovskaya Spit 
Figure 19- The characteristic view of the shore in the area of \u200b\u200bthe village. Shabelskoye
Spit Sazalnitskaya - Port Caton
Sasalnitskaya spit has a form of symmetric accumulative protrusion. The length of the axis oriented in the northern direction is 3 km, the foundation width along the dead cliff is about 7 km. The beaches whose width is 10-13 m in the root part and 20-25 m - in central and distal, are composed of 50-60% material of abrasion - finely and medium-trunk sand, gravel, pebbles. The biogenic part of the nanos is 40%, in the cross-section to 85%. The flat surface of the braid in the northern part is violated by numerous extrovers of "amateur" sand quarries.
And in the south, at the high root shore, against the mouths opening with the beams, there are slightly convex cones of the removal. The shores in the area of \u200b\u200bthe farm of the Molchanovka - ripples, are folded by lozhlinkami. A sheer abrasion cliff with wave-bearing niches has a height of 10-12 meters. The beach under the cliff varies within 3-10 m and is complicated by clay, in separate places with sand. Shore from the farmland in the side of Sazalnitskaya braid mainly abrasion. Wrapped cliffs are composed of clay and lesing loams. The beaches are narrow and only in front of the beams their width increases, are folded with sand and rocus. On the northern segment of the plot to the village. Port-Caton Casting Obligious-landslide. There are constantly active landslide collars, opposite each large landslide in the sea there is a shallow, composed of Absheron clays. Cliff height is up to 45 m. Speed \u200b\u200blandslides are observed. Beaches are narrow, their width increases to 15-20 m opposite the beams.
Conclusion
Considered four main types of shores: abrasion, abrasion-landslide, accumulative and neutral. The length of the abrasion coast is 227 km, accumulative - 230 km. Relatively stable shores has a length of 116 km. A feature of the modern dynamics of the eastern and northeast coast of the Sea of \u200b\u200bAzov is the predominance of abrasion and the local nature of accumulation. Not only indigenous shores, but also accumulative forms are spacious. The erosion continues unique azov Koswhich are of greater value in recreational relationships.
At a considerable extent Azov coast Obligor-landslide processes actively proceed. The average speed of erosion of the coast reaches 3-4 m / year, the maximum - up to 6-8 m / year. Significant levels of levels are largely enhanced by the abrasion effect of exposure to storm waves on the shore. This also contributes to the geological structure of the coast, composed of predominantly lesident loams and clays. With a blurry of such breeds, they are almost completely laundered and in the form of a suspension are taken out into the deep sea zone of the sea, not giving material to form the beaches.
This causes the high rates of the banks of the shores, even with relatively weak wave effect. The accumulative style of the coast is presented very diverse in structure, genesis and modern dynamics of the shores. Their morphology is somehow related to the sources of the material and its composition, the regime of excitement and the distance. The wide distribution has accumulative forms that receive food at the expense of bottom nansions - Perespi Lake Khansky, Baysugan and Akhtaniz Limanov.
Neutral shores are isolated, where clearly abrasion or accumulative processes are currently not expressed. Their total length is 116 km. They are usually distributed in limans and in areas blocking braids, as well as between the mouths of the r. Doubles and Kuban. It should be noted that the term "neutral" is applicable only in the sense of relatively weak effects of waves directly ashore. At the same time, for more of them, especially in Mezhda Kuban and Dukes, the coastline retreats, which is explained by the relative rise in sea level and other processes.
The stabilization of abrasion shores requires protective events about 45 km. This is primarily a high clay cliff within the city of Jeiska and further towards a long braid, some sites within the boundaries of settlements from the root part of the Glafirovskaya Kosh to Molchanovka, as well as the plots of the Abrazion shore between Kosy Long and Kamyshevatskaya. To date, on the surveyed part of the coast of the Sea of \u200b\u200bAzov, the progenic works were carried out in 12 sites (33 km). The implementation of the implementation of the processed measures is only within 5-10% of the previously planned.
The carrying out of both cases has led to the stabilization of the coast. In some sections, the complex of the Beregazashny structures is destroyed completely or partially destroyed. Protection of the main shores of the shores is solved with the help of suggesting fortifications of different designs without taking into account the width of the existing beaches and the influence of the designed structures on their future condition. At the same time, absolutely not enough attention was paid to the preservation or improvement of the coastal landscape. In the future, in the development and implementation of progenic measures on the Sea coast, it is necessary to conduct forecast assessments of the development of the coast in vivo and after the proceeding measures, taking into account the existence of lithodynamic systems.
For those who often visit the Azov Sea, in particular Primorsko-Akhtarsk, Yasenskaya Spit - one of the natural attractions of these places is perhaps the most memorable. Unusually pure sea water, although not distinguished by diversity and abundance of paints, beautiful and untouched by the disadvantage of man nature, calm and measured atmosphere, attracts here sophisticated tourists.
However, it is necessary to enjoy the wonderful species, it is quite difficult to get to the braid, because it is under guard, environmentalists and border guards, which makes access to it extremely difficult. But not all it is a protected area: one part of it has a resort status, but the most interesting thing is in the one that still belongs to the reserve.
Where is the Yasen Spit on the map
She is divided between two districts - Yeisk (in the north) and Primorsko-Ahtar (in the south). The nearest settlements - Khutor Morozovsky and Yassensky crossing. Near you also discover already described on our website.
Origin. Geography. Nature
The exact time of formation of Yasenskaya Spit is unknown: there is an assumption that her age is several millennia. There is no scientific substantiation in this loud version; Turning to the geographical data relating to Azov, this means that in the period from V c. BC e. by i c. n. e. The current sea had a thoughtty name of the Meoty swamp, and from i to VII centuries. - Scythian lake.
The very same spit, as, however, and any other, has a manual character. In addition, the famous geographer of antiquity Ptolemy senior, described in detail these edges, does not mention it. The most likely time to create it is in the interval between the XV and the beginning of the XIX centuries.
But the mechanism of its formation is known good: Actually, it is not necessary to have a degree, it is enough to observe the tides. This is the action of persistent Western and Northwestern winds, almost never subscribe in the area. When they become especially ferocious, then they raise the so-called "standing waves" reaching 3 m in height, with the force that fell on the coast.
Standing waves wash the sand and shelf chaotic and here the correctioner is entering the phenomenal features of the adorption. At the moments when the gusts of the wind subscribe, the water is rapidly moving away from the coast, it can last up to several days, and then, just as suddenly returns, facing the area of \u200b\u200bthe braid by two separate streams, fiercely breaking over each other. These processes are manifested in other areas of the water area, forming Koski.
Nature and features
Made popular resort A small district center of the Krasnodar Territory Primorsko-Akhtarsk Yasenskaya Spit is 3 km north-west of him. Located in the eastern part of the Azov Sea, it shares the freshwater baseugan estuary from the salty waters of the Yassen Gulf, becoming a kind of barrier between them.
Winning and constantly changing the direction - then on the southern, then to the eastern, it, as a huge snake, stretched almost to the Yasen crossing, for a distance of a little more than 14 km. The braid mainly consists of a coarse-grained quartz sand, in color resembling Ohru, a mixture with a small white shell, prevailing on the tip, resting in the girlo.
The appearance and the location of the sandy braid is constantly changing, its gradual destruction occurs, almost all over, especially in the center where it is especially unstable. The devastating effects are on it and natural, and technogenic manipulations, significantly and the influence of changing climatic conditions.
In the last time, violent hurricanes are collapsed in late time, the level is gradually increasing - these natural processes systematically blur the root part of the spit. According to the estimates of scientists for 60 years, the Yasenskaya Spit due to the spacious erosion lost 2900,000 square meters. M of its area and 70,000,000 cubic meters. m Sand, about 20% in general.
If marine gladies can break through the sandy barrier and turn it into a chain of small islets, the consequences can be catastrophic. Salt water, whining in the neighboring Liman, transforms him into a shallow prize of the bay, which will cause irreparable damage to local fish farm and will lead to a deterioration in the environmental balance in a huge territory.
Interestingly, while the root plot is inexorably destroyed, the northern is steadily growing, which is promoted by strong underwater flows and tidal waves. But the most remarkable here is the hook-like crochetic tip of the braid, moving under the influence of wind, capable of turning around in the opposite direction.
Types of relaxation on the Yasen Space
The main and practically the only kind of leisure is that the Yasenskaya Spit can offer - recreation by savage. There are no luxurious, where prices are rapidly, you will not meet the tourist camping or other vacationers, which is rather strange with such popular attractions.
In a word, the shortest manifestation of at least some infrastructure at this point simply does not exist - only the bottomless blue sky, the crystal clear sea, and the pursuit of the rustic sand under his feet. But from Berezhka to Spit, you still have to get there, you can do this in two ways: to hire a boat in the Yasen's crossing or climbing, by its own way, from the road going to the farm Morozovsky.
It should be borne in mind that most of the Yassen Spit is a natural reserve, except for the one that is assigned to public. This explains the absence of tourists. There are many rare varieties of birds under protection, such as white herons, for example, can be found and not at all familiar to our latitudes, like Pelicans.
It is not known whether it is possible to put tents - neither there are no tables nor forbidding signs anywhere, but it is strictly forbidden to dry fires, the violators are waiting for serious fines. The pastime is an infinite bathing in the purest driver, where, unlike the beach, there are deep-water points, and for this it will not be necessary to move 800 meters from the shore.
An excellent alternative to this rest is fishing, characterized by great productivity. A variety of fish is small here, but the Black Sea bull is hung well and especially the taran, who does not get bored. Fishermen There a lot, although it also depends on the time of year - sometimes Kleva is not at all.
How to get there?
You can get to Morozovsky by bus that follows the farm and regularly. And from Yeisk, you can easily drive on a bus number 33 to Yasenski.
By car get to x. Morozovsky is most convenient in this way:
Tourist on note
- Address: Yeisk - Primorsko-Akhtarsk, Krasnodar region, Russia.
- GPS coordinates: 46.214206, 38.250921.
Yasenskaya Spit is truly an excellent place to relax, where you have fun and pleasantly you can spend the weekend, make me memorable photos, to divide and buy enough. True, at your own risk, for official stay, it is recommended to register, and it is not enough to do it. Reading the reviews of people who visited the spit, they seem implausible, I can not believe that there are still such corners, and when you see everything in person, it even more seems to be unreal. In conclusion - video clip from YouTube in the topic, pleasant viewing!
1. We are going to Akhtari!
Attention! Canevskaya - Primorsko-Akhtarsk are canceled by flight buses. At 7 am, a certain minibus costs 150 p in PA from Kanevskaya. You can say lucky. Taxi, of course, are available, but this pleasure is not cheap. So it is better to go by train to Timashevskaya, and there on some passing bus can be reached to the place. The price of the ticket is also in the area of \u200b\u200b150 rubles, the time on the way is about 2 hours. Bus station and railway station, both in Kanevskaya and Timashevskaya are located next door. In Timashevskaya near the station there is a hypermarket "Magnit" with huge queues in the cashier.
2. Primorsko-Akhtarsk, he is ahtari (emphasis on the last syllable).
This city is predominantly rural type, pretty green and clean. Through the center of the city passes Tamarovsky Street, which begins at the bus station. Perpendicular to her after 3 quartersch bar goes st. Proletarskaya, on which the market and shops are located, incl. Supermarket "Magnit". Further, this street leads to the sea. On the right on the embankment is the armored car. The sea is rightful of this monument is quite muddy, apparently, somewhere at the bottom of the departure of Ila. To the left, in the direction of the fish region it is quite dumping and not too small. On the beach sand is a mixture with a shell and pebbles.
There are several cafes on the waterfront, incl. "Plain" and "tourist". In the first good diverse menu, the second is an inexpensive diner, but you can also have lunch there. On ul. 50 years of October, too, there is a good fast-service café and other catering establishments.
From the attractions - the historical and local history museum (near the bus station), a non-working railway station Akhtari, Kurgan "Suvorovskaya Gorka" on Limanaya st., Church in the city center, various monuments, incl. Heroes of the Second World War.
Most of all housing is rented on the streets between the bus station and the sea. So it is not very far to walk. Next to the bus station is the placement service. You can contact there to make the appropriate option.
3. Farm Morozovsky.
In 20 with a small KM from PA at the very beginning of the Yasenskie Koshu is farm Morozovsky. This is small
settlement where there are no cafes, only shops.
The sea is very clean, but smaller than in PA. First, this is the most, then for a long time on the belt and only then on the neck. The bottom is sandy, on the shore - a seven.
There is an equipped beach of Yasensky autocomping, various drinks, ice cream, and so on are sold. Next by spit wild beachWater is also very clean. Housing in Morozovsky give a little. Basically, people come there from neighboring villages on their cars. The farm himself is fenced from the sea waves by the concrete promenade-wave of a great length, which is good walking in the evening.
In Morozovsky, very clean ecology. Therefore, there are a lot of fish, different birds, as well as mosquitoes: (however, there is no mosquito during the day.
4. Yasenskaya Spit.
The 14-kilometer braid passes between the Azov Sea Yasean Bay and Baseugian Liman.
At the end of the Spit is a wide and deep limana girlo with a rapid flow. For crossings in the village of Yasenskaya Crossing No (although it seems this is a good place to relax, since the sea in the vicinity of the village is clean and deep.
