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2024/02/29 18:04:21

Krasnodar Territory

Content

Main article: Subjects of the Russian Federation

Krasnodar Territory is a constituent entity of the Russian Federation located in the south-west of the country.

Geography

It is part of the Southern Federal District.

The area is larger than that of Azerbaijan or Ireland

The area is 75.485 thousand km ². For comparison, the area of ​ ​ Azerbaijan is 75.1 thousand km ², Ireland - 70.273 thousand km ².

Illustration: maps-rf.ru

Great Caucasian Range

Main article: Main Caucasian Range

Navagir Range

The Navagir Range (Navagir Range) is a small low-mountain range near the northwestern tip of the Caucasus Mountains, one of the two (along with the Kuznya Range) main mountain systems of the Abrau Peninsula.

The Indo-European version of the name "Navagir" is confirmed by the fact that the word has an accurate translation from Sanskrit, which has a clear toponymic meaning. "Nava" नव - young, new, recent, "gir" गिर् (or "giri" गिरि) - mountain. "Navagir" is a new, young mountain (mountains). The version of the Turkic origin of the toponym Navagir has no confirmation.

The Navagir ridge differs from other mountains of the Caucasus in that it was formed as a result of a strong compression of the earth's crust. The length of the ridge on the Abrau Peninsula reaches about 5 km, along the valley of the Sukko River. The peaks of the Navagir Range are the Sugar Head Mountains (540 m) and the Sorcerer (440 m). Mount Sorcerer is a remnant of a coastal ridge, part of which went under water as a result of earthquakes and formed the entrance to Tsemes Bay. An extension of this ridge on the other side of the bay is Mount Doob (452 m).

Most of the streams are temporary in nature and are associated with snowmelt, spring thunderstorms and winter drizzle. The slopes of the Navagir ridge between Anapa and Sukko are covered with juniper gorelnik, in the spring many poppies also bloom here.

Markoth and Tuaphat Ranges

The Markoth Range is a mountain range in the northwestern part of the Greater Caucasus, running parallel and south of the Main Caucasus Range. The average height of Markoth is 350-500 meters, and individual peaks rise above 600 meters.

On the site between Novorossiysk and Gelendzhik in the Kabardinka region passes the low Tuaphat ridge. In a depression between the two ridges, the Kabardinka-Gelendzhik highway was laid.

Seismic activity

Map of earthquakes in the Krasnodar Territory in 2012-2022

Federal authorities

Territorial branches of federal authorities:

Government

Main article: Administration of the Krasnodar Territory

Settlements

Transport

Ministry of Transport and Roads of the Krasnodar Territory

Airports

Digitalization

2022: How the digitalization of the Krasnodar Territory goes

In May 2023, the head of the department of informatization and communications of the Krasnodar Territory Stanislav Zavalny spoke about the results of the ICT development of the region for 2022. In particular, he pointed to the achievement of the 95% import substitution rate during procurement procedures by the executive authorities of domestic software. In terms of the implementation of the digitalization program for small and medium-sized businesses, the region entered the top 5 regions in terms of the number of licenses sold for domestic software.

According to Zavalny, in 2022, 94 schools in the Krasnodar Territory carried out measures to form an IT infrastructure in accordance with the approved standard for ensuring safe access to information systems and the Internet in premises. 106 mass socially significant services were transferred to the unified portal of State Public services, of which 68 were state and 38 were municipal. In 331 state institutions of the region in 2022, electronic document management was introduced. In large municipalities of the region, the MPSC has 18 Cryptobiokabina software and hardware systems.

How is the digitalization of the Krasnodar Territory

Stanislav Zavalny also said that in 2022 measures were taken to support IT companies and the telecom industry - tax rates were reduced for companies using a simplified tax system.

As part of the development of the regional geo-information system of the Krasnodar Territory, a strategic module has been created for the purpose of digitalization and ensuring urban planning, access to which is provided to all municipalities. Five executive authorities were connected to the regional geo-information system of the Krasnodar Territory.

In addition, in 2022, the construction of an IT park in Krasnodar continued. The basement and first floors of the complex were erected.[1]

Power

Real estate

2023

For three years, real estate in Sochi has risen in price by 187.9% to 445 thousand rubles

For three years, real estate in Sochi has risen in price by 187.9%, follows from the data of the Nedvex Group agency. The average price per square meter in new buildings in April 2023 reached 445 thousand rubles. In 2020, this figure was equal to only 154 thousand rubles.

Sochi overtook London, New York and Dubai at the price of luxury housing

In 2023, Sochi overtook New York and London in terms of the cost of luxury housing. Luxury apartments in Sochi turned out to be more expensive than in New York, London and Dubai, analysts at NF Group calculated. The price of 1 sq. m of a few elite residential complexes in the resort city exceeds 1.4 million rubles.

Culture

Ministry of Culture of the Krasnodar Territory

Education

Ministry of Education, Science and Youth Policy of Krasnodar Kra Ministry of Education, Science and Youth Policy of Krasnodar Territory]]

Korenovsky district]]

Educational centers

Universities of the Krasnodar Territory

Colleges and organizations of DPO

Tourism

2023: Decrease in income from resort fees to 742.19 million rubles

In the Krasnodar Territory, at the end of 2023, revenues from the resort tax decreased - to 742.19 million rubles against 747.03 million rubles a year earlier. This is evidenced by the data of the regional Ministry of Resorts, Tourism and Olympic Heritage, released at the end of February 2024.

As RBC writes with reference to the materials of the department, the reduction in the resort failure in the Krasnodar Territory occurred for technical reasons - due to the withdrawal of the Sirius city district from the list of territories of the experiment on the collection of resort tax. Against this background, the number of tourists who paid the resort fee in 2023 decreased by 0.5 million people - to 3.1 million.

Sanatorium named after Ordzhonikidze, Krasnodar Territory

At the same time, the decrease in the volume of resort fees in the region occurred against the background of a record flow of tourists recorded in Kuban resorts in 2023. According to Vice Governor Alexander Ruppel, more than 17.5 million people rested in the region in 2023, which is almost a million more than in 2022.

According to RBC, about half of tourists paid tourist tax in hotels in the Krasnodar Territory that charge a resort fee in 2023. The publication notes that tourists renting private houses, apartments and rooms do not pay the resort fee - it is provided only for hotel and hotel guests.

As of the end of December 2023, resort fees in the Krasnodar Territory were charged in 17 municipalities, including in the resort cities of Sochi, Anapa, Gelendzhik, in the cities of Goryachiy Klyuch, Tuapse, Yeisk, Novorossiysk, on the federal territory of Sirius, as well as in rural settlements of the Tuapse region (seaside settlements Shepsi, Nebug, Dzhubga, etc.) and Mostovsky district (mountain resort territories). In Sochi, tourists are charged 50 rubles per day, on the rest of the territory - 30 rubles per day.[2]

2022: Income from the resort fee increased 4.5 times to 747 million rubles

In 2022, the budget of the Krasnodar Territory received 4.5 times more funds from the resort fee than in 2021 - 747 million against 165 million rubles, respectively. This is evidenced by the data of the Ministry of Resorts, Tourism and Olympic Heritage of the region, which were released on March 13, 2023.

The high growth of the indicator in the department was explained by an increase in the collection rate. In Sochi, the size of the resort tax was increased from 10 to 50 rubles, at other resorts - up to 30 rubles.

In Sochi, the resort tax increased fivefold

According to published statistics, in 2022, 3.6 million people paid a resort fee in the Krasnodar Territory, a year earlier - 3.1 million tourists. At the same time, only every fifth tourist paid for the resort fee. A significant share of hotel guests are preferential categories of citizens exempted from paying resort fees. In addition, the fee is not charged to tourists in guest houses and in the private sector.

However, according to the governor, 17.4 Veniamin Kondratyeva million tourists rested in the region in 2022. Based on this assessment, the number of those who paid the resort fee could be almost five times less than the number of all vacationers, the publication calculated. RBC

According to the reports of 12 municipalities included in the experiment on resort collection, a total of about 6.5 million tourists stopped in the accommodation facilities located on their territory for the year (22% more than in 2021). Based on the assessment of the Ministry of Resorts, Tourism and Olympic Heritage of the Krasnodar Territory on the number of holiday tax payers, 55% of tourists paid the tax.

Against the background of restriction of trips of Russians abroad in 2022 because of the sanctions which affected aircraft and the banking sector, internal tourist flow across Russia grew, the founder of Hot Consulting management company Roman Sabirzhanov says. The closure of the airports of part of the southern resorts in 2022 affected the travel time to the resort rather than the[3] of[4]fifth tourist

Health care

Ministry of Health of the Krasnodar Territory

Clinics

Organizations of the Krasnodar Territory

History

Main article: History of Russia

1981

Fashionistas in "firmé" look for prey at a disco, Sochi, 1981.

1973

Bright and colorful embankment in Soviet Sochi, 1973.

1961

Yuri Gagarin resting in Sochi, 1961

1907: Opening of the monument to Catherine II

Monument to Catherine II in Krasnodar. It was discovered in 1907, destroyed by the Bolsheviks in 1920, restored in 2006.

1828: The beginning of the construction of Russian fortifications on the coast of the West Caucasus

200 BC: Bosporus Kingdom

III thousand BC: Dolmen culture

Place of dolmenny culture on chronological scheme of cultures of Stavropol, Kuban and North Caucasus, V.A. Trifonov, 2001

In the Middle Bronze era of the XX-XIV centuries BC. The territory of the Sochi region is included in the cultural center covering Prikuban and Georgia. This stage here is represented by dolmenny cultural monuments.

The Volkon dolmen is the only surviving full-size dolmen of the monolithic type in the world. It is located on the bottom of the Godlik River valley in the village of Volkonka, Lazarevsky District, near the Novorossiysk-Sochi highway.
Dolmen trough-shaped in the Kuapse river basin in the Lazarevsky district.

IV thousand years BC.

1.6 million hp: Taman faunal complex: elephants, rhinos, hyenas and leopards on the Taman Peninsula and the Lower Don

Main article: Faunistic complexes of quaternary mammals

1.6-0.8 million years ago - Taman (Absheron) faunal complex. As a result of a number of factors, the death and burial of skeletons of large, mainly thick-skinned animals - elephants and rhinos - took place in the caldera of one of the large mud volcanoes (Blue Balka/Bogatyri). Animals died in this place, bogged down in a furnace of mud, unable to get out of the basin with steep banks, became easy prey for predators or died from poisonous gases periodically emitted by the volcano. The accumulation of carcasses did not occur simultaneously, but over a relatively long time. Read more here.

2.05 million hp: The first tools of human labor

Main article: Paleolithic in Russia

175 mln hp: Formation of the Big Caucasus basin

The split of South America and Africa (with Arabia) led to an increase in the oceanic lithosphere between them and, which is very important for the Caucasus, to a reduction in the distance between Africa and Eurasia. The Tethys Ocean began to shrink in size.

Where the oceanic crust of the Tethys Ocean pushed hard under the edge of the Scythian Plate, this edge weakened. This is due to the fact that the ocean plate, going down, melts, and the excess of molten matter tries to break up.

Rifting began to occur on the weakened edge of the plate - the formation of rifts with the extension of the split fragments of the previous base. The new crust was expanding toward the ocean. The crust was generally continental, granite, but broken by outpourings of basalts. So (at the end of the Lower and beginning of the Middle Jurassic, something about 175 million hp) the so-called Big Caucasus basin was formed. It was a marginal sea. It was separated from the main ocean of Tethys by an island volcanic arc, the existence of which is also explained by the weakening of the lithosphere in the subduction zone, the sub-wave, and the breakthrough of magma to the surface with the formation of volcanoes. The Big Caucasus Basin was extended 1700-1800 km long and 300 km wide.

270 million hp: Collapse of the mountains and the formation of the Scythian platform

Main article: The history of the Earth before the appearance of hominids

In the Permian period (its time interval from 299 to 250 million hp), the orogen (mountain structure) began to experience collapse, the rapid disappearance of mountains. The reasons for the collapse are the following. Since this orogen was not sandwiched between the mainland massifs, but arose due to the departure of the ocean plate under the continent, with the weakening of pressure and immersion of the ocean plate, the forces raising mountains weakened. The blocks forming the mountains began to slide down. The crumpled, compressed, compressed folds were then permeated with granite intrusions (incursions). These intrusions, as it were, reinforced and fixed the folds. Pressure and temperatures turned sedimentary and volcanic rocks into chlorite and sericite shales, which mainly form the Scythian Plate[5].

So along the northern edge of the Tethys Ocean, on the site of today's plains of the Ciscaucasia, a young (compared to the ancient Russian platform) Scythian platform was formed from a movable belt. Its latitudinally extending folds and slightly still mobile heterogeneous blocks hold memories of the processes of compression and life of the mountain structure. Despite the fact that we practically cannot see them.

As a result, the main result of the events of that time, the end of the Paleozoic, was the formation of the Scythian platform, soldered to the Russian platform along its current southern edge.

335 million hp: The rapprochement of Laurasia and Gondwana leads to subduction and volcanic activity

In the second half of the Paleozoic, there is a rapprochement between Laurasia (North America plus Europe) and Gondwana (Africa plus South America).

In the process of rapprochement in the south of the Russian platform, where the Ciscaucasia is spread today, an area of ​ ​ folding is formed, a movable belt associated with the existence of a subduction zone, when the oceanic crust is absorbed under the mainland, weakening its edge and ensuring volcanic activity and mobility of the crust of the entire region.

Globally, the approach at the end of the Paleozoic ended with the collision of Laurasia and Gondwana and the formation of the supermateric or supercontinent Pangaea.

Locally, in the process of rapprochement, the mentioned mobile belt experienced its evolution, lived its history. His story is a local episode of the global picture of the convergence of lithospheric plates.

Compression deformations in the movable belt, which created a folded structure, began in the middle of the Visean age of the early Carboniferous period, Carboniferous (about 335 million hp). The cause of the deformations was the pressure of the oceanic crust on the belt during the approach of the mainland blocks. They turned the movable belt, the future Scythian platform, into an orogen, a mining structure.

Notes