scholarly journals The Huns in the Plains of Crimea

Author(s):  
Aleksandr Aibabin

The article reviews some evidence of written sources about the Huns in the Crimea and the Huns’ burials found in the plains of the Crimea. Many researchers of the Crimean history dated the invasion of the Huns in the Northern Black Sea region to the time of the reign of Emperor Valens (364–378) taking into account the information of only some narrative sources. However, there is no information about the Huns’ crossing through the Cimmerian Bosporus Strait and the attack on the Bosporus cities in the 370s in the written sources. According to Syrian and Greek sources, N.V. Pigulevskaya reasonably attributed Huns’ crossing through Meotida and the Caucasus Mountains to Mesopotamia and the Syrian coast to 395. This date is confirmed by the updated chronology of nomadic burials known in the Crimea and ceramics from Bosporan cities and settlements. Apparently, the Huns appeared on the peninsula after their settlement in the Northern Black Sea region at the end of the 4th – 5th centuries. Huns tombs on the hillside of Koklyuk, from the State Farm named after Kalinin, from Belyaus and on the necropolis of Ust-Alma are dated back to the first half of the 5th century by polychrome things. According to the funeral rite, the described Crimean graves of the first half of the 5th century are similar to the graves excavated under the kurgans with horse skin known in steppes of the Northern Black Sea region. I.P. Zasetskaya reasonably associated them with the Turks, who were part of the Hunnic tribal union. Nomad burials in Izobilnoe were attributed to the second half of the 5th century, in Marfovka – to the end of the 5th century, and in Chykarenko – to the first half of the 6th century. The graves of nomads of the first half of the 5th century belonged to the Akatziri, and the graves of the second half of the 5th century – first half of the 6th century belonged to Huns-Altziagiri.

2021 ◽  
Vol 43 (5) ◽  
pp. 60-79
Author(s):  
V. Burmin ◽  
O. Kendzera ◽  
L. Shumlianska ◽  
T. Amashukeli

The question of the existence of foci of deep earthquakes in the region of the Crimea-Black Sea-Caucasus is extremely important from the point of view of the geodynamics of the region. Previously it was thought that only crustal earthquakes could occur in this region. Recently, results have been obtained that show that earthquakes with depths of at least 300 km occur in this region. The article discusses the question of how plausible these results are and why they were not obtained earlier. Seven specific examples of the ambiguous determination of the depth of earthquake hypocenters in the Crimea-Black Sea-Caucasus region are considered. These examples clearly show that determining the coordinates of earthquake hypocenters using algorithms based on the Geiger method does not allow one to uniquely determine the depth of the hypocenters. The article gives an idea of the authors about the origin of mantle earthquakes in the Caucasian and Crimean-Black Sea regions. For the Caucasus region, mantle earthquakes are associated with two reasons: submersion of the lithospheric layer; in the asthenospheric layer, represented in the seismotomographic sections by a low-velocity anomaly, the nature of earthquake foci is associated with fluids formed during phase transition reactions. In the Crimean-Black Sea region, earthquake foci are located in the lithosphere layer, and the sliding of the lithosphere along the less viscous underlying layer of the upper mantle causes tectonic movements in the lithosphere accompanied by earthquakes. In addition, to determine the coordinates of the hypocenters of the Crimean and Caucasian earthquakes during routine processing, hodographs were used for depths not exceeding 35 km for the Crimea and 50 km for the Caucasus and 150 for the North Caucasus. This circumstance is the main reason why deep earthquakes could not be detected.


2021 ◽  
Vol 6 (1(34)) ◽  
pp. 4-7
Author(s):  
Yuri Georgievich Shcherbina

According to the qualitative and quantitative assessment of springtails communities since 2007, the dynamics of the state of the Colchis boxwood ecosystems in the Sochi Black Sea region has been estimated. The conclusion about the dynamics of degradation of forest communities, unique for the coast, after the Olympic Games-2014 is substantiated.


Author(s):  
Gerard Toal

It was supposed to be China’s coming-out party, a moment in the global spotlight affirming its arrival as an economic superpower. But hours before the opening ceremonies of the 2008 Beijing Olympics, news of a war in the Caucasus flashed across the world’s TV screens. On the southern slopes of the Caucasus Mountains, the state of Georgia launched a military offensive against South Ossetia, a small breakaway territory beyond its control since the Soviet collapse. Georgia’s offensive quickly brought Russia to the defense of its local Ossetian allies. As Soviet-era tanks rolled through the Roki tunnel, the only land connection between South Ossetia and Russia, Russian aircraft bombed Georgian targets in the region and beyond. For the first time since the Cold War ended, Russia was invading a neighboring state. Instead of glowing stories about China, speculation about a new Cold War filled the front pages of the Western press. Yet within a week the war was over and a ceasefire agreed. Thereafter a rapidly moving global financial crisis displaced what seemed a harbinger of geopolitical rupture to an afterthought. As quickly as it had flared, the Russo-Georgian war disappeared, and with it talk of a return to geopolitics past. Six years later Russia was in the global spotlight as host of the XXII Olympic Winter Games in Sochi, located on the shores of the Black Sea at the western end of the Caucasus Mountains. Despite well-grounded fears of terrorism, the Olympics were a triumph for Russia and its leadership. Yet a few days later, the world recoiled in shock as Russia once again invaded a neighboring state. Responding to a perceived “fascist coup” in Kyiv, unmarked Russian military personnel seized control of the Ukrainian province of Crimea, once part of Soviet Russia and home to Russia’s Black Sea Fleet. A hastily organized referendum followed, creating the appearance of legitimacy for Russia to formally annex the province, and the city of Sevastopol, in late March 2014.


2018 ◽  
Vol 931 ◽  
pp. 790-796
Author(s):  
Viktoria V. Pishchulina

A one-apsidal hall church is always a reflection of so-called “vulgar” Christianity, thus revealing the important peculiarities of the spatial culture of the region where it is erected. In this region we can mark two periods when such temples were built: VI-VII c. and X-XII c. The first period is associated with the missionary activity by Byzantine Empire, Antioch, Caucasian Albania which was conditioned by both geopolitical interests (Byzantian Empire, Antioch) and the shift of The Great Silk Way to the north (Caucasian Albania). The second, as the research has shown, is connected with the migration of the peoples of Abkhazia, the abzakhs to this territory in the XII-XIII c. and the development of contacts with the Crimea. In the North Black Sea Region the one-apsidal hall church appears as early as in the VI c. – in the territory of Abkhazia we know about ten such temples. The temples of this type in the area of Big Sochi are dated back to the VII-VIII c. In the first Abhzaian temples we can reveal the influence of denominational centers – Byzantian Empire, Antioch, Caucasian Albania. In the temples of the Black Sea coast of both periods – introduction of the samples from Abkhazia.


2012 ◽  
Vol 3 (2) ◽  
pp. 149-167 ◽  
Author(s):  
Andrew Robarts

The Black Sea region from 1768-1830s has traditionally been characterized as a theater of warfare and imperial competition. Indeed, during this period, the Ottoman and Russian empires engaged in four armed conflicts for supremacy in the Balkans, the Caucasus, and on the Black Sea itself. While not discounting geo-strategic and ideological confrontation between the Ottoman and Russian empires, this article - by adopting the Black Sea region as its primary unit of historical and political analysis - will emphasize the considerable amount of exchange that took place between the Ottoman and Russian empires in the Black Sea region in the late eighteenth and early nineteenth centuries. Building upon a case study of Bulgarian migration between the Ottoman and Russian empires and as part of a broader discussion on Ottoman-Russian Black Sea diplomacy this article will detail joint Ottoman-Russian initiatives to control their mutual Black Sea borderland.


2011 ◽  
Vol 17 (1) ◽  
pp. 125-133
Author(s):  
Pantelis Charalampakis

Abstract The author examines the question of the place name Trapezus recorded by ancient sources as being located north of the Black Sea. This toponym indicates a mountain which bears no relation to the Pontic city of Trapezus. According to the written sources only, this place name cannot be identified. On the contrary, as suggested by archaeological evidence and the testimony of Procopius about the Goths Trapezitae, the predominant opinion of Chatÿr Dag appears to provide the most satisfactory solution for the identification of Mount Trapezus. This mountain was never known as Hermonassa and is not related to the Taman peninsula.


Author(s):  
Vodotyka S. ◽  
Robak I.

The article is devoted to reviewing the book by the well-known Turkish historian İlber Ortaylı "Ottomans on Three Continents". The authors consistently analyze the main postulates of the work in the history of Ottoman possessions in the Crimea and the Northern Black Sea region, focusing on the role of the Ottoman Empire in the interaction of Black Sea civilizations in the late Middle Ages and early modern times.The authors prove that the history of the Ottoman Empire is essential for understanding the history of Ukraine. Ottoman influences significantly impacted the history of the Ukrainian people and other indigenous peoples of Ukraine – Crimean Tatars, Karaites and Krymchaks, Crimean Greeks.The authors agree with the thesis of the Turkish researcher about the significant and sometimes decisive influence of the Ottomans on the situation in the Black Sea region in the XV–XVIII centuries. Furthermore, the authors express their views on certain statements of the book. In particular, İlber Ortaylı proves that the Ottoman Empire was a "state of the Middle Eastern Islamic type". Its presence in the Black Sea resulted in the interaction of Islamic Mediterranean civilization with Eastern European Orthodoxy and Ukraine were at the centre of this interaction. However, the authors cannot agree with the historian's statement about the primary basis of the empire – the system of the state, especially military, slavery (devshirme). It allowed to creation of a vast empire, The Sublime or Ottoman Porte. However, slavery could not create social mechanisms of progress. The civilizational basis of the Ottoman Empire was its steppe, Turkic-steppe, essence.In the Ottoman Empire, Western modernization borrowings were superficial, served utilitarian-pragmatic purposes, and did not change the foundations of civilization. Such selectable reforms were the reason why the Omans lost their possessions in the Crimea and the Northern Black Sea region to the Russian Empire in the eighteenth century. Significantly, both empires claim the imperial, not civilizational, heritage of the Roman Empire. The intelligence emphasizes that these claims are not sufficiently substantiated.Key words: İlber Ortaylı, Ottoman Empire, heritage, history of Ukraine, Northern Black Sea Coast, Crimea. Стаття присвячена огляду-рецензії книги відомого турецького історика Ільбера Ортайли «Османи на трьох континентах». Автори послідовно проаналізували основні постулати праці в координатах історії османських володінь в Криму і Північному Причорномор’ї, приділивши головну увагу ролі Османської імперії у взаємодії цивілізацій Чорномор’я у періоди пізнього середньовіччя і раннього модерного часу.Доведено, що історія Османської імперії має важливе значення для розуміння історії України. Османські впливи відіграли значну роль в історії українського народу та інших корінних народів України – кримських татар, караїмів і кримчаків, кримських греків.Автори погоджуються з тезою турецького дослідника про значний, а часом визначальний, вплив Османів на ситуацію у Чорномор’ї у ХV–ХVІІІ ст. та висловлюють свої міркування щодо окремих положень праці. Зокрема, І. Ортайли кваліфіковано доводить, що Османська імперія була «державою близькосхідно-ісламського типу» і її присутність у Чорномор’ї мала наслідком взаємодію ісламської середземноморської цивілізації зі східноєвропейською православною, причому Україна знаходилась у центрі цієї взаємодії. Однак, не можна погодитись з твердженням історика щодо головної основи імперії – системи державного, передусім військового, рабства (девшірме). Вона дозволило створити величезну імперію, Сяючу Порту, але рабство не може створити суспільних механізмів поступу. Цивілізаційною основою Османської імперії стала її степова, тюрксько-степова, сутність. В Османській імперії західні модернізаційні запозичення були поверховими, служили утилітарно-прагматичним цілям і не змінювали цивілізаційних основ. Власне це і стало основною причиною того, що у ХVІІІ ст. Омани втратили свої володіння в Криму і Північному Причорномор’ї, які дістались Російській імперії. Показово, що обидві імперії висувають претензії на імперську, а не цивілізаційну, спадщину Римської імперії. У розвідці наголошується, що ці претензії не є достатньо обґрунтованими. Ключові слова: І. Ортайли, Османська імперія, спадщина, історія України, Північне Причорномор’я, Крим.


2020 ◽  
Vol 28 ◽  
pp. 272-288
Author(s):  
Anna Mastykova ◽  

The article deals with the discovery of a great multifaceted crystal bead in the settlement of the Kolochin culture of Kartamyshovo-3 in Upper Psel (Oboyansk district, Kursk region). Findings of such beads are given in the Northern Black Sea region, in the Caucasus, in Central and Western Europe. Thanks to these parallels, the chronology of crystal faceted beads is established within the framework of the end of the III / IV — the second half of the VII century. These beads, of Mediterranean or Sassanian origin, most likely fall into the Middle Dnieper as a result of contacts with the South-Western Crimea in the last third of the VI — first half of the VII century.


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