scholarly journals Anatolia as a bridge from north to south? Recent research in the Hatti heartland

2007 ◽  
Vol 57 ◽  
pp. 65-75
Author(s):  
Thomas Zimmermann
Keyword(s):  
Bronze Age ◽  
Black Sea ◽  
Central Anatolia ◽  
Early Bronze Age ◽  
The Black Sea ◽  
Southeast Europe ◽  
The Caucasus ◽  
Black Sea Region ◽  
The Third ◽  
The North

AbstractThis paper aims to reappraise and evaluate central Anatolian connections with the Black Sea region and the Caucasus focusing mainly on the third millennium BC. In its first part, a ceremonial item, the knobbed or ‘mushroom’ macehead, in its various appearances, is discussed in order to reconstruct a possible pattern of circulation and exchange of shapes and values over a longer period of time in the regions of Anatolia, southeast Europe and the Caucasus in the third and late second to early first millennium BC. The second part is devoted to the archaeometrical study of selected metal and mineral artefacts from the Early Bronze Age necropolis of Resuloğlu, which together with the contemporary settlement and graveyard at Kalınkaya-Toptaştepe represent two typical later Early Bronze Age sites in the Anatolian heartland. The high values of tin and arsenic used for most of the smaller jewellery items are suggestive of an attempt to imitate gold and silver, and the amounts of these alloying agents suggest a secure supply from arsenic sources located along the Black Sea littoral in the north and probably tin ores to the southeast of central Anatolia. This places these ‘Hattian’ sites within a trade network that ran from the Pontic mountain ridge to the Taurus foothills.

THE ECONOMIC-MILITARY IMPORTANCE OF THE BLACK SEA – NORTH SEA CORRIDOR FOR ENSURING STABILITY IN SOUTHEAST EUROPE

2021 ◽  
Vol 17 (1) ◽  
pp. 141-146
Author(s):  
Valentin-Costinel TOTIR ◽  
Roxana ALEXANDRU
Keyword(s):  
Eastern Europe ◽  
Black Sea ◽  
North Sea ◽  
The Black Sea ◽  
Southeast Europe ◽  
European Continent ◽  
Black Sea Region ◽  
South Eastern ◽  
South Eastern Europe ◽  
The Impact

Abstract: During history, the main channel of communication and cooperation between countries was through commerce and, consequently, through transport. Among all the transport ways, the maritime transport is the one that offers the best cost – benefits ratio. This article is addressed to all the people involved or interested in the economic and military fields and aims to highlight the importance of the Black Sea and North Sea connecting corridor in ensuring peace and stability in Europe in general and in South-Eastern Europe in special. To achieve this goal, we will review the historical conflicts among European countries for waterway control and make a descriptive analysis of the stability situation in the areas affected by them. Furthermore, using the hypothetical-deductive method, we will highlight the manner in which the connection of the Black Sea with the North Sea has influenced economic and military exchanges between riparian states and the impact on stability across European continent. At the end of the article, we will show how economic and military stability in south-eastern Europe is influenced and threatened by geopolitical changes in the wider Black Sea region and how this stability can be maintained and strengthened due to the great possibilities for economic cooperation among the countries of Western and South-Eastern Europe. The novelty of this approach is that it aims to analyze the importance of the Black Sea-North Sea channel in the context of fundamental changes in the politico-military situation in South-East Europe, generated by the expansion of the Russian Federation and the conflict between Turkey and Greece, NATO member countries.

Introduction

2016 ◽  
pp. 1-8
Author(s):  
Paul Huddie
Keyword(s):  
Black Sea ◽  
Russian Empire ◽  
The Black Sea ◽  
Western Balkans ◽  
Crimean War ◽  
Black Sea Region ◽  
The North ◽  
The Russian Empire ◽  
North Western

The year 2014 marked the 160th anniversary of the beginning of the Crimean War, 1854–6. It was during that anniversary year that the names of Crimea, Sevastopol, Simferopol and the Black Sea re-entered the lexicon of Ireland, and so did the terms ‘Russian aggression’, ‘territorial violation’ and ‘weak neighbour’. Coincidentally, those same places and terms, and the sheer extent to which they perpetuated within Irish and even world media as well as popular parlance, had not been seen nor heard since 1854. It was in that year that the British and French Empires committed themselves to war in the wider Black Sea region and beyond against the Russian Empire. The latter had demonstrated clear aggression, initially diplomatic and later military, against its perceived-to-be-weak neighbour and long-term adversary in the region, the Ottoman Empire, or Turkey. As part of that aggression Russia invaded the latter’s vassal principalities in the north-western Balkans, namely Wallachia and Moldavia (part of modern-day Romania), collectively known as the Danubian Principalities. Russia had previously taken Crimea from the Ottomans in 1783....

Architecture of One-Apsidal Churches of North Black Sea Coast VI-XII c.

2018 ◽  
Vol 931 ◽  
pp. 790-796
Author(s):  
Viktoria V. Pishchulina
Keyword(s):  
Black Sea ◽  
The Black Sea ◽  
Byzantine Empire ◽  
Black Sea Region ◽  
The North ◽  
Black Sea Coast ◽  
The Crimea ◽  
The One ◽  
Sea Coast

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.

Imperial confrontation or regional cooperation?: Bulgarian migration and Ottoman-Russian relations in the Black Sea region, 1768-1830s

2012 ◽  
Vol 3 (2) ◽  
pp. 149-167 ◽  
Author(s):  
Andrew Robarts
Keyword(s):  
Black Sea ◽  
Regional Cooperation ◽  
Armed Conflicts ◽  
The Black Sea ◽  
The Caucasus ◽  
Black Sea Region ◽  
The Balkans ◽  
Political Analysis ◽  
Primary Unit

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.

scholarly journals The spatial pattern of selected extreme precipitation indices for Turkey (1975-2012)

2020 ◽  
Vol 19 (1) ◽  
pp. 19-30
Author(s):  
Faize Sarış
Keyword(s):  
Coastal Zone ◽  
Black Sea ◽  
Extreme Precipitation ◽  
Precipitation Extremes ◽  
The Black Sea ◽  
The South ◽  
Black Sea Region ◽  
North East ◽  
The North ◽  
Rainy Days

AbstractThis paper analyses extreme precipitation characteristics of Turkey based on selected WMO climate change indices. The indices – monthly total rainy days (RDays); monthly maximum 1-day precipitation (Rx1day); simple precipitation intensity index (SDII); and monthly count of days when total precipitation (represented by PRCP) exceeds 10 mm (R10mm) – were calculated for 98 stations for the 38-year overlapping period (1975–2012). Cluster analysis was applied to evaluate the spatial characterisation of the annual precipitation extremes. Four extreme precipitation clusters were detected. Cluster 1 corresponds spatially to Central and Eastern Anatolia and is identified with the lowest values of the indices, except rainy days. Cluster 2 is concentrated mainly on the west and south of Anatolia, and especially the coastal zone, and can be characterised with the lowest rainy days, and high and moderate values of other indices. These two clusters are the most prominent classes throughout the country, and include a total of 82 stations. Cluster 3 is clearly located in the Black Sea coastal zone in the north, and has high and moderate index values. Two stations on the north-east coast of the Black Sea region are identified as Cluster 4, which exhibits the highest values among all indices. The overall results reveal that winter months and October have the highest proportion of precipitation extremes in Turkey. The north-east part of the Black Sea region and Mediterranean coastal area from the south-west to the south-east are prone to frequent extreme precipitation events.

scholarly journals Polish Consulate in Odessa in 1918 – 1920 and its Archive

2017 ◽  
pp. 415-424
Author(s):  
Tomasz Ciesielski ◽  
Keyword(s):  
Black Sea ◽  
The Black Sea ◽  
Black Sea Region ◽  
Large Group ◽  
The Third ◽  
The Republic ◽  
The City

General Consulate of the Republic of Poland established in Odessa in 2003 is the third Polish diplomatic mission in the Black Sea region of present – day Ukraine. The second Polish consulate, representing the reviving Polish statehood, functioned at the Black Sea between January 1919 and the beginning of February 1920, with almost a 5-month-long break, during the first Bolshevik occupation of Odessa. Zenon Belina Brzozowki was the consul in office during the period of January, 4, 1919 to March, 3, 1919 and then again since the end of August, (between April and August he stayed in Istanbul), in October and November, 1919 he was replaced by Stanisław Srokowski, a diplomat in the rank of I class consul, i.e. the present general consul. The consulate changed its location few times, and in different months the number of its employees varied from a few people to over a dozen. The consulat functioned in Odessa until March, 3, 1920 when it was evacuated along with a large group of Polish citizens because of the inevitability of the Bolshevik takeover of the city. Consulate staff and archives reached Warsaw in March 1920. Not many archival materials regarding the functioning of Polish consulat in the Black Sea region were saved.

scholarly journals Mantle earthquakes in the Crimea-Black Sea-Caucasus regions

2021 ◽  
Vol 43 (5) ◽  
pp. 60-79
Author(s):  
V. Burmin ◽  
O. Kendzera ◽  
L. Shumlianska ◽  
T. Amashukeli
Keyword(s):  
Black Sea ◽  
North Caucasus ◽  
Low Velocity ◽  
The Caucasus ◽  
Black Sea Region ◽  
Caucasus Region ◽  
The North ◽  
Deep Earthquakes ◽  
The Crimea ◽  
Mantle Earthquakes

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.

Dolmens of North Caucasia

Antiquity ◽  
1933 ◽  
Vol 7 (26) ◽  
pp. 190-202 ◽  
Author(s):  
A. M. Tallgren
Keyword(s):  
Bronze Age ◽  
Black Sea ◽  
The Black Sea ◽  
High Mountain ◽  
Mountain Range ◽  
The Caucasus ◽  
Western Influence ◽  
Mountain Chain ◽  
Kuban River ◽  
High Level

The Caucasus is by no means a homogeneous region. It consists of a very high mountain-chain, the main parts of which reach to a height of over 5000 metres, with others of 1000–1600 metres. Forming an isthmus between two seas, the Asiatic Caspian and the Mediterranean Black Sea, it is open to both eastern and western influence. There is no distinct boundary between its northern part and the endless Eurasiatic grasslands, and in the south it is connected with the Armenian and Anatolian highlands. South of the mountain-chain the Caucasus has a Mediterranean climate: vines, rice and tea are cultivated and it is rich in metals. North of the mountain-range also the soil is very fertile, especially in the valley of the Kuban river. There, in the northeast corner of the Euxine, prehistoric culture flourished very early and reached a high level. I shall here give an outline sketch of its character, and especially of the so-called Kuban culture of the Early Bronze Age, which takes its name from the Kuban river. This river flows into the Black Sea, but its upper course lies in the high mountains not far from the Elbruz. It has many tributaries, especially on the left, the Caucasian, side. Among these the Laba, the Belaya and the Abin may be mentioned.

Sign in / Sign up

Export Citation Format

Share Document