Geopolitical Factor in the Political Turbulence of the Black Sea-Caspian Region and the North Caucasus

2020 ◽  
pp. 203-210
Author(s):  
М. Васьков
Author(s):  
Valenina Mordvinceva ◽  
Sabine Reinhold

This chapter surveys the Iron Age in the region extending from the western Black Sea to the North Caucasus. As in many parts of Europe, this was the first period in which written sources named peoples, places, and historical events. The Black Sea saw Greek colonization from the seventh century BC and its northern shore later became the homeland of the important Bosporan kingdom. For a long time, researchers sought to identify tribes named by authors such as Herodotus by archaeological means, but this ethno-deterministic perspective has come under critique. Publication of important new data from across the region now permits us to draw a more coherent picture of successive cultures and of interactions between different parts of this vast area, shedding new light both on local histories and on the role ‘The East’ played in the history of Iron Age Europe.


Author(s):  
I.Y. Matasova ◽  

The article considers the results of studying the features of Sr distribution in rocks of various ages and composition and soils of landscapes of the Black Sea coast of Russia (in the humus horizon and soil profile). The content of elements in the studied soils is compared with the regional background for the soils of the North Caucasus. A direct relationship between the content of the element in soils and underlying rocks, as well as the influence of technogenesis on the processes of accumulation and removal of the element in the soils of agricultural landscapes, has been revealed. The results of a comprehensive study of the south of Russia became the basis for studying the peculiarities of the distribution of Sr landscapes of the Black Sea coast of Russia. To establish the main parameters of the distribution of chemical elements in rocks and soils of various landscapes and the region as a whole, to identify geochemical features of geographical and technogenic differentiation, to assess the impact of various types of environmental management on changes in the geochemical spectrum of soils, to determine the influence of landscape-forming factors on the migration of chemical elements and the formation of geochemical barriers. The highest concentration of Sr was observed in carbonate-terrigenous rocks of the Paleogene and Cretaceous ages (marls and limestones). In the humus horizon of soils, the average metal concentrations vary in the range from 13.0∙10–3 to 95.0∙10–3 % with a regional clark of 22.0∙10–3 %.


2010 ◽  
Vol 16 (1-2) ◽  
pp. 217-551
Author(s):  
Marie-Françoise Billot

Abstract Architectural Terracottas of the Archaic to the Hellenistic Period from SinopeDecorated architectural terracottas held in the Sinope Museum are re-examined here from several angles: techniques of manufacture, combinations of different series on one and the same building, importing of models, export of these exclusively local products to cities of the North Pontic region, style and chronology. Reconsidered so as to take into account all significant features, this form of production ‐ recorded from as early as the 6th century BC ‐ provides some continuation of the ‘Milesian’ tradition, which was widespread in the North of the Aegean and in the poleis of the Black Sea region. Yet, from the second quarter of the 4th century BC onwards, this production also manifests real originality of its own. Sinope would, however, probably not have developed its own style, if it had not received specific orders from Panticapaeum and the main cities of the Bosporan Kingdom. After gradually being deprived of this stimulus for production towards 300 BC, the workshop in Sinope quickly lost its impressive reputation, even though the volume of its tile production remained considerable. From all points of view, it would appear to have been subject to the political and economic vicissitudes experienced by its clients.


2020 ◽  
Vol 16 (3) ◽  
pp. 83-88
Author(s):  
S.G. POLOVKA ◽  
S.I. MATKOVSKA ◽  
O.A. POLOVKA ◽  
S.M. DOVBISH

The material in the article contains biographical information from the life and scientific activity of the doctor of geological and mineralogical sciences, professor, academician Academy of Sciences of the USSR A.D. Arkhangelsky. A wide range of the scientist is shown and a description of the main directions of research in the field of regional geology, fauna and stratigraphy of the Paleogene and Upper Cretaceous deposits of the Volga and Central Asia, lithology and paleography, issues of tectonics and the relationship of gravitational and magnetic anomalies with the geological structure of the territory of the USSR is given. The main attention is paid to his work in the study of the geology of oceans and seas. The main contribution of the scientist to the study of Mesozoic bauxites, their structure and mineral composition is described. On this basis, the scientist developed and substantiated a new sedimentary theory of their formation. This theory opened the possibility for geologists to approach the study of bauxite as sedimentary rocks; this played an important role in the search for new deposits of this valuable mineral. The complex of geological and geophysical work carried out by him on expeditions along the East European Plain provided an answer to important questions about the distribution of oil, coal and iron ores on the territory of the Russian Platform. Much attention was paid to the study of the geology of the Black Sea. Processing materials collected by a hydrographic expedition and a comparative study of the columns of the Black Sea silt and oil-bearing sediments of the Crimean-Caucasian region led the scientist to important conclusions about the conditions of accumulation of oil-producing suites. Long-year research A.D. Arkhangelsk sediments of the Black Sea, their lithology, geochemistry, structure, subsequent changes and deformations were summarized in a number of works, among which are “Conditions for the formation of oil in the North Caucasus” (1927), “Geological history of the Black Sea” (1932), “Geological structure and the history of the development of the Black Sea“ (1938), written together with N.M. Strakhov. In 1926—1928 Arkhangelsky lead the field geological survey work on the Kerch Peninsula for the study of oil fields.


2014 ◽  
Vol 7 (3) ◽  
pp. 108-122 ◽  
Author(s):  
Vyacheslav L. Baburin ◽  
Sofia A. Gavrilova ◽  
Peter Koltermann ◽  
Yury G. Seliverstov ◽  
Sergey A. Sokratov ◽  
...  

Author(s):  
Irina Gabsatarova ◽  
L. Koroletski ◽  
A. Sayapina ◽  
S. Bagaeva ◽  
Z. Adilov ◽  
...  

In 2014 a seismic network consisting of 60 stations, 57 of which were equipped with digital equipment, operated in the region. 1695 earthquakes and 63 explosions in industrial quarries were recorded within the region boundaries. In the settlements of the Caucasus, 21 earthquakes were felt. The maximum intensity did not exceed Imax=4 on the MSK-64 (SIS-17) scale. Such intensity was observed from earthquakes in the territories of Ingushetia–Chechnya and Azerbaijan. The aftershock process of the strong East Black Sea earthquake on December 23, 2012 (Мw=5.8) off the coast of Abkhazia continued. In 2014 about a hundred earthquakes with KP=5.3–9.5 were recorded. In the central part of Azov sea, two earthquakes with KP=9.9 and 7.4 were recorded in January and December. The earthquakes with intermediate depths in the Tersko-Caspian trough (Tersko-Sunzhenskaya zone) with КР> 9.5 were not recorded. Two strong earthquakes with KP=12 and intermediate depths occurred in the Kurin Depression of Azerbaijan and in the Caspian Sea. A swarm of weak earthquakes with КР=5.7–8.8 was recorded on December 13–15 in the Black Sea near Tuapse. In 2014 the most part of the earthquakes were recorded in the Tersko-Caspian and Kurin troughs, in the eastern part of the Greater Caucasus. According to the level of energy released, the seismicity of the territory of the North Caucasus in 2014 was characterized in accordance with the “SOUS-09” seismicity scale as “background average” for the observation period from 1962 to 2014.


Author(s):  
PILIPENKO S. ◽  

The use of birch bark in the design of knife sheaths and sabers have become the subject of our research more than once. These theses are no exception. Research carried out in recent years in the Black Sea region, and the study of museum collections, allow us not only to identify new pieces of cold steel weapons of the 17th-18th centuries, with the scabbard made of birch bark, but also to identify common technological traditions with earlier samples of cold weapons from the archaeological sites of medieval nomads in the south of Western Siberia. One of the topical issues in the study of the design features of the sheath of bladed weapons of the 16th -18th centuries. In the North Caucasus and Eastern Poland, there are issues of continuity in the use of birch bark in their design. Keywords: Saber-chechugi, Armenian saber, scabbard, birch bark, medieval nomads, western Siberia, Eastern Poland, north Caucasus, Black Sea region


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