Ottoman and Habsburg Legacies in the Balkans. Language and Religion to the North and to the South of the Danube River

2010 ◽  
Traditio ◽  
1953 ◽  
Vol 9 ◽  
pp. 213-279 ◽  
Author(s):  
Giles Constable

The years between 1146 and 1148 were signalized in the annals and chronicles of Medieval Europe by Christian campaigns on all fronts against the surrounding pagans and Moslems. The most important of these was directed towards the Holy Land, against the Moslems, who had recently seized Edessa. It consisted of no less than five expeditions. The two largest armies, commanded by the Emperor Conrad III and King Louis VII of France, followed the same route overland across the Balkans to Constantinople; both met with crushing defeats in Asia Minor and finally reached the Holy Land, as best they could, by land and sea. A third force, under Amadeus III of Savoy, moved down Italy, crossed from Brindisi to Durazzo, and joined the army of Louis at Constantinople late in 1147. In August of the same year a naval expedition led by Alfonso of Toulouse left the South of France and arrived in Palestine probably in the spring of 1148. At the same time, a joint Anglo-Flemish naval force sailed along the north coast of Europe, assisted the King of Portugal in the capture of Lisbon, proceeded around the peninsula early in 1148, attacked Faro, and presumably reached the Holy Land later that year. Meanwhile, in the northeast, four armies co-operated in a campaign against the pagan Wends across the river Elbe: a Danish army joined the Saxons under Henry the Lion and Archbishop Adalbero of Bremen in an attack on Dubin; another, larger, army led by Albert the Bear of Brandenburg and many other temporal and spiritual lords advanced against Demmin and Stettin; a fourth expedition, finally, under a brother of the Duke of Poland attacked from the southeast. In 1148, on the south shore of the Mediterranean, a powerful fleet under George of Antioch extended the control of Roger II of Sicily over the entire littoral from Tripoli to Tunis. In the West, four campaigns were directed against the crumbling power of the Almoravides. The Genoese in 1146 sacked Minorca and besieged Almeria. During the following year, the Emperor Alfonso VII of Castile advanced south through Andalusia and captured Almeria with the aid of a strong Genoese fleet, which in 1148 sailed north and joined the Count of Barcelona in his campaign against Tortosa. In the previous year, Alfonso Henriques of Portugal had captured Santarem and secured the assistance of the Anglo-Flemish fleet for an attack on Lisbon, which fell late in 1147.


Radiocarbon ◽  
1986 ◽  
Vol 28 (2B) ◽  
pp. 939-941 ◽  
Author(s):  
AFM de Jong ◽  
Bernd Becker ◽  
WG Mook

This paper contains 14C results obtained by the special high-precision proportional gas counter, designed by Tans and Mook (1978), on tree rings from the South German oak chronologies: Donau 7, 3, 10, and 12, originating from the Danube River basin (48° 24’ N, 10° 5’ E).


2001 ◽  
Vol 52 (1) ◽  
Author(s):  
Manfred Hainzmann

Celtic tribes once occupied a vast area which stretched from Ireland to Spain and northern Italy, down the Danube river to the Balkans. Even in Asia a small province named Galatia was held by the Galati, who were of Celtic origin and survived till late antiquity. Throughout these territories we find many archaeological traces of ancient Celtic religion. Highly important for the reconstruction of the Celtic pantheon are the widespread epigraphic testimonies on various votive objects from Celtic sanctuaries and shrines (e. g.: altars, columns, bronze tablets etc.) as well as the anepigraphic reliefs representing indigenous deities. With the ever increasing number of such significant finds this invaluable epigraphic source material has never been documented, analysed or interpreted in its entirety. Scholarly documentation, systematic analysis are nevertheless an essential premise to study ancient Celtic religion. It will not only allow us to recognise the linguistic origins, the meaning and the spread of Celtic deities, but will also improve our understanding of the phenomenon of


1994 ◽  
Vol 22 (2) ◽  
pp. 427-434 ◽  
Author(s):  
Arqile Berxholli ◽  
Sejfi Protopapa ◽  
Kristaq Prifti

Albania, founded at the Congress of Vlora on November 12, 1912, has a far more homogeneous national population than its neighboring states in the Balkans. The Sixth London Conference of the great powers in 1912–1913 ruthlessly divided the territories inhabited by Albanians. The conference fragmented more than half the territories inhabited by ethnic Albanian regions as follows: in the east and the northeast—Kosova, Dibra, Ohri, Struga and Pollugu up to Shkup (Scoplje); in the north—Tivari, Ulqini, Tuzi, Plava and Gucija; and in the south—Camerija. These lands, with an autochthonous Albanian population, were annexed by Serbia, Montenegro (in 1918 by the new Yugoslav State) and by Greece in 1913. Thus, the borders of Albania were confined to an area of 28,748 square kilometers and a population of a little more than 800,000.


Starinar ◽  
2009 ◽  
pp. 89-108 ◽  
Author(s):  
Aleksandar Bulatovic

Slightly biconical shaped bowls, the upper cone (rim and shoulder) of which is decorated with horizontal and slanted facets or slanted channels, as well as semi-globular bowls of inverted rim decorated with horizontal facets or slanted channels are characteristic of the end of Bronze Age and mark the beginning of Iron Age in many cultural groups within the Balkan Peninsula. Problem of their origin, chronology and distribution is present in archaeological literature for a long time. Many authors perceived the significance of this ceramic shape for the chronological, ethnic and cultural interpretation of the Late Bronze, that is, of the Early Iron Ages within the territory of the Balkans. Pottery from the burned layers in Vardina and Vardaroftsa sites in the north of Greece, among which there were bowls with inverted, slanted channeled rim, was designated way back by W. Heurtley as Danubian pottery or Lausitz ware, connecting its origin with the Danube Basin. Anumber of conclusions have been reached upon the study of finds of slightly biconical bowls and bowls of inverted rim, decorated with channels or facets, from several indicative sites from Late Bronze and Early Iron Ages within the Balkan Peninsula and south part of the Middle Europe. It has been stated that the bowls appear first within the southwest Slovakia and northwest Hungary in the Br D period, to spread very fast, already in the Br D/Ha A1 period, from its home territory to the east, to the northeast Hungary and northwest Romania. Namely, this first spreading wave into these territories brought along only variety Ia bowls, which were further distributed to the south, during the Ha A1 period, to the central parts of the Balkan Peninsula and consequently it can be concluded that these bowls are somewhat older than other varieties. In the period Br D - Ha A1, in north Hungary, under the influence of Gava Culture, on one hand, and Caka Culture, on the other, appear also variety IIa bowls (turban dish), distributed to the east with a new migration wave, in the same manner as was the case with the first migration wave, but also to the south, along the Bakonjska Range, to the present day Croatia and Slovenia, where, in the Ha A1/A2 periods, were stated exclusively variety IIa bowls. Representatives of the variety Ia bowls remained in the Pomoravlje region and Juzna Morava Basin, as confirmed by a large number of these bowls and also by other ceramic shapes of that stylistic and typological pattern, prevailing within this region in the Ha A1/A2 periods. First variety IIa bowls (Mediana, Krzince) appear only during the second migration wave coming from the north of the Balkans to the central part of the Balkan Peninsula (Ha A2 period). These bowls, however, are particularly characteristic of Macedonia and lower Povardarje, where variety Ia bowls were not stated at all. The second migration wave representatives, with turban dish bowls (variety IIa), were much more aggressive as witnessed by many burned settlements from that period in the Vranjska-Bujanovacka Valleys and Povardarje. During Ha B-C periods, bowls of both types (particularly variety IIa) became inevitable part of ceramic inventory of nearly all cultural groups in the Balkan Peninsula, which could be explained by the spread of cultural influence of the new stylistic trend, though, however, it could be possible that migrations, which at the time were numerous and of greater or lesser intensity, were one of the spreading causes of this ceramic shape into the east, south and west parts of the Balkan Peninsula in the Ha B period. Representatives of the mentioned migrations, which were carried out in at least two larger migration waves, bringing along bowls to the Balkan Peninsula, are protagonists of historically known migrations from that period, known under names of Doric and Aegean migrations. The assumed direction of these migrations coincides mainly with the distribution direction of bowl types I and II. Migrations spreading the bowl types I and II started in the south part of the Middle Europe, but were initiated by the representatives of the Urnenfelder cultural complex from the Middle Europe, as observed in certain ceramic shapes, stated together with type I bowls and originating from cultures of the Urnenfelder complex, and in numerous metal finds, which were produced in Middle European workshops. It is of interest to point out that bowl movements could be followed up to the northwest shores of the Aegean Sea, but they are not stated in the south Trace and in Troy, thus imposing conclusion that their representatives did not reach Troy. Consequently, their possible participation in destruction of VIIb2 layer settlements is utterly uncertain. The migrations, however, started chain reaction of ethnic movements in the Balkans, causing many ethnic and cultural changes within this territory which will lead to creation of new cultural groups to mark the developed Iron Age. To what extent bowls of this type, particularly variety IIa, left deep trace in the Iron Age Cultures in the central Balkans, is shown in the fact that survivals of this variety remained within these regions even several centuries later, in late phases of the Ha C period (VI/V century BC).


2021 ◽  
pp. 187-190
Author(s):  
William Klinger ◽  
Denis Kuljiš

This chapter recounts Marshall Tito's departure from Vršac to Belgrade, in which the Purga radio (renamed Alpha) had a much stronger transmitter under the competence of the Soviet embassy in Yugoslavia. It talks about the failure of the Soviet thrust across the Danube after a fierce fight ended with an unsuccessful attempt of a combined landing at Vukovar. It also examines the members of the NOVJ 51st Division and Soviet marines that tried to form a bridgehead with the support of the Danube River flotilla of Admiral Sergey Georgyevich Gorshkov, future commander of the Soviet navy. The chapter explains why the NOVJ did not attempt a westward thrust on the Slavonian front. It demonstrates how the Soviet army crossed over to the Danube's left bank, while Tito's army attacked Thessalonica and Trieste.


Atmosphere ◽  
2020 ◽  
Vol 11 (11) ◽  
pp. 1182
Author(s):  
Bin Liu ◽  
Jian Liu ◽  
Liang Ning ◽  
Weiyi Sun ◽  
Mi Yan ◽  
...  

In this study, the role of AD 1258 Samalas mega volcanic eruption in the summer hydroclimate change over Europe and the corresponding mechanisms are investigated through multi-member ensemble climate simulation experiments based on the Community Earth System Model (CESM). The results show that the CESM simulations are consistent with the reconstructed Palmer Drought Severity Index (PDSI) and the historical records of European climate. Europe experiences significant summer cooling in the first three years after the Samalas mega volcanic eruption, peaking at −3.61 °C, −4.02 °C, and −3.21 °C in year 1 over the whole Europe, Southern Europe, and Northern Europe, respectively. The summer surface air temperature (SAT, °C) changes over the European continent are mainly due to the direct weakening of shortwave solar radiation induced by volcanic aerosol. The summer precipitation over the European continent shows an obvious dipole distribution characteristic of north-south reverse phase. The precipitation increases up to 0.42 mm/d in year 1 over Southern Europe, while it decreases by −0.28 mm/d in year 1 over Northern Europe, respectively. Both simulations and reconstructions show that the centers with the strongest increase in precipitation have always been located in the Balkans and Apennine peninsulas along the Mediterranean coast over Southern Europe, and the centers with the strongest precipitation reduction are mainly located in the British Isles and Scandinavia over northwestern Europe. The negative response of North Atlantic Oscillation (NAO) with significant positive sea level pressure (SLP) anomaly in the north and negative SLP anomaly in the south is excited in summer. The low tropospheric wind anomaly caused by the negative phase of NAO in summer affects the water vapor transport to Europe, resulting in the distribution pattern of summer precipitation in Europe, which is drying in the north and wetting in the south. The knowledge gained from this study is crucial to better understand and predict the potential impacts of single mega volcanic eruption on the future summer hydroclimate change in Europe.


2007 ◽  
Vol 15 (1) ◽  
pp. 210-215
Author(s):  
Barbara Gügold

This article is a book review about Claudi Magris' book, Danube, which presents an engaging journey along the Danube River. Claudio Magris guides the reader from the river’s source in the Bavarian hills through Austro-Hungary and the Balkans to its mouth at the Black Sea. The book is unique in its successful intertwining of travel impressions, prose, historical insights and philosophical reflection. 


Author(s):  
Miroslava Mirkovic

In the agreement which followed the first war between Constantine and Licinius and Constantine?s victory on the Campus Ardiensis, Licinius was forced, as generally accepted, to surrender Illyricum where he was undisputed ruler until 316. However he was not neutralized politically and reigned together with Constantine between AD 316 and 324. Some kind of division of the sphere of interest seems to have existed between them. Constantine, whose movements in the Balkans are known from the places of editing laws, visited only the western half, i.e. Illyricum after 316. If we follow the evidence of the places and dates of the promulgation of Constantine?s laws, we can consider the line dividing the region controlled by Constantine and that under Licinius? command, running from the North to the South and leaving Constantine the Pannonian provinces, Moesia I, Dacia Ripensis, Dacia Mediterranea and Dardania, as well as Macedonia, with the legionary camps on the Danube in Pannonia and Moesia I; the provinces on the East of that line, Moesia II, Scythia Minor and Thracia belonged to the region in which Licinius had command. However, there is evidence indicating that the territorial division of the Balkans between Constantine and Licinius after the battle of Cibalae was not strictly observed except on the Danube, in the zone where the military camps were located. In spite of Constantine?s presence in Illyricum, Licinius?s influence on the high commanders on the Danube never disappeared nor did his presence in the provinces he lost after the Bellum Cibalense. Licinius had the jubilee silver plates made for his decennalia in Naissus in Dacia Mediterranea. The siver plates which have been produced in Naissus, in the part of the Balkans which was under Constantine?s control, bear the inscription LICINI AVGVSTE SEMPER VINCAS. The co-operation between Constantine and Licinius concerned the defense of the frontiers and the administration in both parts of the Empire, but it was not based on the subordination of one to another as it was in the time of Diocletian who created the system tetrarchy.


Sign in / Sign up

Export Citation Format

Share Document