scholarly journals Strefy dialektalne języka białoruskiego jako przykład językowych kontaktów z sąsiednimi narodami

2016 ◽  
Vol 51 ◽  
pp. 139-166
Author(s):  
Mirosław Jankowiak
Keyword(s):  
South Eastern ◽  
Polish Language ◽  
The Baltic ◽  
North Western

Dialectal zones of the Belarusian language as an example of language contacts between neighbouring nationsThe article regards dialectal zones of the Belarusian language, which, as opposed to the traditional division into dialectal belts and dialectal groups, were marked out mainly on the basis of lexical and not grammatical features. While the traditionally delineated dialects indicate ethnographic unity of the Belarusian nation, dialectal zones present cultural and historical contacts with neighbouring nations. We can distinguish five zones: north-western (contacts with the Baltic languages, mainly with Lithuanian, and the Polish language of the northern borderland), south-eastern (contacts with Russian and Ukrainian), western (contacts with Polish), eastern (contacts with Russian) and central. Strefy dialektalne języka białoruskiego jako przykład językowych kontaktów z sąsiednimi narodami Artykuł traktuje o strefach dialektalnych języka białoruskiego, które, w odróżnieniu od tradycyjnego podziału na pasy dialektów i grupy gwarowe, zostały wyznaczone przede wszystkim w oparciu o cechy leksykalne, a nie gramatyczne. O ile tradycyjne dialekty wskazują na etnogenetyczną wspólnotę narodu białoruskiego, o tyle strefy dialektalne na kulturowo-historyczne kontakty z narodami sąsiednimi. Wyróżnia się pięć stref: północno-zachodnią (kontakt z językami bałtyckimi, głównie litewskim, i polszczyzną północnokresową), południowo-wschodnią (z rosyjskim i ukraińskim), zachodnią (z językiem polskim), wschodnią (z językiem rosyjskim) oraz centralną.

1649: Revolutionary Turnpike

2020 ◽  
pp. 300-308
Author(s):  
Jonathan Scott
Keyword(s):  
Eighteenth Century ◽  
The Netherlands ◽  
American Frontier ◽  
South Eastern ◽  
Relative Decline ◽  
The Baltic ◽  
City Of London ◽  
The City ◽  
And Diffusion ◽  
Dramatic Growth

This concluding chapter discusses how the Anglo-Dutch revolution of 1649–1702 stood at the centre of a succession of wider transformations which were agricultural, political, and commercial. All of these had their origins in the Netherlands before spreading to south-eastern England and across the Atlantic. Understanding their development and diffusion has required attention to religion, migration, and war as well as to economic, social, and cultural life. The result connected a series of unique local human environments, including the Dutch water world, the city of London, and the American frontier into a world-altering imperial system. By the later eighteenth century the Atlantic reorientation of the European economy had thrown the Baltic into relative decline, sparking the dramatic growth of Liverpool, Manchester, and Glasgow while Stockholm, Copenhagen, and Amsterdam stagnated.

scholarly journals Ships and their timber source as indicators of connections between regions

AmS-Skrifter ◽  
2020 ◽  
pp. 133-143
Author(s):  
Aoife Daly
Keyword(s):  
Western Europe ◽  
The Baltic Sea ◽  
The North ◽  
Baltic Coast ◽  
Art Objects ◽  
The North Sea ◽  
The Baltic ◽  
North And South ◽  
North Western

The precise dating and determination of the source of timbers in shipwrecks found around the coasts of the North Sea and the Baltic Sea, through dendrochronology allows us to see connections between north and  south, east and west throughout the region and to a high chronological precision. In this paper we take a look at results of recent analyses of timber from ships, and timber and barrel cargoes, to try to draw a chronological picture, from the twelfth to seventeenth centuries, of links between regions, through transport in oak ships and trade of timber. Archaeological finds of oak from timber cargos in shipwrecks and fine art objects (painted panels and sculpture) show the extent to which timber was shipped from Hanseatic towns along the southern Baltic coast, to western and north-western Europe.

scholarly journals UKRAINE BETWEEN PEACE AND WAR WITH RUSSIA

2021 ◽  
Vol 10 (2) ◽  
pp. 95-106
Author(s):  
Ilie Răsvan DUMITRU
Keyword(s):  
Russian Federation ◽  
Soviet Bloc ◽  
The West ◽  
Crimean Peninsula ◽  
Future Evolution ◽  
South Eastern ◽  
Baltic Countries ◽  
Limited Warfare ◽  
The Baltic ◽  
Peace And War

  After the Crimean Peninsula was invaded and the amplification of conflicts in South-Eastern Ukraine, it has become obvious that Russia's policy is concentrated on preserving its influence and strategic control over the decisions and political directions taken by the States from the former Soviet bloc. To understand the consequences of the Russian-Ukrainian war on the West, as well as to anticipate and counteract a possible future evolution of similar events not only in geopolitical risk states such as Moldavia, but also even in NATO members such as the Baltic countries, Romania or Bulgaria, it is worth paying attention to the geopolitical consequences of the loss of Crimea and the South-Eastern provinces by Ukraine. The article analyses the reason, mechanisms and stakes behind the Russian-Ukrainian war, from both a geopolitical and historical perspective. To understand the way in which different hybrid instruments can be used by the Russian Federation to influence the States in its proximity and, in particular, how their combination leads to effective satisfaction of the aims, it is useful to assess and address the systemic risks and vulnerabilities of States in the concerned areas of Russia and the West in recent years.   Keywords: Ukraine; Russian Federation; Crimea; Russian-Ukrainian war; hybrid warfare; limited warfare; maskirovka.

scholarly journals NOTES ON THE LIISSILÄ INGRIAN FINNISH DIALECT

2019 ◽  
Vol 13 (4) ◽  
pp. 568-575
Author(s):  
Mehmet Zakirovich Muslimov
Keyword(s):  
The Other ◽  
The South ◽  
Special Group ◽  
South Eastern ◽  
Imperfect Form ◽  
Other Hand ◽  
The Baltic

The article focuses on some peculiarities of the Ingrian Finnish dialect spoken in the former Lutheran parish of Liissilä in Central Ingria.Two main pecularities of the Liissilä dialect are the imperative 2Sg -kai and a special group of verb type with the -oi stem ending. Most of the isoglosses, which were previously proposed as typical of the Äyrämöinen dialect, are currently absent in the Liissilä dialect. The dialect of Liissilä partially preserves two old pecularities of the Äyrämöinen dialect, namely nouns ending in - ее and verbs ending in - oi. On the other hand, there are quite a lot of areal isoglosses, which are common in local dialects of both Savakko (Inkere, Venjoki) and Äyrämöinen (Liissilä, Tuutari) parishes. These isoglosses include tarttu ‘potato’, potra ‘beautiful’, hirvitä ‘to be afraid’, the presence of the diphthong in the 3Sg imperfect form, the 1Pl affix -mma , the vowel ö in the verb pölästyy ‘to be scared’, the present stem niäe- of the verb nähhä ‘to see’ and some others. In the Linguistic Atlas of the Baltic-Finnish Languages the dialect zones of the Finnish language, including such units as the “South-Eastern Southern dialect” or the “dialect of Northern Khyame” are classified as “Evremeysky dialect”, “Savaksky dialect” and “dialect of Narvusi” in the territory of Ingria.

scholarly journals The ethnic composition of the population of Prinevye area and the Southern Ladoga area at the end of the XV century

2020 ◽  
Vol 12 (1) ◽  
pp. 62-72
Author(s):  
Boris I. Chibisov
Keyword(s):  
Economic History ◽  
Ethnic Composition ◽  
Rural Settlements ◽  
North West ◽  
Introduction History ◽  
The North ◽  
History Of ◽  
The Baltic ◽  
North Western ◽  
Descriptive Method

Introduction. History of the North-West area of Novgorod land at the end of the XV century attracted the attention of researchers mainly in the socio-economic aspect. This is due to the fact that Novgorod scribal books are dated by the end of the XV century. From the standpoint of socio-economic history their value is not in doubt, but from an ethno-historical point their onomastic content is underestimated. Materials and methods. The main source of research was the scribe book of the Vodskaya Pyatina 1499/1500. The descriptive method of research is to identify and record the Baltic-Finnish oikonyms (names of rural settlements) and anthroponyms mentioned in the scribe books. Baltic-Finnish anthroponyms are identified on the basis of an analysis of formal indicators of borrowing the anthroponyms. Results and Discussion. There are several areas where the Baltic-Finnish oikonymy and anthroponymy were concentrated, namely Korboselsky graveyard in the northern Prinevye, Lopsky and Terebuzhsky graveyards in the southern Ladoga, as well as Dudorovsky and Izhora graveyards south of the Neva. Archaeological sources record a significant presence of the Izhora antiquities. The presence of Karelians is noted in the northern Prievye and southern Ladoga. Slavic onomastic materials are recorded throughout Orekhovsky and Ladoga counties, but to mostly in the cities of Oreshka, Ladoga and their nearest areas. Conclusion. By the end of the XV century the north-western graveyards of Novgorod land were inhabited by representatives of various ethnic groups: Slavs, Vodians, Izhora and Karelians, as evidenced by the data of anthroponyms and toponyms of the scribe’s books and confirmed by archaeological sources.

scholarly journals New data on the palaeo–incisions network of the south–eastern Baltic Sea

Baltica ◽  
2014 ◽  
Vol 27 (1) ◽  
pp. 1-14 ◽  
Author(s):  
Dmitrij Gerok ◽  
Leonora Živilė Gelumbauskaitė ◽  
Tom Flodén ◽  
Algimantas Grigelis ◽  
Albertas Bitinas
Keyword(s):  
Baltic Sea ◽  
Ice Sheet ◽  
The South ◽  
The Baltic Sea ◽  
Distinctive Features ◽  
South Eastern ◽  
Fracture Systems ◽  
Present Study Area ◽  
Eastern Segment ◽  
The Baltic

The present study area is located within the south–eastern segment of the Baltic Sea framed by 55o30’–56o30’ N and 19o00’–21o15’E. The area is re-visited with the aim to describe in more detail the geologic prerequisite and development of the palaeo–incisions as well as the timing of their subsequent infillings. The channels form distinctive features in the sedimentary bedrock along the outer limits of pre–Weichselian ice sheets, on average reaching depths into the bedrock of 50 m in the nearshore zone of Lithuania to 100 m along the slope to the Gotland depression in the west. The development of palaeo–incisions systems is governed by the easily eroded late Palaeozoic to Mesozoic bedrock of the present area. Only rare ocurrences of channels have been reported from the middle and lower parts of the Palaeozoic further west in the Baltic Sea. The present investigation supports a mechanism that the channels formed below the ice near the ice sheet margin by melt water erosion under high pressure. The channels start at random where a fracture in the ice develops forming outlet of water contained below the central part of the ice sheet. The channels often merge together in the direction of the ice margin, possibly gradually adapting to previous fracture systems in the bedrock. The investigated incisions were infilled prior to the advance of the Weichselian ice sheet and some have been reopened and repeatedly infilled.

scholarly journals Балцкія элементы ў граматыцы традыцыйных мясцовых гаворак паўночна‑заходняй Беларусі

2015 ◽  
Vol 36 ◽  
pp. 51-59
Author(s):  
Вера [Vera] Астрэйка [Astrėĭka]
Keyword(s):  
The Other ◽  
North West ◽  
Language Support ◽  
The North ◽  
The Status ◽  
Formal Level ◽  
The Baltic ◽  
Language Assimilation ◽  
The Given ◽  
North Western

The Baltic elements in the grammar of traditional local dialects of north-western BelarusThe article analyzes a number of grammatical features typical for the North-West dialect zone of the Belarusian language. These peculiarities are interpreted as a possible result of Slavic-Baltic contacts in the region. Some phenomena can be explained as a Baltic (mainly (great)Lithuanian) substratum in North-West Belarusian dialects.The factor of areal neighborhood has to be taken into consideration too. Such phenomenon as language support has effect just in connection with the last one. A lot of the appropriate lingual facts are in restricted and inconsistent use. However, it is possible to be said about more or less significant (now or/and before) tendencies of regional lingual development. These tendencies has not got the status of a structural (= constitutional) lingual regularity. As a rule the wide and compact areas are characterized of some lingual facts (= lexemes), which illustrate the given transformations in the system of Belarusian dialects. Baltic influence upon the North-West Belarusian dialects grammar is detected on as the formal level so the structural one. And it is not noticeable at all times. The definite changes in the sphere of morphology and syntax can provoke different modifications in the other parts of a language system (word building, semantics). The results of this process are the evidences of ethnic and language assimilation of native Balts by Slavs in the region. That comes in support of forming the singular North-West Belarusian regiolect (= the regionally marked variety of a dialect language). Балтийские грамматические элементы в говорах северо-западной БеларусиВ статье анализируется ряд грамматических черт, характерных для говоров северо-западной диалектной зоны беларусского языка. Эти особенности квалифицируются автором как весьма вероятное следствие славяно-балтского языкового взаимодействия в соответствующем регионе. Отдельные явления есть основания рассматривать в качестве возможного проявления балтского (главным образом (пра-) литовского) субстрата в северо-западных беларусских говорах. Фактор ареальной смежности здесь также должен быть принят во внимание. В связи с последним следует упомянуть и действие феномена языковой поддержки. Многие соответствующие языковые факты имеют существенные ограничения в употреблении, в говорах выступают не всегда последовательно и регулярно. В некоторых случаях, однако, можно говорить о действии более или менее выраженных (в настоящем и/или прошлом) тенденций регионального языкового развития, которые пока не приобрели статус структурно значимой (= конститутивной) языковой закономерности. Широкие и компактные ареалы образуют, как правило, лишь отдельные языковые факты (= лексемы), иллюстрирующие данные трансформации в системе традиционных беларусских говоров. Балтское влияние на грамматический строй беларусских говоров северо-западной диалектной зоны выявляется как в плане формального выражения, так и на внутриструктурном уровне. Оно не всегда может быть заметно на первый взгляд. Определенные сдвиги в сфере морфологии и синтаксиса могут повлечь за собой изменения в других областях языковой системы (словообразовании, семантике). Результаты этого процесса являются ярким свидетельством того, что на отмеченной территории действительно имела место этноязыковая ассимиляция неславянского (= балтского) населения и происхо- дило формирование своеобразного северо-западного беларусского региолекта (= регионально обусловленной разновидности диалектной речи).

Phenology of Migratory Bat Activity Across the Baltic Sea and the South-Eastern North Sea

2014 ◽  
Vol 16 (1) ◽  
pp. 139-147 ◽  
Author(s):  
Jens Rydell ◽  
Lothar Bach ◽  
Petra Bach ◽  
Laura Guia Diaz ◽  
Joanna Furmankiewicz ◽  
...  
Keyword(s):  
Baltic Sea ◽  
North Sea ◽  
The South ◽  
The Baltic Sea ◽  
Bat Activity ◽  
South Eastern ◽  
The Baltic

Aeolian Environments

2005 ◽  
Author(s):  
Eduard Koster
Keyword(s):  
Sand Dunes ◽  
Ural Mountain ◽  
Aeolian Processes ◽  
The North ◽  
Aeolian Deposits ◽  
The World ◽  
Western Border ◽  
Late Weichselian ◽  
The Baltic ◽  
North Western

The literature on aeolian processes and on aeolian morphological and sedimentological features has shown a dramatic increase during the last decade. A variety of textbooks, extensive reviews, and special issues of journal volumes devoted to aeolian research have been published (Nordstrom et al. 1990; Pye and Tsoar 1990; Kozarski 1991; Pye 1993; Pye and Lancaster 1993; Cooke et al. 1993; Lancaster 1995; Tchakerian 1995; Livingstone and Warren 1996; Goudie et al. 1999). However, not surprisingly the majority of these studies discuss aeolian processes and phenomena in the extensive warm arid regions of the world. The results of aeolian research in the less extensive, but still impressive, cold arid environments of the world are only available in a diversity of articles. At best they are only briefly mentioned in textbooks on aeolian geomorphology (Koster 1988, 1995; McKenna-Neuman 1993). Likewise, the literature with respect to wind-driven deposits in western Europe is scattered and not easily accessible. The aeolian geological record for Europe, as reflected in the ‘European sand belt’ in the north-western and central European Lowlands, which extends from Britain to the Polish–Russian border, is known in great detail (Koster 1988; van Geel et al. 1989; Böse 1991). Zeeberg (1998) showed that extensive aeolian deposits progress with two separate arms into the Baltic Region, and into Belorussia and northernmost Ukraine. Recently, Mangerud et al. (1999) concluded that the sand belt extends even to the Pechora lowlands close to the north-western border of the Ural mountain range in Russia. Sand dunes and cover sands are widespread and well developed in this easternmost extension of the European sand belt. The northerly edges of this sand belt more or less coincide with the maximal position of the Late Weichselian (Devensian, Vistulian) ice sheet, while the southern edges grade into coverloams or sandy loess and loess (Mücher 1986; Siebertz 1988; Antoine et al. 1999). However, along these southern edges the dune fields and sand sheets regionally are derived from different sources, such as the sands of the Keuper Formation or the floodplains of the Rhine and Main rivers.

Roman Wales: Aerial Discoveries and New Observations from the Drought of 2018

Britannia ◽  
2020 ◽  
Vol 51 ◽  
pp. 117-145
Author(s):  
Toby G. Driver ◽  
Barry C. Burnham ◽  
Jeffrey L. Davies
Keyword(s):  
Royal Commission ◽  
South Eastern ◽  
Historical Monuments ◽  
Drought Conditions ◽  
Aerial Reconnaissance ◽  
North Western

ABSTRACTThis paper provides description and context for some of the discoveries made by the Royal Commission on the Ancient and Historical Monuments of Wales during aerial reconnaissance in the drought conditions of the summer of 2018. New discoveries include two marching camps, three auxiliary forts and a remarkable series of stone buildings outside the fort at Pen y Gaer. The photographs also clarify the plan of several known villas as well as identifying some potential villa sites and enclosure systems of probable Romano-British date in south-eastern, south-western and north-western Wales. The recognition of a new road alignment south of Carmarthen is suggestive of another coastal fort at or near Kidwelly.

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