scholarly journals The North or the South? Early medieval ceramics decorated with a zoned ornament – the result of local changes or interregional contacts?

2021 ◽  
Vol 73 (3) ◽  
pp. 423-454
Author(s):  
Justyna Kolenda ◽  
Kinga Zamelska-Monczak
Keyword(s):  
Middle Ages ◽  
The South ◽  
The West ◽  
Native Communities ◽  
The North ◽  
North Eastern ◽  
Close Relationship ◽  
North Eastern Part ◽  
Lower Silesia ◽  
South Bohemia

The article underlines the need to re-discuss the prevailing views in archaeological literature on the provenance and transformation stages of completely wheel-turned ceramics decorated with zoned ornament. This class of ceramics was used in the Early Middle Ages (for about 100 years) by communities living in the area of southern Greater Poland and the north-eastern part of Lower Silesia. The previous ideas suggesting a close relationship between zoned ceramics and vessels produced in northern Bohemia are reconsidered, with the internal diversity of zoned ceramics being pointed out. We argue that inspiration in ceramics manufacturing came not only from the south (Bohemia), but also from the north (Pomerania) and the west (the middle Elbe region), and that there were also changes that appeared independently of these impulses in the ceramics production of small, native communities.

scholarly journals XI. An Account of Observations, made by Lord Webb Seymour and Professor Playfair, upon some Geological Appearances in Glen Tilt, and the adjacent Country

1815 ◽  
Vol 7 (2) ◽  
pp. 303-375 ◽  
Author(s):  
Webb Seymour
Keyword(s):  
Peat Moss ◽  
The South ◽  
The North ◽  
South West ◽  
North Eastern ◽  
Principal Branch ◽  
Adjacent Country ◽  
The Common ◽  
Common Character ◽  
North Eastern Part

1. The river Tilt is a principal branch of the Tay, which rises on the borders of Aberdeenshire, and runs towards the south-west, through the north-eastern part of the county of Perth. A portion of the valley along its course, for about ten miles above Blair of Atholl, is called Glen Tilt.The adjacent country presents the common character of the Highlands. It is mountainous and rugged, and the surface, except in the lower parts of the valleys, is chiefly covered with heath. Peat-moss frequently occurs.

scholarly journals Die geographische und familiäre Herkunft der Ordensgebietiger Konrad von Kyburg und Rudolf von Kyburg

2021 ◽  
Vol 26 ◽  
pp. 253-283
Author(s):  
Piotr Gotowko
Keyword(s):  
Sudden Death ◽  
High Rank ◽  
The South ◽  
The North ◽  
The Poor ◽  
North Eastern ◽  
North Eastern Part

The geographical and familial origins of the Teutonic Order’s officials Konrad von Kyburg and Rudolf von Kyburg   The researchers of the Teutonic Order have placed the brethren Konrad (before 1336 – 12. April 1402) and Rudolf (before 1337–1404) von Kyburg in the north-eastern part of present-day Switzerland – either in the castle of Kyburg near Winterthur in the eastern Canton of Zurich, or in the Canton of Turgovia, lying in the East of Canton Zurich and to the South of Lake Bodensee. Their family lost those areas by 1265, after a sudden death of Hartmann V von Kyburg (1263) and the childless death of his uncle, Hartmann IV (1264). The only successor, the minor daughter of Hartmann V, Anna von Kyburg, was not able to keep her inheritance, which was quickly taken by her nephew Rudolf IV von Habsburg, latter known as German King Rudolf I. He arranged a marriage between Anna and his relative, Eberhard von Habsburg-Laufenburg, leaving them only Burgdorf and Thun in the nowadays Canton Berne. Their son, Hartmann, had taken the name of the maternal dynasty, calling himself since 1297 Hartmann I von Kyburg. His son, Eberhard II  von Kyburg, succeeded him. He was the father of eleven children with Konrad von Kyburg and Rudolf von Kyburg among them. Despite their name, they came from Burgdorf and had joined the Teutonic Order because the poor parents could not guarantee them a subsistence. The carreer of Konrad von Kyburg started in the late 1380s. In 1392 he was promoted to the Comtur of Balga and from 1396–1402 had even reached the high rank of the Great Hospitaller. The carrier of his younger brother, Rudolf, was less impressive for he became 1391–1402 the Comtur of Rehden.

scholarly journals Defensive Structures of Severynivka Hillfort (Excavations of 2009 and 2012-2013)

2016 ◽  
Vol 21 (1) ◽  
pp. 69-90
Author(s):  
Oleksandr Shelekhan ◽  
Oksana Lifantii ◽  
Yuriy Boltryk ◽  
Marcin Ignaczak
Keyword(s):  
The South ◽  
Floor Level ◽  
Research Results ◽  
The North ◽  
North Eastern ◽  
North Eastern Part

Abstract The article focuses on the research results of Severynivka hillfort fortifications. In 2009 a rampart and a moat on a cliff on the south floor-level side. In 2012-2013 there was made a rampart and escarp sections in the north-eastern part of the fortification. Separate stages of its construction are distinguished; the possible reconstruction of the defensive structures is suggested.

Belarusian

2020 ◽  
pp. 1-18
Author(s):  
Sonya Bird ◽  
Natallia Litvin
Keyword(s):  
Eastern Europe ◽  
The Other ◽  
Slavic Language ◽  
The South ◽  
The West ◽  
The North ◽  
North Eastern ◽  
The Republic

Belarusian (ISO 639-3 BEL) is an Eastern Slavic language spoken by roughly seven million people in the Republic of Belarus (Zaprudski 2007, Census of the Republic of Belarus 2009), a land-locked country in Eastern Europe, bordered by Russia to the north and east, Ukraine to the south, Poland to the west and Lithuania and Latvia to the northwest (Figure 1). Within the Belarusian language, the two main dialects are North Eastern and South Western (Avanesaǔ et al. 1963, Lapkoǔskaya 2008, Smolskaya 2011). Two additional regional forms of Belarusian can be distinguished: the Middle Belarusian dialectal group, incorporating some features of North Eastern and South Western dialects together with certain characteristics of its own, and the West-Polesian (or Brest-Pinsk) dialectal group. The latter group is more distinct linguistically from the other Belarusian dialects and is in many respects close to the Ukrainian language (Lapkoǔskaya 2008, Smolskaya 2011). The focus of this illustration is Standard Belarusian, which is based on Middle Belarusian speech varieties. For details on the phonetic differences across dialects, the reader is referred to Avanesaǔ et al. (1963) and Lapkoǔskaya (2008).

scholarly journals SOME ASPECTS OF LOCALIZATION OF PRECIOUS METAL MINERALIZATION IN THE LOWER PERMIAN CONGLOMERATES WITHIN THE NORTH-EASTERN PART OF THE O-40-XXIX SHEET (SHALINSKAYA PLOSHAD)

2021 ◽  
Author(s):  
A.K. Trutnev ◽  
◽  
E.A. Zhuklin ◽  
L.A. Demina ◽  
◽  
...  
Keyword(s):  
Precious Metal ◽  
Lower Permian ◽  
The West ◽  
The North ◽  
Iron Copper ◽  
Marginal Part ◽  
North Eastern ◽  
The World ◽  
Weathering Crusts ◽  
North Eastern Part

“Metal-bearing” conglomerates are known in various regions of the world. They are associated with ore occurrences and industrial deposits of gold, uranium, silver, iron, copper and other minerals. At the junction of the Western marginal part of the West Ural folding zone with the pre-Ural regional trough, rocks were recorded, during petrographic and mineralogical studies of which it was possible to establish direct (signs of gold) and indirect signs of gold localization in the lower Permian polymictic conglomerates and in the eluvial weathering crusts formed along them.

Mixing of brine waste in Puck Bay (the south Baltic Sea) in the light of in-situ measurements

2016 ◽  
Vol 45 (1) ◽  
Author(s):  
Małgorzata Robakiewicz
Keyword(s):  
Baltic Sea ◽  
Coastal Waters ◽  
Near Field ◽  
Monitoring Program ◽  
The South ◽  
The North ◽  
North Eastern ◽  
North Eastern Part ◽  
Puck Bay

AbstractIn the north-eastern part of Poland, the underground gas stores are being constructed by diluting salt deposits. Brine, a by-product of the technology applied, is discharged into the coastal waters of the south Baltic Sea by a system of diffusers. To assess the intensity of brine mixing in the near-field of the discharge installation, a monitoring program was carried out. The results demonstrated that under the mildly dynamic conditions of Puck Bay, the discharge of brine (saturation 250 kg m

scholarly journals Phylogenetic placement and new data on the morphology and ecology of Calathella eruciformis (Agaricales, Basidiomycota), a cyphelloid fungus new to Poland

2019 ◽  
Vol 64 (1) ◽  
pp. 91-99
Author(s):  
Marek Halama ◽  
Bartosz Pencakowski ◽  
Wiesław Fałtynowicz ◽  
Katarzyna Patejuk ◽  
Agnieszka Kowalewska ◽  
...  
Keyword(s):  
Type Species ◽  
Its Rdna ◽  
Populus Tremula ◽  
Molecular Evidence ◽  
Phylogenetic Placement ◽  
The North ◽  
Rdna Sequences ◽  
North Eastern ◽  
Close Relationship ◽  
North Eastern Part

AbstractCalathella eruciformis, a species hitherto unknown in Poland, is reported from four localities in the north-eastern part of the country. This wood-inhabiting saprotroph was found on dead decorticated but still attached twigs and branches of living Populus tremula in an oak-hornbeam forest (Carpinion betuli). Macro- and microcharacters of the recently collected material are presented in detail, together with selected illustrations. Examination of ITS rDNA sequences indicated that Calathella is not monophyletic and that the type species of the genus C. eruciformis is alien to the heterogeneous genus Flagelloscypha. Furthermore, molecular evidence is provided for a close relationship between C. eruciformis and the type species of the genus Sphaerobasidioscypha, Sphaerobasidioscypha citrispora.

scholarly journals Disko Bugt Project, central West Greenland

1990 ◽  
Vol 148 ◽  
pp. 21-24
Author(s):  
F Kalsbeek
Keyword(s):  
Mineral Resources ◽  
Precambrian Basement ◽  
Economic Potential ◽  
The West ◽  
North East ◽  
The North ◽  
North Eastern ◽  
Second Year ◽  
Proterozoic Basement ◽  
North Eastern Part

One of GGU’s major field activities in 1989 took place in July and August in the north-eastern part of the Disko Bugt region, mainly north of Illulissat (Jakobshavn) (fig. 1). This was the second year of the ‘Disko Bugt Project’, planned for 1988–1991, with one summer's break in 1990. The project spreads over various activities and over two very different geological provinces: the Archacan-Proterozoic basement east and north-east of Disko Bugt and in the eastern part of Nugssuaq, and the Cretaceous-Tertiary basin in the west, on Disko and the western part of Nugssuaq. The main aim of the project is to provide a background for the evaluation of the economic potential of the region mineral resources in the Precambrian basement, and the hydrocarbon potential of the basin.

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