The Galician Canal—An unrealized project that changed the rivers in the northern part of the Carpathians

2021 ◽  
Author(s):  
Karol Witkowski
Keyword(s):  
The Carpathians

WHO WHO'S STRATEGY IN THE NATIONAL MEDICINE SECTOR FOR 2013-2023 AND NEW APPLICATIONS OF PHYTOTIC PRODUCTION IN THE CARPATHIANS

Fitoterapia ◽  
2019 ◽  
Vol 4 (4) ◽  
pp. 74-75
Author(s):  
O. I. Voloshуn ◽  
◽  
M. M. Stovpyuk ◽  
O. V. Hyndych ◽  
L. O. Voloshina ◽  
...  
Keyword(s):  
The Carpathians ◽  
New Applications

Obsidian in the Early Neolithic of the Upper Vistula basin: origin, processing, distribution and use – a case study from Tominy (southern Poland)

2021 ◽  
Vol 0 (0) ◽  
Author(s):  
Marcin Szeliga ◽  
Zsolt Kasztovszky ◽  
Grzegorz Osipowicz ◽  
Veronika Szilágyi
Keyword(s):  
River Basin ◽  
Prompt Gamma Activation Analysis ◽  
Raw Material ◽  
Published Data ◽  
Prompt Gamma ◽  
Early Neolithic ◽  
Musical Note ◽  
Southern Poland ◽  
The Carpathians ◽  
Vistula River

Abstract The inflow of the Carpathian obsidian into the areas on the northern side of the Carpathians and the Sudetes is confirmed as early as in the Palaeolithic. However, its greatest intensity occurred in the Early Neolithic, i. e. in the late 6th and in the first half of 5th millennia BC. During that period, the phenomenon was closely related with the development of the Danubian cultural groups in the upper Vistula river basin, including especially Linear Pottery culture (LBK) and Malice Culture. The constant presence of this raw material products in mentioned areas is documented from the classical (musical-note) phase of LBK, constituting one of the most expressive pieces of evidence of permanent and intense intercultural contacts with communities of the northern Carpathian Basin. This phenomenon has been repeatedly emphasized in the literature. One of the most numerous LBK obsidian inventories in the upper Vistula river basin was obtained at site 6 in Tominy, located in southern Poland, in the non-loess zone of the Sandomierz Upland northern foreground. The above-mentioned collection, its non-destructive elemental analysis, using Prompt Gamma Activation Analysis (PGAA) and also traceological analysis, is the subject of this article. The results supplement the published data to a significant extent, simultaneously providing partial verification and updating of the current state of knowledge on the basic issues related to the Early Neolithic obsidian inflow into areas located North of the Carpathians, including primarily the origin of the raw material, the scale of its processing and distribution ways, as well as the range of its use by the LBK communities.

Karyological and morphological differentiation of the Tanacetum corymbosum group (Asteraceae) in the Slovak part of the Carpathians

Biologia ◽  
2021 ◽  
Author(s):  
Kristína Pulišová ◽  
Katarína Skokanová ◽  
Barbora Šingliarová ◽  
Judita Kochjarová
Keyword(s):  
Morphological Differentiation ◽  
The Carpathians

The Carpathian Mountain range and the enclosed interior

2009 ◽  
Vol 1 (3) ◽  
Author(s):  
Gabor Földvary
Keyword(s):  
Plate Tectonics ◽  
Ore Deposits ◽  
Carpathian Basin ◽  
Mountain Range ◽  
Great Hungarian Plain ◽  
The Carpathians ◽  
Carpathian Mountain ◽  
Micro Plates ◽  
Basin System ◽  
Hungarian Plain

AbstractThe baffling duality of the Carpathian Mountain Range and the Basin it surrounds is briefly discussed. The various attempts at solving the nature of this duality, including plate tectonics with its micro-plates are mentioned. The component ranges of the Carpathians and the structural belts are given, followed by the discussion of the Carpathian Basin System, the Interior, consisting of the Great Hungarian Plain, Transdanubia, the two groups of Central Mountains, also the Apuseni (Bihar) Mountains and the Banat Contact Belt. Economic ore deposits are featured in the relevant sections.

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