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Tytuł:
Характерологічні назви в говірках українського Карпатського регіону
Valuable words in the dialect of the Ukrainian Carpathian region
Autorzy:
Колєснік, Людмила
Powiązania:
https://bibliotekanauki.pl/articles/2008027.pdf
Data publikacji:
2020-12-15
Wydawca:
Poznańskie Towarzystwo Przyjaciół Nauk
Tematy:
evaluable words
the Carpathian region
linguistic borrowings
motivation
характерологічна назва
Карпатський регіон
запозичення
мотивація
Opis:
У статті представлено спостереження автора щодо функціонування оцінних слів у говірках українського Карпатського регіону, а саме в гуцульських, закарпатських, бойківських, лемківських говірках та суміжних говірках Буковини й Покуття. Проаналізовано стандартні моделі творення нових віддієслівних та відіменникових похідних. Значну увагу присвячено виокремленню мотиваційних моделей постання метафоричних характерологічних назв. Описано форми міжмовної взаємодії в межах цієї лексичної групи, акцентовано на тісному зв’язку діалектів аналізованого ареалу, що проявляється в спільних тенденціях оцінної номінації.
The article deals with the functioning of the evaluable words in the dialects of the Ukrainian Carpathians, in particular the Hutsul, Transcarpathian, Boyko, Lemko, Bukovyna and Pokuttya dialects. In these dialects, the lexical system of characterological names is formed according to the same general principles. In the studied dialects, the main universal tendencies inherent in this vocabulary are manifested. On the other hand, original nominations have been observed, resulting from non-linguistic factors.An analysis has been carried out of creating standard models оf new words via dialectal nouns and verbs. Much attention has been given to the identification of motivational models behind the emergence of metaphorical characterological names. Unlike standard names, characterological vocabulary is not entered to the passive vocabulary of dialect speakers simultaneously with the disappearance of the actual thing. Secondary names or set similes last longer when they are connected with the material signs of a local culture. The forms of the interlingual interaction in this lexical group have been described. Attention has been drawn to the connections between the dialects spoken in the analysed area, which is reflected in the general trends of the evaluation nomination.
Źródło:
Gwary Dziś; 2020, 12; 81-93
1898-9276
Pojawia się w:
Gwary Dziś
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wpływ aktywności gospodarczej na kształt przestrzeni małych miast w Karpatach Polskich
The influence of economic activity on the shape of small towns in Polish Carpathians Mountains
Autorzy:
Węcławowicz-Bilska, Elżbieta
Powiązania:
https://bibliotekanauki.pl/articles/691514.pdf
Data publikacji:
2016
Wydawca:
Uniwersytet Łódzki. Wydawnictwo Uniwersytetu Łódzkiego
Tematy:
Region karpacki
małe miasta
rozwój gospodarczy
Carpathian region
small towns
economic development
Opis:
The Carpathian region is characterized by the accumulation of numerous natural and cultural resources protected by law. The traditional function of these areas was agriculture and herding. Natural resources are the basis for development of the therapeutic spa function. Construction of railway lines in the second half of the nineteenth century resulted in more dynamic economic development based on industry and tourism. Subsequent actions have contributed to increasing the urbanized area, often in a piecemeal manner, without due attention to spatial order. The consequences of these decisions for landscape, aesthetics, society and economy can have a lasting impact on spatial order and the possibility of sustainable development.
Region karpacki charakteryzuje nagromadzenie licznych zasobów środowiska przyrodniczego i kulturowego chronionych prawnie. Historyczną, tradycyjną funkcją tych obszarów było rolnictwo i pasterstwo. Zasoby naturalnych surowców leczniczych są podstawą rozwoju lecznictwa uzdrowiskowego. Przeprowadzenie linii kolejowych w II połowie XIX wieku zdynamizowało rozwój gospodarczy oparty na przemyśle oraz turystyce i wypoczynku. Kolejne działania przyczyniły się i nadal powodują zwiększenie powierzchni zurbanizowanej, często w sposób nieuporządkowany przestrzennie. Konsekwencje krajobrazowe, estetyczne, społeczne, a także w końcu gospodarcze tych decyzji mogą mieć długotrwały wpływ na ład przestrzenny oraz możliwości trwałego i zrównoważonego rozwoju.
Źródło:
Space – Society – Economy; 2016, 17; 85-99
1733-3180
2451-3547
Pojawia się w:
Space – Society – Economy
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Consequences of the War for the Labour Market of the Carpathian Region of Ukraine: Priorities of Stabilisation Policy
Autorzy:
Vasyltsiv, Taras
Levytska, Olha
Rudkovsky, Olexandr
Powiązania:
https://bibliotekanauki.pl/articles/2171519.pdf
Data publikacji:
2022
Wydawca:
Uniwersytet Warszawski. Instytut Ameryk i Europy. Centrum Europejskich Studiów Regionalnych i Lokalnych (EUROREG)
Tematy:
Carpathian region
war
socioeconomic destabilisation
labour market
employment
forced migration
Opis:
The article addresses the structural–temporal changes in the characteristics of the labour market in the oblasts of the Carpathian region of Ukraine (Lvivska, Zakarpatska, Ivano-Frankivska and Chernivetska) due to the large-scale Russian military invasion of Ukraine. Regional, sectoral and market condition–related changes in the labour market and employment in the region during the war are identified. The article defines the threats to the functioning of the regional labour market, which are related to growing unemployment, increasing pressure on social infrastructure and the domestic labour market, reduction in human resources and the growing trend of relocation of business and skilled workers from the western oblasts of Ukraine to other countries. The policy for social-labour stabilisation of the oblasts in the Carpathian region of Ukraine in conditions of war and post-war recovery is substantiated.
Źródło:
Studia Regionalne i Lokalne; 2022, 4, 90; 29-38
1509-4995
Pojawia się w:
Studia Regionalne i Lokalne
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wskaźnik średniej rocznej erozyjności deszczu i spływu powierzchniowego (R) na przykładzie stacji meteorologicznej w Łazach k. Bochni (region klimatu Pogórza Karpackiego)
Mean annual R factor for Łazy near Bochnia meteorological station (Carpathian Foothills climatic region)
Autorzy:
Święchowicz, J.
Powiązania:
https://bibliotekanauki.pl/articles/294797.pdf
Data publikacji:
2013
Wydawca:
Stowarzyszenie Geomorfologów Polskich
Tematy:
wskaźnik erozyjności deszczu [EI30]
wskaźnik R
USLE
region klimatu Pogórza Karpackiego
Polska
rainfall erosivity index [EI30]
R factor
Carpathian Foothills climatic region
Polska
Opis:
Wskaźnik rocznej erozyjności deszczu i spływu powierzchniowego (R) jest jednym z parametrów empirycznego równania USLE (Uniwersalnego Równania Strat Glebowych) oraz innych modeli (np. RUSLE – Revised Universal Soil Loss Equation, USPED – Unit Stream Power based Erosion/Deposition). Jak dotąd nie dokonano szczegółowej charakterystyki erozyjności deszczów w Polsce, a wartości wskaźnika R zgodnie z procedurą opracowaną przez Wischmeiera i Smitha (1965, 1978) obliczono jedynie dla 13 stacji meteorologicznych. Celem pracy jest określenie wskaźnika erozyjności deszczu i spływu powierzchniowego (R) dla regionu klimatu Pogórza Karpackiego na podstawie pomiarów opadów atmosferycznych w wieloleciu 1987–2008 pochodzących ze stacji meteorologicznej w Łazach k. Bochni (Pogórze Wiśnickie). Średnia roczna z wielolecia 1987–2008 wartość wskaźnika R wynosi w Łazach 106,6 MJ cm ha–1 h–1. Jest ona większa od wartości podawanych dla Polski zachodniej (Wrocław-Swojec), północnej (Elbląg), północno-wschodniej (Suwałki), centralnej (Otwock, Sandomierz, Puczniew), zbliżona do wartości podawanych dla Karpat (Lesko, Limanowa, Szymbark). Roczne wartości wskaźnika R zmieniały się w Łazach w bardzo szerokim zakresie od 27,7 do 455,9 MJ cm ha–1 h–1. Maksymalne miesięczne wartości wskaźnika Rr w roku zmieniały się od 6,1 w lipcu (1993) do 428,7 MJ cm ha–1 h–1 w czerwcu (2006). Największa potencjalna erozja wodna gleby uzależniona od erozyjności deszczu możliwa była w czerwcu, lipcu, maju i sierpniu.
Rainfall and runoff erosivity factor (R) is a key input parameter to the USLE (Universal Soil Loss Equation) and many other models (RUSLE – Revised Universal Soil Loss Equation, USPED – Unit Stream Power based Erosion/Deposition). There is still no precise characteristic of rainfall erosivity in Poland. Local R factor values, according to Wischmeier and Smith procedure (1965, 1978) were calculated only for 13 meteorological stations. The main aim of the paper is to estimate rainfall and runoff erosivity factor (R) for the Carpathian Foothills climatic region on the basis of 1987–2008 rainfall data for Łazy near Bochnia meteorological station (Wiśnicz Foothills). The average rainfall and runoff factor (R) for Łazy calculated for the years 1987–2008 equalled 106.6 MJ cm ha–1 h–1. This value was bigger in comparison with the values for other locations in western (Wrocław-Swojec), northern (Elbląg) northeastern (Suwałki) or central Poland (Otwock, Sandomierz, Puczniew) and similar to the values for the Carpathians (Lesko, Limanowa, Szymbark). The annual values of R factor for Łazy ranged between 27.7 in 1993 and 455.9 MJ cm ha–1 h–1 in 2006. Maximum monthly values of rainfall factor Rr in a year varied from 6.1 in July (1993) to 428.7 MJ cm ha–1 h–1 in June (2006). The most intensive potential soil erosion by water due to erosivity of rains is likely to happen in June, July, May and August.
Źródło:
Landform Analysis; 2013, 24; 85-95
1429-799X
Pojawia się w:
Landform Analysis
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Chronostratigraphy and changes of environment of Late Pleistocene and Holocene at Starunia palaeontological site and vicinity (Carpathian region, Ukraine)
Autorzy:
Sokołowski, T.
Stachowicz-Rybka, R.
Powiązania:
https://bibliotekanauki.pl/articles/191571.pdf
Data publikacji:
2009
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
Late Pleistocene
Holocene
fluvial deposits
environment
Starunia
Carpathian region
Ukraine
Opis:
This paper presents the results of absolute dating and biostratigraphical analysis carried out for alluvial sediments of an abandoned Starunia ozokerite mine located in the Velyky Lukavets River valley, in which large mammal remains were discovered in the first half of the 20th century. The sediments build up three terrace levels. The highest one, up to 8 m high (terrace II), is likely to be associated with a stage of aggradation, as well as with a short episode of valley broadening, which occurred in the Weichselian Late Pleniglacial. The lower one, 4 m high (terrace I), is most likely to be linked with the Holocene, despite a considerable transformation of its top due to mining activity. The lower part of this terrace cover bears coarse-grained channel sediments dated to 120.6-58.9 ka BP (Eemian Interglacial?-Early Pleniglacial - OIS 5e, 4 and 3), and overbank (distal floodplain) mud with intercalations of biogenic deposits (peat, peat mud and biogenic mud). The overbank deposits are dated to 48.2-11.11 ka BP (Glinde Interstadial?-Younger Dryas, OIS 3-2) and are overlain by Holocene (OIS 1) mud and biogenic deposits. In boreholes drilled in the vicinity of the present-day river channel, younger sediments occur more frequently. These include sediments originating from the Late Weichselian overlain by Holocene sediments. However, sediments originating exclusively from the Holocene are infrequent. The deposition of sediments took place in specific conditions of a permanent saturation of the environment with brine, petroleum and thickened bitumen. In the longest period of deposition (48.2-1.27 ka BP), ephemeral swamps, ponds and lakes were developed in different parts of the floodplain. They were marked by the presence of: Juncus glaucus/effusus, J. articulatus, Typha sp., Batrachium sp., Potamogeton filliformis, Bidens tripartita, Ranunculus sceleratus and Phragmites communis, as well as by halophytic species, like: Zannichellia palustris, Triglochin maritimum, Schoenoplectus tabernemontani, Puccinelia distans and Eleocharis palustris. Rhythmic oscillations between cold and warm climatic conditions, typical of the Weichselian age and well identified in Western Europe, are here marked by the changes of plant communities (woody assemblages passing into steppe and tundra), but are not noticeably recorded in the sediments of the Velyky Lukavets River. This shows that the greatest part of the discussed period involved the formation of poorly differentiated silty overbank sediments with intercalations of biogenic sediments. However, the variability of sediments provides evidence for extreme events which occurred in the Holocene.
Źródło:
Annales Societatis Geologorum Poloniae; 2009, 79, No 3; 315-331
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Development of relief of the Velyky Lukavets River valley near Starunia palaeontological site (Carpathian region, Ukraine)
Autorzy:
Sokołowski, T.
Powiązania:
https://bibliotekanauki.pl/articles/191554.pdf
Data publikacji:
2009
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
geomorphology
river terraces
Starunia
Carpathian region
Ukraine
Opis:
In Quaternary sediments filling the Velyky Lukavets River valley, at the abandoned ozokerite mine (= Ropyshche) in Starunia, perfectly preserved carcasses of large mammals were discovered in the first half of the 20th century. The study area includes a fragment of the valley between Molotkiv and Starunia, and its close vicinity. The area belongs to several morphostructural and geomorphic units of the Outer Eastern Carpathians and the Carpathian Foreland. The asymmetric, subsequent valley is a part of the Mizhbystrytska Upland, where flattened ridges and flat bulges represent fragments of planation surfaces: the upper (the Krasna level), elevated 170 m above the valley bottom and linked with the Late Pliocene, and the lower one (the Loyova level), rising at 100 m and linked with the Eopleistocene. Several flat surfaces are visible on valley slopes, probably representing river terraces formed before the Late Pleistocene. The valley attained its maximum depth during the Eemian Interglacial (OIS 5e). In the Ropyshche area, probably three terrace steps built of Weichselian and Holocene sediments (OIS 5d - 1) were developed, but their top surfaces are almost completely destroyed by mining operations. The recent, meandering river bed follows the zones of decreased cohesiveness of rocks resulting from mining activity and is becoming somewhat deepened during inundations. The transported material is mostly coarse-clastic one. The two latter factors may suggest that the river is underloaded due to declining agriculture and decreasing intensity of outwash. The top surface of the sub-Quaternary basement is deformed by subsidence and collapse of mine workings, but the relief of valley bottom allows for further exploration for remnants of large mammals not only in the Ropyscche area but along the whole studied segment of the valley, as well.
Źródło:
Annales Societatis Geologorum Poloniae; 2009, 79, No 3; 243-254
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Upper Pleistocene and Holocene deposits at Starunia palaeontological site and vicinity (Carpathian region, Ukraine)
Autorzy:
Sokołowski, T.
Stachowicz-Rybka, R.
Woronko, B.
Powiązania:
https://bibliotekanauki.pl/articles/191556.pdf
Data publikacji:
2009
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
Quaternary fluvial sediments
Velyky Lukavets River valley
Starunia
Carpathian region
Ukraine
Opis:
An abandoned ozokerite mine (= Ropyshche), where large mammal remains were discovered in the first half of the 20th century, is located in the Velyky Lukavets River valley covered with Quaternary sediments. The catchment area includes a flysch sequence unconformably overlain by salt-bearing Lower Miocene molasses of the Vorotyshcha beds. Both the Upper Pleistocene and Holocene are represented by: channel (gravel, sandy gravel) and overbank alluvium (mud, peat, biogenic mud) and colluvium (mud, sandy mud) as well as by mine wastes. The channel sediments are usually found in the lowest fragments of the borehole logs and represent mainly material deposited in the straight segments of meandering river-beds. The most common, fine-grained (Mz = 61.33 to 7.11 ?m), distal floodplain sediments are locally up to 10 m thick and are dominated by massive mud lithofacies, which contain frequent burrows, root hairs or slightly larger root traces and reed rods. These sediments are characterized by rather stable grain size distribution, quite monotonous mineral composition, presence of resistant heavy minerals and quartz grains with traces of chemical weathering. Angular grains with conchoidal fractures and sharp edges also occur. Therefore, textural features show that the main sources of material were, most probably, weathering crusts of various ages developed on relatively poorly lithologically diversified Carpathian flysch strata and on Miocene deposits of the Carpathian Foredeep. With time, an increase of the content of material originating from mechanical weathering (frost action) occurred in the floodplain deposits, which can be linked to an increase of climate severity and reduction of vegetation. However, these changes are not recorded in the deposits, which developed mostly in closed hollows and accumulated mainly from suspension or from low-energy flows. This calm sedimentation was periodically interrupted by supply of more coarse-grained material (sand, gravel). A distinct predominance of overbank deposits in the sections documented by their thickness suggests that the northward flow of the Velyky Lukavets River was blocked as a result of either neotectonic movements or damming of the valley by landslide tongues. From the lithological point of view, the most favourable conditions for preservation of large, extinct mammals still exist in the two selected areas, where the total thickness of Pleistocene muds exceeds 2 metres. The first area is located in the vicinity of boreholes Nos 2, 3, 21, 22, 23, 28, 30 33 and 36N, and the other, smaller one, is placed around borehole No. 42.
Źródło:
Annales Societatis Geologorum Poloniae; 2009, 79, No 3; 255-278
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Surface geochemical survey at Starunia palaeontological site and vicinity (Carpathian region, Ukraine)
Autorzy:
Sechman, H.
Kotarba, M. J.
Dzieniewicz, M.
Powiązania:
https://bibliotekanauki.pl/articles/191493.pdf
Data publikacji:
2009
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
surface geochemical survey
stable carbon isotopes
methane origin
gaseous hydrocar bon C2-C5
carbon dioxide origin
woolly rhinoceros
Starunia
Carpathian region
Ukraine
Opis:
A surface geochemical survey was carried out in an abandoned ozokerite mine in Starunia, where remnants of a mammoth and three woolly rhinoceroses and one almost completely preserved rhinoceros carcass were found in 1907 and 1929. In total, 689 measurement sites were defined within the selected 300×350 m rectangle (ca. 10.5 ha). The analysed soil gases vary in their molecular and isotopic compositions. Several zones with anomalous methane concentrations over 10 vol% were identified in the study area. These anomalous concentrations correlate well with total C2-C5 alkane anomalies (over 1 vol%). The zones with carbon dioxide concentrations over 15 vol% are generally shifted SW of those, where the methane and the sum of C2-C5 alkanes anomalies were identified. High helium concentrations of crustal origin (over 0.001 vol%) are clustered near fault zones. In a majority of cases methane is of thermogenic origin, migrating to the near-surface zone from deep-seated accumulations. Microbial methane, or methane with a high microbial component, is genetically related to recent swamps. The high variability of concentrations of gaseous components together with the highly variable isotopic composition of individual gases in the soil, indicate their thermogenic and/or microbial origin, and point to the lithological diversity of Quaternary sediments in the study area. Several zones with thermogenic gaseous hydrocarbons and helium were delineated. It is likely that during the Pleistocene winters, under a thick ice and snow cover, the tundra lake and swamp zones around outflows of brines, oil, helium and thermogenic gases had a higher temperature, which resulted in melting and cracking of the ice cover. These sites would be more prospective for future search of well-preserved large vertebrates.
Źródło:
Annales Societatis Geologorum Poloniae; 2009, 79, No 3; 375-390
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
New wooden recreational objects of the Carpathian region of Ukraine. Features of architectural and planning decisions
Nowe drewniane obiekty rekreacyjne Karpackiego regionu Ukrainy. Właściwości architektoniczno-planistyczne
Autorzy:
Savchuk, A.
Powiązania:
https://bibliotekanauki.pl/articles/369152.pdf
Data publikacji:
2018
Wydawca:
Zachodniopomorski Uniwersytet Technologiczny w Szczecinie. Wydawnictwo Uczelniane ZUT w Szczecinie
Tematy:
Carpathian recreational region
wooden recreational architecture
architectural and planning decisions
Karpacki teren rekreacyjny
drewniana architektura rekreacyjna
decyzje architektoniczne i planistyczne
Opis:
In the research, based on the analysis of natural examination results and project documentation it was discovered the features of architectural and planning decisions of wooden recreational objects. By identifying the characteristic features of architectural and compositional signs of buildings and constructions an attempt is made to determine their stylistics.
Badania przeprowadzono na podstawie analizy wyników badań terenowych i dokumentacji projektowej, ujawniono właściwości objętościowo-planistycznych rozwiązań obiektów drewnianych, rekreacyjnych. Poprzez określenie charakterystycznych cech architektonicznych i kompozycyjnych budynków oraz ich konstrukcji podjęto próbę określenia ich stylu.
Źródło:
Przestrzeń i Forma; 2018, 36; 83-100
1895-3247
2391-7725
Pojawia się w:
Przestrzeń i Forma
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Detection of near-surface geological heterogeneity at Starunia palaeontological site and vicinity (Carpathian region, Ukraine) based on microgravity survey
Autorzy:
Porzucek, S.
Madej, J.
Powiązania:
https://bibliotekanauki.pl/articles/191491.pdf
Data publikacji:
2009
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
geophysics
microgravity
Quaternary sediments
Starunia
Carpathian region
Ukraine
Opis:
Results of a microgravity survey performed in the abandoned Starunia ozokerite mine (Carpathian region, Ukraine), where in the early 20th century well preserved remains of large, extinct mammals were found, are discussed in the paper. A number of gravity anomalies indicating the geological heterogeneity at the sub-Quaternary strata have been observed. The assumed measurement observations also enabled the authors to interpret the results in view of density changes in the Quaternary strata. Most of the registered microanomalies coincide with the high-halite and ozokeritic Miocene salt-bearing Vorotyshcha beds. The distribution of the microanomalies reveals neither their correlation with the thickness of overburdens, nor any gravity impact of numerous abandoned wells. Gravity anomalies were mostly connected with the lithology of sediments and rocks obtained from geological boreholes drilled in the years 2007 and 2008, on the basis of which the anomalies' origin could be determined. A concentric, relatively negative gravity microanomaly of ca. 25 m in diameter was registered in the place, where very well preserved relics of the woolly rhinoceros had been found. They may be indicative of the existence of Pleistocene lakes (and/or palaeoswamps), into which the woolly rhinoceroses had sunk. Hence, an assumption can be made that the further search for successive zoological relics can be made in areas with similar anomalies under the low-density sub-Quaternary subcrop.
Źródło:
Annales Societatis Geologorum Poloniae; 2009, 79, No 3; 365-374
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Recognition of geological structures at Starunia palaeontological site and vicinity (Carpathian region, Ukraine) based on gravity surveys
Autorzy:
Porzucek, S.
Madej, J.
Powiązania:
https://bibliotekanauki.pl/articles/191495.pdf
Data publikacji:
2009
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
Starunia
Carpathian region
Ukraine
Opis:
In the early 20th century, relics of Pleistocene mammals were found near the village of Starunia. Gravity surveys performed in the place of the discovery revealed a low-density bed in the Miocene Vorotyshcha salt-bearing beds. The lowered density resulted from high halite content and probably an increased number of ozokerite veins. The localization of zoological relics can be attributed to the existence of this bed. Surface gravity surveys enabled scientists to determine its course and horizontal range. Gravity surveys also confirmed the existence of the Rinne fault. In the western part of the study area gravity modelling showed an interface between Miocene Vorotyshcha salt-bearing beds and Sloboda Conglomerates, differing in average bulk density. Geologic data indicate that this interface may have the form of an overthust rather than of a fault.
Źródło:
Annales Societatis Geologorum Poloniae; 2009, 79, No 3; 357-363
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
INTRODUCING COMPULSORY PROPERTY INSURANCE - AS A MEANS OF IMPROVING THE ORGANIZATIONAL AND ECONOMIC MECHANISM DAMAGES FROM FLOODS IN THE CARPATHIAN REGION
WPROWADZENIE OBOWIĄZKOWEGO UBEZPIECZENIA MAJĄTKOWEGO - JAKO ŚRODKA POPRAWY ORGANIZACYJNEGO I EKONOMICZNEGO MECHANIZMU ODSZKODOWAŃ POWODZI W REGIONIE KARPACKIM
ВНЕДРЕНИЕ ОБЯЗАТЕЛЬНОГО СТРАХОВАНИЯ ИМУЩЕСТВА – КАК СПОСОБ УСОВЕРШЕНСТВОВАНИЯ ОРГАНИЗАЦИОННО-ЭКОНОМИЧЕСКОГО МЕХАНИЗМА ВОЗМЕЩЕНИЯ УЩЕРБА ОТ ПАВОДКОВ В КАРПАТСКОМ РЕГИОНЕ
Autorzy:
Petruk, Irina
Petruk, Viktor
Powiązania:
https://bibliotekanauki.pl/articles/576926.pdf
Data publikacji:
2016-06-30
Wydawca:
Międzynarodowy Instytut Innowacji Nauka – Edukacja – Rozwój w Warszawie
Tematy:
emergency, flood, damage, targeted programs, compensation, costs, reserve fund, compulsory insurance of property, Carpathian region
awaryjne, powodzie, uszkodzenie, ukierunkowane programy, odszkodowania, koszty, fundusz zapasowy, obowiązkowe ubezpieczenie mienia regionu karpackiego
чрезвычайные ситуации, паводкии, убытки, целевые программы, возмещение, расходы, резервный фонд, обязательное страхование имущества, Карпатский регион
Opis:
W artykule uzasadnia konieczność poprawy mechanizmu organizacyjnego i ekonomicznego zapobiegania, łagodzenia i reagowania kryzysowego, analizuje główne czynniki, które wywołują powodzi i szkód z nimi w regionie karpackim i istniejącego mechanizmu rekompensaty na Ukrainie i za granicą, skłoniły wprowadzenie obowiązkowe ubezpieczenia mienia na terenach zalewowych niebezpiecznych od klęsk żywiołowych w celu ułatwienia pełniejszego szkód i zmniejszyć koszty budżetów stanowych i lokalnych.
The article substantiates the need to improve the organizational and economic mechanism of prevention, mitigation and emergency response, analyzes the main factors that induce the flooding and damage from them in the Carpathian region. It is here described the existing mechanism of its compensation in Ukraine and abroad. Author prompted the introduction of compulsory property insurance on flood dangerous areas from natural disasters to facilitate more complete damage compensation and reduce the costs of state and local budgets.
В статье обоснована необходимость совершенствования организационноэкономического механизма предупреждения, уменьшения негативного влияния и ликвидации последствий чрезвычайных ситуаций, проанализированы основные факторы, которые вызывают формирование паводков и ущерба от них в Карпатском регионе, а также существующий механизм их возмещения в Украине и за рубежом, предложено введение обязательного страхования имущества на паводкоопасных территориях от стихийных бедствий, что будет способствовать более полному возмещению убытков, а также уменьшению расходов из государственного и местных бюджетов.
Źródło:
International Journal of New Economics and Social Sciences; 2016, 3(1); 171-181
2450-2146
2451-1064
Pojawia się w:
International Journal of New Economics and Social Sciences
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
FUNKCJONOWANIE PARTNERSTW MIĘDZYSEKTOROWYCH W OPINII ICH CZŁONKÓW. PRZYKŁAD LOKALNYCH GRUP DZIAŁANIA WOJEWÓDZTWA PODKARPACKIEGO
THE FUNCTIONING OF MULTISECTOR PARTNERSHIPS IN THE OPINION OF THEIR MEMBERS. CASE STUDY OF THE LOCAL ACTION GROUPS IN THE SUB-CARPATHIAN REGION
Autorzy:
Pawłowska,, Agnieszka
Gąsior-Niemiec, Anna
KOŁOMYCEW, ANNA
Powiązania:
https://bibliotekanauki.pl/articles/513645.pdf
Data publikacji:
2013
Wydawca:
Uniwersytet Rzeszowski. Wydawnictwo Uniwersytetu Rzeszowskiego
Tematy:
inter-sector partnerships
rural areas
Local Action Group
Sub-Carpathian region
Opis:
The notion of intersectoral partnership is understood in the paper in terms of vol-untary and institutionalized cooperation between stakeholders representing public, private and civic sectors. The idea of this kind of partnership is related to new ap-proaches to regional and local development in the European Union. One of the main fields in which these approaches are implemented is the field of rural areas develop-ment, where partnerships take the form of Local Action Groups (LAGs). The paper discusses selected aspects of the partnerships’ functioning, basing on an analysis of opinions expressed by their individual members in the Sub-Carpathian region.
Źródło:
Polityka i Społeczeństwo; 2013, 11, 2; 71-87 (17)
1732-9639
Pojawia się w:
Polityka i Społeczeństwo
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Salinity of Quaternary sediments and halophytes at Starunia palaeontological site and vicinity (Carpathian region, Ukraine)
Autorzy:
Mościcki, W. J.
Toboła, T.
Zarzyka-Ryszka, M.
Powiązania:
https://bibliotekanauki.pl/articles/191501.pdf
Data publikacji:
2009
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
salinity
geoelectric electromagnetic survey
penetrometer-based resistivity profiling
botanical studies
halophytes
Starunia
Carpathian region
Ukraine
Opis:
Interdisciplinary geophysical, geochemical and botanical studies were performed to recognize the problem of salinity of Quaternary sediments in the place, where woolly rhinoceroses were discovered at the beginning of the 20th century. Geoelectric methods (high resolution geoelectric research with electromagnetic conductivity meter) enabled construction of maps of the distribution of conductivity of near-surface sediments. Variation of conductivity with depth was recognized with penetrometer-based geoelectric measurements. Measured conductivity mainly depends on the level of mineralization (salinity) of underground water filling the pores and voids of poorly consolidated Quaternary sediments and partly underlying Miocene strata. Several samples were taken from geological boreholes. The analysis of these cores enabled estimation of salt (chloride ion) content in the solid phase of sediments. This content varies from place to place and with depth in an unpredictable way. The highest values reached 8.5 wt%. Generally, on the basis of a qualitative comparison, the salinity data gained from sampled cores correlate with distribution of apparent conductivity obtained with geoelectric methods. Nevertheless, in some places there is a discrepancy between geophysical and geochemical data, especially for penetrometer versus borehole data. It may be partly explained by an unavoidable difference in location of the geological borehole and penetrometer site (technically this cannot be the same place). During botanical field studies a group of vascular plants growing on saline soils (halophytes) was found. Halophytes indicate a higher salt concentration in the soil. Their aggregations are extremely rare in the Carpathian region. The pattern of halophytes distribution reflected the presence of saline water sources, and their flows and soils affected by them. Generally, the distribution of halophytes showed a good correlation with the distribution of high-conductivity anomalies determined with the surface geoelectric survey.
Źródło:
Annales Societatis Geologorum Poloniae; 2009, 79, No 3; 391-402
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The Medieval Christian Necropolis in the Kopachyntsi hillfort (Ukraine). Unpublished Research Materials
Autorzy:
Lutsyk, Iryna
Powiązania:
https://bibliotekanauki.pl/articles/2085881.pdf
Data publikacji:
2021
Wydawca:
Uniwersytet Rzeszowski. Instytut Archeologii Uniwersytetu Rzeszowskiego. Muzeum Okręgowe w Rzeszowie
Tematy:
Sub-Carpathian region
burial
funeral culture
under the slab burial
pilgrimage relics
Opis:
The article deals with unpublished research materials from the medieval Christian cemetery located on the territory of the hillfort in the village of Kopachyntsi in Sub-Carpathian region (Ukraine) which were conducted in 1953. Excavations were verified, objects and artefacts were analysed, and an attempt to attribute and date them was made. The site is represented by inhumations in pits, as well as burials under stone slabs. The so-called “under the slab burials” are a separate category of monuments of funeral culture, which is characterized by its diffusion only on the territory of Halician-Volhynian state, but not the whole of Kyiv Rus’. At the same time, such monuments are known in Slovakia, Czech Republic, Germany, Bulgaria, Romania, Macedonia and Poland. Data on most of the under the slab monuments discovered on the territory of Ukraine are often uninformative, and therefore the publication of the results of stationary archaeological excavations is extremely important for understanding this cultural and religious phenomenon. Special attention is paid to a rare stone cross that was found by the deceased. The search for analogies allows us to conclude that it may be a pilgrimage relic.
Źródło:
Analecta Archaeologica Ressoviensia; 2021, 16; 125-145
2084-4409
Pojawia się w:
Analecta Archaeologica Ressoviensia
Dostawca treści:
Biblioteka Nauki
Artykuł
Wyświetlanie 1-15 z 36

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