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Tytuł:
Ziemia Kłodzka jako region kultu św. Jana Nepomucena
Klodzko Land as the region of the cult of Saint John of Nepomuk
Autorzy:
Marek, Aneta
Powiązania:
https://bibliotekanauki.pl/articles/965740.pdf
Data publikacji:
2014
Wydawca:
Uniwersytet Łódzki. Wydawnictwo Uniwersytetu Łódzkiego
Tematy:
Ziemia Kłodzka
św. Jan Nepomucen
kult
Opis:
The article presents the cult of St. John of Nepomuk in the Klodzko Region. The history of this region evolved differently to neighboring Silesia. This area was often the disputed territory between the Czech Republic and Poland. The Klodzko Region changed its nationality a few times and it caused the religious changes. In the Baroque period, during resilient Counter-Reformation activities there was spread of the cult of St. John of Nepomuk, the fourteenth century martyr. The cult has spread since the death of his murderer – Waclaw IV, the Czech king (1419) to reach its zenith in 18th century, which can be reflected in the number of figures of the saint both in the Czech Republic and many regions in Poland. Clergy, mainly Jezuits, the representatives of the tsar’s court, rich gentry and aristocracy contributed to the spread of the cult. The landscape of the Klodzko Region has 220 images of him. On the basis of literature research and field inventory some objects of religious architecture connected with Nepomuk were pointed out.
W artykule zaprezentowano kult św. Jana Nepomucena na Ziemi Kłodzkiej. Historia tego regionu kształtowała się odmiennie niż sąsiedniego Śląska. Obszar ten często stanowił terytorium sporne między Czechami a Polską. Ziemia Kłodzka kilkakrotnie zmieniała swoją przynależność państwową, czego konsekwencją były zmiany religijne. W baroku, podczas prężnych działań kontrreformacyjnych rozpowszechnił się kult XIV-wiecznego męczennika – św. Jana Nepomucena. Rozprzestrzeniał się on od czasu śmierci jego oprawcy – króla czeskiego Wacława IV (1419 r.), by w XVIII w., po dokonanej kanonizacji męczennika, osiągnąć apogeum, co ma odzwierciedlenie w liczbie stawianych figur świętego zarówno w Czechach, jak i w różnych regionach Polski. Do rozpowszechnienia kultu przyczynili się duchowni, głównie jezuici, i przedstawiciele dworu cesarskiego, zamożnej szlachty oraz magnaterii. W krajobrazie Ziemi Kłodzkiej znajduje się ponad 220 jego wizerunków. Podstawowym celem artykułu jest identyfikacja i inwentaryzacja obiektów architektury sakralnej związanych z opisywanym męczennikiem.
Źródło:
Studia z Geografii Politycznej i Historycznej; 2014, 3; 321-342
2300-0562
2450-0127
Pojawia się w:
Studia z Geografii Politycznej i Historycznej
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Sudeckie wapienniki jako spuścizna dziedzictwa górniczego
Sudety lime kilns as examples of mining heritage
Autorzy:
Marek, Aneta
Powiązania:
https://bibliotekanauki.pl/articles/2048434.pdf
Data publikacji:
2020
Wydawca:
Politechnika Wrocławska. Wydział Geoinżynierii, Górnictwa i Geologii. Instytut Górnictwa
Tematy:
dziedzictwo przemysłu
dziedzictwo techniki
dziedzictwo górnicze
wapiennik
Sudety
industrial heritage
technical heritage
mining heritage
lime kiln
Sudetes
Opis:
Celem artykułu jest wskazanie wybranych wapienników jako elementów dziedzictwa górniczego w kontekście ich zachowania i możliwości wykorzystania na inne funkcje. Większość obiektów, po zakończeniu swojej pierwotnej działalności, ulega dewastacji. Obiekty te po odpowiedniej rewitalizacji i zagospodarowaniu mogą pełnić nowe funkcje, jak: użytkowe, turystyczne, rekreacyjne, edukacyjne, kulturowe, czego przykładem może być wapiennik w Starej Morawie, Złotym Stoku czy Javorníku.
The aim of the article is to indicate selected lime kilns as elements of the mining heritage in the context of their preservation and possible use for other purposes. Most of the facilities are subject to devastation after the termination of their original operation. These facilities, after appropriate revitalization and development, can perform new functions, such as: utility, tourist, recreational, educational, cultural, as exemplified in Stara Morava, Złoty Stok or Javorník.
Źródło:
Hereditas Minariorum; 2020, Vol. 6; 39-43
2391-9450
2450-4114
Pojawia się w:
Hereditas Minariorum
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Ślady geologii i górnictwa Sudetów oraz ich przedgórza w relacjach polskich podróżników XVIII i XIX wieku
Traces of geology and mining in the Sudetes Mts. and their foreland in accounts of Polish travellers of the 18th & 19th century
Autorzy:
Marek, Aneta
Powiązania:
https://bibliotekanauki.pl/articles/2075906.pdf
Data publikacji:
2019
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
geologia
górnictwo
odpowiedzialność
przewodnik
spa
geology
mining
account
guide
Opis:
The aim of the article is to present selected geological and mining information concerning the area of the Sudetes Mts. and their foreland, which was published in the 19th century publications. The visitors were interested not only in natural outcrops and geological formations, but also in industrial facilities, such as quarries, mines, adits that were the part of the Sudetes landscape, thus increasing its attractiveness for tourists. Thanks to scientists, but also travellers and health resort visitors, such information was frequently published in periodicals (dailies, weeklies, annuals, etc.), or in the form of diaries, letters, textbooks, guides or brochures. The most important magazines included: Kroniki Wiadomości Krajowych i Zagranicznych, Kłosy, Wieniec, Pamiętnik Warszawski, Roczniki Gospodarstwa Krajowego. The manuscripts by S. Poniatowski and B.Z. Stęczyński as well as compact publications, including those by R. Saulson, Z. Urbanowska, A. Ostrowicz, I. Czartoryska, J.U. Niemcewicz were also published. This article presents the descriptive method and the method of historical analysis.
Źródło:
Przegląd Geologiczny; 2019, 67, 11; 878--882
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Obiekty militarne jako element krajobrazu kulturowego Półwyspu Helskiego
Military objects as an element of the cultural landscape of the Hel Peninsula
Autorzy:
Marek, Aneta
Marszałek, Łukasz
Powiązania:
https://bibliotekanauki.pl/articles/684353.pdf
Data publikacji:
2018
Wydawca:
Uniwersytet Łódzki. Wydawnictwo Uniwersytetu Łódzkiego
Tematy:
Półwysep Helski
krajobraz militarny
bunkry
fortyfikacje
Hel Peninsula
military landscape
bunkers
fortifications
Opis:
The aim of this paper is to present the military objects of the Hel Peninsula which played a key role during the defense of September 1939. What has served as an object of this research is the two regions of the Hel Peninsula, in the landscape of which many fortifications have survived, namely, The Jastarnia Resistance Center and The Hel Fortified Area. The article indicates the location, military characteristics and purpose of individual elements of fortifications in both areas. These objects were later extended to cater for the needs of the army, however, they lost their rank when the military unit was disassembled. Due to the growing number of military enthusiasts The Jastarnia Resistance Center and The Hel Fortified Area had soon become a local attraction, which contributed to the revitalisation of various facilities and making them available for cultural purposes.
Celem artykułu jest zaprezentowanie militarnych obiektów Półwyspu Helskiego, które odegrały kluczową rolę podczas obrony we wrzeniu 1939 r. Badaniem objęto dwa rejony Półwyspu Helskiego – Ośrodek Oporu Jastarnia i Rejon Umocniony Hel, w których krajobrazie zachowało się wiele fortyfikacji. W artykule wskazano lokalizację poszczególnych elementów umocnień obu obszarów oraz podano ich charakterystykę militarną i przeznaczenie. Obiekty te w późniejszym okresie były rozbudowywane na potrzeby wojska, natomiast w momencie rozformowania jednostki wojskowej straciły swoją rangę. Stały się miejscami zainteresowania miłośników militariów, co przyczyniło się do rewitalizacji obiektów i udostępnienia ich do celów kulturowych.
Źródło:
Studia z Geografii Politycznej i Historycznej; 2018, 7; 233-249
2300-0562
2450-0127
Pojawia się w:
Studia z Geografii Politycznej i Historycznej
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geotourism valorisation of selected quarries of kłodzko region and cieszyn foothills
Autorzy:
Kasprowska-Nowak, Katarzyna
Marek, Aneta
Powiązania:
https://bibliotekanauki.pl/articles/1051068.pdf
Data publikacji:
2019-03-31
Wydawca:
Uniwersytet im. Adama Mickiewicza w Poznaniu
Tematy:
Eastern and Central Sudetes
Outer Western Carpathians
quarries
valorisation criteria
geotourism
Opis:
The article presents a geotourism valorisation of selected quarries located in different mountainous regions in southern Poland, diverse in geological and tectonic terms. The regions of Kłodzko (with quarries Kletno I, Krzyżnik, Sinica, Czarne Urwisko, Szczytna Zamek) and of Cieszyn Foothills (quarries Na Jasieniowej, Na Mołczynie, Grota na Rudowie, Nad Kalembianką, Ondraszkowa Dziura) were proposed as a case study. The survey describes the most exposed disused quarries of marble, gneiss, sandstone, teschenites and Cieszyn limestone of high natural and cultural significance. As a result of the geotourist valorisation, the analysed geological objects were given point score under various criteria (educational value, scientific value, visual value, location/accessibility value, cultural value, geo-infrastructural value and the value of legal protection). It was found that the discussed quarries reveal high natural and educational value, and they are very significant in education and promotion of geologically attractive areas.
Źródło:
Quaestiones Geographicae; 2019, 38, 1; 41-51
0137-477X
2081-6383
Pojawia się w:
Quaestiones Geographicae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Natural and anthropogenic transformations of the natural environment in the “Kępa Redłowska” reserve
Autorzy:
Marek, Aneta
Olszak, Ireneusz J.
Powiązania:
https://bibliotekanauki.pl/articles/2024719.pdf
Data publikacji:
2020
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Kępa Redłowska
Gdynia
Polska
cliff
fortification
Opis:
The “Kępa Redłowska” reserve is located in the southern part of Kępa Redłowska. The location of the reserve is quite unique. Its eastern border runs along the coastline of the Baltic Sea, while on the other sides it is surrounded by highly urbanized districts of Gdynia. Its coastal location means that it is exposed to natural factors that operate in the coastal zone, whereas its urban surroundings are a threat to the natural environment through more or less controlled human activity. The landscape of the reserve owes its attractiveness mainly to the cliff coast it encompasses. Diversified geological structure of this area, both in terms of lithology and age, combined with progressive erosion, causes a continuous change in its appearance. It is this part of the reserve that is most exposed to the destructive activity of natural factors, mainly coast erosion as well as aeolian processes. The intensity of these processes is closely related to climate changes over the centuries, e.g. a significant reduction in the number of winters, during which there is ice cover in the shore zone means that cliffs are not protected against erosion by winter storms. A spectacular effect of winter storms in this area was a large landslide in the southern part of the cliff on February 15, 2018. The retreat of cliffs is a common phenomenon, however observations in recent decades clearly indicate its acceleration. The remaining part of the reserve area, not directly connected with the shore zone, is subjected to continuously growing anthropopressure. As mentioned above, the “Kępa Redłowska” reserve is located in Gdynia. The expansion of the Redłowo district has resulted in the housing development being located directly adjacent to the eastern border of the reserve. An additional element of anthropopressure is the creation of interpretive trails and tourist routes within the reserve. On the one hand, this is an attempt to “channel” tourist traffic in this area, on the other hand, it causes an increase in tourist traffic with all the negative phenomena associated with it, mainly for vegetation. Human interference in the reserve began already at the end of the 1930s. At that time, military facilities, such as bunkers and artillery positions, were built there. This process continued uninterrupted until the 1960s. Post-military objects are on the one hand an attraction for tourists, on the other hand they attract the attention of various types of seekers of military remnants who, during their explorations, cause additional damage to the surface of the area and vegetation.
Źródło:
Studia Quaternaria; 2020, 37; 5-14
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geotourism potential of show caves in Poland
Autorzy:
Zieliński, Artur
Marek, Aneta
Zwoliński, Zbigniew
Powiązania:
https://bibliotekanauki.pl/articles/15804550.pdf
Data publikacji:
2022
Wydawca:
Uniwersytet im. Adama Mickiewicza w Poznaniu
Tematy:
geotourism
show caves
commercial caves
visitors
Polska
Opis:
In the modern world, tourism is a very dynamically growing industry with significant impact on the eco-nomic prosperity of many regions or even countries. The paper presents the geotourism potential of the 12 show (com-mercial) caves in Poland before and during the current pandemic time. Survey results demonstrate that caves are major geotourist attractions. In 2019, they were visited by a total of almost 950,000 people. The attendance might have exceed-ed even a million if the popular Mroźna Cave in the Tatras had not been temporarily closed to visitors due to a rockfall in winter period 2018/2019. In 2020, all the show caves combined were visited by a more than 390,000 people, which amounted to about 41% of the total attendance recorded for 2019. The most visited cave proved to be Smocza Jama (Dragon’s Den) in the centre of Kraków, which recorded almost 422,000 visitors in 2019. A preliminary assessment of the attractiveness of the caves as geosites is given. The most attractive caves as geosites were identified as: Bear Cave, Upper Wierzchowska Cave, and Bat Cave. It is possible to confidently assert that the celebration of the International Year of Caves and Karst (IYCK) in 2021–2022 will increase interest in caves and translate into a revival of cave tourism.
Źródło:
Quaestiones Geographicae; 2022, 41, 3; 169-181
0137-477X
2081-6383
Pojawia się w:
Quaestiones Geographicae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Pseudo-shallow marine features in deep marine gravity-flow successions: lessons from the Menilite Beds at Skrzydlna (Oligocene; Western Outer Carpathians)
Autorzy:
Wendorff, Marek
Siemińska, Aneta
Powiązania:
https://bibliotekanauki.pl/articles/24202106.pdf
Data publikacji:
2023
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
Oligocene
Carpathians
Opis:
Quite common in publications devoted to the marine and lacustrine environments are differences of opinion on bathymetry of the basin receiving detrital sediment, especially when sedimentary structures are interpreted as indicators of specific depth-defined environments (following classic textbooks). However modern studies of deep-water environments, experimental work, modelling and numerous outcrop studies of ancient successions mitigate against such an approach. In this respect, the flysch succession of the Menilite Beds strata at Skrzydlna, which contains a variety of features that can confuse a cursory observer seems to serve as a universally applicable example. The succession at Skrzydlna records deposition in the western part of the synorogenic Dukla Basin during the Oligocene. The Menilite Beds are considered by most authors as deep marine deposits (the bathyal zone). The exposed section, almost 200-metre thick, is divided into three lithological intervals, each of which represents a radically different type of sedimentation. These are: i) a fine-grained association of terrigeonous and hemipelagic sediments; ii) infill of a canyon incised by about 40–50 m into the underlying strata, wider than outcrop and dominated by an olistostromal succession of debris flows with pebbles, boulders, slide and slump sheets; iii) succession of turbidites forming three fining-upwards sequences and ranging from thick, massive, amalgamated sandstones deposited by high-density flows in laterally migrating outcrop-scale channels, through ‘normal’ turbidites forming complete Bouma sequences (Ta-e), containing dunes and fining to Tce in the uppermost associations of thin-bedded sandstones and shales. These features suggest rapid uplift of the source area resulting in canyon incision and sudden onset of the olistostrome deposition that evolved upwards into proximal turbidite-fan sequence, which subsequently retrograded due to decreasing intensity of supply. The oldest interval (i) consists of predominantly finegrained facies, most characteristic of the Menilite Beds at their regional development. These are dark mudstones deposited in anoxic to dysoxic conditions and containing thin layers of fine-grained sandstones — turbidites with Bouma Tab; Tbc; Tabc; Tabe intervals, a 2–3 m thick intercalation of massive amalgamated sandstone, dark cherts, and locally silicified marls and limestones. The latter contain isolated lenses of medium-grained sandstone current ripple marks indicating three palaeocurrent directions. Two sets represent bipolar distribution of palaeocurrents, typical of shallow sea/ shelf sediments reworked by tidal currents. However, these are interpreted here as the products of tidal currents reworking bottom sediments of the bathyal zone, the case known from contemporary environments. In this context, the third direction, perpendicular to the bipolar flows does not represent reworking by littoral current on shelf but deep marine contour current. The main channel, or canyon (ii) incised into the slope sediments fed the depositional system with olistostrome deposits supplied from the rapidly uplifted source zone. Above there is a thinning upwards, turbidite sequence of four sub-complexes (A-D): A – conglomerate and sandstone fill three laterally migrating narrow, outcrop-scale erosional channels with a maximum depth of 15 m; B  – two shallow (up to 2 m deep) distributary channels filled with very thick, massive or normally graded sandstones; C  – turbidites Tb, Tc, Tbc with single occurrences of hummocky-like cross stratification and sandstone beds forming dunes at the mouth of distributary channels; D  – less ordered interval of thick-, medium- and thin-bedded sandstones interbedded with mudstones, forming various incomplete sequences of Bouma intervals. Interbeds of hummocky-like cross stratification, commonly found on the shelf, are interpreted in the deep-sea environment as the effect of Kelvin-Helmholtz instability or other complex flow processes, e.g. reflections of turbidity currents. A few occurrences of ripplemarks symmetrical in outer shape show unidirectional cross-lamination in cross section. These were modified by erosion that could have resulted from occasional extremely violent storms or flow reflections off channel margins. In spite of the external shape reminiscent of symmetrical ripplemarks these features do not possess the internal structure of composite cross laminae characteristic for oscillatory reworking of sand by prolonged, rhythmic action of waves. Solitary current ripplemarks showing flow directions opposite to the main transport direction are antidunes or deposits of currents reflected/deflected by channel sides. In summary, in spite of geometrical and structural similarity to the features traditionally considered as formed on shelf, the structures described here, assessed in association with facies and evidence referred to in the introductory paragraphs, fall into the category of deposits known also from below the ‘normal’ wave base and below the shelf edge, i.e. in the slope region. Hence from deep-sea environment for which the occurrence of bipolar currents, dunes, hummocky cross-stratification and symmetrical ripplemarks are neither typical nor diagnostic, but do exist.
Źródło:
Geotourism / Geoturystyka; 2023, 1-2 (72-73); 79--80
1731-0830
Pojawia się w:
Geotourism / Geoturystyka
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Ocena stabilności sytuacji finansowej przedsiębiorstw sektora przemysłu spożywczego na podstawie TMAI
Evaluation of the stability of financial condition of the food industry sector companies on the basis of TMAI
Autorzy:
Włodarczyk, Aneta
Szajt, Marek
Powiązania:
https://bibliotekanauki.pl/articles/452830.pdf
Data publikacji:
2012
Wydawca:
Szkoła Główna Gospodarstwa Wiejskiego w Warszawie. Katedra Ekonometrii i Statystyki
Tematy:
TMAI
spółki sektora spożywczego
współczynnik korelacji Spearmana
food industry sector companies
Spearman rank correlation coefficient
Opis:
W niniejszym artykule na podstawie oszacowanych wartości Taksonomicznej Miary Atrakcyjności Inwestycji sporządzono rankingi spółek z sektora przemysłu spożywczego notowanych na GPW w Warszawie w latach 2009-2011. Przy konstrukcji wskaźnika syntetycznego uwzględniono następujące grupy zmiennych opisujących kondycję ekonomiczno-finansową spółek: wskaźniki płynności, wskaźniki rentowności, wskaźniki zadłużenia, wskaźniki sprawności zarządzania oraz wskaźniki rynkowe. Następnie przeanalizowano stabilność pozycji zajmowanych w rankingach przez badane spółki w latach 2009-2011.
In this paper, the rankings of the food industry sector companies listed on the Warsaw Stock Exchange were made on the basis of Taxonomic Attractiveness Measure of Investment. The following groups of variables were included in this study: liquidity ratios, profitability ratios, debt ratios, activity ratios, market-based ratios. Then analyzed whether the positions in the rankings of investigated companies remained stable over the period 2009-2011.
Źródło:
Metody Ilościowe w Badaniach Ekonomicznych; 2012, 13, 1; 234-244
2082-792X
Pojawia się w:
Metody Ilościowe w Badaniach Ekonomicznych
Dostawca treści:
Biblioteka Nauki
Artykuł

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