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EN
a few months in 1938 and 1939 - from the time Hitler made his claims towards Czechoslovakia until the moment the state was dismantled. The author has focused on presenting the Polish-Czechoslovakian relations as reported by the press published in Siedlce, a district town located in the centre of pre-war Poland. At that time four periodicals were published there. The analysis of these publications has allowed the author to determine that the editors informed their readers about the situation of the disputed territories on a regular basis. The editors tried to make their message more attractive by posting photos or accounts by special correspondents. They built among its readers a negative image of the Czechoslovakian state, which was presented as an artificial creation where the rights of national minorities were not respected. The incorporation of these lands into Poland was presented as a symbol of historical justice. The press also played an important part in mobilising the local community to act for fellow countrymen from the lands being the object of the Polish-Czechoslovakian dispute. However, it did not recognise the growth of Slovakian independence activities, which were important for the internal affairs of Poland’s southern neighbour.
EN
The evolution of the Central Carpathian Paleogene Basin (CCPB) reflects an important role of relative sea level changes on a tectonically active basin margin. After the initial upper Lutetian/Bartonian transgression, the next regressive-transgressive cycle played a key role in a formation of the late Eocene fan delta facies associations in the southern Orava region of Northern Slovakia. Detailed sedimentary analysis allowed the separation of the following three facies associations which represent distinct depositional environments: alluvial fan (subaerial fan delta; Unit 1); subaqueous fan delta (Unit 2); and prodelta/slope and basin (Unit 3). The first stage of delta development is connected with eustatic sea level fall at the Bartonian/Priabonian boundary, accompanied by subaerial exposure, fluvial incision and deposition of alluvial fan sediments. Subaerial deposition was characterized by a variety of mass flow conglomerates with a red muddy matrix, interfingering with stream or sheetflood deposits. The next stage of the delta corresponds to high-amplitude transgression related to rapid tectonic subsidence along the CCPB margins during the Priabonian. The vertical arrangement of facies suggests retrograde delta development that shows rapid submergence of the subaerial parts and onlap of subaqueous mass flow conglomerates, often reworked by waves or wave-induced shallow-marine currents. Continuous deepening of the depositional environment during the late Priabonian/early Rupelian led to the relatively rapid superposition of prodelta/slope and basin facies associations by slowly accumulated hemipelagic deposis.
EN
The paper presents Lusatian culture bronze artefacts recovered in the Orava region in northern Slovakia, which allows for tracing connections with the territory of present-day Poland in the Late Bronze Age and the Early Iron Age. The object is to discuss the provenance of the Lusatian bronze artefacts and analyse possible intercultural contacts with the north, across the Carpathians.
EN
The thin- and medium-bedded, turbiditic deposits that are exposed in the Bystrica Zone of the Magura Nappe in the Slovak Orava region are the subject of this study. On the basis of lithological features as well as age and stratigraphic position, they are assigned to the Ropianka Formation. The very well exposed rocks of this formation, recognized in the Biela Farma profile in the Slovak part of the northwestern Orava region, are compared with analogous deposits in the Polish Orava and the Beskid Wysoki Mountains. Lithological and biostratigraphical documentation of the Ropianka Formation is presented. This documentation allowed the determination of the age of the rocks studied. Abundant and taxonomically diverse foraminiferal assemblages of agglutinated, benthonic and occasional planktonic forms indicate a Middle Paleocene age for the upper part of the Ropianka Fm. A new stratigraphic position for the Szczawina Sandstone, considered to be a member of the Ropianka Fm, is proposed. The lithostratigraphy of the Ropianka Fm in the Magura Nappe in Poland, Slovakia and the Czech Republic requires further investigation, including the establishment of new type and reference sections. The large outcrop at Biela Farma should be taken into consideration as a potential reference section. Studies of the new sections will lead to a new monographic elaboration of the Ropianka Fm in Poland, Slovakia and the Czech Republic.
Lud
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2023
|
tom 107
|
nr 1
307-328
EN
Juliusz Zborowski, a graduate of Polish Philology at the Jagiellonian University, moved to Podhale in 1913, as he started working as a teacher in a junior high school in Nowy Targ. The historical events of those years, related to the establishment of new borders of the Second Polish Republic, made him engaged in activities for the protection of cultural heritage in the disputed areas of Spisz and Orawa. He was a member of the Main Plebiscite Committee of Spisz-Orawa, then the head of its press section of Gazeta Podhalańska (1919–1920), from 1918 a member of the Tatra Society, and in 1922 he became the first director of the Tatra Museum. In 1920, the Main Plebiscite Committee was liquidated, and the money collected for its activities was allocated to the purchase of ethnographic artefacts from the so-called southern borderlands of the Second Polish Republic. Zborowski started sourcing them for the museum. As a result, over two hundred examples of paintings painted on glass and colored ceramics as well as numerous objects from private collectors enriched the collections of the Tatra Museum.
PL
Juliusz Zborowski, absolwent polonistyki Uniwersytetu Jagiellońskiego w 1913 roku zamieszkał na Podhalu, bo podjął pracę nauczyciela w nowotarskim gimnazjum. Wydarzenia historyczne tamtych lat związane z ustalaniem nowych granic II Rzeczpospolitej sprawiły, że zaangażował się w działania na rzecz ochrony kulturowego dziedzictwa na spornych terenach Spisza i Orawy. Był członkiem Głównego Komitetu Plebiscytowego Spisko-Orawskiego, następnie kierownikiem jego referatu prasowego „Gazety Podhalańskiej” (1919–1920), od 1918 roku członkiem Towarzystwa Tatrzańskiego, by w 1922 roku zostać pierwszym dyrektorem Muzeum Tatrzańskiego. W 1920 roku Główny Komitet Plebiscytowy uległ likwidacji, a zebrane na jego działalność pieniądze zostały przeznaczone na zakup etnograficznych okazów z tak zwanych kresów południowych II Rzeczpospolitej. Zborowski zajął się ich pozyskiwaniem dla muzeum. W efekcie ponad dwieście egzemplarzy obrazów malowanych na szkle i barwnej ceramiki oraz liczne obiekty od prywatnych kolekcjonerów wzbogaciły zbiory Muzeum Tatrzańskiego.
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2020
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nr 4 (27)
18-37
EN
The article describes the role of the problem of national minorities (Poles in Zaolzie, Czechs mainly in Kłodzko, and Slovaks in Polish parts of Spiš and Orava) in Polish-Czechoslovakian relations during the communist era. In the light of the author’s research, the nationalist heritage of border disputes from the first half of the 20th century influenced relations between the two countries also in later years, although the minority problem in their mutual relations was marginal and officially did not exist for both sides.
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