61 resultados para Messianism, Polish.
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The article discusses the formula for a new Polish bibliometric indicator, i.e., the Polish Impact Factor (Polski Współczynnik Wpływu) from the point of view of the humanities. Our study examines two prestigious Polish humanities journals (Pamiętnik Literacki and Diametros – An Online Journal of Philosophy) to evaluate the underlying assumptions of the Polish Impact Factor. We have analyzed all articles published from 2004 to 2014 (N = 850, N = 555, respectively) and all references included in these articles (N = 21,805, N = 8,298, respectively). When interpreting the findings, we have assumed that different groups of sciences are characterized by different citation cultures. Our findings show that the formula for the Polish Impact Factor does not take into account the most cited sources in the humanities, i.e., books and chapters. Moreover, many citations will not be included in the formula because of the citation age: the formula for the Polish Impact Factor is provided for the citations whose age is not higher than 5 years. We have analyzed the citation age of all citations and used Price’s Index to interpret the result. We have found out that most of citations are older than 5 years (84,2 percent and 73,2 percent, respectively). Our analysis shows that the Polish Impact Factor is not an adequate tool for a bibliometric evaluation of the journals in the humanities in Poland. The article concludes with a discussion of how the Polish Impact Factor could be improved.
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The subject of the text is the issue of the "political", which is defined as the nature and level of the final judgment and ultimate reasoning. The issues of this kind of the "political" has been attempted to distinguish in political sciences. The text focuses on: (1) the scientist as an agent for the final judgment and reasoning, (2) the subject of study of political science, (3) "theoretical strategies" in the science of politics. The latter problem has been discussed mainly on the example of Polish political science. Discussed were among others: (1) "the dilemma of scale", (2) limited operational capacity (methodological and theoretical), (3) aesthetic imagery of political life, (4) structural ignorance in the field of ontology, epistemology and methodology.
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Filologii Polskiej i Klasycznej: Zakład Dydaktyki Literatury i Języka Polskiego
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Wydział Filologii Polskiej i Klasycznej: Instytut Filologii Polskiej
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Wydział Filologii Polskiej i Klasycznej
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Wydział Filologii Polskiej i Klasycznej
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The article deals with not well known theory of personality of Polish Neojacsonist psychiatrist Jan Mazurkiewicz. It describes its scientific background, biography and basic ideas and assumptions. The accent is put here on its, based on Lévi- Bruhl’s ideas but mostly original mythocentricity in psychological perspective and description of human symbolic thinking and acting.
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The aim of this article is to investigate how the European university education sector is being internationalized. The authors test „European Studies” programs, assuming that due to their peculiar character they are the forerunners of change, which results, among other things, from Europeanization processes. The field of „Teaching Europe” is mapped in the European Union and then a more detailed analysis is conducted in Poland and Germany. These allow the authors to formulate three models describing how universities in Europe are answering the challenges created by the integration process. The Polish and German cases further illustrate the dynamics of „European Studies” development, as well as differences in general aims, disciplinary construction as well as level of internationalization. Various geographical patterns of enhanced collaboration are revealed by the research when checking Double Degree programs.
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We report sedimentological evidence for a tsunami from a coastal lake at Innaarsuit, Disko Bugt (west Greenland), which was most likely generated by a rolling iceberg. The tsunami invaded the lake c. 6000 years ago, during a period of time when relative sea level (RSL) was falling quickly because of isostatic rebound. We use the background rate of RSL fall, together with an age model for the sediment sequence, to infer a minimum wave run-up during the event of c. 3.3 m. The stratigraphic signature of the event bears similarities to that described from studies of the early-Holocene Storegga slide tsunami in Norwegian coastal basins. Conditions conducive to iceberg tsunami include a supply of icebergs, deep water close to the shore, a depositional setting protected from storms or landslide tsunami, and a coastal configuration that has the potential to amplify the height of tsunami waves as water depths shallow and the waves approach and impact the coast. Future warming of polar regions will lead to increased calving and iceberg production, at a time when human use of polar coasts will also grow. We predict, therefore, that iceberg-generated tsunami will become a growing hazard in polar coastal waters, especially in areas adjacent to large, fast-flowing, marine-terminating ice streams that are close to human populations or infrastructure.
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High-resolution swath-bathymetry data from inner Kongsfjorden, Svalbard, reveal characteristic landform assemblages formed during and after surges of tidewater glaciers, and provide new insights into the dynamics of surging glaciers. Glacier front oscillations and overriding related to surge activity lead to the formation of overridden moraines, glacial lineations of two types, terminal moraines, associated debris lobes and De Geer moraines. In contrast to submarine landform assemblages from other Svalbard fjords, the occurrence of two kinds of glacial lineations and the presence of De Geer moraines suggest variability in the landforms produced by surge-type tidewater glaciers. All the landforms in inner Kongsfjorden were deposited during the last c. 150 years. Lithological and acoustic data from the innermost fjord reveal that suspension settling from meltwater plumes as well as ice rafting are dominant sedimentary processes in the fjord, leading to the deposition of stratified glacimarine muds with variable numbers of clasts. Reworking of sediments by glacier surging results in the deposition of sediment lobes containing massive glacimarine muds. Two sediment cores reveal minimum sediment accumulation rates related to the Kongsvegen surge from 1948; these were 30 cm a-1 approximately 2.5 km beyond the glacier front shortly after surge termination, and rapidly dropped to an average rate of 1.8 cm a-1 in ∼1950, during glacier retreat.
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Wydział Nauk Społecznych: Instytut Kulturoznawstwa