This study is dedicated to documenting the relationship between these two important musicians on the basis of excerpts from extant written sources. The most important documentation of contacts between Vaclav Jan Tomasek (1774-1850) and Carl Maria von Weber (1786-1826), who worked in Prague from 1813 until 1817 as Kapellmeister of the Estates Theatre, is Tomaseks autobiography published in Prague in 1845-1850 in a yearbook titled Libussa. We find additional brief documentation in Weber's diaries and in the correspondence of both men addressed to other persons. Tomasek's autobiography is also important documentation of how Weber's works were viewed by the German public and music critics., Obsahuje seznam literatury, and Anglické resumé na s. 82.
The contribution explores the Prague origines of the first Prague and Austrian female author of the Enlightenment, Maria Anna Sager, born Rosskoschny (1719-1805). The reconstruction of the carreer of her father Anton Ferdinand Rosskoschny (1679-1734) at the Böhmische Statthalterei - he ended as "Registrator" and "Expeditor" - proves his social ambitions. On the other hand egodocuments of him conserved in the National Archives at Prague reveal the sorrows and the "stress" of the wellestablished fonctioner, not only his fear in front of the people, but also for his reputation, his family and his soul., Helga Meise., and Obsahuje bibliografické odkazy
Karst landforms can result from a single stage process in which chemical dissolution and mechanical erosion proceed simultaneously or from a two stage process in which chemical dissolution precedes mechanical erosion. During the second of these processes, chemical dissolution leads to the creation of karst features hosting a residual weathering product, here referred to as alterite. An example of one such feature is the enclosed mass of altered rock at Červený Quarry near Klukovice which represents one of the richest localities for exceptionally preserved echinoderm ossicles in the Prague Synform. In this study the processes responsible for the formation of this feature have been investigated. Nineteen samples were obtained from the bioclastic Slivenec Limestone and from these it has been possible to calculate the carbonate volume content, which defines the weathering intensity, and the carbonate rock weathering index, which defines the weathering state. The results demonstrate that carbonate dissolution has not been accompanied by gravitational compaction or the incorporation of mineral inputs. Thin sections analysed under polarised light and under cathodoluminescence emphasise heterogeneous dolomitisation of the limestone. As the weathering grade intensifies, empty rhomboidal pores become increasingly common until, ultimately, the rhomboidal forms are lost due to corrosion and enlargement. In contrast it is rare to find evidence of calcite dissolution and, therefore, the altered mass still hosts almost all of its post dolomitisation micrite, sparite, and bioclasts. Negligible calcite dissolution helps to explain the exceptional nature of the fossil preservation at the site while the dolomite dissolution accounts for the ease with which it is possible to extract the fossils. Further research should focus on better understanding the role of dolomite dissolution in the formation of other important palaeontological localities in the Prague Synform., Matt Rowberry, Caroline Dubois, Olivier Kaufmann, Jean-Marc Baele and Jan Blahůt., and Obsahuje bibliografii
Staroměstský orloj je zřejmě nejlépe zachovaný středověký orloj na světě, který dosud funguje. Tvoří součást historického centra Prahy a je zapsán na seznam kulturních památek UNESCO. Již po staletí jej provázejí děsivé legendy, které zastrašují každého, kdo by do něj chtěl nevhodným způsobem zasáhnout. Ani ty však nedokázaly zabránit potyčkám, jež se kolem orloje v současné době rozpoutaly., Michal Křížek, Jana Žďárská., and Obsahuje bibliografické odkazy