U radu autor s aspekta povijesti institucija obrađuje ustroj i djelovanje Dioničarskog društva dunavsko-savske vicinalne željeznice u periodu Austro-Ugarske Monarhije. Sjedište društva, kao i kod ...većine vicinalnih željeznica, bilo je u Budimpešti. Poslove dioničarskog društva obavljali su: glavna skupština dioničara, ravnateljstvo i nadzorni odbor. Pruge društva bile su Vukovar-Ilača i Šid-Rača-Sava. Navedene privatne pruge bile su u državnoj eksploataciji, odnosno upravi. U Austro-Ugarskoj Monarhiji pruge društva potpadale su pod nadležnost Prometne uprave Kr. ugarskih državnih željeznica u Pečuhu (Pécs). Društvo je poslovalo s financijskim dobitkom.
In the paper the author outlines from the aspect of the history of institutions the structure and the activity of the Danube-Sava Vicinal Railway Stock Company during the Austro-Hungarian Monarchy. Like the majority of other vicinal railways, the company had its headquarters in Budapest. The stock company’s tasks were performed by: the stockholders’
general assembly, headquarters and the inspecting committee. The company’s railway lines were: Vukovar-Ilača and Šid-Rača-Sava. These private railway lines were exploited i.e. administrated by the state. During the Austro-Hungarian Monarchy the company’s railway lines came under the jurisdiction of the Traffic Administration of the Royal Hungarian State Railways in Pecs. The railway’s purpose was to connect Sava with Danube through fertile Syrmia, as well as to make accessible the famous oak woods of the Petrovaradin Proprietary District Council, which were situated between Morović and Rača. Apart from that the railway line had the direction to cross by Rača into Bosnia and through the rich Bosnian Posavina through Bjeljina and Janja by Glavčica to connect the upper Drina and the main roads that intersect from southern Serbia. More precisely, the plan was to establish a trade-traffic railway link that would connect the entire Podrinje, particularly the rich Serbian Mačva and the fertile Bosnian plain, entering in Rača into the Kingdom of Croatia and Slavonia and further to world markets (Budapest, Vienna, etc.). The construction of railway opened the possibility for rational exploitation of the vast layers of pebbles lying around Rača. Due to the stock company’s capital of 8.252,00 crowns
and being solvent we can conclude that the stock company represented a minor, but successful private vicinal railway.
An in situ electron microprobe study of detrital minerals yielded important insights into the diagenetic history of the Cretaceous-to-Paleogene flysch sandstones from the Chvalčov site, Rača Unit, ...Flysch Belt of the Outer Western Carpathians. Detrital titanite and a Fe-Ti mineral (probably ilmenite) were almost completely altered to TiO2 minerals, which also newly crystallized in intergranular spaces of sandstone. Brookite, anatase, and, exceptionally, rutile were identified by Raman spectroscopy. Authigenic TiO2 phases show complex composition with occasionally elevated contents of Fe, Nb, Zr, V, Sc, Cr, Al, Y, and/or P, which were likely sourced from altered neighboring heavy minerals. In addition, rare authigenic LREE- and Y-enriched apatite rims were observed on detrital apatite. The remobilization of REE, Y, and HFSE was likely mediated by acidic early diagenetic fluids enriched in fluoride and sulfate anions. The superimposed formation of calcite cement was associated with the dissolution of detrital garnet, feldspars, and quartz. The compositions of detrital apatite and garnet (Alm60-82Prp4-30Sps0-24Grs0-19) are comparable with those from adjacent parts of the Flysch Belt. Detrital rutile is enriched in Nb, V, Cr, and Zr. Our study illustrates the intensity of diagenetic alteration of detrital minerals in flysch sandstones as well as the usefulness of in-situ electron-microprobe investigations for the recognition of processes influencing heavy minerals in diagenetically altered sediments.
This paper deals with the structure, activity, and liquidation of the Danube-Sava Vicinal Railway Stock Company during the Kingdom of Serbs, Croats, and Slovenes/Yugoslavia. The company, founded in ...1912, was based in Budapest and constructed the following railway lines: Vukovar-Ilača and Šid-Sremska Rača-Sava. These private railway lines were exploited by the state. The stock company was solvent. After the collapse of the Austro-Hungarian Empire, the company’s headquarters moved from Budapest to Zagreb. Shortly after the establishment of the Kingdom of Serbs, Croats, and Slovens/Yugoslavia, the railway lines were exploited by the Directorate of State Railways in Zagreb, but after 1921 they came under the jurisdiction of the Directorate of State Railways in Belgrade. According to the Agreement of February 7, 1931, the state redeemed the railway lines of the abovementioned company and thus the company ceased to exist. The company went into liquidation in 1932 and was shut down on April 12, 1933.
The attractiveness of rural areas is the basis for development of tourist offer of rural tourism destination. Bearing in mind that the villages are ecologically and environmentally preserved ...integrities, it is a sustainable form of tourism, which contributes to the development of rural economy. Villages that foster traditional values are of attractive tourist destinations. Staying of tourists in the villages enables active involvement of other economic activities in the creation of the integrated tourism product. Tourism of the Rača Municipality, despite the existence of attractive resources, is not adequately developed. Tourist offer is of a modest scale and based on the sites of cultural and historical heritage and events. The development of tourism in this municipality requires institutional support of local government, investments and cooperation of holders of the tourism offer. In this paper, the emphasis is on the analysis of the current situation of tourism development in the municipality of Rača, with emphasis on resources for the development of rural tourism. Based on examples of good practice - rural tourism destinations in Europe and Serbia, the contribution of labor is reflected in providing guidelines for the future development of rural tourism in Rača.
The development of viticulture and wine producing has brought forward some unique elements of cultural land and introduced culture itself into the landscape. This culture has affected lives of many ...generations and determined the development of the society and the living environment. The form, the shape and the type of use of the respective elements of landscape structure has changed according to the change in technology, cultivation processes, orientation of production and the value system of the society. However, the recent viticultural rural land (together with residual areas of historical structure elements) in the vicinity of the capital city of Slovakia -- Bratislava has been under growing pressure caused by suburbanisation. This pressure directly threatens the existence of this kind of landscape and causes irreversible changes to landscape character. Landscape ecologists and architects have to face the issue of how to identify the valuable characteristics of the land and how to protects and keep them for the future generations. The main aim of this paper is to evaluate the role of viticulture in the formation, existence and change of the elements of historical structures of agricultural landscape (HSAL). In addition, this paper presents the layout of various types of these elements, the methodical approach to their mapping and their present status. The results show that out of 141 localities where the HSALs were present in 1951, they could have been located only in 25 localities in 2011. These localities are mainly situated in private properties. However, many of the mapped HSALs are no longer used and in the state of deterioration. The lack of their management gradually causes their demise.
In the study area by geological mapping we localized Zlín Formation, situated in north - east area of Outer Western Carpathians,near the Nová Polianka village. In Zlín Formation (Middle – Upper ...Eocene) we have distinguished 3 types of lithofacies - sandstonelithofacies (Makovica sandstones), sandstone - mudstone lithofacies and mudstone lithofacies. Sediments represent part of a deepmarinedeposition system as well as depositional environment of submarine slope. Sandstone intrusions in the Zlín Formation wereinterpreted in terms of their geometry and relating to ambient sediments like sandstone dykes. Their distribution is connected only withmassive mudstone, in which they extend in two vertical directions. The sandstone dikes are evidence of extensional opening faultsand joint systems in time of the sediment deposition of Magura basin. They were injected during tectonic movements connected withthe earliest stage of deformation of the basin in this part. This assumption is supported presence of synsedimentary structures, which aredocumentations of the active basin margin. These are synsedimentary slide solids in overhead part of the Makovica sandstonesand presence of the sediments distribution channel. This indicates the orientation of local dynamic evolution in time of their formation.
In the study area by geological mapping we localized Zlín Formation, situated in north - east area of Outer Western Carpathians,near the Nová Polianka village. In Zlín Formation (Middle – Upper ...Eocene) we have distinguished 3 types of lithofacies - sandstonelithofacies (Makovica sandstones), sandstone - mudstone lithofacies and mudstone lithofacies. Sediments represent part of a deepmarinedeposition system as well as depositional environment of submarine slope. Sandstone intrusions in the Zlín Formation wereinterpreted in terms of their geometry and relating to ambient sediments like sandstone dykes. Their distribution is connected only withmassive mudstone, in which they extend in two vertical directions. The sandstone dikes are evidence of extensional opening faultsand joint systems in time of the sediment deposition of Magura basin. They were injected during tectonic movements connected withthe earliest stage of deformation of the basin in this part. This assumption is supported presence of synsedimentary structures, which aredocumentations of the active basin margin. These are synsedimentary slide solids in overhead part of the Makovica sandstonesand presence of the sediments distribution channel. This indicates the orientation of local dynamic evolution in time of their formation.
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