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Szkoły w krajobrazie miasta na przykładzie szkół neorenesansowych w Oleśnicy

Lisowska A.

Zeszyty Naukowe. Architektura / Politechnika Śląska

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2009

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z. 49

127-135

PL

W pracy zaprezentowane zostaną dwie oleśnickie szkoły: gimnazjum męskie oraz szkoła elementarna dla chłopców. Obie neorenesansowe szkoły powstały na początku XX wieku. Budynki szkół doskonale wpisały się w zastany krajobraz, swą architekturą oraz detalem nawiązują do zamku książąt oleśnickich, miasta Oleśnicy i regionu. W referacie omówiona zostanie architektura obiektów, znaczenie poszczególnych rozwiązań, symbolika detalu oraz ich powiązania z zastanym miejscem.

EN

The subject of this research is a presentation of two schools in Oleśnica: a male gymnasium and an elementary school for boys. Both Neo-Renaissance schools originate from the early 20th century. The buildings correspond with their surroundings and their design and details refer to Zamek Książąt Oleśnickich, the city of Oleśnica and the region. This research covers the architecture of the objects, the significance of particular solutions, the symbolism of details and their interrelation with the surroundings.

2

Ewangelicka szkoła dla chłopców w Oleśnicy. Treści ideowe dekoracji budynku szkolnego

Lisowska A.

Kwartalnik Architektury i Urbanistyki

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2008

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T. 53, z. 3

52-63

PL

W latach 1911-13 wybudowano w Oleśnicy nowoczesny obiekt szkolny mający pomieścić około 1000 uczniów. Neorenesansowy budynek nawiązywać miał do tradycji książęcego zamku. Szkoła spełniała ówczesne wymogi nauczania, posiadała salę sportowo-bankietową, nowocześnie urządzone sale lekcyjne, takie jak do fizyki czy rysunku. Budynek był bardzo dobrze doświetlony dzięki dużym oknom. Na dziecińcu szkolnym oprócz boiska do gimnastyki znalazł się również ogródek do lekcji botaniki. Duży gmach posiadał bogaty detal o symbolice związanej bezpośrednio z funkcją obiektu, jak również podkreślający związki szkoły z miastem (herby). W 1930 roku oddano do użytku nową część dobudowaną do obiektu. Przeznaczona ona była na szkołę średnią mającą kształcić pracowników administracji, handlu i przemysłu. Część ta została doskonale zharmonizowana z istniejącą bryłą.

EN

The modern school building in Oleśnica, holding approximately 100 pupils, was built in 1911-13. The shape of the neo-renaissance building was intended to refer to the tradition of a prince's castle. The school fulfilled the educational requirements of that time, has a sport-banquet room, and physics and drawing classrooms with modern equipment. The building was very well lit thanks to large windows. The school courtyard, as well as an athletic field, also hosted a garden for botanical classes. The large edifice had a rich detail of symbols related to the building's function, and also emphasising the relationship of the school and the city (coats of arms). The new extension to the building was completed in 1930. It was dedicated to a high school intended to educate employees of administration, trade and industry. This part was harmonised with the existing building.

3

Szkoła w zieleni

Lisowska A.

Architektura Krajobrazu

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2008

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nr 3

44-47

EN

At the end of the 19th and beginning of the 20th century experts underlined the vital meaning of light, greenery and kind of materials in equipping new school buildings. School buildings were surrounded by greenery which gave them shade and protected them from wind. Together with introducing nature as a subject into the teaching program small botanical gardens were designed near buildings. Gym classes were also very important. Sports grounds an playgrounds for smaller children became an inseparable element of schools. A well with drinking water was usually placed next to them.

4

Cenozoic tectonic evolution of the Poznań-Oleśnica Fault Zone, central-western Poland

Widera M., Ćwikliński W., Karman R.

Acta Geologica Polonica

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2008

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Vol. 58, no. 4

455-471

EN

The Poznań-Oleśnica Fault Zone (P-OFZ) of central-west Poland is an over 150 km long, up to 10 km wide, and up to 200 m deep graben that developed during Early Oligocene to Pliocene times on the flank of the NE-dipping Fore-Sudetic Homocline. Fault systems of this extensional structure appear to reach pre-Zechstein basement in the area ofthe Fore-Sudetic Homocline that forms an integral part of the Bohemian Massif. The P-OFZ was affected by several stages of subsidence, separated by periods of inversion and/or tectonic quiescence between the Triassic and Cenozoic. Structurally, this dislocation zone can be linked with the Variscan faults, reactivated at that time. During the second half of the last century, the northern parts of the P-OFZ graben were intensively explored by cored boreholes because of their lignite content. Conventional back-stripping methods could not be applied to the tectonic analysis of the POFZ due to the limited thickness of the graben fill, its poor dating and the presence of relatively thick lignite seams. Therefore, phases of accelerated subsidence were determined by comparing the thickness of individual lithostratigraphic units within the graben and on its flanks. The total subsidence of the different graben segments was quantified by determining the aggradation coefficient (AC) and by taking the consolidation coefficient (CC) of lignite seams into consideration. Subsidence analyses indicate that the initial Early Oligocene extensional phase of the P-OFZ was followed by an Early.Middle Miocene extensional subsidence phase and a probably latest Miocene.Pliocene final extensional phase.

5

Tradycje czeskie w zabytkach Dolnego Śląska

Przyłęcki M.

Wiadomości Konserwatorskie

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2000

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Nr 7/8

82--91