在克拉科夫师范大学主楼的室内设计中使用自然资源

A. Wolska, Agnieszka Ciurej, Szymon Kowalik
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引用次数: 1

摘要

本文介绍了一个有趣的装饰地板解决方案,从1973年开始,在克拉科夫师范大学主楼的地面和一楼,以国家教育委员会命名。地板由不规则的、颜色各异的天然石板组成:所谓的圣十字山“大理石”。它们代表了Chęciny附近石灰岩采石场的几种岩石类型,主要包括Bolechowice,但也包括Szewce, Łabędziów和Jaźwica。这些岩石传统上被称为弹珠。然而,实际上,从岩石学上看,它们不是变质岩,而是强烈的岩化和块状,部分结晶的石灰石,有许多化石。它们属于古生代:中、上泥盆世。这种由不同尺寸和颜色的不规则面板组成的地板目前很少用于室内设计,尽管它具有有趣的图案,具有令人愉悦的马赛克效果。由各种圣十字山“大理石”制成的地板具有很高的教育价值和地理旅游意义。选择和描述不同岩性类型的岩石可用于创建地理旅游教育路径,这将有助于教授与地球科学相关的学科(例如地质学,古生物学,岩石材料)。
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THE USE OF A NATURAL RESOURCE IN THE INTERIOR DESIGN OF THE MAIN BUILDING OF THE PEDAGOGICAL UNIVERSITY OF CRACOW
The paper presents an interesting decorative flooring solution from 1973 on the ground and first floors of the main building of the Pedagogical University of Cracow, named after the Commission of National Education. This flooring is composed of irregular, variably coloured natural stone slabs: the so-called Holy Cross Mountains „marbles”. They represent several rock types from limestone quarries near Chęciny, including mainly Bolechowice, but also Szewce, Łabędziów and Jaźwica. These rocks are traditionally called marbles. However, in fact, petrographically, they are not metamorphic rocks, but strongly lithified and massive, partially crystallized limestones with numerous fossils. They are of Paleozoic age: Middle and Upper Devonian. The type of flooring composed of irregular panels of different sizes and colours is currently rarely used in interior design despite giving an aesthetically pleasing mosaic effect with an interesting pattern. The flooring made of assorted Holy Cross Mountains “marbles” can have a great educational value and great geotouristic significance. Selected and described rocks of different lithological types can be used to create a geotouristic educational path that will be helpful in teaching of subjects related to Earth sciences (e.g. geology, paleontology, rock materials).
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ZŁOTO W POTOKACH I PEGMATYCIE Z REJONU STRZELINA ROZPOZNANIE LOKALIZACJI WYROBISK PIASKÓW I ŻWIRÓW WZGLĘDEM GRANIC GZWP ORAZ CIEKÓW POWIERZCHNIOWYCH NA OBSZARZE WOJEWÓDZTWA ŚLĄSKIEGO INTERPRETACJA ZMIENNOŚCI TEMPERATURY WODY W ŹRÓDLE NA WSCHODNIM STOKU ZAMECZKÓW (TATRY ZACHODNIE) NA PODSTAWIE CIĄGŁYCH OBSERWACJI MONITORINGOWYCH I NUMERYCZNEGO MODELU TRANSPORTU CIEPŁA PARAMETRY MIGRACJI ZANIECZYSZCZEŃ W ODPADACH FLOTACYJNYCH NA PODSTAWIE TERENOWEGO EKSPERYMENTU ZNACZNIKOWEGO NA PRZYKŁADZIE OBIEKTU UNIESZKODLIWIANIA ODPADÓW WYDOBYWCZYCH „GILÓW” ZRÓŻNICOWANIE TŁA HYDROGEOCHEMICZNEGO WÓD PODZIEMNYCH EKSPLOATOWANYCH W ZLEWNI BIEBRZY
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