Geodziedzictwo w lesie – o śladach lądolodu na Pałukach

M. Górska-Zabielska
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引用次数: 0

Abstract

The aim of the research is to make an inventory of nine large erratic boulders lying in situ in the forested areas of Pałuki in the north-east Wielkopolska (West Poland). Due to their location unchanged since the deglaciation times, they can be used to establish the chronology of the deglaciation of the last ice sheet in north-western Poland. The knowledge of large erratic boulders along with other elements of geodiversity of Pałuki, a peripheral tourist region, is a potential for the development of geotourism, which in turn can be a driving force for the sustainable development of the region. Field work was used to collect data characterizing individual boulders and indicating their source area in Scandinavia, if they represent the indicator type of an erratic. Attention was paid to the record of sub/inglacial and periglacial processes affecting the foreland of the melting ice sheet, as well as contemporary morphogenetic processes. The detailed description of the boulders emphasized their scientific, cognitive, educational, upbringing, cultural, conservation, pro-environmental and recreational importance. The location of the erratic boulders in the forest makes them interesting targets for tourism in naturally valuable areas. In the age of changing social expectations with regard to forest functions in favor of social, educational (ecological education) and tourist and recreational functions, their good promotion is necessary, preceded by expert research. This paper provides such knowledge transfer.
这项研究的目的是对位于东北Wielkopolska(西波兰)Pałuki森林地区的9块不稳定的巨石进行清点。由于它们的位置自消冰期以来没有改变,因此可以用来确定波兰西北部最后一个冰盖的消冰期的年表。对Pałuki周边旅游区的大型不稳定巨石和其他地质多样性元素的了解,是地质旅游发展的潜力,反过来又可以成为该地区可持续发展的动力。实地工作用于收集单个巨石的特征数据,并指出它们在斯堪的纳维亚半岛的来源区域,如果它们代表了不稳定的指示类型。重点记录了影响融化冰盖前陆的冰下/冰内和冰周过程,以及当代的形态形成过程。对这些巨石的详细描述强调了它们在科学、认知、教育、养育、文化、保护、环保和娱乐方面的重要性。森林中飘忽不定的巨石的位置使它们成为自然资源宝贵地区旅游的有趣目标。在社会对森林功能的期望朝着有利于社会、教育(生态教育)和旅游娱乐功能的方向转变的时代,在专家研究之前,有必要对森林功能进行良好的推广。本文提供了这种知识转移。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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0.80
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