确定历史和城市化地区山体滑坡的困难——以Przemyśl要塞为例

Q4 Earth and Planetary Sciences
Edyta Rycio
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引用次数: 0

摘要

确定历史和城市化地区山体滑坡的困难——Przemyśl要塞的案例研究。Przemyoel堡垒是19世纪和20世纪之交的一座巨大的防御工事。时至今日,该地区还不同程度地保存着各种各样的文物、堡垒的废墟和遗迹以及战斗的迹象。在确定滑坡时,它们构成了一个巨大的问题。最大的困难是由植被覆盖的堡垒废墟、战壕、城墙和防御沟的遗迹以及一些地方保存的战斗迹象造成的。这些残留物可以被解释为滑坡或其一部分,特别是如果它们发生在附近或滑坡内部。然后出现了清楚识别滑坡边界和正确识别其内部形式的问题,例如,堡垒周围被破坏的沟渠可以被标记为滑坡。许多不活跃的采石场、挖掘、粘土坑也带来了类似的困难,例如位于Kruhel Wielki的19世纪关闭的石灰石露天矿。旧矿山的元素似乎让人想起了场内形式,并且很难将其与邻近滑坡的真实崩积形式区分开来。确定滑坡的困难不仅源于该地区的历史及其地质结构,还源于该区域的城市化程度。强烈的人类压迫模糊了斜坡的自然形态,该地区的有限可用性使制图工作变得困难。在这些地区很难区分自然形态和人工形态。滑雪场、市政公墓、城堡公园以及军事区、住宅区和分配区的山体滑坡就是很好的例子。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Trudności w wyznaczaniu osuwisk na obszarach historycznych i zurbanizowanych na przykładzie Twierdzy Przemyśl
Difficulties in determining landslides in historical and urbanized areas – a case study of the Przemyśl Fortress. A b s t r a c t.The Przemyoel Fortress is a huge complex of defensive objects from the turn of the 19 th and 20 th centuries. Various types of objects, ruins and remains of the fortress and signs of fights have been preserved to different extents in the area to this day. They constitute a huge problem when determining landslides. The greatest difficulties are caused by vegetation-covered ruins of forts, trenches, remnants of ramparts and defense ditches, and signs of fights preserved in places. Such residues can be interpreted as a landslide or a part of it, especially if they occur in a neighbourhood or inside a landslide. The problem then arises of clearly identifying the boundaries of the landslide and the correct identification of its internal forms, e.g. a devastated trench around the fort can be marked as a landslide. Similar difficulties are provided by numerous inactive quarries, excavations, clay pits, e.g. a closed limestone open-pit mine from the 19 th century, located in Kruhel Wielki. Elements of the old mine are deceptively reminiscent of intra-field forms and they are difficult to separate from the real colluvial forms of the neighbouring landslide. Difficulties in determining landslides arise not only from the history of this region and its geological structure, but also from the degree of urbanization of the area. Strong anthropopression blurs the natural morphology of the slopes, and the limited availability of the area makes cartographic work difficult. It is difficult to distinguish between natural and artificial forms in such areas. Good examples are landslides on the ski slope, on the municipal cemetery, in the castle park and in the area of military areas, housing estates and allotments.
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来源期刊
Przeglad Geologiczny
Przeglad Geologiczny Earth and Planetary Sciences-Geology
CiteScore
0.70
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0.00%
发文量
24
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