The role of geological conditions in the disintegration of historical structures on the escarpment of the Lower Vistula Valley, on the example of Chełmno (Poland)

Pub Date : 2017-05-31 DOI:10.1515/bgeo-2017-0007
Ewa Labak-Mechowska, M. Dąbrowski
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Abstract

Abstract Chełmno is a town in the north-western part of the Chełmno Lakeland. It is one of few towns in Poland to have fully preserved its medieval defensive walls. Its touristic and natural environs make it a popular tourist destination. The town’s location near the escarpment of the Vistula valley mean that the preserved historical structures (including the defensive walls) are under threat. A few years ago a buttress became detached and two sections of the defensive walls collapsed. One part was rebuilt (the site where the studies were conducted), while the second part remains unrestored. Bricks are also progressively coming away. This situation may be the result of several factors, although the authors claim that the most important are the geological structure and the wall foundations (which are shallow, at a depth of 1-2 m, with the wall having been built up higher in the 16th century).
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下维斯瓦河谷悬崖上的历史结构解体中地质条件的作用,以Chełmno为例(波兰)
Chełmno是位于Chełmno湖区西北部的一个小镇。它是波兰少数几个完整保存中世纪防御墙的城镇之一。它的旅游和自然环境使它成为一个受欢迎的旅游目的地。该镇的位置靠近维斯瓦山谷的悬崖,这意味着保存下来的历史建筑(包括防御墙)正受到威胁。几年前,一个扶壁脱落,两段防御墙倒塌。其中一部分被重建(进行研究的地点),而第二部分仍未修复。砖块也在逐渐消失。这种情况可能是由几个因素造成的,尽管作者声称最重要的是地质结构和墙壁基础(它们很浅,深度为1-2米,墙壁在16世纪建得更高)。
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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