Abstract

Landslides and rock falls are among the many phenomena that have an impact on sustainable construction and infrastructure safety. The main causes of landslides are natural meteorological and hydrological phenomena. In building design and construction, environmental monitoring by identifying geotechnical hazards must be taken into account, as appropriate hazard assessment contributes to ensuring future construction safety. The Carpathian region in southern Poland is particularly predisposed to landslide formation. This may be favored by the nature of the shapes associated with the high and steep slopes of the region’s valleys. Another reason for concern is the flysch geological structure, which is characterized by alternating layers of water-permeable sandstones and poorly permeable shales, clays, and marls. Furthermore, the presence of a quaternary weathering cover makes the geological structure more susceptible to landslide processes and tectonic formations. The paper presents the results of a study whose aim was to elaborate a detailed landslide hazard map for a selected area in the Polish Carpathians, using statistical methods. The approach is based on the Hellwig method, which seems particularly useful in the assessment of susceptibility and landslide hazards on a local scale for a relatively small area. A two-stage study was conducted. The first stage of the research involved the creation of a database associated with environmental parameters and triggering factors, whereas the second stage consisted of the adoption of weights for seven thematic sections and their special features on the basis of expert knowledge. The hazard map developed as a result was compared to the mapping made using the weight-of-evidence method. The proposed data normalization method allows the use and analysis of both qualitative and quantitative data collected from various sources. The advantage of this method is the simple calculation procedure. A large-scale (1:2000) map might be used to assess the landslide hazard for specific cadastral units. Such a map becomes the basis for municipal spatial planning and may be able to influence investment decisions. Detailed landslide hazard maps are crucial for more precise risk evaluation for specific cadastral units. This, in turn, allows one to reduce serious economic and social losses, which might be the future results of landslides.

Highlights

  • Over the past few decades, extreme natural phenomena, such as heavy or prolonged precipitation and the associated increased landslide risk, have caused significant economic and financial losses in the affected areas

  • The colluvial material is composed of silty clays, clays (Cl), and clayey gravels

  • According to the final landslide hazard maps for the village of Gwozdzianka (Figure 11), approximately 74% (2.41 km2 ) of the cadastral unit area is located in hazard zones and about 26% (1.07 km2 ) of the area is situated in the no-hazard zone

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Summary

Introduction

Over the past few decades, extreme natural phenomena, such as heavy or prolonged precipitation and the associated increased landslide risk, have caused significant economic and financial losses in the affected areas. Slope failure is one of the most frequent geological hazards. Quantitative risk assessment for slope failure is a powerful tool for hazard mitigation and has been widely applied around the world [1]. 2021, 13, 317 in assessing risks in a large and a small area. One major problem is related to the efficiency of the assessment of landslide risk. The current situation should compel constant improvement of the principles and research methods used in defining landslide areas, including monitoring landslides and mapping landslide probability, or mapping landslide hazard

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