Abstract

Landslide is that the downslope movement of debris, rocks, or earth material under the influence of the force of gravity. Although the causes and mechanisms of landslides are complicated, human action, earthquakes, and severe rainfall can trigger them. It can happen when the driving force surpasses the resisting force due to natural soil or rock slope destabilization. Landslide is one of the foremost destructive and dangerous natural hazards that cause numerous fatalities and economic losses worldwide. Therefore, landslide investigation, susceptibility, hazard, and risk mapping are vital tasks to disaster loss reduction and performance as a suggestion for sustainable land use planning. The determination of the cause variables, identification of existing landslides, and production of a landslide susceptibility, hazard, and risk map are all necessary steps in the mitigation of landslide incidence on the globe. Landslide susceptibility, hazard, and risk maps are the outcome of a statistical relationship between environmental conditions and previously occurring landslides. It provides critical scientific support for the government’s reaction to land use practices and the management of landslide threats. The type, concept of landslides, factor, inventories, susceptibility, hazard, and risk, as well as mapping and validation methodologies, have all been examined in this chapter. The distinction between landslide susceptibility and hazard has surely been debated.

Highlights

  • Landslide inventory, susceptibility, hazard, and risk mapping may be a complex job thanks to a good spectrum of conditioning and triggering factors, lack of record data, and non-uniqueness of mapping methods

  • Hazard, and risk mapping, mapping and analysis of previous and active landslide incidence are demanding tasks that can be used for landslide prevention and mitigation

  • Chen and Wang [9] explained that susceptibility, hazard, and risk maps of landslides are the results of the statistical relationship in between landslide governing factors and preexisting landslides

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Summary

Introduction

The evaluation of landslide conditioning and triggering factors is a very important task. The force of gravity and the progressive weakening of geological materials, mainly thanks to weathering, alongside the action of other natural and environmental phenomena, make mass movements relatively common on the earth’s surface [20] These processes create potential geological risks, as they will cause economic loss and social damage if they affect human activities, buildings, and infrastructure [20]. To carry out this research, it is necessary to understand the characteristics and the geological, geotechnical, and hydrogeological properties of the soil and rock materials involved and their mechanical behavior because the factors that condition and trigger such movements [20]. Studies during this field should specialize in the investigation of [20]. Factors that control landslides are classified into two such as intrinsic/inherent/static and external/ dynamic landslide factors [21–23]

Definition and concepts
Type of landslide or failure mechanism
Rotational landslides
Translational slides
Mud or earth flows
Debris flows
Solifluction
Rock falls
Toppling
Rock avalanches
Debris avalanches
2.1.10 Lateral displacements
States and distribution of landslide
Recognition of landslides
Intrinsic controlling factors
Lithology
Discontinuities
Hydrogeological conditions
Properties of soil and rock masses
Geomorphological factors (slope, aspect, and curvature)
External triggering factors
Objectives
Landslide susceptibility, hazard and risk mapping
Landslide susceptibility and hazard mapping approaches
Qualitative (expert evaluation) method
Heuristic method
Landslide inventory method
Landslide Hazard evaluation factors (LHEF)
Slope stability evaluation parameters (SSEP)
Semi quantitative method
Quantitative (statistical) method
Bivariate statistical analysis
Multivariate statistical analysis
Data mining method
Physical based approach
Landslide risk mapping approaches
Landslide susceptibility, hazard, and risk model validation
Success and predictive rate curve
Landslide density
Relative landslide density index (R: Index)
Relative error
Receiver operating characteristics (ROC)
Findings
2.10.1 Landslide susceptibility mapping using statistical methods in Uatzau catchment area, Northwestern Ethiopia
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