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Littérature scientifique sur le sujet « Landslide hazard maps »

Auteur : Grafiati

Publié le 7 juin 2025

Mis à jour le 2 août 2025

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Articles de revues sur le sujet "Landslide hazard maps"

Wahba, Mohamed, Mustafa El-Rawy, Nassir Al-Arifi, and Mahmoud M. Mansour. "A Novel Estimation of the Composite Hazard of Landslides and Flash Floods Utilizing an Artificial Intelligence Approach." Water 15, no. 23 (2023): 4138. http://dx.doi.org/10.3390/w15234138.

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Landslides and flash floods are significant natural hazards with substantial risks to human settlements and the environment, and understanding their interconnection is vital. This research investigates the hazards of landslides and floods in two adopted basins in the Yamaguchi and Shimane prefectures, Japan. This study utilized ten environmental variables alongside categories representing landslide-prone, non-landslide, flooded, and non-flooded areas. Employing a machine-learning approach, namely, a LASSO regression model, we generated Landslide Hazard Maps (LHM), Flood Hazard Maps (FHM), and

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Ivanov, Plamen, Nikolai Dobrev, Boyko Berov, Antoaneta Frantzova, Miroslav Krastanov, and Rosen Nankin. "Landslide risk for the territory of Bulgaria by administrative districts." Geologica Balcanica 51, no. 3 (2022): 21–28. http://dx.doi.org/10.52321/geolbalc.51.3.21.

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An assessment of the landslide risk (Rls) for the territory of Bulgaria by administrative districts has been made by combining the vulnerability (V) and landslide hazard (Hls) maps. Landslides are a significant part of geological hazards and are widespread throughout the country. In order to assess the landslide risk for the territory of Bulgaria, it is necessary to take into account not only all landslides for a given region, but also its vulnerability, and thus to assess the level of landslide risk for this region, Rls = f (V, Hls). Landslide risk is determined by a risk matrix, using select

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An assessment of the landslide risk (Rls) for the territory of Bulgaria by administrative districts has been made by combining the vulnerability (V) and landslide hazard (Hls) maps. Landslides are a significant part of geological hazards and are widespread throughout the country. In order to assess the landslide risk for the territory of Bulgaria, it is necessary to take into account not only all landslides for a given region, but also its vulnerability, and thus to assess the level of landslide risk for this region, <em

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Hidayah, Radhitya Adzan, and Nurul Dzakiya. "Analysis Geological and Geophysical Data for Prediction Landslide Hazard Zone with Weight of Evidence Method in Pacitan District East Java." Journal of Applied Geospatial Information 2, no. 1 (2018): 117–23. http://dx.doi.org/10.30871/jagi.v2i1.830.

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Pacitan district have an interesting anomaly. Every time mostly impacted by disaster especially landslide. Landslides in their various forms are common hazard in mountainous terrain, especially in seismically active areas and regions of high rainfall. Landslides are one of the most common natural hazards in the Southern Range East Java terrain, causing widespread damage to property and infrastructure, besides the loss of human lives almost every year. The aim of this study predicted the potential landslide using Weight of Evidence Method. The geological data used lithological data, structural

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Kawagoe, S., S. Kazama, and P. R. Sarukkalige. "Probabilistic modelling of rainfall induced landslide hazard assessment." Hydrology and Earth System Sciences 14, no. 6 (2010): 1047–61. http://dx.doi.org/10.5194/hess-14-1047-2010.

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Abstract. To evaluate the frequency and distribution of landslides hazards over Japan, this study uses a probabilistic model based on multiple logistic regression analysis. Study particular concerns several important physical parameters such as hydraulic parameters, geographical parameters and the geological parameters which are considered to be influential in the occurrence of landslides. Sensitivity analysis confirmed that hydrological parameter (hydraulic gradient) is the most influential factor in the occurrence of landslides. Therefore, the hydraulic gradient is used as the main hydraulic

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Zhafran, Muhammad Naufal, Moh Yanuar Jarwadi Purwanto, and Heriansyah Putra. "Analysis of settlement distribution in relation to landslide hazard areas in Pamijahan, Bogor Regency." BIO Web of Conferences 171 (2025): 02012. https://doi.org/10.1051/bioconf/202517102012.

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A landslide hazard map is a useful tool for assessing and mitigating slope instability. Landslides are influenced by static factors (soil type, permeability, topography), and dynamic factors (rainfall, land cover changes). Recently, the number of developing areas has increased to meet population growth; thus, the presence of landslide hazard maps has become crucial to avoid residents developing in prone areas. This study developed a map of the settlement distribution within landslide-prone zones in Pamijahan, Bogor Regency. It assesses the feasibility of residential areas by classifying them a

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Mohammed, Endris Jemal. "Landslide hazard mapping in Wuchale Town, South Wollo, Ethiopia: An expert approach." International Journal of Applied Research 10, no. 1 (2024): 52–65. https://doi.org/10.5281/zenodo.13621916.

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The present study was conducted in the northern part of the Ethiopian Plateau, specifically in Wuchalle town and its surrounding area. The study area has been facing recurrent landslide issues over the past years, prompting this research study to address the severity of landslides and related instability problems.  The main objective of this study was to evaluate landslide susceptible areas and create landslide hazard zonation map. To achieve the goals of the present study, Slope Stability Suitability Evaluation Parameter rating scheme techniques were used. Nine factors were identified as

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Rachmawati, Turningtyas Ayu, Adi Susilo, Dwi Rahmawati, and Yunita Ratih Wijayanti. "LANDSLIDE HAZARD LEVEL IN PASURUAN REGENCY." Proceedings of the 1st International Conference on Social Science (ICSS) 1, no. 1 (2022): 459–66. http://dx.doi.org/10.59188/icss.v1i1.60.

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Pasuruan Regency is an area with potential for landslides, particularly along the Arjuno-Welirang Slope and the Bromo Tengger Semeru National Park (TNBTS). Geographical conditions, high slopes, and andosols and litosols that are easily eroded, further exacerbated by human activities such as land-use changes, lead to increasingly high landslide potentials. The TNBTS Area and Arjuna-Welirang Mountains are priority destinations for national tourism. Therefore, efforts for disaster risk reduction are imperative. Assessment of landslide hazard levels is necessary as a basis for landslide mitigation

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Kawagoe, S., S. Kazama, and P. R. Sarukkalige. "Probabilistic modelling of rainfall induced landslide hazard assessment." Hydrology and Earth System Sciences Discussions 7, no. 1 (2010): 725–66. http://dx.doi.org/10.5194/hessd-7-725-2010.

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Mabaquiao, L. C. "PERFORMANCE EVALUATION OF TEMPORAL MODEL AND SPATIAL CORRELATION METHODS FOR PERSISTENT SCATTERER DETERMINATION IN LANDSLIDE PRONE AREAS." International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XLVIII-4/W8-2023 (April 25, 2024): 343–49. http://dx.doi.org/10.5194/isprs-archives-xlviii-4-w8-2023-343-2024.

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Abstract. The Philippines is no stranger to natural hazards. Aside from flooding, landslides emerge as a primary contributor to damage dealt by natural hazards. Traditional methods for landslide monitoring require on-site field measurements, which makes them resource-intensive and time-consuming. Moreover, the frequency of updating of existing landslide hazard maps is limited by resources and manpower. This research introduces the application of remote sensing technology, specifically Persistent Scatter Interferometry (PSI), as a complementary tool for updating hazard maps. PSI enables the ide

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Thèses sur le sujet "Landslide hazard maps"

Tyoda, Zipho. "Landslide susceptibility mapping : remote sensing and GIS approach." Thesis, Stellenbosch : Stellenbosch University, 2013. http://hdl.handle.net/10019.1/79856.

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Thesis (MSc)--Stellenbosch University, 2013. Landslide susceptibility maps are important for development planning and disaster management. The current synthesis of landslide susceptibility maps largely applies GIS and remote sensing techniques. One of the most critical stages on landslide susceptibility mapping is the selection of landslide causative factors and weighting of the selected causative factors, in accordance to their influence to slope instability. GIS is ideal when deriving static factors i.e. slope and aspect and most importantly in the synthesis of landslide susceptibility ma

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McCarley, Justin Craig. "Using Repeat Terrestrial Laser Scanning and Photogrammetry to Monitor Reactivation of the Silt Creek Landslide in the Western Cascade Mountains, Linn County, Oregon." Thesis, Portland State University, 2018. http://pqdtopen.proquest.com/#viewpdf?dispub=10748247.

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Landslides represent a serious hazard to people and property in the Pacific Northwest. Currently, the factors leading to sudden catastrophic failure vs. gradual slow creeping are not well understood. Utilizing high-resolution monitoring techniques at a sub-annual temporal scale can help researchers better understand the mechanics of mass wasting processes and possibly lead to better mitigation of their danger. This research used historical imagery analysis, precipitation data, aerial lidar analysis, Structure from Motion (SfM) photogrammetry, terrestrial laser scanning (TLS), and hydrologi

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Clarke, Samantha. "Submarine landslides of the upper east Australian continental margin." Thesis, The University of Sydney, 2014. http://hdl.handle.net/2123/12456.

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Stable continental margins experience submarine landslides relatively frequently and some of the largest slides on record have been shed from these relatively passive terrains. Despite this, and the obvious accompanying tsunami hazard, slides from passive margins such as Australia are poorly understood when compared to other settings, such as the flanks of volcanic islands, active subduction-zone margins and submarine fans. This work presents an investigation into the submarine landslides occurring along east Australia’s (EA) continental margin, with a focus on investigating the causes, timing

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Obregón, Christian, and Julio Lara. "Landslide Susceptibility Map: A tool for sustainable land management." Pontificia Universidad Católica del Perú. Centro de Investigación en Geografía Aplicada, 2014. http://repositorio.pucp.edu.pe/index/handle/123456789/119875.

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This study aims to show the importance of Landslide Susceptibility Map as a tool for land use planning, prevention and risk mitigation. This will be shown through MM evaluation processes affecting high sector of El Paraíso gorge - Villa María del Triunfo (Lima - Peru).The work consisted of two phases: in the first one (field) the intrinsic characteristics of geology and geomorphology were identified. The second one, included the Landslide Susceptibility Map generation, using the multivariate Heuristic Model consisting of overlapping maps variables (Carrara et al. 1995, Lain et al. 2005), devel

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Leal, Pedro Carignato Basilio. "Mapeamento de perigo de escorregamento na bacia hidrográfica do Rio Grande de Ubatuba - Ubatuba (SP): comparação dos métodos analítico e sintético." Universidade de São Paulo, 2014. http://www.teses.usp.br/teses/disponiveis/8/8135/tde-11062015-155431/.

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O perigo geológico de escorregamentos é a probabilidade da ocorrência de eventos ou fenômenos desta natureza, induzidos ou não pela atividade humana que podem causar danos humanos, socioeconômicos e ambientais. A cartografia de perigos geológicos de escorregamentos é um importante instrumento para gestão dos territórios para Estados Nacionais, setor privado, ONGs, comunidades locais, organizações científicas, etc. O desenvolvimento da ciência e das técnicas fez surgir diversos métodos de avaliação de perigos de escorregamento. No presente trabalho, o método sintético e o método analítico foram

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Chu, Sheng Shin, and 朱聖心. "Seismic and Rainfall Landslide Hazard Maps with GIS." Thesis, 2001. http://ndltd.ncl.edu.tw/handle/56368445479371874363.

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碩士 國立臺灣大學 土木工程學研究所 89 Serious earthquakes and torrential rainfall often trigger landslides, which cause damages of lives and properties. Researches of landslides caused by earthquakes in Taiwan are frequently confined by unitary case. The areas and numbers of Landslides induced by a single earthquake are related to earthquake magnitude, the distance from earthquake epicenter etc. The above researches usually use the multi-variable analysis to figure out the weighting of the factors mentioned above. By these methods, the suspenseful potential maps of landslides caused by

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Sawyer, Derek Edward. "Failure mechanics, transport behavior, and morphology of submarine landslides." Thesis, 2010. http://hdl.handle.net/2152/ETD-UT-2010-12-2518.

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Submarine landslides retrogressively fail from intact material at the headwall and then become fluidized by strain weakening; the final deposits of these flows have low porosity, which controls their character in seismic reflection data. Submarine landslides occur on the open slope and also localized areas including margins of turbidite channel-levee systems. I develop and quantify this model with 3-D seismic reflection data, core and log data from Integrated Ocean Drilling Program Expedition 308 (Ursa Basin, Gulf of Mexico), flume experiments, and numerical modeling. At Ursa, multiple submari

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Livres sur le sujet "Landslide hazard maps"

Italy) Giornata di studio Lo stato di attuazione delle carte di rischio da frana per la difesa preventiva del territorio italiano dalle catastrofi naturali (2009 Milan. Giornata di studio Lo stato di attuazione delle carte di rischio da frana per la difesa preventiva del territorio italiano dalle catastrofi naturali: Milano, 3 dicembre 2009. GEAM, Associazione georisorse e ambiente, 2009.

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Kusky, Timothy M. Landslides: Mass wasting, soil, and mineral hazards. Facts on File, 2008.

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Willerich, Sebastian. Charakterisierung tiefgründiger Hangbewegungen vor dem Hintergrund der Gefahrenzonierung am Beispiel Algund/Südtirol. Verlag Dr. Friedrich Pfeil, 2013.

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K, Agrawal D., G. B. Pant Institute of Himalayan Environment & Development., International Centre for Integrated Mountain Development., and Workshop on "Perspectives of MRE in the Himalayan Region" (1997 : International Centre for Integrated Mountain Development), eds. Perspectives of mountain risk engineering in the Himalayan Region. Gyanodaya Prakashan, 1997.

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Peter, Jordan, Orban Julie, Forest Renewal BC, Forest Science Program (B.C.), and Forestry Continuing Studies Network, eds. Terrain stability and forest management in the interior of British Columbia: Workshop proceedings, May 23-25, 2001, Nelson, British Columbia, Canada. British Columbia Forest Science Program, 2002.

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Eric, Kramers R., Canada. Office of Critical Infrastructure Protection and Emergency Preparedness., Canada Environment Canada, and Canada Natural Resources Canada, eds. Natural hazards of Canada: A historical mapping of significant natural disasters. Government of Canada, 2001.

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1950-, Wilford David J., ed. Managing forested watersheds for hydrogeomorphic risks on fans. British Columbia, Ministry of Forests and Range, Forest Science Program, 2009.

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Wilford, David J. Forest management on fans: Hydrogeomorphic hazards and general prescriptions. British Columbia, Ministry of Forests, Forest Science Program, 2005.

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Mosher, David C. Submarine Mass Movements and Their Consequences. Springer Science+Business Media B.V., 2010.

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Landslide hazard mitigation in the Hindu Kush-Himalayas. International Centre for Integrated Mountain Development, 2001.

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Chapitres de livres sur le sujet "Landslide hazard maps"

Frodella, William, Daniele Spizzichino, Giacomo Lazzeri, Claudio Margottini, Veronica Tofani, and Nicola Casagli. "Assessing Landslide Hazard in the High City of Antananarivo, Madagascar (UNESCO Tentative Site)." In Progress in Landslide Research and Technology. Springer Nature Switzerland, 2023. http://dx.doi.org/10.1007/978-3-031-44296-4_21.

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AbstractBuilt on the hilltop of a granite ridge rising above the Ikopa River valley (the Analamanga Hill), the High City of Antananarivo (Madagascar) is renowned for its baroque-style palaces the Rova royal complex and gothic cathedrals dating back to the nineteenth Century, and therefore is part of the UNESCO Tentative List. Due to the frequent cyclonic heavy cyclonic rain, geological and geomorphological conditions, and a general lack of urban planning the study area is particularly prone to landslides (as shown by events of the winter of 2015, 2018 and 2019). As a first step towards underst

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Fujita, Kumiko. "Introducing Japanese Landslide Warning and Evacuation System to Sri Lanka: Field Survey of Social Aspect in the Arayanake Area." In Progress in Landslide Research and Technology, Volume 3 Issue 1, 2024. Springer Nature Switzerland, 2024. http://dx.doi.org/10.1007/978-3-031-55120-8_16.

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AbstractThe central highland in Sri Lanka has a landslide-prone geo-hydrological condition. In addition, Sri Lanka has extreme rainfalls in two monsoon seasons, and most of the landslides occur during two monsoon seasons. Landslides in the central highland had been isolated events. However, the area has been developed for agriculture and human settlements, a series of landslides occurred in the mid-1980s. Since the topography, such as mountains with steep slopes and weather, such as high precipitation, are similar in Japan and Sri Lanka, similar landslide phenomena have been seen. One of the c

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Nguyen, Chi Cong, Phuoc Vo, Viet Long Doan, Quang Binh Nguyen, Tien Cuong Nguyen, and Quoc Dinh Nguyen. "Assessment of the Effects of Rainfall Frequency on Landslide Susceptibility Mapping Using AHP Method: A Case Study for a Mountainous Region in Central Vietnam." In Progress in Landslide Research and Technology, Volume 1 Issue 2, 2022. Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-18471-0_7.

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AbstractVietnam’s mountainous regions often encounter landslides, frequently resulting in fatalities, infrastructure damage, and landscape destruction. A landslide susceptibility map is an effective tool for mitigating disaster impacts on hazard-prone areas. This study investigates the applicability of the Analytic Hierarchy Process to produce a landslide susceptibility index. Eight major impact factors are analyzed using SAGA, a GIS-based toolkit, including slopes, aspect, land use, soil type, elevation, distance to road, distance to stream, and antecedent rainfall. Four landslide susceptibil

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Karnawati, Dwikorita, Teuku Faisal Fathani, Wahyu Wilopo, and Budi Andayani. "TXT-tool 4.062-1.1: Community Hazard Maps for Landslide Risk Reduction." In Landslide Dynamics: ISDR-ICL Landslide Interactive Teaching Tools. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-57777-7_36.

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Lucà, Federica, Maria Vittoria Avolio, Donato D’Ambrosio, et al. "High Detailed Debris Flows Hazard Maps by a Cellular Automata Approach." In Landslide Science and Practice. Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-31319-6_93.

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Posch-Trözmüller, Gerlinde, and Richard Bäk. "Minimal Standards for Susceptibility and Hazard Maps of Landslides and Rock Falls." In Landslide Science and Practice. Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-31325-7_51.

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Wang, Yan, Wei Shan, Ying Guo, Chengcheng Zhang, and Shuai Liu. "Evaluation of Assessment Models for Landslide Susceptibility Mapping in Permafrost Areas." In Progress in Landslide Research and Technology, Volume 3 Issue 1, 2024. Springer Nature Switzerland, 2024. http://dx.doi.org/10.1007/978-3-031-55120-8_11.

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AbstractChina's permafrost regions are affected by global warming and the thawing of permafrost, and the occurrence of landslide disasters has become more and more frequent, which makes the evaluation of the susceptibility to geologic hazards in China's permafrost regions is an urgent work to be carried out. Most of the existing geohazard susceptibility models have fewer test cases in the permafrost regions. Twelve evaluation factors, such as altitude, slope, slope direction, land use, and lithology, were selected to draw landslide hazard susceptibility maps by using three commonly used landsl

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Cordero, Cathleen Joyce, Kenneth Gesmundo, and Arturo Daag. "Assessing and Contextualizing Site-Specific Landslide Risk in the Philippines." In Progress in Landslide Research and Technology. Springer Nature Switzerland, 2025. https://doi.org/10.1007/978-3-031-72736-8_12.

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AbstractAs an attempt to understand and reflect on the unique circumstances of communities in assessing landslide risk, the Dynaslope Project, under the Department of Science and Technology-Philippine Institute of Volcanology and Seismology (DOST-PHIVOLCS), conducts community landslide risk assessment (CLRA). It is a participatory process of assessing landslide hazards, exposure, vulnerabilities, and capacities of at-risk communities. CLRA includes hazard assessment, participatory community workshops, focus group discussions, and surveys. Risk components are assessed, and results are integrate

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Majidi, Reza Feijani, Mohammad Reza Mahdavifar, and Mohammad Kashanchi. "Estimating the Strength Parameters of Geological Formations Using Fuzzy Sets and its Application in Generating Seismic–Landslide Hazard Maps." In Earthquake-Induced Landslides. Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-32238-9_88.

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Legorreta-Paulín, Gabriel, Marcus Bursik, Lilia Arana-Salinas, and Miguel Medina-Jaen. "Assessing Landslide Distribution for Landform Hazard Zoning Purposes: A Case Study on the Western Flank of Iztaccíhuatl Volcano, Puebla, México." In Progress in Landslide Research and Technology, Volume 3 Issue 1, 2024. Springer Nature Switzerland, 2024. http://dx.doi.org/10.1007/978-3-031-55120-8_25.

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AbstractIn volcanic terrains, landslides are major natural hazard, posing risks to human settlements and economic activity. The characterization and analysis of landslide distribution is important in understanding their behavior in the landscape. The aim of this paper is to present results of the ongoing research project in the Institute of Geography at the National Autonomous University of Mexico (UNAM), to analyze the distribution of landslides, and characterize landforms that are prone to slope instability. For the Río Xopanac watershed on the western flank of Iztaccíhuatl volcano, landform

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Actes de conférences sur le sujet "Landslide hazard maps"

Ermini, Andrea, Riccardo Salvini, and Pier Simone Marrocchesi. "LANDSLIDE SUSCEPTIBILITY MAPPING IN LUNAR SOUTH POLE RIGION." In SGEM International Multidisciplinary Scientific GeoConference 24. STEF92 Technology, 2024. https://doi.org/10.5593/sgem2024/6.1/s28.65.

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The study addresses a challenge in planetary exploration, focusing on landslide susceptibility on the Lunar South Pole Region (LSPR), fundamental for future lunar missions. Features like permanently shadowed regions and water ice deposits attract scientific attention but issues related to rugged terrain and dynamic geological processes must also to be considered. The photointerpretation of data from Lunar Reconnaissance Orbiter (LRO) mission, allowed to create a landslides inventory map. The Frequency Ratio (FR) model was applied to generate a landslide susceptibility map (LSM). Geological and

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Singh, Ankit, Tarun Singh, and K. S. Rao. "Comparative Study of Machine Learning Vs. BIS Approach for Landslide Hazard Zonation in Kashmir Himalayas, India." In 57th U.S. Rock Mechanics/Geomechanics Symposium. ARMA, 2023. http://dx.doi.org/10.56952/arma-2023-0917.

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ABSTRACT Presently slope stability analysis and landslide hazard monitoring are the most challenging tasks in mountainous regions like the Himalayas. These events which were earlier considered as a process of attaining equilibrium in the topographic surface of the earth by nature, with the increase in population and onset of industrial revolution in the past few decades, changed the scenario of this natural phenomenon and transformed it into a disaster. The main reason for this is the utilization of inaccessible terrains for engineering mega projects and urbanization. Today, landslides are con

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Kati, Meyendris Walu, Meirliany Anjelina Leonora Eluama, and Frederika Rambu Ngana. "Landslide Mapping from the Cylcone Seroja in Kupang City Using Remote Sensing." In The 5th International Conference on Science and Technology Applications. Trans Tech Publications Ltd, 2024. http://dx.doi.org/10.4028/p-wi1ooc.

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On April 2-4, 2021, severe cyclone Seroja occurred in Kupang City, resulting in a landslide hazard. Landslide disaster management is essential for disaster mitigation. However, the susceptibility landslide map for the cyclone Seroja in Kupang City has not yet been done. In this paper, we map landslide locations using remote sensing. We used free remote sensing data. The data are Landsat 8 imagery, Digital Elevation Model (DEM), and rainfall. To create a landslide map in Kupang City, we overlaid three maps. Those are landcover, slope and rainfall maps. We created a landcover map using the Lands

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Depountis, Nikolaos, Zoe Misiri, and Katerina Kavoura. "Landslide susceptibility models at a regional scale. The case study of the Region of Epirus in Greece." In 4th European Regional Conference of IAEG. University of Zagreb Faculty of Civil Engineering, 2024. https://doi.org/10.5592/co/euroengeo.2024.199.

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The current study presents the results of a landslide susceptibility model applied in the Region of Epirus, Greece. Initially, a detailed archive of 286 active landslides was created for the research area. Furthermore, four basic landslide predisposing factors were selected, geology, slope angle, elevation and land use, as they contribute to the landslide susceptibility assessment. The susceptibility assessment was based on the analysis of the relationships between the above factors and the occurrences of landslides applying the Frequency Ratio (FR) prediction model. FR is a statistical model

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M, Dilsa, Greeshma G, S. P. Balasubramaniam, Sona Mary John, Alice Thoma, and Jainet Johny. "Impact of Threshold Rainfall on Landslides: A Case Study of Kerala." In Second International Conference in Civil Engineering for a Sustainable Planet. AIJR Publisher, 2025. https://doi.org/10.21467/proceedings.179.10.

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A major natural hazard, landslides can seriously endanger infrastructure, property, and human life, especially in areas like Kerala that have high rainfall and steep terrain. To improve landslide risk assessment and aid in the creation of early warning systems, this research intends to examine the connection between past landslide incidents and rainfall patterns throughout Kerala. The study aims to determine crucial rainfall thresholds that can serve as triggers for slope instability by comparing rainfall data from neighboring rain gauge stations with historical landslide events. The study use

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Bopche, Litesh, and Priti P. Rege. "Feature-Based Landslide Susceptibility and Hazard Zonation Maps using Fuzzy Overlay Analysis." In 2020 IEEE Pune Section International Conference (PuneCon). IEEE, 2020. http://dx.doi.org/10.1109/punecon50868.2020.9362469.

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Segoni, Samuele, Ascanio Rosi, Veronica Tofani, Filippo Catani, and Nicola Casagli. "Landslide hazard forecasting combining rainfall thresholds and susceptibility maps: from scientific to operational issues." In 4th Regional Symposium on Landslides in the Adriatic - Balkan Region. Društvo za geotehniku u Bosni i Hercegovini, 2019. http://dx.doi.org/10.35123/resylab_2019_16.

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Ye, R. Q., R. Q. Niu, Y. N. Zhao, Q. Y. Jiang, T. Wu, and Q. L. Deng. "Integration of LIDAR data and geological maps for landslide hazard assessment in the Three Gorges Reservoir area, China." In 2010 18th International Conference on Geoinformatics. IEEE, 2010. http://dx.doi.org/10.1109/geoinformatics.2010.5567616.

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R. M, Pooja Raj. "Building Design Techniques to Withstand Landslides." In The International Conference on scientific innovations in Science, Technology, and Management. International Journal of Advanced Trends in Engineering and Management, 2023. http://dx.doi.org/10.59544/nmur9181/ngcesi23p61.

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Landslides are among the many natural disasters causing massive destructions and loss of lives across the globe. India has a high degree of vulnerability towards the occurrence of Landslides. Landslides and avalanches are among the major hydro-geological hazards that affect large parts of India. Around 15% of the country’s region is prone to landslides. The Himalayas of Northwest and Northeast India and the Western Ghats are two regions of high vulnerability. Some major recent incidents are Kerala (2018), Himachal Pradesh (2018), Uttarakhand (2018), Tamenglong-Manipur (2018), and Kalikhola, Ma

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Hengesh, James V., Michael Angell, William R. Lettis, and Jeffery L. Bachhuber. "A Systematic Approach for Mitigating Geohazards in Pipeline Design and Construction." In 2004 International Pipeline Conference. ASMEDC, 2004. http://dx.doi.org/10.1115/ipc2004-0147.

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Pipeline projects are often faced with the challenge of balancing efficient design and construction with mitigation of potential hazards posed by low probability events, such as earthquakes and landslides. Though systematic characterization of geological hazards is sometimes perceived as an added project expense, failure to recognize and mitigate hazards at an early stage can lead to schedule delays and substantial liability, repair, and business interruption costs. For example, it is estimated that failure of the 660-mm Trans-Ecuador pipeline in the 1987 earthquake cost roughly $850 million i

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Rapports d'organisations sur le sujet "Landslide hazard maps"

Hults, Chad, Jeffrey Coe, and Nikita Avdievitch. Fractures, scarps, faults, and landslides mapped using LiDAR, Glacier Bay National Park and Preserve, Alaska. National Park Service, 2023. http://dx.doi.org/10.36967/2300706.

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This map of fractures, scarps, faults, and landslides was completed to identify areas in Glacier Bay National Park and Preserve that may present a landslide-generated tsunami hazard. To address the potential of landslide and tsunami hazards in the park, the National Park Service (NPS) and the US Geological Survey (USGS) partnered to conduct a multi-year hazard assessment of Glacier Bay National Park and Preserve. To produce the map described in this report, we used the newly acquired (2019-2020) light detection and ranging (LiDAR) 0.5 to 1.0 m digital elevation models (DEMs) that cover all the

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Bornaetxea, T., A. Blais-Stevens, and B. Miller. Landslide inventory map of the Valemount area, British Columbia. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/330911.

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Landslides are a recurring geomorphological process in high mountainous areas like Valemount (Canadian Rocky Mountains, British Columbia). The compilation of detailed information about the spatial distribution and characteristics of past landslides is essential for assessing future potential hazards. To provide baseline geoscience information to stakeholders and decision-makers, we carried out a landslide inventory that covers roughly 1200 km2. Using visual interpretation of aerial orthophotos, a digital elevation model of 5x5 meter resolution and satellite imagery, we compiled up to 1286 land

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Lanik, Amanda, Jason Rogers, and Ronald Karpilo. Lake Clark National Park and Preserve: Geologic resources inventory report. National Park Service, 2021. http://dx.doi.org/10.36967/nrr-2288490.

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Geologic Resources Inventory reports provide information and resources to help park managers make decisions for visitor safety, planning and protection of infrastructure, and preservation of natural and cultural resources. Information in GRI reports may also be useful for interpretation. This report synthesizes discussions from a scoping meeting held in 2005 and a follow-up conference call in 2018. Chapters of this report discuss the geologic setting and significance, geologic features and processes, and geologic resource management issues within Lake Clark National Park and Preserve. Informat

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Wilson, A. M., and M. C. Kelman. Assessing the relative threats from Canadian volcanoes. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328950.

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This report presents an analysis of the threat posed by active volcanoes in Canada and outlines directives to bring Canadian volcano monitoring and research into alignment with global best practices. We analyse 28 Canadian volcanoes in terms of their relative threat to people, aviation and infrastructure. The methodology we apply to assess volcanic threat was developed by the United States Geological Survey (USGS) as part of the 2005 National Volcano Early Warning System (NVEWS). Each volcano is scored on a number of hazard and exposure factors, producing an overall threat score. The overall t

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Wilson, A. M., and M. C. Kelman. Assessing the relative threats from Canadian volcanoes. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328950.

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Houck, Karen, Jay Temple, Kassandra Lindsey, Lauren Broes, and Daniel Miggins. OF-20-02 Geologic Map of the Agate Mountain Quadrangle, Park County, Colorado. Colorado Geological Survey, 2024. https://doi.org/10.58783/cgs.of2002.gfnp2602.

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The Agate Mountain quadrangle contains Proterozoic igneous and metamorphic rocks, Paleozoic sedimentary rocks, and Cenozoic volcanic and volcaniclastic rocks. Proterozoic rocks include granite, granitic gneiss, gabbro porphyry, pegmatite, mylonite, and microbreccia. Paleozoic sedimentary rocks include the Manitou Formation, Harding Sandstone, Fremont Formation, Dyer Dolomite, Leadville Limestone, Belden Formation, Minturn Formation, and Maroon Formation. Cenozoic volcanic and volcaniclastic rocks include Wall Mountain Tuff, Thirtynine Mile Andesite, volcanic breccias, trachybasalt, Tallahassee

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Morriss, Matthew C. Interim Geologic Map of the Blanding North Quadrangle, San Juan County, Utah. Utah Geological Survey, 2025. https://doi.org/10.34191/ofr-771dm.

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The Blanding North 7.5′ quadrangle is near the southeastern corner of Utah, centered in San Juan County. The quadrangle is within the Colorado Plateau physiographic province and the Blanding Basin sub-province (Fenneman and Johnson, 1946), and is on the south flank of the Abajo Mountains. The Abajo Mountains are cored by an Oligocene suite of laccoliths coeval with other mountain ranges across the plateau including: the Henry, La Sal, and Navajo Mountains of Utah; the Ute and La Plata Mountains of Colorado; and the Carrizo Mountains of Arizona (Witkind, 1964). The Abajo intrusive rocks are not

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Maps showing seismic landslide hazards in Anchorage, Alaska. US Geological Survey, 2014. http://dx.doi.org/10.3133/70058880.

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