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Land slide A case of Malpa
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Oana Elena Colt
Maurizio Lazzari
Landslides – Disaster Risk Reduction
Giacomo Falorni
Mahesh Tripathi
In this work, a methodology for landslide hazard zonation mapping using GIS and remote sensing data and technology with their applications. The study has been carried out along NH-58 road corridor Nand Prayag to Badrinath in Garhwal Himalaya as this terrain is prone to the landslide hazards. This research work study has been made to derive and identify the important terrain factors and variables contributing to landslide occurrences in the region and corresponding thematic data layers are generated in GIS domain. These terrain data are collected from the topographic maps, satellite imageries, field visits and available published maps. Geodatabases are prepared by digitizing the maps and with satellite data (LISS-III & LISS-IV) along with tabular data Information value method the hazard zonation in terms of factor of importance for a given decision problem in terms of thematic parameters, categories and their normalized weights. Statistically integrating weightages from these thematic maps, a specific landslide hazard map was developed on a GIS platform and verified with field invetigations. The resulting landslide hazard zonation map delineates the area into different zones of six classes of landslide hazard zones like as, very high, high, medium and low. I. Introduction Landslide is among the major hydro-geological hazards that affect the large part of India; especially the Himalayas. Every year during intense rainfall periods, several incidences of landslides and related casualties are reported from different parts of the Rishikesh-Badrinath National highway 58, in the state of Uttarakhand, India. Remote sensing techniques have a vital and significant role in landslide and mapping. Prediction of landslide susceptibility of an area largely depends on spatial and temporal occurrence of landslides. Each landslides hazard study should start by making a landslide catalogue that is complete as possible in both time and space (Isben and Brundsen, 1996). Characterization of landslides requires three dimension perspectives which is possible by satellite images. Therefore, stereoscopic visual interpretation is stereo widely used for landslide monitoring, although it requires lot of expertise on image interpretation techniques (Guzzeti 2005). Landslides can be mapped in various ways using satellite images (Soeters et al. 1996), aerial photographs (Turner. and Schuster, 1996) and geomorphologic field mapping (Brunsden, 1993). Numbers of techniques have been introduced by many workers for extraction of landslide related information from satellite images and aerial photos which include feature extraction image extraction from high resolution satellite images, digital stereoscopic image interpretation, landslide change detection method (van Westen, 2005). On the basis of investigation it has been found that the landslides and its effects are major problem in study area. The problem under study is to assess the nature of lanslides and to determine specifically the extent of this type of disaster, in details through data generated from Indian Space Organization (ISRO) Department of Space and Geological Survey of India. The other main problem is to construct of road network which had easily collapsed by the tremor,
Miroslav Todorov , Mihail Todorov
Landslide processes are a distinct phenomenon with a huge impact on human way of life. Those gravitational movements in the upper layers of the crust can have a dramatic effect in river valleys, coastal regions and mountainous terrains. The reasons for their existence and development lie in naturally occurring processes in the lithosphere and the atmosphere and large-scale human activity. Investigating various natural and anthropogenic phenomena is vital, with attention to climate change processes. In the report of the European Commission (2012) an alarming level of erosion and abrasion is observed, with more than 630 000 areas with landslide processes. According to MRRB in Bulgaria there are near 2000 zones with active movements. The current investigation focuses on a fragment of the Bulgarian coast prone to landslide that was researched in 2017. The first registered movements date back to 2010. Characterizing for this case is the relatively quick developments of the movements which affect urban areas. This publication revolves around a complex engineering investigation, which provides an understanding how and why activation processes in the researched zone form, while using well-known proven methods. The used techniques for investigation focus on usability issues, as well as on the opportunity to corelate different sets of data, gather important information and reinforce it with monitoring. The focus here is on these three combined steps: information, prediction, monitoring.
WIT Transactions on The Built Environment
ch abdullah
Anuruddha Vijekumara
With the increase in impact of landslide disaster to the human life, the government of Sri Lanka took a decision to implement a landslide clearance process in identified landslide prone areas (presently known as landslide risk assessment process). This decision was implemented in March 2011 with the issuance of circular under the Ministry of Disaster Management. National Building Research Organisation (NBRO) was given the authority to issue the landslide clearance certificate for development/ construction in identified landslide prone areas of the country by this circular. Since, landslide disaster has highly impacted on human lives, mapping of landslide hazard areas was initiated in 1989 by NBRO. This landslide hazard zonation mapping project undertook mapping of hazard areas in 1:50,000 scale and 1:10,000 scale. 1:50,000 scale maps covering the entire districts of Matale, Kandy, Nuwara Eliya, Bdulla, Kegalle, Ratnapura and Kalutara are available for the use of planners, developers, decision makers , and general public. As, there are safe slopes areas available within the identified landslide prone districts; government of Sri Lanka took a decision to exempt the safe areas from landslide clearance process. With the implementation of this decision, NBRO was asked to distribute 1:50,000 landslide hazard zonation maps to local authorities, to use them as safe area identification tools. Although, local authorities were given these maps to identify safe areas , it is not clear that whether these maps are really suit for exempting safe areas. This study analyses data from landslide clearance process and landslide hazard maps, and discusses the suitability of landslide maps and finally gives recommendations to the issues identified.
Cees van Westen
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Malpa Rockfalls of 18 August 1998 in the Northeastern Kumaun Himalaya
- P. Pant , Khayingshing Luirei
- Published 1 October 1999
- Geology, Environmental Science
- Journal of The Geological Society of India
25 Citations
Hill slope instability of nainital city, kumaun lesser himalaya, uttarakhand, india, slope stability analysis of balia nala landslide, kumaun lesser himalaya, nainital, uttarakhand, india, landslides and neotectonic activities in the main boundary thrust (mbt) zone: southeastern kumaun, uttarakhand, a report on tectonically sculptured unique glacier landform: a case study from the tethys kumaun himalaya, india, landslides over two places of uttarakhand; an observation, glacial burst triggered by triangular wedge collapse: a study from trisul mountain near ronti glacier valley, tectonic footprints and landscape evaluation along kulur river valley, kumaun lesser himalaya, india, geomorphic characteristics of landscape development and formation of lakes in the zone of munsiari thrust, garhwal himalaya, uttarakhand, india, tectonic and structural controlled landslide: a case study of hardiya nala landslide, inner kumaun lesser himalaya (uttarakhand), india, impact of main boundary thrust (mbt) on landslide susceptibility in garhwal himalaya: a case study, related papers.
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Malpa, a village that has become synonymous with disaster
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- Neeraj Dahiya ORCID: orcid.org/0009-0008-0307-946X 1 , 2 ,
- Koushik Pandit 1 , 2 ,
- Shantanu Sarkar 3 &
- Anindya Pain 1 , 2
1 Altmetric
The mountainous regions of India are highly susceptible to rockfall due to several factors, including intense rainfall, seismic activity, and often due to extensive road cutting leading to significant terrain alteration. Such occurrences pose substantial risks to human life, property, and economic stability, underscoring the importance of strategic land-use planning to mitigate rockfall hazards. The Himalayan mountain roads are the most vulnerable ones to rockfall events in India; however, hilly roads in the Western Ghats and the Eastern Ghats are also prone to rockfall. In recent years, the frequency of these disasters in India has escalated, likely influenced by climate change and anthropogenic interventions. The roadways often pass through rock masses characterized by extremely jointed and steep rock slopes, particularly vulnerable to rockfall incidents. Unfortunately, engineers have often overlooked the significance of geological and geotechnical investigations before developing in hilly areas. To mitigate the risks associated with rockfall, a rockfall hazard study is an essential solution for stakeholders. Numerous researchers have developed different methodologies to assess rockfall hazards in India. Limited studies exist on specific rockfall hazard assessments in India due to the lack of past rockfall occurrence data. Hence, it becomes imperative to critically review the ongoing studies addressing rockfall hazards in various regions of India. The paper discusses major rockfall events and existing rockfall hazard assessment methodology in India and reviews research articles on rockfall hazards published up to 2023. It aims to gain insights into the techniques and methods researchers often utilize. This review highlights crucial points from different researchers, comprehensively analysing rockfall risks applicable to practitioners worldwide. This review is a valuable compendium of insights and methodologies for scholars investigating rockfall hazards, particularly in India’s mountainous regions.
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Acknowledgements
The authors would like to thank the Director, CSIR–Central Building Research Institute, Roorkee, for giving his kind permission to communicate this research work for publication. The first author acknowledges AcSIR (Ghaziabad, India) for providing the opportunity to carry out this doctoral research.
The authors declare that no funds were received for the research work carried out in the present study.
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Academy of Scientific and Innovative Research (AcSIR), Ghaziabad, 201 001, India
Neeraj Dahiya, Koushik Pandit & Anindya Pain
CSIR–Central Building Research Institute (CBRI), Roorkee, 247 667, India
Uttarakhand Landslide Mitigation and Management Center (ULMMC), Dehradun, 246001, India
Shantanu Sarkar
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Neeraj Dahiya involved in literature review, review methodology development, future research scope identification, manuscript writing. Koushik Pandit took part in review methodology conceptualization, manuscript preparation. Shantanu Sarkar involved in discussion and manuscript preparation. Anindya Pain took part in manuscript preparation and overall presentation.
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Dahiya, N., Pandit, K., Sarkar, S. et al. Various Aspects of Rockfall Hazards along the Mountain Roads in India: a Systematic Review. Indian Geotech J (2024). https://doi.org/10.1007/s40098-024-01015-3
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Received : 27 October 2023
Accepted : 20 June 2024
Published : 01 July 2024
DOI : https://doi.org/10.1007/s40098-024-01015-3
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unknown. The Malpa landslide was one of the worst landslides in India. On 18 August 1998 at 3.00 a.m., massive landslide wiped away the entire village of Malpa in the Pithoragarh district of Uttarakhand, then in Uttar Pradesh in Kali Valley of Higher Kumaon division of the Himalayas . The rockfall started on 16 August bringing down huge rocks ...
Land_slide_A_case_of_Malpa.ppt. The document provides information about a landslide that occurred in Malpa, Uttarakhand, India on August 18, 1998 that killed over 200 people. It summarizes the causes of the landslide as being prolonged heavy rainfall which decreased the stability of slopes composed of weak rocks and soils.
A devastating landslide on 18 August 1998 near Malpa Village in Kali Valley of Higher Kumaun Himalaya killed 221 persons. The landslide was a complex rock fall-debris flow. The mass movement ...
Land slide at Malpa, Uttarakhand Landslide Risk Management >The Malpa landslide tragedy brought the attention of the Central Government to the problem of landslides >3 national level task forces constituted by Dept. of Sc.& Tech. >Enactment of disaster management act in 2005,
The Malpa landslide occurred on 18 August 1998 after prolonged and concentrated precipitation for about a week. ... Landslide hazards: some case studies from the Satluj valley, Himachal Pradesh. Himalayan Geol., 17 (1996), pp. 193-207. Google Scholar. Bhandari and Gupta, 1985.
This research work study has been made to derive and identify the important terrain factors and variables contributing to landslide occurrences in the region and corresponding thematic data layers are generated in GIS domain. These terrain data are collected from the topographic maps, satellite imageries, field visits and available published maps.
Paul et al. conducted a study of a similar landslide that occurred on 18 August 1998 (monsoon period) in Malpa village, Kumaun Higher Himalaya region, along the Indo-Nepal border. It was a complex type of landslide (i.e., combination of rockfall and debris flow) triggered due to high precipitation (maximum 113 mm/day for the month of August ...
A devastating landslide on 18 August 1998 near Malpa Village in Kali Valley of Higher Kumaun Himalaya killed 221 persons. The landslide was a complex rock fall-debris flow. The mass movement generated around one million cubic metres of debris and partially blocked the Kali River, Malpa Gad (a tributary of Kali) being blocked completely. The ...
This paper presents the case history of Malpa rockfall of 18 August 1998, which has claimed a toll of 250 lives, including 60 pilgrims in transit camp, under the shadow of Malpa peak, 40 km north of Dharchula. The slope failure which caused the rockfall was aggravated by high angle of hillslope (78°), conducive conditions of bedrock, particularly enlarged joint space and proximity to the Main ...
A devastating landslide on 18 August 1998 near Malpa Village in Kali Valley of Higher Kumaun Himalaya killed 221 persons. The landslide was a complex rock fall-debris flow.
A massive landslide in Malpa, Uttarakhand in 1998 killed 210 people. Prolonged heavy rainfall from August 13-16 decreased slope stability, leading to rock falls and debris flows on August 17-18. The landslide wiped out the village of Malpa. It disrupted road networks and damaged public infrastructure like huts and buildings. An analysis of the costs found that over 65% was due to damage to ...
Malpa village is located almost 50 km away from Dharchula in Pithoragarh district. Malpa village became a name synonymous with disaster when a series of massive landslide struck the region, early in the morning of 18th August, 1998. It is a small stop on the route of Kailash Mansarovar yatra, situated between Gala and Bundi.
Malpa village, located almost 50 km away from Dharchula in Pithoragarh district became a name synonymous with disaster when on August 18, 1998 early in the morning, a series of massive landslides ...
A famous example is the catastrophic 1998 Malpa landslide that occurred along the drainage Malpa Gad. The landslide washed away the entire Malpa village killing >220 people, including number of tourists en route to Lake Mansarovar (Paul et al., 2000). ... (GIUH); implications for watershed management—a case study of the Varada River basin ...
A disastrous landslide in 1998 in the upper Kali valley near village Malpa is one such example. This landslide has washed away the entire Malpa village, killing > 220 people, ... (2017) Geomorphologic proxies for bedrock rivers: a case study from the Rwenzori Mountains, East African Rift system. Geomorphology 285:374-398. Google Scholar
The Malpa landslide of 1998 in India was one of the worst in the country's history. Prolonged heavy rainfall combined with steep slopes and tectonic plate activity caused a massive landslide that wiped out the entire village of Malpa, killing 221 people total. Over one million cubic meters of rock and debris were generated, blocking the nearby Kali River. Landscape architects have recommended ...
Download scientific diagram | Post-disaster view of Malpa Landslide from publication: Hazards in Himalaya 51-99 Pages from Proceeding-of-Botany | | ResearchGate, the professional network for ...
During the initial period, the major landslide took place in Malpa in Sept, 1998 along the Kali River (district Pithoragarh, Uttarakhand) which is also a prominent route for the Indian pilgrimage visiting the holy shrine in Mansarovar, China. Afterwards this area was studied. In this study efforts were made to map the landslide prone areas ...
The geological factors are often considered for the Landslide Hazard Zonation (LHZ), as they play a dominant role in the prognosis of landslide. PROJECT AREA (ROUTES) The study area for this project is the pilgrim / tourist routes of Uttaranchal and H.P. Himalayas. A total of 20 km buffer, i.e. 10 km on either side of the road keeping ridge
Malin Landslide : A Case study - Download as a PDF or view online for free. ... The 1998 Malpa landslide in Uttarakhand, India killed over 200 people after heavy rains caused a massive rock fall. Proper land use planning, drainage, afforestation, and early warning systems can help reduce landslide risks. Landslide disaster management.
The study was carried out in the Inner Lesser Himalaya along the Karnprayag-Gwaldam-Jauljibi state highway near Thal (town) district Pithoragarh, Uttarakhand (India). This highway is of significance as it connects the interior part of the Kumaun region to other parts of the state. In the past, several landslides have occurred along Hardiya Nala, damaging the road and highway bridge, and even ...
1. Introduction. Landslide is a common natural disaster often in hilly terrain, which causes huge loss of natural resources and human life (Ering & Babu, Citation 2016).It is mainly attributed by natural factors, such as earthquakes and rainfall occurred on these regions (Collins & Znidarcic, Citation 2004; Rahardjo, Li, Toll, & Leong, Citation 2001).A sudden downward movement of the ...
Landslide susceptibility zonation (LSZ) is necessary for disaster management and planning development activities in mountainous regions. A number of methods, viz. landslide distribution, qualitative, statistical and distribution-free analyses have been used for the LSZ studies and they are again briefly reviewed here. In this work, two methods, the Information Value (InfoVal) and the Landslide ...
The mountainous regions of India are highly susceptible to rockfall due to several factors, including intense rainfall, seismic activity, and often due to extensive road cutting leading to significant terrain alteration. Such occurrences pose substantial risks to human life, property, and economic stability, underscoring the importance of strategic land-use planning to mitigate rockfall ...