Landslides and human interference in Darjiling Himalayas, India

Landslides are among the nature's primarily ways of adjustment to slope stability. In Darjiling Himalayas the process has been intensified by human interference mainly through rapid deforestation, incorrect construction procedure and unplanned tapping of natural resources. The present paper ai...

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Main Author: Sunil Kumar DE
Format: Article
Language:English
Published: Romanian Association of Geomorphologists 2017-12-01
Series:Revista de Geomorfologie
Subjects:
Online Access:http://revistadegeomorfologie.ro/geo/index.php/revista/article/view/8
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spelling doaj-9a3321c4b94149f9b84fe35bd44751982021-02-02T14:00:57ZengRomanian Association of GeomorphologistsRevista de Geomorfologie1453-50682285-67732017-12-0119110.21094/rg.2017.014Landslides and human interference in Darjiling Himalayas, IndiaSunil Kumar DE0Department of Geography, North Eastern Hill University, Meghalaya, India Landslides are among the nature's primarily ways of adjustment to slope stability. In Darjiling Himalayas the process has been intensified by human interference mainly through rapid deforestation, incorrect construction procedure and unplanned tapping of natural resources. The present paper aims at investigating the occurrence of landslides mainly due to human intervention. For analyzing the acuteness of the problem, important events of landslides over time, landslide susceptibility map using traditional check-list and investigation of the nature of human intervention for landslide occurrences have been carried out. From the study it is found that extreme rainfall events of consecutive days accumulating an amount of 1000 to 1200 mm, coupled with deep weathering in susceptible structure could trigger to 5 to 10 m-thick landslides. Being saturated with percolating rainwater, such slopes even with a rainfall 50 of mm/h would cause disastrous landsllides. Common occurrence of landslides is found along the springs, where thick debris is removed along the slope, ontop of the bedrock.. Generally deforested urbanized tracts, illegal coal mining sites, tea gardens, artillery roads connecting hills with the plains are the most susceptible areas to sliding. http://revistadegeomorfologie.ro/geo/index.php/revista/article/view/8Slope stabilitydeforestationincorrect constructionstructural elementsjoints and shear plane
collection DOAJ
language English
format Article
sources DOAJ
author Sunil Kumar DE
spellingShingle Sunil Kumar DE
Landslides and human interference in Darjiling Himalayas, India
Revista de Geomorfologie
Slope stability
deforestation
incorrect construction
structural elements
joints and shear plane
author_facet Sunil Kumar DE
author_sort Sunil Kumar DE
title Landslides and human interference in Darjiling Himalayas, India
title_short Landslides and human interference in Darjiling Himalayas, India
title_full Landslides and human interference in Darjiling Himalayas, India
title_fullStr Landslides and human interference in Darjiling Himalayas, India
title_full_unstemmed Landslides and human interference in Darjiling Himalayas, India
title_sort landslides and human interference in darjiling himalayas, india
publisher Romanian Association of Geomorphologists
series Revista de Geomorfologie
issn 1453-5068
2285-6773
publishDate 2017-12-01
description Landslides are among the nature's primarily ways of adjustment to slope stability. In Darjiling Himalayas the process has been intensified by human interference mainly through rapid deforestation, incorrect construction procedure and unplanned tapping of natural resources. The present paper aims at investigating the occurrence of landslides mainly due to human intervention. For analyzing the acuteness of the problem, important events of landslides over time, landslide susceptibility map using traditional check-list and investigation of the nature of human intervention for landslide occurrences have been carried out. From the study it is found that extreme rainfall events of consecutive days accumulating an amount of 1000 to 1200 mm, coupled with deep weathering in susceptible structure could trigger to 5 to 10 m-thick landslides. Being saturated with percolating rainwater, such slopes even with a rainfall 50 of mm/h would cause disastrous landsllides. Common occurrence of landslides is found along the springs, where thick debris is removed along the slope, ontop of the bedrock.. Generally deforested urbanized tracts, illegal coal mining sites, tea gardens, artillery roads connecting hills with the plains are the most susceptible areas to sliding.
topic Slope stability
deforestation
incorrect construction
structural elements
joints and shear plane
url http://revistadegeomorfologie.ro/geo/index.php/revista/article/view/8
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