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Triggering Factors of Landslides and Determination of Rainfall Threshold: A Case Study from North East India

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Landslide Science and Practice

Abstract

The North Eastern Region of India because of its relatively immature topography, fragile geologic base and active tectonics is vulnerable to landslide activities and the scenario is further accentuated due to various developmental activities. Almost one fifth of India’s landslide prone areas are located in this region. Guwahati, a major city in North East India is one such fast developing city that falls under medium to high category of the Global Landslide Susceptibility Map. The hills of the city have slopes between 15° and 25° where numbers of landslide affected sites are scattered. Almost 50 % of the soil samples analyzed from landslide affected sites showed low strength of the soils. Compared to the global threshold, Guwahati needs less intensity of rainfall (I = 28.7 D-0.890) for landsliding. Moreover, change in land use over a period of 30 years shows correlation between hill slope alteration and increment in landslide incidences.

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Acknowledgement

Thanks are due to Dr S Sudhakar, Director, North Eastern Space Applications Centre, Umiam, Meghalaya, India for allowing us to publish this paper. Thanks are also due to Dr. J.J. Laskar, Asst. Prof. Dept. of Geological Sciences, Gauhati University, India for his guidance during sample collection and geo-technical analysis.

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Correspondence to Kuntala Bhusan .

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Bhusan, K., Goswami, D.C. (2013). Triggering Factors of Landslides and Determination of Rainfall Threshold: A Case Study from North East India. In: Margottini, C., Canuti, P., Sassa, K. (eds) Landslide Science and Practice. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-31337-0_11

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