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- Arindam Guha
- E. N. Dhananjaya Rao
- Reshma Parveen
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- A. Mohan Vamsee
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- Sumit Pathak
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Journals
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Vinod Kumar, K.
- An Image Processing Approach for Converging ASTER-Derived Spectral Maps for Mapping Kolhan Limestone, Jharkhand, India
Abstract Views :186 |
PDF Views:51
Authors
Affiliations
1 National Remote Sensing Centre, Balanagar, Hyderabad 500 625, IN
2 Andhra University, Visakhapatnam 530 003, IN
3 Jharkhand Space Application Centre, Ranchi 834 004, IN
1 National Remote Sensing Centre, Balanagar, Hyderabad 500 625, IN
2 Andhra University, Visakhapatnam 530 003, IN
3 Jharkhand Space Application Centre, Ranchi 834 004, IN
Source
Current Science, Vol 106, No 1 (2014), Pagination: 40-49Abstract
In the present study, we have attempted the delineation of limestone using different spectral mapping algorithms in ASTER data. Each spectral mapping algorithm derives limestone exposure map independently. Although these spectral maps are broadly similar to each other, they are also different at places in terms of spatial disposition of limestone pixels. Therefore, an attempt is made to integrate the results of these spectral maps to derive an integrated map using minimum noise fraction (MNF) method. The first MNF image is the result of two cascaded principal component methods suitable for preserving complementary information derived from each spectral map. While implementing MNF, noise or non-coherent pixels occurring within a homogeneous patch of limestone are removed first using shift difference method, before attempting principal component analysis on input spectral maps for deriving composite spectral map of limestone exposures. The limestone exposure map is further validated based on spectral data and ancillary geological data.Keywords
Limestone, Minimum Noise Fraction, Spectral Mapping, Image Processing.- Assessment of the Sunkoshi (Nepal) Landslide Using Multitemporal Satellite Images
Abstract Views :244 |
PDF Views:61
Authors
Affiliations
1 Geosciences Group, National Remote Sensing Centre, Indian Space Research Organisation, Hyderabad 500 037, IN
1 Geosciences Group, National Remote Sensing Centre, Indian Space Research Organisation, Hyderabad 500 037, IN
Source
Current Science, Vol 107, No 12 (2014), Pagination: 1961-1964Abstract
No Abstract.- A Bird's-Eye View of Landslide Dammed Lakes in Zanskar Himalaya, India
Abstract Views :351 |
PDF Views:26
Authors
Affiliations
1 Geosciences Group, Remote Sensing Applications Area, National Remote Sensing Centre, Indian Space Research Organisation, Balanagar, Hyderabad 500 037, IN
1 Geosciences Group, Remote Sensing Applications Area, National Remote Sensing Centre, Indian Space Research Organisation, Balanagar, Hyderabad 500 037, IN
Source
Current Science, Vol 112, No 06 (2017), Pagination: 1109-1112Abstract
The landslide lakes or dams are temporary lakes in the river valleys formed by landslide debris. Landslide dammed lakes and their outburst floods (LLOFs) are not uncommon in the Indian Himalaya. Breaching of such temporary lakes with huge amount of accumulated water and sediments can create devastating floods in the downstream areas.References
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- Cui, P., Zhu, Y. Y., Han, Y. S., Chen, X. Q. and Zhuang, J. Q., Landslides, 2009, 6(3), 209–223.
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- http://en.wikipedia.org/wiki/Attabad_ Lake (accessed on 10 May 2016).
- http://en.wikipedia.org/wiki/2014_Sunkoshi_ blockage (accessed on 10 May 2016).
- Korup, O., Prog. Phys. Geogr., 2002, 26(2), 206–235.
- Schuster, R. L. and Costa, J. E., In Landslide Dams: Processes, Risk, and Mitigation. In Proceedings of a Session in Conjunction with the ASCE Convention, 1986, pp. 1–20.
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- Martha, T. R., Govindharaj, K. B. and Kumar, K. V., Geosci. Front., 2015, 6(6), 793–805.
- Martha, T. R. and Kumar, K. V., Landslides, 2013, 10(4), 469–479.
- Weidinger, J. T., In Natural and Artificial Rockslide Dams, Springer-Verlag, Berlin, Heidelberg, 2011, pp. 243–277.
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- Assessment of the Valley-Blocking ‘So Bhir’ Landslide near Mantam Village, North Sikkim, India, Using Satellite Images
Abstract Views :199 |
PDF Views:32
Authors
Affiliations
1 Geosciences Group, National Remote Sensing Centre, Indian Space Research Organisation, Hyderabad 500 037, IN
1 Geosciences Group, National Remote Sensing Centre, Indian Space Research Organisation, Hyderabad 500 037, IN
Source
Current Science, Vol 113, No 07 (2017), Pagination: 1228-1229Abstract
A massive landslide occurred near Mantam village (opposite the Passingdang– Mantam Road) in Sikkim, India around 13:30 h (IST) on 13 August 2016 (Figure 1 a). The location (at the centre of the zone of depletion) of the landslide was 27°32'22.92"N and 88°30'2.47"E. According to the news reports, formation of a lake and consequent rise in water level had submerged the bridge over Kanaka river and washed away about 300 m stretch of the road. Five houses in Mantam village were also submerged. The villages of Tingvong, Lingdem, Laven, Kayeem, Lingzya, Bay, Sakyong Pentong and Ruklu Kayeem were cut-off due to damage to the connecting road. However, there were no human deaths reported due to the incident.References
- Mantovani, F., Soeters, R. and van Westen, C. J., Geomorphology, 1996, 15(3–4), 213–225.
- Huang, R. and Fan, X., Nature Geosci., 2013, 6, 325–326.
- Martha, T. R., Roy, P., Mazumdar, R., Govindharaj, K. B. and Vinod Kumar, K., Landslides, 2017, 14(2), 697–704.
- Martha, T. R., Govindharaj, K. B. and Vinod Kumar, K., Geosci. Front., 2015, 6, 793–805.
- GSI, Seismotectonic Atlas of India, 2000.
- Ravi Kumar, M., Hazarika, P., Srihari Prasad, G., Singh, A. and Saha, S., Curr. Sci., 2012, 102, 788–792
- Ghosh, S., Chakraborty, I., Bhattacharya, D., Bora, A. and Kumar, A., Indian J. Geosci., 2012, 66, 27–38.
- Roy, P., Martha, T. R. and Vinod Kumar, K., Curr. Sci., 2014, 107(12), 1961–1964.
- Martha, T. R. et al., Landslides, 2017, 14(1), 373–383.
- Detection of Coastal Landforms in a Deltaic Area Using a Multi-Scale Object-Based Classification Method
Abstract Views :135 |
PDF Views:34
Authors
Affiliations
1 Geosciences Group, National Remote Sensing Centre, Indian Space Research Organization, Hyderabad 500 037, IN
2 Department of Geo-Engineering, Andhra University College of Engineering (A), Vishakhapatnam 530 003, IN
3 Department of Physical Sciences, Mahatma Gandhi Chitrakoot Gramodaya Vishwavidyalaya, Chitrakoot 485 780, IN
1 Geosciences Group, National Remote Sensing Centre, Indian Space Research Organization, Hyderabad 500 037, IN
2 Department of Geo-Engineering, Andhra University College of Engineering (A), Vishakhapatnam 530 003, IN
3 Department of Physical Sciences, Mahatma Gandhi Chitrakoot Gramodaya Vishwavidyalaya, Chitrakoot 485 780, IN
Source
Current Science, Vol 114, No 06 (2018), Pagination: 1338-1345Abstract
Coastal landforms play an important role in protecting deltaic areas from erosion due to the action of waves. However, landforms in the deltas are dynamic and vulnerable to changes due to the effect of natural disasters like floods and cyclones. Automatic detection of dynamic landforms from satellite data can provide important inputs for effective coastal zone management. In this study, we developed an Object-Based Image Analysis (OBIA) technique to identify and map landforms in the Krishna delta, east coast of India using Resourcesat-2 LISS-IV multispectral image (5.8 m) and digital elevation model (DEM) (4 m). Since landforms are represented at multiple scales, the plateau objective function method was used to select appropriate scales during multiresolution segmentation. Knowledge-based rules in OBIA, using the parameters tone, texture, shape and context derived from satellite images and height from DEM were developed for classification of landforms. A total of 11 landforms (beach, beach ridge, swale, tidal creek, marsh, spit, barrier bar, mangrove, natural levee, channel island and channel bar) were mapped using this approach. High detection accuracy of these landforms indicates that the method developed has the potential for geomorphological mapping of dynamic landforms in low lying deltaic areas.Keywords
Beach, Cyclone, DEM, Image Segmentation, Mangrove, OBIA, Resourcesat-2.References
- SAC (ISRO), Coastal Zones of India, Space Applications Centre (ISRO), Ahmedabad, India, 2012; http://sac.gov.in
- Nageswara Rao, K., Evolution and dynamics of the Krishna Delta, India. Natl. Geograph. J. India, 1985, 31, 1–9.
- Prabaharan, S., Srinivasa Raju, K., Lakshumanan, C. and Ramalingam, M., Remote sensing and GIS applications on change detection study in coastal zone using multi temporal satellite data. Int. J. Geomatics Geosci., 2010, 1, 2.
- Saranathan, E., Chandrasekaran, R., Soosai Manickaraj, D. and Kannan, M., Shoreline changes in Tharangampadi village, Nagapattinam district, Tamil Nadu, India – a case study. J. Indian Soc. Remote Sensing, 2011, 39, 107–115.
- Bishop, M. P., Shroder, J. J. F. and Colby, J. D., Remote sensing and geomorphometry for studying relief production in high mountains. Geomorphology, 2003, 55(1–4), 345–361.
- Iwahashi, J. and Pike, R. J., Automated classifications of topography from DEMs by an unsupervised nested-means algorithm and a three-part geometric signature. Geomorphology, 2007, 86(3–4), 409–440.
- Smith, M. J. and Pain, C. F., Applications of remote sensing in geomorphology. Progress Phys. Geography, 2009, 33(4), 568–582.
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- Shroder Jr, J. F. and Bishop, M. P., A perspective on computer modeling and fieldwork. Geomorphology, 2003, 53, 1–9.
- Martha, T. R., Sharma, A. and Vinod Kumar, K., Development of meander cutoffs – a multi-temporal satellite-based observation in parts of Sindh River, Madhya Pradesh, India. Arabian J. Geosci., 2015, 8(8), 5663–5668.
- Martha, T. R., Ghosh, D., Vinod Kumar, K., Lesslie, A. and Ravi Kumar, M. V., Geospatial technologies for national geomorphology and lineament mapping project – a case study of Goa state. J. Indian Soc. Remote Sensing, 2013, 41, 905–920.
- Xiaojun, Y., Damen, M. C. J. and Van Zuidam, R. A., Use of thematic mapper imagery with a geographic information system for geomorphologic mapping in a large deltaic lowland environment. Int. J. Remote Sensing, 1999, 20(4), 659–681.
- Dragut, L. and Blaschke, T., Automated classification of landform elements using object-based image analysis. Geomorphology, 2006, 81(3/4), 330–344.
- van Asselen, S. and Seijmonsbergen, A. C., Expert-driven semiautomated geomorphological mapping for a mountainous area using a laser DTM. Geomorphology, 2006, 78(3–4), 309–320.
- Schneevoigt, N. J., van der Linden, S., Thamm, H. P. and Schrott, L., Detecting Alpine landforms from remotely sensed imagery – A pilot study in the Bavarian Alps. Geomorphology, 2008, 93(1–2), 104–119.
- Dragut, L. and Eisank, C., Automated object-based classification of topography from SRTM data. Geomorphology, 2012, 142/141, 21–33.
- Hay, G. J. and Castilla, G., Object-based image analysis: Strengths, weaknesses, opportunities and threats (SWOT). In Proceedings OBIA, Commission VI, WG VI/4, Calgary, CA, 2006.
- Myint, S. W., Gober, P., Brazel, A., Grossman-Clarke, S. and Weng. Q., Per-pixel vs object-based classification of urban land cover extraction using high spatial resolution imagery. Remote Sensing Environ., 2011, 115, 1145–1161.
- Babu, P. V. L. P., Morphological evolution of the Krishna delta. Photonirvachak, 1975, 3, 21–27.
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- Baatz, M. and Schäpe, A., Multiresolution Segmentation: an optimization approach for high quality multi-scale image segmentation. In Angewandte Geographische Informationsveraarbeitung XII, Beitrage zum AGIT Symposium Salzburg (eds Strobl, L. J., Blaschke, T. and Griesebener, T.), Herbert Wichmann Verlag, Heidelberg, 2000, pp. 12–23.
- Martha, T. R., Kerle, N., Jetten, V., van Westen, C. J. and Vinod Kumar, K., Characterizing spectral, spatial and morphometric properties of landslides for automatic detection using object-oriented methods. Geomorphology, 2010, 116(1–2), 24–36.
- Vamshi, G. T., Martha, T. R. and Vinod Kumar, K., An object-based classification method for automatic detection of lunar impact craters from topographic data. Adv. Space Res., 2016, 57, 1978–1988.
- Martha, T. R., Kerle, N., van Westen, C. J., Jetten, V. and Vinod Kumar, K., Segment optimisation and data-driven thresholding for knowledge-based landslide detection by object-based image analysis. IEEE Trans. Geosci. Remote Sensing, 2011, 49(12), 4928–4943.
- GSI, ISRO, Manual for National Geomorphological and Lineament Mapping on 1 : 50,000 scale. A Project under National (Natural) Resources Census (NRC), 2010.
- Shufelt, J. A., Performance evaluation and analysis of monocular building extraction from aerial imagery. IEEE Trans. Pattern Anal. Mach. Intell., 1999, 21(4), 311–326.
- Spectral Response of Few Important Textural Variants of Chromitite and its Potential in Estimating Relative Grades of Chromitite – A Case Study for Chromitite of Nuggihalli Schist Belt, India
Abstract Views :157 |
PDF Views:30
Authors
Affiliations
1 Geosciences Group, National Remote Sensing Centre, Indian Space Research Organization, Balanagar, Hyderabad 500 625, IN
2 Department of Geology, University of Calcutta, 35 Ballygunge Circular Road, Kolkata 700 019, IN
1 Geosciences Group, National Remote Sensing Centre, Indian Space Research Organization, Balanagar, Hyderabad 500 625, IN
2 Department of Geology, University of Calcutta, 35 Ballygunge Circular Road, Kolkata 700 019, IN
Source
Current Science, Vol 114, No 08 (2018), Pagination: 1721-1731Abstract
We have collected, processed and analysed the reflectance spectra of representative chromitite samples of spot type, clot type and disseminated type textural variants to understand the diagnostic spectral features of each of these samples. We have found that the reflectance spectrum of each textural variant is distinct from the spectra of other variants despite having few common absorption features. Spectral features of chromitite samples are governed by the spectra of two dominant minerals, chromite and chlorite. Spectral features of chromitite at 550 nm and 1100 nm are governed by electronic transition process in Fe3+ and crystal field effect in Fe2+ ions present in chromite structure respectively. On the other hand, spectral features at 1400 nm, 1900 nm and 2300 nm are related to the vibration of O–H, H–OH and metal hydroxide bonds in chlorite. Amongst these features, the spectral feature at 1100 nm (due to Fe2+ in chromite grains) is common to all three major textural varieties of chromitite samples studied here. Electron probe micro analysis (EPMA) data of chromite and chlorite grains of each texture are used to relate the presence and abundance of Fe2+ (in chromite grains) with absorption feature. Width of the 1100 nm feature has a correlation value 0.95, while depth of the same feature has a correlation value 0.94 with the abundance of chromite mineral estimated using modal analysis of chromite samples. Therefore, spectrometric parameter of 1100 nm spectral feature of chromitite can be used as proxy for estimating modal abundance of chromite in chromitite samples after estimating deposit specific correlation coefficient.Keywords
Chromitite, Electronic Processes, Modal Analysis, Spectral Feature, Texture, Vibrational Processes.References
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- Reactivation of Minor Scars to Major Landslides–A Satellite-Based Analysis of Kotropi Landslide (13 August 2017) In Himachal Pradesh, India
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PDF Views:32
Authors
Affiliations
1 Geosciences Group, National Remote Sensing Centre, Indian Space Research Organisation, Hyderabad - 500 037, IN
1 Geosciences Group, National Remote Sensing Centre, Indian Space Research Organisation, Hyderabad - 500 037, IN
Source
Current Science, Vol 115, No 3 (2018), Pagination: 395-398Abstract
On 13 August 2017, a massive landslide occurred close to the village of Kotropi (near Kotropi bus stop) in Mandi district, Himachal Pradesh, India. It occurred on National Highway 154, the road between Mandi and Pathankot. Media reports suggest that a section of the slope totally collapsed and two buses of the Himachal State Transport Corporation along with few other vehicles were buried under the debris. News reports also suggest that there have been 46 fatalities from the incident. Around 300 m of the highway has been completely buried under debris, thus disrupting communication on an important route1.References
- www.indiatoday.in
- Martha, T. R. et al., Landslides, 2015, 12(1), 135–146.
- Martha, T. R. et al., Landslides, 2017, 14(2), 697–704.
- Martha, T. R. et al., Landslides, 2017, 14(1), 373–383.
- Roy, P., Martha, T. R. and Vinod Kumar, K., Curr. Sci., 2014, 107(12), 1961– 1964.
- https://employee.gsi.gov.in/cs/groups/public/documents/document/b3zp/mtyx/~edisp/dcport1gsigovi161798.pdf
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- Martha, T. R., Roy, P. and Vinod Kumar, K., Curr. Sci., 2017, 113(7), 1228–1229.
- Landslides Mapped using Satellite Data in the Western Ghats of India After Excess Rainfall During August 2018
Abstract Views :199 |
PDF Views:31
Authors
Affiliations
1 Geosciences Group, National Remote Sensing Centre, Indian Space Research Organisation, Hyderabad 500 037, IN
1 Geosciences Group, National Remote Sensing Centre, Indian Space Research Organisation, Hyderabad 500 037, IN
Source
Current Science, Vol 117, No 5 (2019), Pagination: 804-812Abstract
Excess rainfall during August 2018 triggered numerous landslides in the Western Ghats region of India covering the states of Kerala, Karnataka and Tamil Nadu. These landslides caused widespread damage to property, loss of life and adversely affected various land resources. In this article, we present an inventory of landslide prepared from the analysis of multitemporal high-resolution images acquired before and after the rainfall event from Resourcesat-2, WorldView-2, GF-2, SPOT-6 and 7, Pleiades-1, Kompsat-3 and Sentinel-2 Earth observation satellites. A total of 6970 landslides with a cumulative area of 22.6 sq. km were mapped for this rainfall event. Majority of landslides have occurred in Kerala (5191), followed by Karnataka (993) and Tamil Nadu (606). Landslides are mostly debris slide and debris flow type with entrainment along the channels. Results show that landslides (83.2%) are triggered by very high rainfall. Also, very high rainfall has resulted in 14.9% of landslides even though slopes are moderate, mainly in the Kodagu district of Karnataka.Keywords
Debris Flows, Disaster Response, Excess Rainfall, Landslides, Satellite Data.References
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- Potential of Airborne Hyperspectral Data for Geo-Exploration over Parts of Different Geological/Metallogenic Provinces in India based on AVIRIS-NG Observations
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Authors
Satadru Bhattacharya
1,
Hrishikesh Kumar
1,
Arindam Guha
2,
Aditya K. Dagar
1,
Sumit Pathak
1,
Komal Rani (Pasricha)
2,
S. Mondal
3,
K. Vinod Kumar
2,
William Farrand
4,
Snehamoy Chatterjee
5,
S. Ravi
6,
A. K. Sharma
1,
A. S. Rajawat
1
Affiliations
1 Space Applications Centre, Indian Space Research Organisation, Ahmedabad 380 015, IN
2 National Remote Sensing Centre, Indian Space Research Organisation, Hyderabad 500 042, IN
3 Department of Geophysics, Indian Institute of Technology (ISM), Dhanbad 826 004, IN
4 Space Science Institute, Boulder, Colorado 80301, US
5 Department of Geological and Mining Engineering and Sciences, Michigan Technological University, Houghton, Michigan 49931, US
6 Geological Survey of India Training Institute, Bandlaguda, Hyderabad 500 068, US
1 Space Applications Centre, Indian Space Research Organisation, Ahmedabad 380 015, IN
2 National Remote Sensing Centre, Indian Space Research Organisation, Hyderabad 500 042, IN
3 Department of Geophysics, Indian Institute of Technology (ISM), Dhanbad 826 004, IN
4 Space Science Institute, Boulder, Colorado 80301, US
5 Department of Geological and Mining Engineering and Sciences, Michigan Technological University, Houghton, Michigan 49931, US
6 Geological Survey of India Training Institute, Bandlaguda, Hyderabad 500 068, US
Source
Current Science, Vol 116, No 7 (2019), Pagination: 1143-1156Abstract
In this article, we discuss the potential of airborne hyperspectral data in mapping host rocks of mineral deposits and surface signatures of mineralization using AVIRIS-NG data of a few important geological provinces in India. We present the initial results from the study sites covering parts of northwest India, as well as the Sittampundi Layered Complex (SLC) of Tamil Nadu and the Wajrakarur Kimberlite Field (WKF) of Andhra Pradesh from southern India. Modified spectral summary parameters, originally designed for MRO-CRISM data analysis, have been implemented on AVIRIS-NG mosaic of Jahazpur, Rajasthan for the automatic detection of phyllosilicates, carbonates and Fe–Mg-silicates. Spectral analysis over Ambaji and the surrounding areas indicates the presence of calcite across much of the study area with kaolinite occurring as well in the north and east of the study area. The deepest absorption features at around 2.20 and 2.32 μm and integrated band depth were used to identify and map the spatial distribution of phyllosilicates and carbonates. Suitable thresholds of band depths were applied to map prospective zones for marble exploration. The data over SLC showed potential of AVIRIS-NG hyperspectral data in detecting mafic cumulates and chromitites. We also have demonstrated the potential of AVIRIS-NG data in detecting kimberlite pipe exposures in parts of WKF.Keywords
Data, Geological Provinces, Host Rocks, Hyperspectral, Mineral Deposits.References
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- Regional Liquefaction Susceptibility Mapping in the Himalayas using Geospatial Data and AHP Technique
Abstract Views :165 |
PDF Views:36
Authors
Affiliations
1 Geosciences Group, National Remote Sensing Centre, Indian Space Research Organisation, Hyderabad 500 037, IN
2 Department of Geophysics, College of Science and Technology, Andhra University, Visakhapatnam 530 003, IN
1 Geosciences Group, National Remote Sensing Centre, Indian Space Research Organisation, Hyderabad 500 037, IN
2 Department of Geophysics, College of Science and Technology, Andhra University, Visakhapatnam 530 003, IN
Source
Current Science, Vol 116, No 11 (2019), Pagination: 1868-1877Abstract
Liquefaction susceptibility (LS) assessment is a necessary input for seismic zonation studies. LS can be done using geospatial models by integration of thematic layers. In this study, we have used analytical hierarchy process for integration of thematic layers (e.g. water table depth, peak horizontal acceleration, etc.) to generate a regional LS map for Uttarakhand and Himachal Pradesh in India. The final map was classified as liquefaction-likely, liquefaction-possible and liquefaction-not-likely zones. Results show Doon valley and Himalayan foothills are more prone to LS than the higher Himalayas.Keywords
Analytical Hierarchy Process, Earthquakes, Geospatial Data, Liquefaction Susceptibility.References
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