Skip to main content

Advertisement

Log in

Environmental geoinformaicts of fast growing Himalaya’s foothill towns and surrounding: concept and implementation

  • Research Article
  • Published:
Earth Science Informatics Aims and scope Submit manuscript

Abstract

Himalaya foothill zone have fragile geo-environment due to active tectonics and dynamic hydrological process and its associated reshaped geomorphology. Rapid urbanization and development of new colonies leads to high rate of land use change and natural resource degradation since last three decades which has been accumulating the fragility of the area. Consequently entire Himalaya foothill zone requires a comprehensive local level geo-environmental appraisal for effective sustainable development planning of the region. Keep in view this; the Ramnagar Himalayan Foothill area (RHFA) in district Nainital, Uttarakhand (India) has been selected for the case illustration. The main objective of the study was to develop a GIS database on Ramnagar environmental geo-informatics (REGI) to facilitate all the concern line departments to implement their socioeconomic developmental activities in the most suitable and safe places throughout the study area. REGI suggests, although landscape of the study area have few favorable conditions for the inhabitant (i.e. maximum proportion (92 %) of the study area enjoys sub-tropical to sub-temperate climatic conditions, easy approachable, thick vegetation cover, rich water resources) but the active tectonics and dynamic hydrological process and its associated reshaped geomorphology poses a stressed geo-environment which need to be consider to formulate a decision support system (DSS) for sustainable development planning.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Institutional subscriptions

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9

Similar content being viewed by others

References

  • Ali A, Qadir DA (1989) Study of river flood hydrology in Bangladesh with AVHRR data. Int J Remote Sens 47:1873–1891

    Article  Google Scholar 

  • Apel H, Thieken AH, Merz B, Blöschl G (2006) A probabilistic modelling system for assessing flood risk. Nat Hazards 38:79–100

    Article  Google Scholar 

  • Bajracharya B, Shrestha AB, Rajbhandari L (2007) Glacial Lake outburst floods in the Sagarmatha Region: hazard assessment using GIS and hydrodynamic modelling. Mt Res Dev 27:336–344

    Article  Google Scholar 

  • Bates PD, Marks KJ, Horritt MS (2003) Optimal use of high-resolution topographic data in flood inundation models. Hydrol Process 17(3):537–557

    Article  Google Scholar 

  • Birkland TA, Burby RJ, Conrad D, Cortner H, Michener WK (2003) River ecology and flood hazard mitigation. Nat Hazard Rev 4(1):46–54

    Article  Google Scholar 

  • Blair TC, McPherson JG (1994) Alluvial fans and their natural distinction from rivers based on morphology, hydraulic processes, sedimentary processes, and facies assemblages. J Sediment Res A64(3):450–489

    Google Scholar 

  • Brivio PA, Colombo R, Maggi M, Tomasoni R (2002) Integration of remote sensing data and GIS for accurate mapping of flooded areas. Int J Remote Sens 23(3):429–441

    Article  Google Scholar 

  • Brody SD, Zahran S, Highfield WE, Grover H, Vedlitz A (2007) Identifying the impact of the built environment on flood damage in Texas. Disasters 32(1):1–18

    Article  Google Scholar 

  • Bull WB (1964) Geomorphology of segmented alluvial fans in western Fresno County, CA. U.S. Geol Surv Professional Paper 352-E: 89–129

  • Burbank DW, Anderson RS (2001) Tectonic geomorphology. Blackwell Science, Massachusetts, 274 p

    Google Scholar 

  • Calvache ML, Viseras C, Fernández J (1997) Controls on fan development – evidence from fan morphometry and sedimentology; Sierra Nevada, SE Spain. Geomorphology 21:60–84

    Article  Google Scholar 

  • Dewey JF, Bird JM (1970) Mountain belts and new global tectonics. J Geophys Res 40:695–707

    Google Scholar 

  • Ferrill DA, Stakamatos JA, Jones SM, Rahe B, McKague HL, Martin RH, Morris AP (1996) Quaternary slip history of the Bare Mountain fault (Nevada) from the morphology and distribution of alluvial fan deposits. Geology 24:559–562

    Article  Google Scholar 

  • Frostick LE, Reid I (1989) Climatic versus tectonic controls of fan sequences: lessons from the Dead Sea, Israel. J Geol Soc Lond 146:527–538

    Article  Google Scholar 

  • Goswami PK, Pant CC (2007) Geomorphology and tectonics of Kota–Pawalgarh Duns, Central Kumaun Sub- Himalaya. Curr Sci 92:685–690

    Google Scholar 

  • Goswami PK, Pant CC (2008) Tectonic evolution of Duns in Kumaun Sub-Himalaya, India: a remote sensing and GIS-based study. Int J Remote Sens 29:4721–4734

    Article  Google Scholar 

  • Gupta P, Anbalagan R, Jain N, Sikdar PK (2001) Landslide hazard evaluation and geostatistical studies in Garhwal Himalaya, India. Rock Mech Tunn Tech 1(1):41–59

    Google Scholar 

  • Haigh MJ, Rawat JS, Bartarya SK (1988) Environmental indicators of landslide activity along the Kilbury road, Nainital, Kumaun Lesser Himalaya. Mt Res Dev 9(1):25–33

    Article  Google Scholar 

  • Hamilton LS (1987) What are the impacts of Himalayan deforestation on the Ganges-Brahmaputra lowland and delta? Assumptions and facts. Mt Res Dev 7(3):256–263

    Article  Google Scholar 

  • Hooke RL, Rohrer WL (1977) Relative erodibility of source area rock types from second order variations in alluvial fan size. Geol Soc Am Bull 88:1177–1182

    Article  Google Scholar 

  • Ives JD (1989) Deforestation in the Himalaya: the cause of increased flooding in Bangladesh and Northern India. Land Use Policy 6:187–193

    Article  Google Scholar 

  • Jain SK, Kumar S, Varghese J (1994) Estimation of soil erosion for a Himalayan watershed using GIS technique. Geol Soc Lond 151(1):217–220

    Google Scholar 

  • Mohindra R, Parkash B, Prasad J (1992) Historical geomorphology and pedology of the Gandak Megafan, Middle Gangetic Plains, India. Earth Surf Process Landf 17:643–662

    Article  Google Scholar 

  • Nakata T (1972) Geomorphic history and crustal movements of the foot-hills of the Himalaya. Tohoku University Science Reports, 7th Series, Japan 22: 39–177

  • Nakata T (1989) Actives faults of the Himalaya of India and Nepal. Geol Soc Am Spec Pap 232:243–264

    Google Scholar 

  • Nearing MA, Jetten V, Baffaut C, Cerdan O, Couturier A, Hernandez M, Le Bissonnais Y, Nichols MH, Nunes JP, Renschler CS, Souchère V, Oost K (2005) Modeling response of soil erosion and runoff to changes in precipitation and cover. Catena 61(2-3):131–154

    Article  Google Scholar 

  • Rawat PK (2013) GIS modeling on Mountain Geodiversity and its hydro-logical responses in view of climate change. Lambert Academic Publishing, Saarbrücken, p 189

    Google Scholar 

  • Rawat PK (2014) GIS Development to monitor climate change and its geohydrological consequences on Non-monsoon crop pattern in Lesser Himalaya. Int J Comput Geom Appl 70:80–95

    Google Scholar 

  • Rawat PK, Tiwari, Prakash C, Pant CC (2011) Modeling of stream runoff and sediment output for erosion hazard assessment in lesser himalaya; need for sustainable land use plane using remote sensing and GIS: a case study. Int J Nat Hazard 59:1277–1297

    Article  Google Scholar 

  • Rawat PK, Tiwari Prakash C, Pant Charu C (2012a) Geo-diversity and its hydrological response in relation to landslide susceptibility in Himalaya: a case study using GIS. Int J Georisk 6(4):229–251

    Google Scholar 

  • Rawat PK, Tiwari Prakash C, Pant Charu C (2012b) Geo-hydrological database modeling for integrated multiple hazard and risks assessment in Lesser Himalaya: a GIS based case study. Int J Nat Hazard 62(3):1233–1260

    Article  Google Scholar 

  • Rawat PK, Tiwari Prakash C, Pant Charu C, Sharama AK, Pant PD (2012c) Spatial variability assessment of river-line floods and flash floods in Himalaya: a case study using GIS. Int J Disaster Prev Manag 21(2):135–159

    Article  Google Scholar 

  • Rawat PK, Tiwari Prakash C, Pant Charu C (2012d) Climate change accelerating land use dynamic and its environmental and socio-economic risks in Himalaya: mitigation through sustainable land use. Int J Clim Change Strategies Manage 4(4):452–471

    Article  Google Scholar 

  • Sastri VV, Bhandari LL, Raju ATR, Dutta AK (1971) Tectonic framework and subsurface stratigraphy of the Ganga basin. J Geol Soc India 12:222–233

    Google Scholar 

  • Shukla UK, Bora DS (2003) Geomorphology and sedimentology of Piedmont Zone, Ganga Plain, India. Curr Sci 84:1034–1040

    Google Scholar 

  • Shukla UK, Singh IB, Sharma M, Sharma S (2001) A model of alluvial megafan sedimentation: Ganga Megafan. Sediment Geol 40:105–129

    Google Scholar 

  • Singh IB (1996) Geological evolution of Ganga Plain – an overview. J Palaeontol Soc India 41:99–137

    Google Scholar 

  • Singh IB (2004) Late Quaternary history of the Ganga Plain. J Geol Soc India 64:431–454

    Google Scholar 

  • Singh V, Tandon SK (2006) Evidence and consequences of tilting of two alluvial fans in the Pinjaur Dun, northwestern Himalayan foothills. Quat Int 159:21–31

    Article  Google Scholar 

  • Srivastava P, Singh IB, Sharma M, Singhvi AK (2003) Luminescence chronometry and Late Quaternary geomorphic history of the Ganga Plain, India. Palaeogeogr Palaeoclimatol Palaeoecol 197:15–41

    Article  Google Scholar 

  • Strahler AN (1956) Quantitative slope analysis. Bull Geol Soc Am 67:571–596

    Article  Google Scholar 

  • Thakur VC (2004) Active tectonics of Himalayan Frontal Thrust and seismic hazard to Ganga Plain. Curr Sci 86:1554–1558

    Google Scholar 

  • Valdiya KS (1976) Himalayan transverse faults and folds and their parallelism with subsurface structures of the northern Indian Plains. Tectonophys 32:353–386

    Article  Google Scholar 

  • Valdiya KS (2003) Reactivation of Himalayan frontal fault: implications. Curr Sci 85:1031–1040

    Google Scholar 

  • Valdiya KS, Bartarya SK (1989) Problem of mass-movement in part of Kmaun Himalaya. Curr Sci 58:486–491

    Google Scholar 

  • Valdiya KS, Bartarya SK (1991) Hydrogeological studies of springs in the catchment of Gaula River, Kumaun Lesser Himalaya, India. Mt Res Dev 1(3):239–258

    Article  Google Scholar 

  • Valdiya KS, Rana RS, Sharma PK, Dey P (1992) Active Himalayan Frontal Fault, Main Boundary Thrust and Ramgarh Thrust in southern Kumaun. J Geol Soc India 40:509–528

    Google Scholar 

  • Wentworth CK (1950) A simplified method of determining the average slope of land surfaces. Am J Sci Ser 5:20

    Google Scholar 

Download references

Acknowledgments

This study is a compiling output of two research reports. First is a multidisciplinary Collaborated project funded by Department of Science and Technology, Gov. of India (Grant no. ES/11/599/01) and second is a consultancy research report funded as a fellowship to the first author by international center for integrated mountain development (ICIMOD), Kathmandu, Nepal.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Pradeep K. Rawat.

Additional information

Communicated by: H. A. Babaie

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Rawat, P.K., Pant, C.C. & Nibanupud, H.K. Environmental geoinformaicts of fast growing Himalaya’s foothill towns and surrounding: concept and implementation. Earth Sci Inform 9, 1–19 (2016). https://doi.org/10.1007/s12145-015-0225-3

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s12145-015-0225-3

Keywords

Navigation