Abstract
The Alaknanda River is the most significant parental river of Ganga and forms an 11.5 km long and 2.5 km wide valley, locally known as the Srinagar Valley. The purpose of the present study is to highlight the recent landform changes in the Alaknanda channel course after the Kedarnath disaster, 2013. The Kedarnath flood completely changed the channel morphology of the Alaknanda river. The river changed its course at Srikot, SSB and Sriyantra Tapu with lower terraces being silted by sands at Ranihat, SSB, Bhaktiyana and Sriyantra Tapu. A new depositional terrace also formed opposite to Sriyantra Tapu. New lateral channel bars, braided channels, back swamp, rapids, pools and river souls were identified in the channel course of the river. Shifting of the channel course at Chauras still remains a serious problem for the Garhwal University Chauras Campus. About 2–5 m silt was deposited on the lower terrace at SSB, and ITI. The Srikot river bed was appended to 4.60 m. Shifting of channel course remains a serious threat to the Srinagar valley. Urbanization, sand and boulders mining, construction of dam, hydrological canal, road and settlements are the prominent example of anthropogenic activities which affect the shifting channel.
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References
Chang, H. H. (1988). Fluvial processes in river engineering. New York: Wiley.
Falkowski, T., et al. (2017). Channel morphology changes and their relationship to valley bottom geology and human interventions: A case study from the Visutula Valley in Warsaw, Poland. Geomorphology, 207, 100–111.
Guneralp, I., et al. (2012). Advances and challenges in meandering channels research. Geomorphology, 163-164, 1–9.
Holland, T. H. (1984). Report on the Gohna Landslip, Garhwal, selections from the records of the Government of India in the public works department: CCCXXIV(324), Office of the Superintendent of Government Printing, Calcutta.
Hooke, J. (1984). Changes in river meanders—A review of techniques and results of analysis. Progress in Physical Geography, 8, 473–508.
Kimothi, M. M., & Juyal, N. (1996). Environmental impact assessment of a few selected watersheds of the Chamoli district (Central Himalaya) using remotely sensed data. International Journal of Remote Sensing, 17, 1391–1405.
Morais, E. S., et al. (2016). Spatiotemporal variations in channel changes caused by cumulative factors in a meandering river: The lower Peixe River, Brazil. Geomorphology, 273, 348–360.
Nand, N., & Prashad, C. (1972). Alaknanda tragedy: A geomorphological appraisal. The National Geographical Journal of India, 18(3 and 4), 206–212.
Nicoll, T. J., & Hicken, E. J. (2010). Plan form geometry and channel migration of confined meandering river on the Canadian prairies. Geomorphology, 116, 37–47.
Pal, S. K. (1986). Geomorphology of river terraces along Alaknanda Valley, Garhwal Himalaya (p. 158). Delhi: BR Publishing Corporation.
Rana, N., Singh, S., Sundriyal, Y. P., & Juyal, N. (2013). Recent and past floods in the Alaknanda valley: Causes and consequences. Current Science, 105(9), 1209.
Schumm, S. A. (1977). The fluvial system. New York, N.Y.: Wiley.
Schumm, S. A. (1985). Patterns of alluvial rivers. Annual Review of Earth and Planetary Sciences, 13, 5–27.
Wasson, R. J., et al. (2008). The mountain-lowland debate: Deforestation and sediment transport in the upper Ganga catchment. Environmental Management, 88, 53–61.
Wasson, R. J., Sundriyal, Y. P., Chaudhary, S., Morhtikai, P., Sati, S. P., & Juyal, N. (2014). A 1000-year history of large floods in the Upper Ganga catchment, central Himalaya, India. Quaternary Science Reviews, 77, 156–166.
Yousefi, S., et al. (2016). Changes in morphometric meander parameters identified on Karoon River, Iran, using remote sensing data. Geomorphology, 271, 55–64.
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Chauniyal, D.D., Dutta, S. & Semwal, S. Changing Pattern of Channel Morphology of Alaknanda River in Srinagar Valley (Garhwal Himalaya), India. J Indian Soc Remote Sens 46, 1379–1387 (2018). https://doi.org/10.1007/s12524-018-0782-2
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DOI: https://doi.org/10.1007/s12524-018-0782-2