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Geomorphometric Analysis of Chamoli and Karnaprayag District, Uttrakhand in Respect to Hazard Zonation of The Area

机译:Uttrakhand的Chamoli和Karnaprayag区的地形地貌分析

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Chamoli and Karnaprayag district of Uttrakhand comprises of fragile lithological formations and lies in highly vulnerable zone in terms of natural disasters. It's latitude and longitude ranges between 29°50’N to 30°40’N and 78°40'E to 79°50'E. The area is highly prone to frequent hazards like landslide, earthquake, cloud burst and flash floods. Advanced Space borne Thermal Emission and Reflection Radiometer (ASTER) has been used for preparing Digital Elevation Model (DEM), slope, aspect and various other maps which have been used for evaluation of linear and areal parameters. The studies have been carried out on 64 selected 4th order river basins in Chamoli and Karnaprayag district using ARC GIS. There are various parameters like stream order, stream number, Bifurcation ratio, Drainage density, Form Factor, Elongation ratio etc. had been analyzed on the river basins. The lower values of Bifurcation ratio in basins represent geological heterogeneity, high permeability and less structural control. The value of Drainage Density varies between 1.3-2.2 Km-1 which implies development of coarse grained texture. The complex relationship between the values of Elongation ratio, Circularity ratio and Form factor in some basins represents that these passing through structural thrust. The anomalous values of linear and areal parameters suggest that basins of the study area are geologically, structurally and lithologically controlled. The occurrences of landslide, earthquake has reliable relation with computed parameters. Since the outcome of the study will act as precursors for natural disasters.
机译:Uttrakhand的Chamoli和Karnaprayag区包括脆弱的岩性地层,就自然灾害而言,它位于高度脆弱的地区。它的纬度和经度范围是北纬29°50′至30°40′N,东经78°40′至79°50′。该地区极易发生滑坡,地震,云爆和山洪等常见灾害。先进的星载热发射和反射辐射计(ASTER)已用于准备数字高程模型(DEM),坡度,纵横比和其他各种地图,这些地图用于评估线性和面参数。使用ARC GIS对Chamoli和Karnaprayag地区的64个选定的四阶流域进行了研究。对流域进行了流序,流数,分流比,排水密度,形态因子,伸长率等各种参数的分析。盆地中分叉比的较低值表示地质异质性,高渗透率和较少的结构控制。排水密度的值在1.3-2.2 Km-1之间变化,这意味着形成了粗糙的纹理。在某些盆地中,伸长率,圆形度和形状因数之间的关系很复杂,表示它们通过结构推力。线性和面积参数的反常值表明研究区域的盆地受到了地质,结构和岩性的控制。滑坡,地震的发生与计算参数具有可靠的关系。由于这项研究的结果将成为自然灾害的先兆。

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