This study presents a comparative analysis of morphometric parameters for two watersheds of Nethravathi river flowing in Karnataka. Delineated watersheds from toposheet are subjected to their physical characterization, using parameters viz; stream order, stream length, bifurcation ratio, drainage density, stream frequency, form factor, circulatory ratio, etc. Both the watershedsBidarthala and Manjotti have fern-like drainage pattern i.e., dendritic type which indicates homogeneity in texture. Biderthala basin with a catchment area of 0.589 km has been observed to have high drainage density and stream frequency indicating impermeable, dense vegetated region with mountainous relief, whereas Manjotti Hole of 0.28 km basin area, has relatively low values of drainage density and stream frequency, which represents the sparse vegetated region with less relief. Manjotti watershed is more circular than Biderthala basin. Both the basins have low value of length of overland flow emphasising the short flow paths, more runoff, and less infiltration. Further, these parameters can also be related with the land use and cover profiles of the regions.
[1]
Shakil Ahmad Romshoo,et al.
Morphometric Analysis to Infer Hydrological Behaviour of Lidder Watershed, Western Himalaya, India
,
2013
.
[2]
S. Govindaiah,et al.
Morphometric analysis of sub-watersheds in the pavagada area of Tumkur district, South India using remote sensing and gis techniques
,
2004
.
[3]
S. Schumm.
EVOLUTION OF DRAINAGE SYSTEMS AND SLOPES IN BADLANDS AT PERTH AMBOY, NEW JERSEY
,
1956
.
[4]
K. N. Rao,et al.
Morphometric Analysis of Gostani River Basin in Andhra Pradesh State, India Using Spatial Information Technology
,
2010
.
[5]
A. N. Strahler.
Quantitative geomorphology of drainage basin and channel networks
,
1964
.
[6]
V. C. Miller,et al.
quantitative geomorphic study of drainage basin characteristics in the Clinch Mountain area, Virginia and Tennessee
,
1953
.