Morphometric Analysis of Kangshabati-Darkeswar Interfluves Area in West Bengal, India using ASTER DEM and GIS Techniques

2013 ◽  
Vol 02 (04) ◽  
Author(s):  
Sumita Gayen Gouri Sankar Bhunia
Keyword(s):  
Morphometric Analysis ◽  
West Bengal ◽  
Gis Techniques

Morphometric Analysis Using GIS Techniques: A Case Study from the Basaltic Terrain of Central India

2018 ◽  
pp. 301-326
Author(s):  
Nisha Sahu ◽  
G. P. Obi Reddy ◽  
Nirmal Kumar ◽  
M. S. S. Nagaraju ◽  
Rajeev Srivastava ◽  
...  
Keyword(s):  
Morphometric Analysis ◽  
Central India ◽  
Gis Techniques ◽  
Basaltic Terrain

scholarly journals Morphometric analysis in basaltic Terrain of Central India using GIS techniques: a case study

2016 ◽  
Vol 7 (5) ◽  
pp. 2493-2499 ◽  
Author(s):  
Nisha Sahu ◽  
G. P. Obi Reddy ◽  
Nirmal Kumar ◽  
M. S. S. Nagaraju ◽  
Rajeev Srivastava ◽  
...  
Keyword(s):  
Morphometric Analysis ◽  
Central India ◽  
Gis Techniques ◽  
Basaltic Terrain

MORPHOMETRIC ANALYSIS OF BICIPITAL GROOVE OF HUMERUS WITH ITS CLINICAL IMPLICATIONS: A STUDY IN WEST BENGAL

2016 ◽  
Vol 4 (4.1) ◽  
pp. 3009-3015 ◽  
Author(s):  
Phalguni Srimani ◽  
◽  
Ritaban Saha ◽  
Biplab Goswami ◽  
Sibani Mazumdar ◽  
...  
Keyword(s):  
Morphometric Analysis ◽  
West Bengal ◽  
Clinical Implications ◽  
Bicipital Groove

scholarly journals MORPHOMETRIC ANALYSIS OF WADI DARNAH WATERSHED NE LIBYA, USING GIS TECHNIQUES

2021 ◽  
pp. 31-49
Author(s):  
Nouria El Hadi. A. Aboshaala
Keyword(s):  
Morphometric Analysis ◽  
Structural Control ◽  
Geological Structure ◽  
High Rate ◽  
Elongation Ratio ◽  
Drainage Pattern ◽  
Infiltration Capacity ◽  
Stream Network ◽  
Gis Techniques ◽  
Drainage Patterns

Wadi Darnah is about 586 km2 and lies in the northern portion of the Al Jabil AL Akhdar. The Wadi drains into the Mediterranean Sea. The present study incorporates a morphometric analysis of Wadi Darnah by using remote sensing and GIS techniques. Digital Elevation Model (DEM) and topographic sheets were processed in ArcGIS software. The study revealed that the drainage patterns of stream network from the basin are mainly of dendritic type which indicates homogeneity in texture and lack of structural control. The bifurcation ratio value of 4.53 indicates that the area is not much influenced by the geological structure and undisturbed drainage pattern. The study area is of the low density group basins (2.09 km-1). The elongation ratio (0.36), circularity ratio (0.14) and form factor (0.10) show elongated basin with steep relief, moderate discharge, and a long main channel. The basin has a high relief up to 850 m, which leads to a high rate of runoff but the effect of this water flow is reduced by the high infiltration capacity due to the high rate of karstification and karst features in the basin area.

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