Himalayan landform: a case study of Dun valleyStudy carried out in Kotadun Valley, India. |
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Contents
CHAPTER I INTRODUCTION 1 | |
CHAPTER II GEOLOGY OF KOTADUN | ii |
CHAPTER III RELIEF ANALYSIS | 26 |
Copyright | |
2 other sections not shown
Common terms and phrases
absolute relief altitude anthropogenic average slope Bangajala basin area Basin Height boulders category land channel circularity ratio contour correlated variables covering an area Dabka Dabka river decreasing deviation dissection index dolomite drainage density drainage pattern dun floor Dun valley erosion erosional factors Fault flow forest Gadela geological geomorphic geomorphic development geomorphological greywacke Haldu Hypsometric Analysis indicates isopleths Kakurar Khairar Kotadun Krol landforms landslide landuse Lesser Himalaya lithology loose lithology Lower Siwalik Main Boundary Thrust Mashani mass wasting maximum Middle Siwalik monsoon morphotectonic Nagthat Nainital observed Outer Himalaya Patkot Pliocene profiles quartzite rainfall region relative height relative relief respectively rocks ruggedness number sandstone shale Siwalik formation Siwalik hills Siwalik ranges slate slope category slope failure slope group slope ranges soil stream frequency stream length stream number structural study area surface synclinal Table tectonic toe to crown total area upliftment Upper Siwalik upto Valdiya vegetation cover village water discharge