Long profiles of rivers provide a platform to analyse interaction between geological and geomorphic processes operating at different time scales. Identification of an appropriate model for river long profile becomes important in order to establish a quantitative relationship between the profile shape, its geomorphic effectiveness, and inherent geological characteristics. This work highlights the variability in the long profile shape of the Ganga River and its major tributaries, its impact on stream power distribution pattern, and role of the geological controls on it. Long profile shapes are represented by the sum of two exponential functions through the curve fitting method. We have shown that coefficients of river long profile equations a...
Rapidly uplifting Himalaya contributes a huge sediment load that governs the morphological character...
The Landsat programme, which started in 1972, initiated an era of space-based Earth observation rele...
The present work addresses the planform dynamics of the Ganga River in the middle-lower portion over...
Understanding the controls on the morphological variability of river systems constitutes one of the ...
Understanding of geomorphic processes and the determination of geomorphic diversity in catchments ar...
The drainage pattern and the morphology of the piedmont zone of the Himalayas are clear indicators o...
Mass movements in mountainous areas are capable of damming rivers and can have a lasting effect on t...
The morphotectonic study was carried out in the Nahan salient, located between the well known Kangra...
The properties of rivers and their catchments can be expressed by statistical relationships between ...
© 2015 Taylor & Francis.ABSTRACT: Neotectonic activity in Mahe (Mayyazhi) river basin and its implic...
The catchment area of the Godavari in Peninsular India shows complex heterogeneous morphologic, clim...
Tectonic activity continues to shape and create challenges for human populations in tectonically act...
The Indian rivers are dominantly monsoon rainfed. As a result, their regime characteristics are dict...
The Bringi watershed of Kashmir Valley has been studied to understand its morpho- tectonic evolution...
© Kaunas University of Technology. Characteristics and spatial variation in geomorphic processes in ...
Rapidly uplifting Himalaya contributes a huge sediment load that governs the morphological character...
The Landsat programme, which started in 1972, initiated an era of space-based Earth observation rele...
The present work addresses the planform dynamics of the Ganga River in the middle-lower portion over...
Understanding the controls on the morphological variability of river systems constitutes one of the ...
Understanding of geomorphic processes and the determination of geomorphic diversity in catchments ar...
The drainage pattern and the morphology of the piedmont zone of the Himalayas are clear indicators o...
Mass movements in mountainous areas are capable of damming rivers and can have a lasting effect on t...
The morphotectonic study was carried out in the Nahan salient, located between the well known Kangra...
The properties of rivers and their catchments can be expressed by statistical relationships between ...
© 2015 Taylor & Francis.ABSTRACT: Neotectonic activity in Mahe (Mayyazhi) river basin and its implic...
The catchment area of the Godavari in Peninsular India shows complex heterogeneous morphologic, clim...
Tectonic activity continues to shape and create challenges for human populations in tectonically act...
The Indian rivers are dominantly monsoon rainfed. As a result, their regime characteristics are dict...
The Bringi watershed of Kashmir Valley has been studied to understand its morpho- tectonic evolution...
© Kaunas University of Technology. Characteristics and spatial variation in geomorphic processes in ...
Rapidly uplifting Himalaya contributes a huge sediment load that governs the morphological character...
The Landsat programme, which started in 1972, initiated an era of space-based Earth observation rele...
The present work addresses the planform dynamics of the Ganga River in the middle-lower portion over...