Digitale Bibliotheek
Sluiten Bladeren door artikelen uit een tijdschrift
 
<< vorige    volgende >>
     Tijdschrift beschrijving
       Alle jaargangen van het bijbehorende tijdschrift
         Alle afleveringen van het bijbehorende jaargang
           Alle artikelen van de bijbehorende aflevering
                                       Details van artikel 21 van 25 gevonden artikelen
 
 
  Technical Note: Remote sensing in the mapping of the Brahmaputra/Jamuna River channel patterns and its relation to various landforms and tectonic environment
 
 
Titel: Technical Note: Remote sensing in the mapping of the Brahmaputra/Jamuna River channel patterns and its relation to various landforms and tectonic environment
Auteur: Das, J. D.
Saraf, A. K.
Verschenen in: International journal of remote sensing
Paginering: Jaargang 28 (2007) nr. 16 pagina's 3619-3631
Jaar: 2007-01
Inhoud: The Brahmaputra River is one of the largest sand-bar braided rivers in the world having a seasonal high discharge, high sediment load and characterized by frequent channel pattern changes and shift. Following natural phenomena, the river has been responding to landform/ground level changes effected by tectonic activity of the region. A satellite image mosaic and temporal Landsat data enabled detailed mapping of the Brahmaputra River revealing some prominent features with regard to change in its course, new channels and influence of landforms and tectonics. Northward shift of the river course are inferred at three different places, which are (1) in the uppermost part of Brahmaputra; (2) in the region north of the Kopili Gap (KG); (3) and north of the Mikir Hills (MH). However, the river appears to have developed a tendency to shift back in the area north of the MH. These shifts are influenced by tectonic activity in the Himalayan foothills. The Brahmaputra River shows remarkable changes downstream of Guwahati, by forming multiple channels south of the island as well as the formation of channels closer to the Shillong Plateau. The sudden and sharp south-westward to southward turn of the river just after longitude 90° E is in fact caused by a landform north of Dhubri. Development of new channels from the main river along the western and northern edges of the Shillong Massif (SM) and the shift of Kopili River towards the SM are indicators of tectonic activities that the massif suffered.
Uitgever: Taylor & Francis
Bronbestand: Elektronische Wetenschappelijke Tijdschriften
 
 

                             Details van artikel 21 van 25 gevonden artikelen
 
<< vorige    volgende >>
 
 Koninklijke Bibliotheek - Nationale Bibliotheek van Nederland