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This may have given rise to the widening and straightening of river courses which provide the favorable room for river ponding, resulting in deposition of about 2 m thick lacustrine mud deposit.
Further, the presence of joints and faults are responsible for local meandering and sudden change of river courses.
Blockages of river courses rarely occur by flows, falls or topples, because the volume of involved material is usually small and no visible traces of the landslide remain.
In Cyprinids, it has been shown that glacial, interglacial and postglacial oscillations have resulted in major changes of distributions and have shaped current distributions by changes of river courses and river confluences in response to falling sea levels [ 13, 14].
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The hazards included a strong earthquake, multiple large landslides, dam-breaching floods, large-scale debris flows, severe sedimentation, change of river course, and flooding/scouring.
The coarse sand bed is deposited by Sone River during the shifting of river course from east to west in the recent geological past and represents high energy conditions.
The factors that affect river bank erosion are; decrease or increase in shear strength, changes of river course, characteristics of erosion prone bank and bed materials, pressure imbalance at the bank face, rapid drawdown, poor vegetation cover, obstacle in the streams, wind wave and boat wakes (Rahman et al. 2015).
This reactivation of transverse faults has given rise to extensional basins leading to widening of the river courses, providing favourable sites for deposition of recent sediments.
The final part of the river courses through a heavily industrialized area of greater Barcelona.
In Nicaragua, the proposed canal will be at least three times as long, but it will also take advantage of several river courses, as well as the waters of Lake Nicaragua, which is some forty miles wide.
It also features numerous marshes and shallow lakes formed out of dead river courses.
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