UPSC GEOGRAPHY

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■ SRUCTURAL BENCHES #Geomorphology #Landforms ◇ The step-like flat surfaces on either side of the present lowest valley floors are called terraces. ◇ The benches or terraces formed due to differential erosion of alternate bands of hard and soft rock beds are called structural benches or terraces because of lithological control in the rate of erosion and consequent development of benches. ▪︎JOIN - @upsc_geography_notes

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■ EROSIONAL LANDFORMS #Geomorphology #Landforms □ Waterfalls ◇ Waterfalls or simply falls are caused because of sudden descents or abrupt breaks in the longitudinal course of the rivers due to a host of factors e.g., variation in the relative resistance of rocks, relative difference in topographic reliefs, fall in the sea level and related rejuvenation, earth movements etc. ◇ Rapids are of much smaller dimension than waterfalls. Generally, they are found upstream from the main falls but they are also found independently. ◇ There is well marked fall line in India. This Indian fall line extends between the Purwa or Tons falls on the Tons river (in the north-west part of the Rewa district of Madhya Pradesh) in the west and Sasaram (Bihar) in the east along the junction of the northern foreland of Peninsular India and the Ganga plains. ▪︎JOIN - @upsc_geography_notes

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■ EROSIONAL LANDFORMS #Geomorphology #Landforms □ Waterfalls ◇ Waterfalls or simply falls are caused because of sudden descents or abrupt breaks in the longitudinal course of the rivers due to a host of factors e.g., variation in the relative resistance of rocks, relative difference in topographic reliefs, fall in the sea level and related rejuvenation, earth movements etc. ◇ Rapids are of much smaller dimension than waterfalls. Generally, they are found upstream from the main falls but they are also found independently. ◇ There is well marked fall line in India. This Indian fall line extends between the Purwa or Tons falls on the Tons river (in the north-west part of the Rewa district of Madhya Pradesh) in the west and Sasaram (Bihar) in the east along the junction of the northern foreland of Peninsular India and the Ganga plains. ▪︎JOIN - @upsc_geography_notes

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◇ They are further transformed into very broad and shallow valleys having concave valley side slope of very gentle gradient during old stage. V-shaped valleys are divided into two types viz (1) gorges and (2) canyons. ▪︎JOIN - @upsc_geography_notes

■ EROSIONAL LANDFORM #Geomorphology #Landforms □ River Valleys ◇ The shape and dimension of fluvially originated valleys change with the advancement of the stages of fluvial cycle of erosion. The valley formed in the youthful stage of fluvial cycle of erosion and in the initial stage of valley development is V-shaped having steep valley side slope of convex element. The valley is very deep and narrow, both the valley sides meet together at the valley floor and thus water always touches the valley sides. Such type of V-shaped valleys are the result of accelerated rate of downcutting (vertical erosion or valley deepening. ◇ The valleys are gradually widened due to lateral erosion with the advancement of the stage of cycle of erosion and they become quite broad with flat valley floor and uniform or rectilinear valley side slopes during mature stage or valley development and fluvial cycle of erosion.

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