KERALA PSC / PHYSICAL GEOGRAPHY / MOVEMENTS OF THE EARTH’S CRUST / NOTES
KERALA PSC / PHYSICAL GEOGRAPHY / MOVEMENTS OF THE EARTH’S
CRUST / NOTES
· The earth movements are to two types:
Ø Vertical Movements
Ø Horizontal Movements
· Vertical movements are responsible for a rise or a fall
of a portion of the earth’s surface
· When a part of the earth’s crust rises in relation to
surrounding portions it is known as uplift or emergence
· When the sinking of a part of the earths crust relative
to surrounding portion takes place, it is called subsidence
· The formation of continents and plateaus are also due to
vertical movement and hence these are also referred to as continent building or
plateau building movements
· Horizontal movements involve compression and tension
· These compressional or tensional forces are horizontal or
tangential movements
· These movements are also referred to as mountain building
movements
· Warping and Isostasy constitute vertical movements, while
folding, faulting and continental drift constitutes horizontal movement
· Warping is the deformation of earth’s crust which affects
very large areas on the earth’s surface. It results in the formation of domes,
shields and depressions
· Isostasy is a condition of gravitational balance between
the crustal segments of different thickness.
· Folding is the process whereby the rock strata are bent
into a series of arches (anticlines) and troughs (synclines) as a result of the
horizontal earth movements which cause compression within the crust.
· Faulting is the process by which the tensional earth
movements under the effect of considerable pressure creates a fracture in the
earth’s crust.
· Faulting gives rise to relief features such as block
mountains and rift valleys
· Continental drift refers to the horizontal movements of
the continents on a vast scale.
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KERALA PSC / PHYSICAL GEOGRAPHY / MOVEMENTS OF THE EARTH’S
CRUST / NOTES

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