L-38 :Mass Movements | Heaving| Soil Creep |Solifluction |Rapid Movements|Earth Flow|Mud flow|Devbri

Описание: Join our telegram channel for free UPSC material and instant updates:
https://t.me/thelaymanway
Sign up for a FREE download of Physical Geography material: https://bit.ly/3sMvCfj
Subscribe: https://bit.ly/2Y8hsa3
Economic survey and budget 2021full playlist for : https://bit.ly/2YuX6bg
Fundamentals of Physical Geography full playlist : https://bit.ly/39Xm7RH
How to clear UPSC prelims in5 months Playlist : https://bit.ly/3cef5L8
Government Schemes for UPSC playlist : https://bit.ly/36A2pKU
Become a Patreon:   / thelaymanway  
Send your business enquires at "[email protected]

The video series would contain GC Leong and Physical geography class 11th books explanation in a very simplified format:

Summary :
Mass Movements: Transfer the mass of rock under the direct influence of gravity. Movements may be slow or rapid. Air, water and other agents do not play a role, its just gravity.
Weathering is not a prerequisite for mass movements though it aids mass movements.
Mass movements do not come under erosion.
Gravity is greater than Resistance b/w rocks.
Causes = Gradient increase, Overloading, Lubrication of supportdue to rainfall, removal of material or load, Earthquakes, excessiveNatural seepage, removal of natural vegetation.
Heave: soil breakage due to upward swelling of soil during freezing conditions caused by increasing presence of ice as it grows towards surface.
Slow movements : Soil Creep – gradual but more or less continuous movement of soil downmoderately steep soil covered hill slopes. Common in damp soils where water acts as a lubricant.
Solifuction: Slow flowing soil mass or fine grained rock debris downslope saturated or lubricated with water. Common in moist temperate areas where surface melting of deeply frozen ground & longcontinued rain occur frequently. Soil acts like a liquid. In Ireland such flows are called bog – bursts.
Rapid movements : Humid conditions . Gentle to steep slopes
Earthflow: Movement of water saturated clayey or silty earth materials downLow angle terraces or hill sides.
Mudflow : Caused by Vegetation cover scarcity, Heavy rainfall, Thick layers of weathered materials get saturated with water flow downwards either slowly or rapidly.
Debris Avalanche : Steep slopes , faster than mudflow, Similar to snow avalanche


My recording equipment:
MacBook: https://www.apple.com/in/macbook-air/

#GCleonggeography #NCERTGeographyExplanation #geographylectureforias #IAS #Studyforcivilservices #UPSC #IASmotivationalvideo #Geography #IndianGeography #UPSClecture #UPSCpreparation #WifistudyUPSC #UPSCmotivationalvideos #iasmotivation #geographyforUPSC #IASpreparation #geographyUPSC #IAScoachingonline #civilservicesstudy #geographynow