Geomorphic Processes - Chapter 6 Geography NCERT Class 11

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Video lecture, lesson summary, revision notes and solutions of CBSE NCERT Geography Class 11 Chapter 6 Geomorphic Processes. This sst video is important and forms foundation for UPSC / IAS, SSC CGL, CDS, NDA and school examinations.
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TABLE OF CONTENT

Meaning of the term Geomorphic Processes - 0:39
Difference between geomorphic agents and geomorphic processes? - 1:21
Endogenic Processes - 2:26
What is Diastrophism - 4:14
Types of Diastrophism (Epeirogenic / Orogenic) - 5:07
Exogenic Prcoesses - 7:10
what are gradients - 7:43
Sole driving force behind all the exogenic processes? - 11:05
What is Weathering - 13:00
Chemical weathering of rocks - 13:28
Physical weathering processes - 16:19
unloading and expansion of rocks - 16:51
BIOLOGICAL ACTIVITY AND WEATHERING - 19:59
Importance / significance of weathering - 21:46
Mass movement geography - 23:06
What is soil creep - 25:31
What is solifluction - 26:21
Rapid movement geography - 26:55
What is earthflow, mudflow, debris avalanche - 27:06
Mass wasting landslide - 28:33
Slump mass movement - 28:53
Debris slide / flow - 29:29
Rockslide - 29:49
Process of Soil Formation - 30:12
Soil forming factors - 32:16
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Video on Geomorphic processes

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laxmimath
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drashtitrivedi
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Hey, great videos. But just wanted to point out a small error that is being continuously repeated over the videos.
So when two tectonic plates of different density/weight collide, the one that is denser or heavier usually subduct's beneath the other. This typically occurs when an oceanic plate collides with a continental plate or another oceanic plate. The denser oceanic plate will usually be forced beneath the less dense continental plate, or in the case of two oceanic plates, the older and colder plate will subduct beneath the younger and warmer one. In case of both continental plates, neither plate is significantly denser or heavier than the other, so subduction typically doesn't occur. Instead, both plates are usually pushed upwards, forming large mountain ranges. The collision results in intense geological activity, such as folding, faulting, and uplifting of the Earth's crust (this is what resulted to what we today called The Himalayas).

sarthakrawal
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14:00 Contents of the chemical weathering process are removed from the new book

16:50 Physical Weathering.

janarthanang
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rajatbawaniwal
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AbhishekYadav-symc
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jadhavpankaj
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sumangupta
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