Thank you very much, Sir, from the bottom of my heart. Your teachings and illustrations have profoundly helped me understand this subject. I used to run away from it, but your method of teaching with numerous images, diagrams, and videos has sparked my interest. I genuinely enjoyed learning from you and feel truly privileged. Thank you once again for your invaluable guidance!
Field mapping delineate various litho units based on colour, gradation of grain size, schistocity, etc.. order of superimposition based on sedimentation, orientation of current bedding etc to ascertain inversion of beds. Trace of strike continuity of each strata as it outcrops. Recumbent folds of regional extent can at times confuse a mapper.
I watched a video where they made a topographic map using clay, where they modeled a hill or mountain out of clay, put the clay on a piece of paper, traced a line around its base, cut a horizontal line a specific distance up the clay mountain, removed the bottom clay, put the less-high cut clay mountain on the paper and traced another line around its base. They kept doing this until they reached the top of the clay and could not draw any more topographic lines. Frank Reiser M.S..
![IITK NPTEL Structural Geology_Lecture 10.1: Rheology Basics I [Prof. Santanu Misra]](http://i.ytimg.com/vi/HGLNBjtGZkI/mqdefault.jpg)
![IITK NPTEL Structural Geology_Lecture 10.1: Rheology Basics I [Prof. Santanu Misra]](/img/tr.png)
![IITK NPTEL Structural Geology_Lecture 01: Introduction I [Prof. Santanu Misra]](http://i.ytimg.com/vi/fiMemypKqEI/mqdefault.jpg)
![IITK NPTEL Structural Geology_Lecture 04: Stereographic Projections [Prof. Santanu Misra]](http://i.ytimg.com/vi/izTQhPzE3Kg/mqdefault.jpg)
Thank you very much, Sir, from the bottom of my heart. Your teachings and illustrations have profoundly helped me understand this subject. I used to run away from it, but your method of teaching with numerous images, diagrams, and videos has sparked my interest. I genuinely enjoyed learning from you and feel truly privileged. Thank you once again for your invaluable guidance!
10Q a lot and it is also good to teach us how to plot such structures on a map in ArcGIS/qgis
Thank you sir this series has been extremely helpful. I hope to be able to meet you in person someday . You are a wonderful teacher.
Thank you prof
Field mapping delineate various litho units based on colour, gradation of grain size, schistocity, etc.. order of superimposition based on sedimentation, orientation of current bedding etc to ascertain inversion of beds. Trace of strike continuity of each strata as it outcrops.
Recumbent folds of regional extent can at times confuse a mapper.
Thanku sir it helps me a lot.......
how to plot geological structures and make the boundaries of their distribution on a geological map?
thank u sir, very informative.
explain how we update the structural map and why
Great Teacher
Thanking u sir happy navratri
Thankyou so much sir!! 🙌
Excellent.
Very informative classes
Very good sir g
Sir, Lab-8 and Lecturer-26 are missing to upload.
I watched a video where they made a topographic map using clay, where they modeled a hill or mountain out of clay, put the clay on a piece of paper, traced a line around its base, cut a horizontal line a specific distance up the clay mountain, removed the bottom clay, put the less-high cut clay mountain on the paper and traced another line around its base. They kept doing this until they reached the top of the clay and could not draw any more topographic lines.
Frank Reiser M.S..