A friend sent me this picture of a section of the Western Ghat escarpment. It is taken from Jivdhan fort, looking north towards the hook nose of Naneghat. This location is about a hundred odd kilometers west-north-west from Ahmednagar town. Naneghat was a mountain pass for travel between the coastal plain and the plateau.
The yellow bloom makes a pretty contrast with the grey basalt. My geology eye was drawn towards something else; a suspiciously straight flowing stream, which I have highlighted with an arrow.
I looked at a satellite imagery of this location and the stream is seen following a fracture zone (black arrows) that cuts across Jivdhan fort as well. The escarpment area is riddled with such fractures. They occur as north-south, northwest-southeast, and northeast-southwest (brown arrows) trending sets.
These fractures are regions of shattered rock. That zone erodes away quicker. Water flowing in the linear depressions that form enhance this topographic difference and eventually cut deep straight valleys.
Large fractures or cracks along slopes causes slabs of rocks to cleave away from mountain sides. Slopes retreat due to such rock falls. A large crack is seen in the picture just a few feet away from where my friend took his photograph. At some point a portion of rock will detach itself and Jivdhan fort will become that much narrower.
Look at the zoomed out satellite imagery of this area. The plateau edge has been fragmented into isolated hillocks, mesas and pinnacles by enhanced erosion along fractures oriented in various directions. You can follow some of these fractures (white arrows) to the straight edges of the escarpment suggesting that slab breakoff has played a role in shaping the morphology of the cliff line.
Such fracture systems not only have formed a landscape of mesas and pinnacles but have caused the Western Ghat escarpment to retreat eastwards for at least tens of kilometers from its original location. The escarpment is a legacy of the breakup of the western margin of India with Seychelles at the end of the eruptions of the Deccan Basalts. At that time in the Paleocene (~60 million years ago), continental stretching caused the formation of a series of north-south oriented faults which sloped (dipped) to the west. The westerly block of each of these fault sets sank, created a staircase like crustal structure descending towards the west, with west facing cliffs. The Western Ghat escarpment would have been the easterly most of these cliffs.
See the schematic below which shows this staircase crustal structure of the western margin of India.
The red portion would have been the original extent of the Deccan plateau. It has retreated eastwards over several millions of years. As a result, the coastal plain became progressively broader. Give a thought to the humongous amount of rock that has been removed by erosion.
Along the west coast the erosional retreat has not wiped clean all evidence of the original plateau. From the coastal plain rise isolated ranges and mesas. The hill station Matheran, where people go to catch the cool wind and a spectacular view, is a fine example.
See the satellite imagery below.
Matheran was where the plateau edge and escarpment once was. It has now moved eastwards (arrows) leaving behind an erosional remnant, a splendid outlier of the Deccan plateau rising abruptly from the plains.
Let's end with a 3D view of the escarpment along the Jivdhan-Naneghat area.
If you take a flight out of Pune to Delhi, the plane will fly a northerly route parallel to the plateau edge for the first 20-25 minutes of your journey. The Western Ghat escarpment appears as it does in the tilted perspective above, a sinuous line of majestic black cliffs, testimony to the forces of volcanism, continental breakup, and erosion.
A section of this stunning landform deserves to be included in our National Geological Monuments list.
Photo credit: Rajesh Sarde
The yellow bloom makes a pretty contrast with the grey basalt. My geology eye was drawn towards something else; a suspiciously straight flowing stream, which I have highlighted with an arrow.
I looked at a satellite imagery of this location and the stream is seen following a fracture zone (black arrows) that cuts across Jivdhan fort as well. The escarpment area is riddled with such fractures. They occur as north-south, northwest-southeast, and northeast-southwest (brown arrows) trending sets.
These fractures are regions of shattered rock. That zone erodes away quicker. Water flowing in the linear depressions that form enhance this topographic difference and eventually cut deep straight valleys.
Large fractures or cracks along slopes causes slabs of rocks to cleave away from mountain sides. Slopes retreat due to such rock falls. A large crack is seen in the picture just a few feet away from where my friend took his photograph. At some point a portion of rock will detach itself and Jivdhan fort will become that much narrower.
Look at the zoomed out satellite imagery of this area. The plateau edge has been fragmented into isolated hillocks, mesas and pinnacles by enhanced erosion along fractures oriented in various directions. You can follow some of these fractures (white arrows) to the straight edges of the escarpment suggesting that slab breakoff has played a role in shaping the morphology of the cliff line.
Such fracture systems not only have formed a landscape of mesas and pinnacles but have caused the Western Ghat escarpment to retreat eastwards for at least tens of kilometers from its original location. The escarpment is a legacy of the breakup of the western margin of India with Seychelles at the end of the eruptions of the Deccan Basalts. At that time in the Paleocene (~60 million years ago), continental stretching caused the formation of a series of north-south oriented faults which sloped (dipped) to the west. The westerly block of each of these fault sets sank, created a staircase like crustal structure descending towards the west, with west facing cliffs. The Western Ghat escarpment would have been the easterly most of these cliffs.
See the schematic below which shows this staircase crustal structure of the western margin of India.
The red portion would have been the original extent of the Deccan plateau. It has retreated eastwards over several millions of years. As a result, the coastal plain became progressively broader. Give a thought to the humongous amount of rock that has been removed by erosion.
Along the west coast the erosional retreat has not wiped clean all evidence of the original plateau. From the coastal plain rise isolated ranges and mesas. The hill station Matheran, where people go to catch the cool wind and a spectacular view, is a fine example.
See the satellite imagery below.
Matheran was where the plateau edge and escarpment once was. It has now moved eastwards (arrows) leaving behind an erosional remnant, a splendid outlier of the Deccan plateau rising abruptly from the plains.
Let's end with a 3D view of the escarpment along the Jivdhan-Naneghat area.
If you take a flight out of Pune to Delhi, the plane will fly a northerly route parallel to the plateau edge for the first 20-25 minutes of your journey. The Western Ghat escarpment appears as it does in the tilted perspective above, a sinuous line of majestic black cliffs, testimony to the forces of volcanism, continental breakup, and erosion.
A section of this stunning landform deserves to be included in our National Geological Monuments list.
Hi. I am Makarand Ketkar. I am a naturalist as a professional and I am deeply interested in geology and wildlife. I take thousands of students on field every year and teach them about nature and it's various living and non living forms.
ReplyDeleteLong back I was told by one my seniors that an oceanic plate subducted under Indian peninsula and tilted it towards east(causing all major rivers to flow eastwards). This subduction accelerated the sinking process of western edge of the plateau. Do you have more info about this event? Thanking you in advance.
Hi Makarand- I think what he may have meant is that the India plate subducted under Asia. There is no oceanic plate subducting under the Indian peninsula. The western and eastern margins of India are divergent margins i.e. they have formed during continental breakup as India separated from Africa, Antarctica and Australia and then moved away. Subsidence of the western margin is because of movement along faults that formed during continental separation and not during subduction. Only the northern margin is convergent i.e. it formed by initial subduction and later collision with Asia.
ReplyDeleteThere are several plausible reasons for the easterly tilt of the Indian Peninsula.. I have listed them in this earlier post -
https://suvratk.blogspot.com/2011/09/easterly-tilt-of-deccan-plateau.html
hope this helps.
thanks for reading!
Wonderful! Thanks for putting this out there! :)
ReplyDeletethanks... glad you liked it!
ReplyDeleteI enjoyed this post on the geology of the northern Western Ghats as the Nane Ghat area was a favorite haunt of mine when I worked in Pune. In 2014 I worked with some Landsat data to create the attached map emphasizing vegetation that might be of interest to readers. https://ianlockwood.files.wordpress.com/2014/06/landsat_pune_part1a6_14.jpg
ReplyDeletePost is at: https://ianlockwood.wordpress.com/2014/06/01/sahyadri-revealed/
Ian..thanks for the link. very informative maps and blog post!
ReplyDeleteThanks Survat. I totally forgot to read your reply and thank you for the same. Somehow I was looking for some information and came across this comment of mine posted ages ago.
ReplyDeleteHello
ReplyDeleteJust came across this. Very interesting. I had always wondered about Matheran and itsi sort of detached position from the escarpment. Now I know the reason! Thanks for sharing this
Vikram
Sir can you please send the link of the map you have used to show the physiography of India(3d). It will be very helpful for me,to understand Geography as I'm studying in tenth. Thank u ❤️☺️
ReplyDeleteVedant
Hi Vedant... there is no link as such. I used Google Earth and navigated to the area around Naneghat and Jivdhan and used the tilt function to create a 3 D rendering.. try it out!
ReplyDeleteIt is always fascinating to read about history of deccan region. Can we study history and geology of deccan beyond 6 cr years ago. Also, can we find remnants of similar geology both on Seychelles as well as Madagascar
ReplyDeletethanks Harshal. Much of the Deccan is covered by basalt. So it is not possible to directly observe older rocks. Geophysical methods can give an idea of the deeper crust. On the fringes of the Deccan plateau, you do get exposures of Proterozoic sedimentary rocks and Archean basement too. Seychelles has a similar geology to our basalt terrain since it broke away from the Indian continent during and after the eruptions. Madagascar too has geology similar to South Indian terrains as it too is a fragment that broke away from the southern part of the Indian continent.
DeleteHI sir, do you have any studies regarding basaltic fissures of northern western ghat(Trimbakeshwar range, anjaneri ) - and how seasonal streams are originating from this basaltic fissures.
ReplyDeletestudent of landscape architecture from cept university ahmedabad.
sorry, I haven't come across any specific literature on that.
DeleteThank you for this post, sir.
ReplyDelete