Show and tell: the geology of Kaas

Thosegarh waterfalls

The region of the Western ghats around Satara and Pune are full of large plateaus and oddly shaped peaks. When you travel through them, the first impression you have of the mountains is that they look like a layered cake. I stood at the Thosegarh waterfall (featured photo) and found that even the monsoon-fed vegetation could not hide this appearance. The layers are a succession of lava flows, laid down in a massive burst of volcanism 60 to 100 million years ago. These successive layers of lava are called the Deccan traps. I found it hard to estimate the thickness of the layers by eye, but going by the heights of trees, perhaps they are between 50 and 100 feet thick. Since each layer of lava covers a considerable area, this means that each burst of volcanism would have lasted long and spewed out immense amounts of rock and ash. Not only would this have killed all life where it flowed, it would have dimmed the sunlight reaching the earth, and contributed to a mass dying of vegetation around the world.

Satara valley

In the 60 million years since it contributed to killing off dinosaurs, the traps have weathered. Today we see them as flat topped hills, cut through by deeply eroded valleys. Some of the waterfalls lead down to rapids extremely suitable for white water rafting. In other places there are very wide valleys. The town of Satara, which you see in the photo above, lies in the extreme western end of the rain-shadowed region of the Deccan. As a result it gets sporadic monsoon rains, enough to keep it green. The urban sprawl gets its drinking water from the river Umboli, which arises in the Kaas plateau, about 25 kilometers away. Traveling in this area, I saw many high plateaus. At one point each of them must have been home to the variety of flowering herbs and bushes whose diversity is now mainly visible in Kaas.

The surface of Kaas plateau

When you reach the top of one of these plateaus you see exposed rock everywhere. This is the volcanic rock called laterite, formed by weathering of the traps. You can see the dark porous rock peeping out from the low cover in the photo of the Kaas plateau above. There is hardly any soil. What little there is forms in little depressions in the rock. This area is covered by tiny herbs: mainly the carnivorous bladderwort (Utricularia) and sundew (Drosera) species, and tiny coexisting herbs. Between such rocky outcrops, there are deeper fissures where a little more soil can collect. There are higher bushes such as the Topli Karvi and arrowroot. There are very few trees on the plateau. What little soil forms is constantly removed by rain and wind. It is a marginal environment where extremely specialized plants grow. Twenty meters below the top, soil can accumulate, and the vegetation changes quite dramatically. It becomes characteristic of the rest of the Sahyadris. As a result, these high plateaus are like islands: the flora of each plateau is isolated from those of its neighbours.

When you walk through the Kaas plateau your eyes take in the evidence that geology determines ecology, that life is shaped by the land.

Author: I. J. Khanewala

I travel on work. When that gets too tiring then I relax by travelling for holidays. The holidays are pretty hectic, so I need to unwind by getting back home. But that means work.

2 thoughts on “Show and tell: the geology of Kaas”

  1. The Western ghats is such a marvelous and beautiful mountain range, indeed. My only experience crossing this range was two years ago when my friend and I went from Munnar in Kerala to Madurai in Tamil Nadu. It was a cloudy day as we went through the Western ghats, but it was spectacular nonetheless.

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