Natural highlights on Baraadsar Lake trek
The Baraadsar lake trek was a visually stunning experience. This post will make mention to the best natural highlights I witnessed.
Hiking to Sarutal campsite on the second day, I saw a pair of serpent eagles majestically swooping low and high in the air. With an impressive wingspan of 100-170 centimetres, I observe how this bird would easily harness on warm thermals for rising in the air, searching for food without unnecessary physical exertion. Such flight behaviour happens especially in the mornings, as the sun rises above the higher peaks in the distance and heat up the surrounding air.
Amaranth fields
Crossing the tree line
On day four, we crossed the tree line, gaining 600 metres in elevation to camp at 3600masl. While the tree line was well-defined from a distance, as we trekked closer, we realised it was more of a gradual transition. There were still juniper trees a few metres below our trail, and shorter but denser rhododendron bushes that are rarely more than 1m in height.
To our left and right, our vistas uninhibited by trees, distant mountain ridges opened up before our eyes, reflecting the golden rays of the sun. We gaped at the snowcapped peaks of Swargarohini, Black Peak and Banderpooch, barely believing our fortunes in being able to see such wondrous scenes of nature.
(Above): Shrub variety of rhododendron; (Below): Various peaks in sight
I was also excited to see dramatic and visible creations of modern plate tectonic forces. Following the subduction of the Tethyan Ocean, located between India and Asia, during the Paleozoic era (541 to 252 million years ago), the collision of continents produced impressive rock structures and lithologies. Having not seen the ocean in three months, I was humbled to reflect on the geology of these structures formed in ancient days, when the “Indian subcontinent, adrift on the earth's mantle, moved northward to collide with the Asian land mass, driving these marine rocks, inch by inch, five miles into the sky” (Peter Matthiessen's The Snow Leopard).
On day five, we hiked 15 kilometers from the campsite to Lake Baraadsar and back, crossing into alpine tundra. Some of our hiking paths were scree – collections of broken rock fragments at the base of cliffs and valley shoulders, which threatened to loosen under my feet. Screes are the result of physical and chemical weathering and erosion acting on a rock face, and mostly attributed to the formation of ice within mountain rock slopes. As rainwater or snowmelt collect in the cracks of rocks, the water freezes and expands at night when temperatures drop below zero. The increases in volume of the ice exerts pressure on the cracks in the rock, causing them to split further. During the day the ice melts and the water seeps deeper into the cracks. At night the water freezes again, and the process repeats itself until a slab breaks off from the larger rock.
(Above, pc to Skye): Ascending the scree field; (Below): Resting at the top
Alpine tundra, a massive bowl-shaped snow field
Lake Baraadsar
An old steel suspension bridge, destroyed by the river’s flow
~End~
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