Kolahoi Peak: Difference between revisions


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| photo_caption = Kolhai Glacier

| photo_caption = Kolhai Glacier

| type = Mountain glacier

| type = Mountain glacier

| location = [[Jammu and Kashmir (union territory)|Jammu and Kashmir, India]]

| location = Sonamarg [[Jammu and Kashmir (union territory)|Jammu and Kashmir, India]]

| coords = {{coord|34|10|20|N|75|20|10|E|type:glacier_region:IN|display=inline}}

| coords = {{coord|34|10|20|N|75|20|10|E|type:glacier_region:IN|display=inline}}

| area =

| area =

Mountain in Jammu & Kashmir, India

Kolahoi Peak (locally called ‘Gashe-braed’ meaning Illuminated Cat) is a mountain with peak elevation of 17799 ft (5425 metres) located in Anantnag j&k. Kolahoi Peak is easily accessible through Aru Pahalgam. The mountain is the highest mountain in Kashmir Division.[a]. Kolahoi Peak is part of the Great Himalayan range, and is located 16 km south of Kashmir. Accessible through the enchanting pathway of Aru Pahalgam, this mountainous marvel stands tall as the crowned jewel of the Kashmir Division, an ascent that whispers legends of majesty.
Kolahoi Peak proudly claims its title as the highest peak in the Great Himalayan range, a majestic sentinel gracing the celestial tapestry. The very name Kolahoi resonates with echoes of distant beauty, weaving tales of adventure across its rugged slopes.
From the icy embrace of Kolahoi’s glacier emerges the lifeblood of the region, the Lidder River Pahalgam. Meandering southward, this crystalline tributary not only quenches the land’s thirst but also nourishes it, becoming a vital source for both drinking and irrigation in the picturesque realms of south Kashmir.
In the heart of this glacial sanctuary, the Kolahoi glacier becomes a magnet for adventurers seeking the thrill of untamed landscapes. The very mention of Kolahoi resonates globally, drawing explorers with the promise of an exhilarating odyssey amid nature’s untamed splendor. For more authentical information visit official website of district Anantnag.h
The allure of Kolahoi Peak transcends geographical boundaries, inviting wanderers to immerse themselves in the enigma of its heights. As the Illuminated Cat stands guard over the expanse, each step toward its summit becomes a pilgrimage, guided by the whispers of foreign winds that carry tales of the indomitable spirit of Kolahoi. [1]
Kolahoi Peak rises from the Kolahoi Glacier is a pyramid-shaped peak with ice falls and ice fields at its bottom. The rock formation of the peak is extraordinary stable with aretes and ridges.[2]

Climbing history and routes
Kolahoi Peak was first climbed by a British medical team headed by Dr Ernest Neve in 1912.[3]
The easiest route to climb Kolahoi Peak is its southern face[2] via the Aru village near Pahalgam, from which a 21 km high altitude alpine trek leads to the glacier of the peak.
On 7 September 2018, a team of mountaineers while descending after successful summit were hit by rockfall debris, which killed two of them.[4]
The first ever for Kolahoi Greater traverse was completed successfully on 11th sep 2023 to 13th September 2023 led by Inayat Ullah Bhat with Raja Waseem and Laway Mudasir local ace climbers. They traversed a total of 6.21 miles from Southern glacier( Musa’s Graveyard) to Northern glacier with successful summit of Neve-Mason couloir of Kolahoi peak.

Kolahoi Glacier

Kolahoi glacier lies at an average elevation of 4,700 metres (15,400 ft). The origin of the glacier is below the cirques on the north flank of Kolahoi Peak.[5] It is the main source of Lidder River, whose water serves the population of Anantnag district, where it is mainly used for drinking and agricultural purposes. It finally drains into the Jhelum River near Khanaba.
Kolahoi Glacier is among the victims of global warming,[6] and has shrunk in area[7] from 13.57 km2 in 1963 to 10.69 km2 in 2005 or a loss of 2.88 km2 in three decades.[8] In 1974 the glacier was about 5 km long and is known to have extended for at least 35 km during the Pleistocene.[5] A detailed analysis by Rafiq and Mishra[9] reported that the glacier has shrunk from 35 to 09.88 Sq Km. The rate of recession measured from 1922 to 2015 is reported to be 73.26 m per year. Furthermore, the rate of recession of snout is found to be 16.41 m per year from 1857 to 2015. The shirking of glacier area is linked to reduction in snow depth which in turn is affected by the increase in black carbon concentration, temperature and reduction in precipitation. Reanalysis data show that there is decrease of about 1.08 ± 0.65 cm per decade in snow depth over Kolahoi glacier during 1979 to 2013. There are decadal increasing trends of about 76 nanogram/m2 (statistically significant) and 0.39 °C (insignificant) in black carbon concentration and temperature, respectively, over Kolahoi. A decreasing trend of about 2.9 mm/month per decade in precipitation over the study area is also reported. It is reported that there is decrease of about 71 ± 24% in snow depth for each degree increase in temperature over Kolahoi.[10] Reduction in snow depth as a result of increase in black carbon concentration, temperature and reduction in precipitation might have resulted in the shrinking of the Kolahoi glacier. According to another report,[11] Kolahoi is a hanging glacier and hollowed inside. It is a matter of great concern for Kashmir Valley. Many expeditions have failed here.


^ The Nun Peak which is 23,409 ft (7,135 metres) in height and lies in the Jammu Division is the highest mountain in Jammu and Kashmir.

See also



^ “Geography of Kashmir”. kousa.org. Retrieved 24 April 2012.

^ a b “EXPEDITIONS : Himalayan Journal vol.16/8”. www.himalayanclub.org. Retrieved 28 January 2019.

^ “Kolahoi first climbed” (PDF). Alpine Journal. Retrieved 25 April 2012.

^ “KAS officer among 2 feared dead in Kolahoi glacier accident”. greaterkashmir.com. 8 September 2018. Retrieved 8 September 2018.

^ a b N. Ahmed and N. H. Hashimi (1974). “Glacial History of Kolahoi Glacier, Kashmir, India” (PDF). Journal of Glaciology. 13 (68): 279–283. Bibcode:1974JGlac..13..279A. doi:10.1017/S002214300002308X. Archived from the original (PDF) on 11 December 2013. Retrieved 16 April 2012.

^ “Goddess glacier melting in war-torn Kashmir”. national geographic.com. 26 March 2010. Archived from the original on 27 March 2010. Retrieved 24 April 2012.

^ “Kashmir’s crown Kolahoi glacier is in deep water”. TERI.

^ Kanth, T.A., Aijaz Ahmad Shah and Zahoor ul Hassan; Geomorphologic Character & Receding Trend of Kolahoi Glacier in Kashmir Himalaya, Recent Research in Science and Technology 2011, 3(9): 68-73 Archived 11 December 2013 at the Wayback Machine, ISSN 2076-5061

^ Rafiq, Mohammd; Mishra, Anoop (25 November 2016). “Investigating changes in Himalayan glacier in warming environment: a case study of Kolahoi glacier”. Environmental Earth Sciences. 75 (23). doi:10.1007/s12665-016-6282-1. ISSN 1866-6280.

^ Mishra, Anoop Kumar; Rafiq, Mohammd (September 2017). “Analyzing snowfall variability over two locations in Kashmir, India in the context of warming climate”. Dynamics of Atmospheres and Oceans. 79: 1–9. Bibcode:2017DyAtO..79….1M. doi:10.1016/j.dynatmoce.2017.05.002. ISSN 0377-0265.

^ “Kolahoi: Hanging and hollowed inside”. hoparoundindia.com. Retrieved 27 April 2012.

^ “Kolahoi: His life would come to an end on the alpines he had become synonymous with”. Mahmood A. Shah. 16 September 2018. Retrieved 25 September 2018.


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