Siachen Glacier

The Siachen Glacier is a glacier located in the eastern Karakoram range of the Himalayas, just northeast of the point NJ9842 where the Line of Control between India and Pakistan ends in northeastern Kashmir. At long, it is the longest glacier in the Karakoram and second-longest in the world's non-polar areas. It falls from an altitude of 5,753 m above sea level at its head at Indira Col on the India–China border down to 3,620 m at its terminus. The entire Siachen Glacier, with all major passes, has been under the administration of India as part of the union territory of Ladakh since 1984. Pakistan maintains a territorial claim over the Siachen Glacier and controls the region west of Saltoro Ridge, lying west of the glacier, with Pakistani posts located 1 km below more than 100 Indian posts on the ridge.
The Siachen Glacier lies immediately south of the great drainage divide that separates the Eurasian Plate from the Indian subcontinent in the extensively glaciated portion of the Karakoram sometimes called the "Third Pole". The glacier lies between the Saltoro Ridge immediately to the west and the main Karakoram range to the east. The Saltoro Ridge originates in the north from the Sia Kangri peak on the China border in the Karakoram range. The crest of the Saltoro Ridge's altitudes range from 5,450 to 7,720 m. The major passes on this ridge are, from north to south, Sia La at 5,589 m, Bilafond La at 5,450 m, and Gyong La at 5,689 m. The average winter snowfall is more than 1000 cm and temperatures can dip to. Including all tributary glaciers, the Siachen Glacier system covers about.

Etymology

"Sia" in the Balti language refers to the rose family plant widely dispersed in the region. "Chen" refers to any object found in abundance. Thus the name Siachen refers to a land with an abundance of roses. The naming of the glacier itself, or at least its currency, is attributed to Tom Longstaff.

Dispute

Both India and Pakistan claim sovereignty over the entire Siachen region. In June 1958, first Geological Survey of India expedition went to the Siachen glacier. It was the first official Indian survey of Siachen Glacier by Geological Survey of India post-1947 and that was undertaken to commemorate the International Geophysical Year in 1958. The study included snout surveying of five glaciers namely Siachen, Mamostong, Chong Kumdan, Kichik Kumdan and Aktash Glaciers in Ladakh region. 5Q 131 05 084 was the number assigned to the Siachen glacier by the expedition. U.S. and Pakistani maps in the 1970s and 1980s consistently showed a dotted line from NJ9842 to the Karakoram Pass, which India believed to be a cartographic error and in violation of the Simla Agreement. In 1984, India launched Operation Meghdoot, a military operation that gave India control over all of the Siachen Glacier, including its tributaries. Between 1984 and 1999, frequent skirmishes took place between India and Pakistan. Indian troops under Operation Meghdoot pre-empted Pakistan's Operation Ababeel by just one day to occupy most of the dominating heights on Saltoro Ridge to the west of Siachen Glacier. However, more soldiers have died from the harsh weather conditions in the region than from combat. Pakistan lost 353 soldiers in various operations recorded between 2003 and 2010 near Siachen, including 140 Pakistanis killed in the 2012 Gayari Sector avalanche. Between January 2012 and July 2015, 33 Indian soldiers died due to adverse weather. In December 2015, Indian Union Minister of State for Defence Rao Inderjit Singh said in a written reply in the Lok Sabha that a total of 869 Army personnel have died on the Siachen glacier due to climatic conditions and environmental and other factors from the date that the Army launched Operation Meghdoot in 1984. In February 2016, Indian Defence Minister Manohar Parrikar stated that India will not vacate Siachen, as there is a trust deficit with Pakistan and also said that 915 people have died in Siachen since Operation Meghdoot in 1984. According to official records, only 220 Indian soldiers have been killed by enemy bullets since 1984 in Siachen area. Both India and Pakistan continue to deploy thousands of troops in the vicinity of Siachen and attempts to demilitarize the region have been so far unsuccessful. Prior to 1984, neither country had any military forces in this area.
Aside from the Indian and Pakistani military presence, the glacier region is unpopulated. The nearest civilian settlement is the village of Warshi, 10 miles downstream from the Indian base camp. The region is also extremely remote, with limited road connectivity. On the Indian side, roads go only as far as the military base camp at Dzingrulma, 72 km from the head of the glacier. The Indian Army has developed various means to reach the Siachen region, including the Manali-Leh-Khardung La-Siachen route. In 2012, Chief of Army Staff of the Indian Army General Bikram Singh said that the Indian Army should stay in the region for strategic advantages, and because a "lot of blood has been shed" by Indian armed personnel for Siachen. The present ground positions, relatively stable for over a decade, mean that India maintains control over all of the Siachen Glacier and all of its tributary glaciers, as well as all the main passes and heights of the Saltoro Ridge immediately west of the glacier, including Sia La, Bilafond La, Gyong La, Yarma La, and . Pakistan controls the glacial valleys immediately west of the Saltoro Ridge. According to TIME magazine, India gained over in territory because of its 1980s military operations in Siachen. India has categorically stated that India will not pull its army from Siachen until the 110-km long AGPL is first authenticated, delineated and then demarcated.
File:Sia plant.jpg|thumbnail|Sia plant in Khaplu. Balti people grow this rose family in their houses as decoration, and its bark is used in payo cha instead of green tea leaves in some areas
The 1949 Karachi agreement only carefully delineated the line of separation to point NJ9842, after which, the agreement states, the line of separation would continue "thence north to the glaciers". According to the Indian stance, the line of separation should continue roughly northwards along the Saltoro Range to the west of the Siachen glacier beyond NJ9842; international boundary lines that follow mountain ranges often do so by following the watershed drainage divide such as that of the Saltoro Range. The 1972 Simla Agreement made no change to the 1949 Line of Control in this northernmost sector.

Drainage

The glacier's melting waters are the main source of the Nubra River in the Indian region of Ladakh, which drains into the Shyok River. The Shyok in turn joins the 3000 kilometre-long Indus River which flows through Pakistan. Thus, the glacier is a major source of the Indus and feeds the largest irrigation system in the world.

Environmental issues

The glacier was uninhabited before 1984, and the presence of thousands of troops since then has introduced pollution and melting to the glacier. To support the troops, glacial ice has been cut and melted with chemicals.
Dumping of non-biodegradable waste in large quantities and the use of arms and ammunition have considerably affected the ecosystem of the region.

Glacial retreat

Preliminary findings of a survey by Pakistan Meteorological Department in 2007 revealed that the Siachen glacier has been retreating for the past 30 years and is melting at an alarming rate. The study of satellite images of the glacier showed that the glacier is retreating at a rate of about 110 metres a year and that the glacier size has decreased by almost 35 percent. In an eleven-year period, the glacier had receded nearly 800 metres, and in seventeen years about 1700 metres. It is predicted that the glaciers of the Siachen region will be reduced to about one-fifth of their 2011 size by 2035. In the twenty-nine-year period 1929–1958, well before the military occupation, the glacial retreat was recorded to be about 914 metres. One of the reasons theorized for the recent glacial retreat is chemical blasting, to construct camps and posts. In 2001 India laid oil pipelines inside the glacier to supply kerosene and aviation fuel to the outposts from base camps. As of 2007, the temperature rise at Siachen was estimated at 0.2-degree Celsius annually, causing melting, avalanches, and crevasses in the glacier.

Waste dumping

The waste produced by the troops stationed there is dumped in the crevasses of the glacier. Mountaineers who visited the area while on climbing expeditions witnessed large amount of garbage, empty ammunition shells, parachutes etc. dumped on the glacier, that neither decomposes nor can be burned because of the extreme climatic conditions. About of waste is produced and dumped in glacial crevasses daily by Indian forces. The Indian army is said to have planned a "Green Siachen, Clean Siachen" campaign to airlift the garbage from the glacier, and to use biodigestors for biodegradable waste in the absence of oxygen and freezing temperatures. Almost forty percent of the waste left at the glacier is plastic and metal, including toxins such as cobalt, cadmium and chromium that eventually affect the water of the Shyok River. The Indus is used for drinking and irrigation. Research is being done by scientists of The Energy and Resources Institute, to find ways to successfully dispose of the garbage generated at the glacier using scientific means. Some scientists of the Defence Research and Development Organisation who went on an expedition to Antarctica are also working to produce a bacterium that can thrive in extreme weather conditions and can be helpful in decomposing the biodegradable waste naturally.

Fauna and flora

The flora and fauna of the Siachen region are also affected by the huge military presence. The region is home to rare species including snow leopard, brown bear and ibex that are at risk because of the military presence.