Ladakh tourism

Historically, the region included the Baltistan (Baltiyul) valleys, the Indus Valley, the remote Zangskar, Lahaul and Spiti to the south, Ngari including the Rudok region and Guge in the east, Aksai Chin in the east, and Nubra valley to the north over Khardung La in the Ladakh mountain range. Contemporary Ladakh borders Tibet to the east, the Lahaul and Spiti to the south, the Vale of Kashmir, Jammu and Baltiyul regions to the west, and the transKunlun territory of East Turkistan in Central Asia on the other side of the Kunlun range across the Karakoram Pass in the far north. Running southwest to northeast, the Altyn Tagh converges with the Kunlun range in Kashmir, which runs southeast to northwest forming a "V" shape to converge at Pulu. The geographical divide between Ladakh in the highlands of Kashmir and the Tibetan Plateau commences in the vicinity of Pulu. It continues southwards along the intricate maze of ridges situated east of Rudok, wherein are situated Aling Kangri and Mavang Kangri and culminates in the vicinity of Mayum La.

Before partition, Baltistan, now under Pakistani control, was a district in Ladakh. Skardu was the winter capital of Ladakh while Leh was the summer capital.

The mountain ranges in this region were formed over a period of 45 million years by the folding of the Indian plate into the more stationary Eurasian Plate. The drift continues, causing frequent earthquakes in the Himalayan region.[] The peaks in the Ladakh range are at a medium altitude close to the Zoji-la (5,0005,500 m or 16,00018,050 ft), and increase towards south-east, culminating in the twin summits of Nun-Kun (7000 m or 23,000 ft).

The Suru and Zangskar valleys form a great trough enclosed by the Himalayas and the Zangskar range. Rangdum is the highest inhabited region in the Suru valley, after which the valley rises to 4,400 m (14,436 ft) at Pensi-la, the gateway to Zangskar. Kargil, the only town in the Suru valley, is the second most important town in Ladakh. It was an important staging post on the routes of the trade caravans before 1947, being more or less equidistant, at about 230 kilometres from Srinagar, Leh, Skardu and Padum. The Zangskar valley lies in the troughs of the Stod and the Lungnak rivers. The region experiences heavy snowfall; the Pensi-la is open only between June and mid-October. Dras and the Mushkoh Valley form the western extremity of Ladakh.

The Indus river is the backbone of Ladakh. Most major historical and current towns Shey, Leh, Basgo and Tingmosgang (but not Kargil), are situated close to the Indus River. After the Indo-Pakistani War of 1947, the stretch of the Indus flowing through Ladakh is the only part of this river, which is greatly venerated in the Hindu religion and culture and still flows through India.

The Siachen Glacier is located in the eastern Karakoram range in the Himalaya Mountains along the disputed India-Pakistan border. The Karakoram range forms a great watershed that separates China from the Indian subcontinent and is sometimes called the "Third Pole." The glacier lies between the Saltoro Ridge immediately to the west and the main Karakoram range to the east. At 70 km 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 (18,875 ft) above sea level at its source at Indira Col on the China border down to 3,620 m (11,875 ft) at its snout. The passes and some dominating heights on the Saltoro ridge, which has a crestline with heights from 5,450 to 7,720 m (17,880 to 25,330 feet), are occupied by troops on both sides.

Saser Kangri is the highest peak in the Saser Muztagh, the easternmost subrange of the Karakoram range in India, Saser Kangri I having an altitude of 7,672 m (25,171 ft).

Monthly average temperature in Leh
The Ladakh range has no major peaks; its average height is a little less than 6,000 m (19,700 ft), and few of its passes are less than 5,000 m (16,400 ft). The Pangong range runs parallel to the Ladakh range about 100 km northwest from Chushul, along the southern shore of the Pangong Lake. Its highest range is 6,700 m (22,000 ft) and the northern slopes are heavily glaciated. The region comprising the valley of the Shayok and Nubra rivers is known as Nubra. The Karakoram range in Ladakh is not as mighty as in Baltistan. The massifs to the north and east of the NubraSiachen line include the Apsarasas group (highest point 7,245 m, 23,770 ft), the Rimo group (highest point 7,385 m, 24,230 ft) and the Teram Kangri group (highest point 7,464 m, 24,488 ft), together with Mamostong Kangri (7,526 m, 24691 ft) and Singhi Kangri (7,751 m, 25,430 ft). North of the Karakoram lies the Kunlun. Thus, between Leh and eastern Central Asia there is a triple barrier the Ladakh range, Karakoram range, and Kunlun. Nevertheless, a major trade route was established between Leh and Yarkand.

Ladakh is a high altitude desert as the Himalayas create a rain shadow, denying entry to monsoon clouds. The main source of water is the winter snowfall on the mountains. Recent flooding of the Indus river in the region has been attributed either to abnormal rain patterns or the retreating of glaciers, both of which might be linked to global warming. The Leh Nutrition Project, headed by Chewang Norphel, also known as the 'Glacier Man', currently creates artificial glaciers as one solution for this problem.
The regions on the north flank of the Himalayas Dras, the Suru valley and Zangskar experience heavy snowfall and remain virtually cut off from the rest of the country for several months in the year. Summers are short, though they are long enough to grow crops in the lower reaches of the Suru valley. The summer weather is dry and pleasant. Temperature ranges are from -3 to 30 C in summer and from -20 to 15 C in winter. There is little moisture to temper the effects of rarefied air. Ladakh lies in the Very High Damage Risk cyclone zone

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