Geography:
Ladakh is the highest plateau of the Indian state of Kashmir with much of it being over 3,000 m (9,800 ft). It spans the Himalayan and Karakoram mountain ranges and the upper Indus River valley.
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 trans–Kunlun 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 (5,000–5,500 m or 16,000–18,050 ft), and increase towards south-east, culminating in the twin summits of Nun-Kun (7000 m or 23,000 ft).