The Himalayas, which have long been a physical and cultural divide between South and Central Asia, form the northern rampart of the subcontinent, and their western ranges occupy the entire northern end of Pakistan, extending about 200 miles (320 km) into the country. Spreading over Kashmir and northern Pakistan, the western Himalayan system splits into three distinct ranges, which are, from south to north, the Pir Panjal Range, the Zanskar Range, and the Ladakh Range. Farther north is the Karakoram Range, which is a separate system adjoining the Himalayas. This series of ranges varies in elevation from roughly 13,000 feet (4,000 meters) to higher than 19,500 feet (6,000 meters) above sea level. Four of the region’s peaks exceed 26,000 feet (8,000 meters), and many rise to heights of more than 15,000 feet (4,500 meters). These include such towering peaks as Nanga Parbat (26,660 feet [8,126 meters]) and K2, also called Godwin Austen (28,251 feet [8,611 meters]), in Gilgit-Baltistan.

Several important rivers flow from, or through, the mountains of Kashmir into Pakistan. From the Pir Panjal Range flows the Jhelum River (which bisects the famous Vale of Kashmir); the Indus River descends between the Zanskar and Ladakh ranges; and the Shyok River rises in the Karakoram Range. South of the Pir Panjal is the northwestern extension of the Shiwalik Range (there rising to about 600 to 900 feet [200 to 300 meters]), which extend over the southern part of the Hazara and Murree hills and include the hills surrounding Rawalpindi and neighboring Islamabad.

Beyond the Karakoram Range in the extreme north lies the Uygur Autonomous Region of Xinjiang, China; to the northwest, beyond the Hindu Kush, are the Pamirs, where only the Vākhān (Wakhan Corridor), a narrow strip of Afghan territory, separates Pakistan from Tajikistan. The Himalayan massif was pierced in 1970 when Chinese and Pakistani engineers completed the Karakoram Highway across the Karakoram Range, linking the town of Gilgit in Gilgit-Baltistan with Kashgar (Kashi) in Xinjiang. The highway, a marvel of modern technology, carries considerable commerce between the two countries but has promoted little cultural exchange.

The northern mountain barrier influences the precipitation pattern in Pakistan by intercepting monsoon (rain-bearing) winds from the south. Melting snow and glacial meltwater from the mountains also feed the rivers, including the Indus, which emerge from the east-west-aligned ranges to flow southward. Siachen Glacier, one of the world’s longest mountain glaciers, feeds the Nubra River, a tributary of the Shyok. The many glaciers in this region, particularly those of the Karakoram Range, are among the few in the world to have grown in size since the late 20th century.

The northern and western regions of the country are subject to frequent seismic activity—the natural consequence of a geologically young mountain system. Minor earth tremors are common throughout the region. However, a number of earthquakes have been severe and highly destructive, given the fact that many buildings are poorly constructed and that those in the mountains are often precipitously perched. Historically recent major quakes in Pakistan include those in 1935, 1945, 1974, and 2005. The latter two were in the far north of the country, and the 2005 quake—centered in the mountainous border region of the North-West Frontier Province (now Khyber Pakhtunkhwa) and Azad Kashmir—killed some 80,000 to 90,000 people and left the entire area devastated.

The population in this inhospitable northern region is generally sparse, although in a few favored places it is dense. In most of the tiny settlements of this region, the usual crop is barley; fruit cultivation, especially apricots, is of special importance. Timber, mainly species of pine, is found in some parts, but its occurrence varies with precipitation and elevation. Many slopes have been denuded of cover by excessive timber felling and overgrazing.

The Hindu Kush and the western mountains

In far northern Pakistan the Hindu Kush branches off southwestward from the nodal orogenic uplift known as the Pamir Knot. The ridges of the Hindu Kush generally trend from northeast to southwest, while those of the Karakorams run in a southeast-northwest direction from the knot. The Hindu Kush is made up of two distinct ranges, a main crest line that is cut by transverse streams, and a watershed range to the west of the main range, in Afghanistan, that divides the Indus system of rivers from the Amu Darya (ancient Oxus River) drainage basin. From the Hindu Kush, several branches run southward through the areas of Chitral, Dir, and Swat, in Khyber Pakhtunkhwa. These branches have deep, narrow valleys along the Kunar, Panjkora, and Swat rivers. In the extreme northern portion, the ranges are capped with perpetual snow and ice; high peaks include Tirich Mir, which rises to 25,230 feet (7,690 meters). The valley sides are generally bare on account of their isolation from the precipitation-bearing influences. Toward the south the region is largely covered with forests of deodar (a type of cedar) and pine and also has extensive grasslands.

The Safid Mountain Range, lying south of the Kābul River and forming a border with Afghanistan, trends roughly east to west and rises throughout to an elevation of about 14,000 feet (4,300 meters). Its outliers are spread over Kohat district, Khyber Pakhtunkhwa. South of the Safid Range are the hills of Waziristan, which are crossed by the Kurram and Tochi rivers, and even farther south is the Gumal River. Comparatively broad mountain passes are located south of the Kābul River. They are, from north to south, the Khyber, Kurram, Tochi, Gomal, and Bolan. The Khyber Pass is of special historical interest: broad enough to allow for the passing of large numbers of troops, it has often been the point of ingress for armies invading the subcontinent.

South of the Gumal River, the Sulaiman Range runs in a roughly north-south direction. The highest point of that range, Takht-e Sulaiman, has twin peaks, the higher of which reaches 18,481 feet (5,633 meters). The Sulaiman Range tapers into the Marri and Bugti hills in the south. The Sulaiman and, farther south, the low Kirthar Range separate the Balochistan plateau from the Indus plain.