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The Lower Himalayan Range, also called the Lesser Himalayas or Himachal, is one of the four parallel sub-ranges of the Himalayas. [1] [2] It has the Great Himalayas to the north and the Sivalik Hills to the south. It extends from the Indus River in Pakistan to the Brahmaputra Valley in North East India traversing across North India, Nepal and ...
Accordingly K2 is only in the table below for reference and not shown on the map on this page. The interactive map on this page ranks Himalayan peaks above 7,500 m (24,600 ft) and is more inclusive. A peak has a different definition to a mountain and different authorities may use different definitions of either.
The range separates the Greater Himalayas from lower fertile valleys in the Shivaliks. [39] The Greater Himalayas (also known as Himadri) form the northernmost and the highest section of the Himalayas. [26] The sub-range has an average elevation of more than 6,100 m (20,000 ft) and contains many of the world's tallest peaks including Mount Everest.
[1] [2] The Himalayas show a gradual elevation towards the Dhauladhar and Pir Panjal ranges. Pir Panjal is the largest and westernmost range of the Lesser Himalayas. Near the bank of the Sutlej River, it dissociates itself from the main Himalayan range and forms a divide between the Beas and Ravi rivers on one side and the Chenab on the other
All are in the two highest mountain ranges in the world, the Himalayas and the Karakoram. Mount Everest - 8,848 m (29,029 ft) K2 - 8,611 m (28,251 ft) Kanchenjunga - 8,586 m (28,169 ft) Mountain
This region begins at the Lower Himalayan Range, where a fault system called the Main Boundary Thrust creates an escarpment 1,000 to 1,500 metres (3,000 to 5,000 ft) high, to a crest between 1,500 and 2,700 metres (5,000 and 9,000 ft). It covers 68% of the total area of Nepal.
Sattal is situated in the Lower Himalayan Range and is the result of tectonic activities and the uplifting of sediments between the Tibetan plain and the Indo-Gangetic plains. The rocks are mainly sedimentary rocks and quartzite. Physiographically the area can be divided into lower Himalayas and terraces.
The Lower Himalayan Ranges, also called the Inner Himalaya, are southward spurs of the Great Himalaya, dominating the midsection of Bhutan.The Dongkya Range forms the trijunction of the Bhutan-Sikkim-Tibet border, separating Sikkim from the Chumbi Valley [5] The Black Mountains in central Bhutan form a watershed between two major river systems, the Mo Chhu and the Drangme Chhu.