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Lower Himalayan Range in Tansen, Nepal with the Great Himalayas in the background. 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.
Nag Tibba ("Serpent's Peak"), at an elevation of 3,022 metres (9,915 ft), is the highest peak in the Lesser Himalayan region of the Garhwal Division of Uttarakhand state in India and of the Bugyals region. It lends its name to the Nag Tibba Range, itself the next-northerly of the five folds of the Himalayas.
The Himalayan mountain chain is a fold and thrust belt that can be divided into four units bounded by thrusts from south to north: the Sub-Himalaya, Lesser Himalaya, Greater Himalaya and Tethyan Himalaya. [1] The Lesser Himalayan Zone has a lower relief and elevation of the mountains compared to Greater Himalaya. The Lesser Himalaya Sequence ...
' The White Range ') [1] [a] is a mountain range which is part of a lesser Himalayan chain of mountains. It rises from the Shivalik hills, to the north of Kangra and Mandi. Dharamsala, the headquarters of Kangra district and the winter capital of Himachal Pradesh, lies on its southern spur in the Kangra Valley. [2] Chamba lies to the North of ...
Fire protection is the study and practice of mitigating the unwanted effects of potentially destructive fires. [1] [2] It involves the study of the behaviour, compartmentalisation, suppression and investigation of fire and its related emergencies, as well as the research and development, production, testing and application of mitigating systems.
It is a thrust fault that continues along 2900 km of the Himalaya mountain belt. [1] The generally accepted definition of the Main Central Thrust is that it is a ductile shear zone along which the High-grade Great Himalayan Crystalline complex was placed above the low-grade to unmetamorphosed Lesser Himalayan Sequence. [2]
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The Lesser Himalayan Sequence is a unit emplaced before the mountain-building processes. [3] The Greater Himalayan Crystalline complex represents a high-grade unit moved towards SW from the hinterland. The Tethyan Himalayan Sequence represents strata deposited in the former passive margin in the Northern edge of Indian plate. [11] [12]