Key Aspects of Himalayan Geology

This book serves as a ready reference book for anyone who is interested in the Himalayan geology and apprises the readers with the latest findings. The Himalayan syntaxes compose about one-third of the India-Asia collision zone and encompass a substantial part of the crustal deformation that occurs within the system. The Darjeeling Sikkim Himalaya (DSH) marks the beginning of the Eastern Himalaya, which is the most active orogenic zone, coupled with variable seismicity. It is located between Bhutan to the east and Nepal to the west. In the west, Sikkim shares Kanchenjunga, Earth's third highest mountain, with Nepal, while the ridge line forming Sikkim's eastern border flanks the Yadong-Gulu rift graben. DSH, craved by the river system of Tista, is a large geodynamic laboratory of nature where orogen is still in youth to early mature phases of evolution. Giant-scale endogenous turmoil thoroughly overhauled terrain mostly within the confines of distinct belts or divisions and spectacularly uplifted the terrain in superlative terms. Resting on the foundation of structure, tectonics, geomorphology, stratigraphy, and evolution, the wings of geology extend much further.