See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/302902544 Quaternary Geomorphic Processes and Landform Development in the Thar Desert of Rajasthan Chapter · January 2011 CITATIONS READS 6 4,293 1 author: Amal Kar Central Arid Zone Research Institute (CAZRI) 90 PUBLICATIONS 1,166 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Thar Desert Natural resources and their management View project Late Quaternary paleoclimate of the Thar Desert View project All content following this page was uploaded by Amal Kar on 11 May 2016. The user has requested enhancement of the downloaded file. acb publications Landforms Processes & Environment Management Kolkata, India Editor: S. Bandyopadhyay et al.
[email protected] ISBN 81-87500-58-1 2011 (223-254) Quaternary Geomorphic Processes and Landform Development in the Thar Desert of Rajasthan Amal Kar1 Abstract: Evolution of landforms in the Thar Desert of Rajasthan is very much influenced by the exogenic and endogenic processes operating in the region during the Quaternary period. Studies have revealed that several fluctuations in climate between drier and wetter phases and periodic earth movements decided the type and intensity of geomorphic processes. The paper describes the broad sedimentation pattern in the desert, known facets of Quaternary climate and landform characteristics. It also discusses the influence of Quaternary climate change, neotectonism and human activities on landform evolution. Introduction The Thar, or the Great Indian Sand Desert, is situated in the arid western part of Rajasthan state in India and the adjoining sandy terrain of Pakistan.