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This book focuses on vulnerability issues associated with urban development over Dehradun paleo-alluvial fan. The city of Dehradun occupies the central part of the elongated piggy back syncline Doon Valley and sits on loose unconsolidated coarse clastic Doon gravels derived from the Lesser Himalayas being deposited by Bindal and Rispana river systems during the Late Pleistocene and Holocene age. Rapid and unmatched conversion of land into continuously built up area over the tectonically active, geomorphologically sensitive, structurally feeble, and hydrologically incapable area has grossly...