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Book ChapterDOI

The Geographic, Geological and Oceanographic Setting of the Indus River

TLDR
The Indus River system was initiated shortly after the collision between the Indian and Eurasian Plates prior to 45 million years ago (Clift et al. as discussed by the authors ), and the discovery of an early advanced civilization in the Indus Valley further increased this interest in the history of the river.
Abstract
. The discovery of an early advanced civilization in the Indus Valley (Meadows and Meadows, 1999 and references therein) further increased this interest in the history of the river. Its source lies in Tibet, close to sacred Mount Kailas and part of its upper course runs through India, but its channel and drainage basin are mostly in Pakiistan. Recent geological and geophysical information suggests that the Indus River system was initiated shortly after the collision between the Indian and Eurasian Plates prior to 45 million years ago (Clift

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Journal ArticleDOI

The Indus flood of 2010 in Pakistan: a perspective analysis using remote sensing data

TL;DR: In this paper, the role of geomorphology in flood analysis and management is emphasized and the authors urge the river managers to take urgent steps to incorporate the geomorphic understanding of Himalayan rivers in river management plans.
Journal ArticleDOI

Weakening and strengthening of the Indian monsoon during Heinrich events and Dansgaard-Oeschger oscillations

TL;DR: In this paper, geochemical and sedimentological data from core SO130-289KL from the Indus submarine slope spanning the last similar to 80 kyr were used to reconstruct its range of environmental impacts.
Journal ArticleDOI

Causation and avoidance of catastrophic flooding along the Indus River, Pakistan

TL;DR: In this paper, the authors investigated the causes of the 2010 Indus River Flood and found that most damage was caused by dam and barrage-related backwater effects, reduced water and sediment conveyance capacity, and multiple failures of irrigation system levees.
Journal ArticleDOI

Sediment fluxes and buffering in the post-glacial Indus Basin

TL;DR: The Indus drainage has experienced major variations in climate since the Last Glacial Maximum (LGM) that have affected the volumes and compositions of the sediment reaching the ocean since that time as mentioned in this paper.
References
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Journal ArticleDOI

Bedrock incision, rock uplift and threshold hillslopes in the northwestern Himalayas

TL;DR: The topography of tectonically active mountain ranges reflects a poorly understood competition between bedrock uplift and erosion as mentioned in this paper, and the Indus river incises through the bedrock at extremely high rates (2-12 mm yr-1).
Journal ArticleDOI

Andean tectonics as a cause for changing drainage patterns in Miocene northern South America

TL;DR: In the early Miocene, a large part of the drainage of northwest Amazonia was directed northward along the paleo-Orinoco river system to a deltain Lake Maracaibo.
Book

The Geological Evolution of the River Nile

Rushdi Said
TL;DR: Bentz et al. as discussed by the authors presented a list of formal names for the Nile Gulf of Egypt, including the Eonile/Paleonile Interval (Tmu/Tplu), the Protonile/Neonile interval (Q2/Q3), and the Neonile/Protonile interval (Q3).
BookDOI

Rivers Over Rock: Fluvial Processes in Bedrock Channels

J. Tinkler, +1 more
TL;DR: In this article, the authors provide an integrated view of the characteristics and operation of these important, though hitherto neglected, classes of channels, including the Bedrock river channels. But their work is limited to the case of the Indus River.
Book ChapterDOI

Beyond Power: Bedrock River Incision Process and Form

TL;DR: In this paper, the authors present a quantitative discussion of the processes active in bedrock-floored river channels, drawn from field observations, erosion rate measurements, and simple scaling rules.
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