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Journal ArticleDOI

River profiles along the Himalayan arc as indicators of active tectonics

Leonardo Seeber, +1 more
- 01 Mar 1983 - 
- Vol. 92, Iss: 4, pp 335-367
TLDR
In this paper, the authors show that the discontinuity in the river profiles and the other features are controlled by a major tectonic boundary between the rising High Himalayas and the Lesser Himalaysas.
About
This article is published in Tectonophysics.The article was published on 1983-03-01. It has received 563 citations till now. The article focuses on the topics: Main Central Thrust & Tectonic phase.

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Citations
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Journal ArticleDOI

Tectonics of the Himalaya and southern Tibet from two perspectives

TL;DR: In this article, the authors synthesize the known geology of this orogenic system, with special attention paid to the tectonic evolution of the Himalaya and southernmost Tibet since India-Eurasia collision at ca. 50 Ma.
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

Active folding of fluvial terraces across the Siwaliks Hills, Himalayas of central Nepal

TL;DR: In this article, the authors analyzed geomorphic evidence of recent crustal deformation in the sub-Himalaya of central Nepal, south of the Kathmandu Basin, using structural geology and fluvial terraces along the Bagmati and Bakeya Rivers.
Journal ArticleDOI

Undesirable evolutionary consequences of trophy hunting

TL;DR: Declines in mean breeding values for weight and horn size have declined significantly over time in an evolutionary response to sport hunting of bighorn trophy rams, resulting in the production of smaller-horned, lighter rams and fewer trophies.
Journal ArticleDOI

Expression of active tectonics in erosional landscapes

TL;DR: In this paper, the authors provide an overview of the analysis and interpretation of channel profiles in erosional mountain ranges and show that existing data support theoretical expectations of positive, monotonic relationships between channel steepness index, a measure of channel gradient normalized for downstream increases in drainage area, and erosion rate at equilibrium, and that the transient response to perturbations away from equilibrium engenders specific spatial patterns in channel profiles that can be used to infer the forcing.
References
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OtherDOI

Tectonics of the Indonesian region

TL;DR: The plate-tectonic evolution of a region can be deduced by following the as-sumptions that subduction zones are characterized by ophiolite, melange, wildflysch, and blueschist, that intermediate and silicic calc-alkaline igneous rocks form above Benioff zones, and that truncations of orogenic belts indicate rifting as mentioned in this paper.
Book

Geology of the Himalayas

Journal ArticleDOI

Concept of the graded river

TL;DR: In this paper, the authors modify and extend the theory of grade originally set forth by Gilbert and Davis, which is indispensable in any genetic study of fluvial erosional features and deposits.
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