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[HTML][HTML] The role of infrequently mobile boulders in modulating landscape evolution and geomorphic hazards
A landscape's sediment grain size distribution is the product of, and an important influence
on, earth surface processes and landscape evolution. Grains can be large enough that the …
on, earth surface processes and landscape evolution. Grains can be large enough that the …
The sha** of erosional landscapes by internal dynamics
Erosional landscapes transport sediment downstream, host natural hazards and are
geologically active. While perturbations in external forcing, particularly climate and tectonics …
geologically active. While perturbations in external forcing, particularly climate and tectonics …
[کتاب][B] Rivers in the Landscape
E Wohl - 2020 - books.google.com
Rivers are the great shapers of terrestrial landscapes. Very few points on Earth above sea
level do not lie within a drainage basin. Even points distant from the nearest channel are …
level do not lie within a drainage basin. Even points distant from the nearest channel are …
Rock-uplift history of the Central Pontides from river-profile inversions and implications for development of the North Anatolian Fault
Major strike-slip fault systems on Earth, like the North Anatolian Fault (NAF), play an
important role in accommodating plate motion, but surprisingly little is known about how …
important role in accommodating plate motion, but surprisingly little is known about how …
[HTML][HTML] Interplay between tectonics and surface processes in the evolution of mountain ranges: Insights from landscape dynamics, uplift, and active deformation of …
Drainage divides are dynamic features of a landscape that migrate over time during the
development of river networks. In this study, we focused on the geomorphic response of a …
development of river networks. In this study, we focused on the geomorphic response of a …
Bedrock fracture density controls on hillslope erodibility in steep, rocky landscapes with patchy soil cover, southern California, USA
Although many steep landscapes comprise a patchwork of soil-mantled and bare-bedrock
hillslopes, models typically assume hillslopes are entirely soil-mantled or bare-bedrock …
hillslopes, models typically assume hillslopes are entirely soil-mantled or bare-bedrock …
River patterns reveal two stages of landscape evolution at an oblique convergent margin, Marlborough Fault System, New Zealand
Here we examine the landscape of New Zealand's Marlborough Fault System (MFS), where
the Australian and Pacific plates obliquely collide, in order to study landscape evolution and …
the Australian and Pacific plates obliquely collide, in order to study landscape evolution and …
Geomorphic complexity and the case for topographic rejuvenation of the Appalachian Mountains
Despite vast scientific inquiry, the evolution of Appalachian Mountain topography in eastern
North America has yet to be robustly explained. After a century and a half of investigation …
North America has yet to be robustly explained. After a century and a half of investigation …
New constraints on bedrock erodibility and landscape response times upstream of an active fault
Considerable progress has been made in modelling the response of rivers to tectonic
perturbation in order to decode the tectonic signals embedded in river long profiles and …
perturbation in order to decode the tectonic signals embedded in river long profiles and …
Evaluating models for lithospheric loss and intraplate volcanism beneath the Central Appalachian Mountains
The eastern margin of North America has been shaped by a series of tectonic events
including the Paleozoic Appalachian Orogeny and the breakup of Pangea during the …
including the Paleozoic Appalachian Orogeny and the breakup of Pangea during the …