Results 131 to 140 of about 1,613 (239)
Indices of hydrological and sediment connectivity - state of the art and way forward [PDF]
Digital elevation models (DEMs) describe the landscape topography, which is both a product and a control of the activity of geomorphic processes. In the same way, the connectivity of landscape units with respect to water and sediment fluxes can be seen ...
Brardinoni, Francesco +9 more
core
ABSTRACT Empirical evidence of population demographic responses to environmental perturbations is a major knowledge gap for aquatic vertebrate populations. Extensive habitat alteration including channelization of headwater streams influences the habitat template on which small‐bodied fish are dependent to carry out distinct life stages and maintain or ...
Joseph Spooner, Jonathan Spurgeon
wiley +1 more source
Thrusting supports the development of diverse landforms and deformational structures in the Himalayan Frontal Thrust (HFT) region between Kathgodam and the Chorgallia sector, according to this study.
Nigar Jahan +5 more
doaj +1 more source
Geomorphic Evolution of the Nushki Segment of the Chaman Fault in Western Pakistan [PDF]
The Chaman strike-slip fault marks the western boundary of the collision zone between the Indian and Eurasian plates. It accommodates both lateral translation and convergence of the Indian plate beneath the Eurasian plate and connects the Makran ...
Abubakar, Yahaya 1983-
core
Abstract Allogenic forcing of sediment production generates sedimentary signals that we use to understand the past. These signals may be buffered or shredded by autogenic processes as they travel through sediment routing systems from source to sink. Studies on signal propagation tend to focus on either signal buffering by deterministic fluvial networks
L. O. Roberge +4 more
wiley +1 more source
Abstract In many areas of active faulting, the continuity of normal faults with short or incomplete historical earthquake records and more subdued topographic expressions is not fully understood and consequently the seismic potential of these faults is often underestimated.
Saoirse M. Coveney +5 more
wiley +1 more source
Study on a Geomorphic Indicator for Evaluating Sediment Transport Capacity in Mountainous Rivers
Flooding of water, sediment, and driftwood and its associated landform changes often occurs downstream of debris-flow deposition zones in small, mountainous river basins. This type of flooding occurs due to a sudden decrease in the sediment transport capacity of river channels, resulting in considerable damage.
Naoko Nagumo +2 more
openaire +1 more source
Abstract Accurate three‐dimensional (3D) lake bathymetry reconstruction is critical for water resources assessment and hydrological modeling yet remains constrained by data scarcity and oversimplified geometric assumptions. To address these challenges, we propose the Geomorphologically informed deep learning (GIDL) framework for high‐resolution 3D lake
Minglei Hou +7 more
wiley +1 more source
Relative Uplift Rates Along the Central Mindoro Fault, Philippines
The Central Mindoro Fault (CMF) is a major active oblique, sinistral strike-slip fault within the Philippine archipelago that accommodates the oblique convergence between the Philippine Sea Plate (PSP) and the Sunda Plate (SP).
Jeremy Rimando, Rolly Rimando
doaj +1 more source
Measuring Sand and Finer Suspended Sediment Concentration Profiles in Gravel Bed Rivers
Abstract Accurate measurement of sand and finer suspended sediment concentration profiles in rivers provides essential data for modeling suspended sediment transport. This study advances the application of an in situ laser diffraction instrument to measure the vertical distribution of suspended sediment concentration across multiple size fractions ...
Arman Haddadchi +6 more
wiley +1 more source

