Results 121 to 130 of about 43,419 (259)
High‐Resolution Channel Geometry Reveals Contrasting Styles of Gravel River Adjustment
Abstract Rivers self‐organize to convey water and sediment, giving rise to robust downstream scaling between channel geometry and drainage area, underpinning landscape evolution models. However, these relations rely on limited observations per watershed. We quantify downstream changes in channel slope and bankfull width for six gravel rivers.
Robert P. Kostynick +2 more
wiley +1 more source
Pleistocene Smoothing and Resurfacing of Appalachian Ridgelines by Periglaciation
Abstract Pleistocene cold periods created widespread periglacial conditions across mid‐latitudes, but isolating their geomorphic impact from modern climate, tectonics, and rock strength is challenging. We studied Appalachian (Eastern U.S.) ridgelines across a paleoclimate gradient, controlling for bedrock and structure, to test if colder periglacial ...
Joanmarie Del Vecchio +2 more
wiley +1 more source
Abstract Soil production, through bedrock weathering, regulates landscape evolution, biogeochemical cycles, and societal sustainability, yet quantifying soil production rates (SPRs) remains difficult due to limited tools. Here, we present a new framework for measuring SPRs based on uranium comminution ages and validate this approach at a deep granitic ...
Shenghui Ouyang +3 more
wiley +1 more source
Fluvial Hazards in the Colombian Amazon Piedmont
The article presents the research results regarding the environmental threats caused by fluvial-volcanic or fluvial-torrential factors that could afect the population of the colombian amazon piedmont.
Kim Robertson, Miguel A. Castiblanco
doaj
Beyond Water: Mapping Sediment Bars to Enhance Satellite Monitoring of River Dynamics
Abstract Unvegetated sediment bars are central to river morphodynamics but are rarely used as indicators of channel dynamicity in satellite‐based studies. Linking sediment dynamics and river lateral mobility requires monitoring sustained changes in both water and sediment—the active channel (AC)—to avoid stage‐dependent noise.
Martina Cecchetto +7 more
wiley +1 more source
Artificial Intelligence and Objective‐Function Methods Can Identify Bankfull River Channel Extents
Bankfull channel extents are of fundamental importance in fluvial geomorphology, to describe the geomorphic character of a river, and to provide a boundary for further processing of morphologic and hydraulic attributes.
Jonathan Garber +5 more
doaj +1 more source
This study reveals that legacy paper mill sludge can generate tufa deposits through calcium leaching and atmospheric CO2 interaction, acting as a carbon sink. The findings highlight its potential for low‐cost carbon sequestration and sustainable waste management.
Md Jahangir Alam, John M. MacDonald
wiley +1 more source
We provide a geomorphological analysis of Cordillera Vilcanota and use morphostratigraphic principles to reconstruct palaeo icefield extent and palaeoglacier readvances, likely during the Antarctic Cold Reversal and Younger Dryas. We find evidence of temperate and polythermal ice margins, with limited glaciofluvial landform generation.
Bethan Davies +11 more
wiley +1 more source
One application of mega-geomorphology in education [PDF]
One advantage of a synoptic view displaying landform assemblages provided by imagery is that one can often identify geomorphic processes which have shaped the region and which may affect the habitability of the area over a human life time.
Blair, R. W., Jr.
core +1 more source
Scour hole behaviour: A field study of the Dutch Rhine Delta
Scour hole behaviour can be divided into dynamic and stable. Dynamic scour holes grow in area, depth and volume during seasonal discharge variations and are typically located in discharge‐dominated river reaches. Stable scour holes are found in tidal rivers with heterogeneous riverbeds and show nearly fixed dimensions.
Marthe Oldenhof +3 more
wiley +1 more source

