Do earthquakes result in higher levels of sediment in rivers in the years following the event? There are several reasons to believe this could be the case. Previous studies have even provided evidence of increased sediment loads in mountainous areas after major earthquakes. However, a study by Graf et al. challenges this perspective. They demonstrate that despite the thousands of landslides triggered by the 2015 Gorkha Earthquake in Nepal, there were only minimal increases in coarse sediment in river channels during the subsequent years. Instead, the study reveals a different story. In June 2021, a single, exceptionally heavy rainfall event mobilized large volumes of sediment, leading to riverbed elevation by as much as 12 meters. This effect greatly overshadowed any sedimentary impact left by the earthquake along the river corridor. The study underscores that earthquake evidence may not always be found in the sedimentary records of alluvial areas. In high-mountainous regions, records of riverbed elevation may be strongly influenced by unique and localized events.

This paper presents a new way of quantifying geometries of drainage networks, moving beyond river long profiles to explore the complexity of planform branching river networks. Using the proposed length asymmetry metric, the paper demonstrates that complexity is correlated with landscape aridity, where arid landscapes have less complex networks compared to humid ones, suggesting this metric could be a new way of exploring the impact of climate on Earth's topography.

River meandering is a long standing source of interest for scientists interested in how the Earths surface is shaped. Here, Noh et al., use a novel probablistic approach to create geomorphic risk maps where areas that have the potential for meandering can be assessed in an arguably more rigorous way than before.

The transition between ripples and dunes dependent upon sediment and flow conditions has been classically represented with a phase space diagram differentiating between the different bedforms based on these drivers. This work, importantly, introduces the role of clay content within the sediment and shows how this shifts these fundamental long standing relationships.

Many previous studies have examined the transfer of organic carbon in river systems within suspended sediment (fine particles carried in suspension making the water appear muddy etc..), however, few have looked at how much carbon is transported with bedload (coarser sand and pebbles that bounce along the base of the channel). This paper looks at the fluxes of carbon in the bedload and finds they are a far smaller percentage than that carried as suspended load, but may be more important for long term sinks or stores of carbon as they are more readily deposited in sediments that may become buried for a considerable period of time.