Bars and subaqueous levees often form at river mouths due to high sediment availability.
Once these deposits emerge and develop into islands, they become important elements of …

Sediment flux from rivers to oceans is the fundamental driver of fluvio‐deltaic
morphodynamics and continental margin sedimentation, yet sediment transport across the …

There is a pressing need to understand how different delta morphologies arise because
morphology determines a delta's ecologic structure, resilience to relative sea‐level rise, and …

River delta complexes are built in part through repeated river‐channel avulsions, which
often occur about a persistent spatial node creating delta lobes that form a fan‐like …

Recent field work at the Wax Lake Delta (WLD) in coastal Louisiana indicates lateral outflow
from channels to islands upstream of the receiving basin; in this region of the delta the flow …

Deltaic systems are composed of distributary channels and interdistributary islands. While
previous work has focused either on the channels or on the islands, here we study the …

We present a general model for channel inception and evolution in the deep sea by
integrating observations from two complementary datasets:(1) high-resolution multibeam …

Abstract The modern Huanghe Delta used to be the most rapid land-building delta in the
world. Its evolution has become a global concern because the sediment load of the …

Densely populated river deltas are losing land at an alarming rate and to successfully
restore these environments we must understand the details of their morphology. Toward this …

Mouth bars are morphological units important for deltas, estuaries, or rivers debouching into
the sea. Several processes affect the formation of these deposits. This paper focuses on the …