The lower shoreface, defined here as between about 8 and 20 m water depth, forms the
transition between the inner shelf and upper shoreface. Knowledge of lower shoreface …

Deltas require sufficient sediment to maintain their land area and elevation in the face of
relative sea-level rise. Understanding sediment budgets can help in managing and …

Many delta systems worldwide are becoming increasingly urbanized following a variety of
processes, including land reclamation, embanking, major engineering and port …

Natural levees are common features in river, delta and tidal landscapes. They are elevated
near‐channel morphological features that determine the connection between channel and …

River deltas commonly have a heterogeneous substratum of alternating peat, clay and sand
deposits. This has important consequences for the river bed development and in particular …

Many Holocene estuaries were infilled to form convergent, single‐channel systems, while
others remained partially or wholly unfilled. This difference in the degree of infilling depends …

To further detail insights into the composition and distribution of Holocene and late
Pleistocene deposits at the surface and in the shallow subsurface of the lower shoreface of …

A re-analysis of soil micromorphology samples and radiocarbon dates was undertaken at
the Middle to Late Neolithic settlement of N11, Hazerswoude-Rijndijk, in the Netherlands …

In the transformation from tidal systems to freshwater coastal landscapes, plants act as eco‐
engineering species that reduce hydrodynamics and trap sediment, but nature and timing of …

The first millennium AD encompasses the Roman period (12 BC to AD 450) and the Early
Middle Ages (AD 450 to 1050). In the Netherlands, this millennium saw population growth …