Hotel Zeezicht Vlieland Live Cam

Geological Setting and Coastal Morphodynamics

The coastline around Havenweg 1 on Vlieland emerges from a dynamic interplay of Wadden Sea tides, wind-blown sands, and underlying Holocene sediments. The island itself is part of a chain of Wadden Islands formed as barrier ridges and tidal marshes accumulated during post-glacial sea-level rise. Beneath the surface, Pleistocene sands overlie older peat layers and marine clay, creating a stratigraphy that affects drainage, foundation design, and dune stability. Near Havenweg 1, where harbor facilities and buildings meet the shore, understanding sediment transport is crucial: tidal currents continually reshuffle fine sediments in the approach channels, while prevailing westerly winds drive aeolian processes that shape adjacent dunes and deposit sand on quays and access roads. Regular monitoring of bathymetry through sonar surveys informs dredging strategies to maintain navigable depths, while dune surveys using GPS or differential leveling ensure the dune belt remains a resilient buffer against storm surges.