Description
The Skeleton Coast of Namibia is defined by a meteorological phenomenon: the cold Benguela Current drives dense marine fog inland over the coastal desert daily, creating a collision of two ecosystems at the fog line — the hyper-arid Namib Desert and the maritime fog zone that supports a unique set of fog-adapted organisms. This aerial image captures the fog bank at the moment of its maximum inland penetration, approximately 50 kilometres from the coast: the wall of grey maritime fog is a vertical boundary advancing eastward over the orange dune field, the transition between fog and desert occurring within a few hundred metres. On the fog side, the dunes are grey and indistinct; on the desert side, the orange sand is fully saturated in morning sun. Shot from a light aircraft at 400 metres, the fog front’s vertical face is its dominant geometric element.
