Verdronken Zwarte Polder
This sea inlet area was created in 1802 as a result of a dike breach, which in 1623 built Black Polder flooded. The lost land has never since reclaimed more all over again. In the past two centuries, the area may develop into a particular area. The inflowing and outflowing seawater formed gullies in the former fields and put clay and silt. Here is a high arisen cope hoarse. The wind caused the remaining pieces dike were stewing by sand dunes so developed that limit the area on the seaward side. At the place where the levee breach occurred in the past, there is still a gap in the dunes. Through this opening the sea can still penetrate into the area. With water and wind every year many cubic meters of sand deposited in the area. Husky increases result in quick succession, and that again causes the area still flooded sparingly. A gradual sweetening of the area is due.