Description
At low discharge of the Rhine or due to a high water level at sea (by storm), salt water from the Nieuwe Waterweg can enter the main water system. As a result, inlet points can become salinised. These lines are an indication of where salinisation may occur
Resources
| Name | Format | Description | Link |
|---|---|---|---|
| OW_SAILING SYSTEMS | Unknown | Open resource | |
| OW_SAILING SYSTEMS | Unknown | Open resource |