The experience of the Noordoostpolder had shown that groundwater from the higher old mainland would flow to the lower new land, causing subsidence and dehydration in the old land. It was decided to use geohydrology to detach the new polders from the mainland. A string of peripheral lakes have been left between the two, requiring a much longer dike of to encircle the polder.
The experience of the Noordoostpolder had shown that groundwater from the higher old mainland would flow to the lower new land, causing subsidence and dehydration in the old land. It was decided to use geohydrology to detach the new polders from the mainland. A string of peripheral lakes have been left between the two, requiring a much longer dike of to encircle the polder.