Abstract: In a sea, lake or other body of water, sedimentation of sedimentary solid material may be obtained in desired areas by reducing the hydraulic pressure in the sea floor or lake bottom layer in the respective area. Such reduction of the hydraulic pressure causes water to flow from the lake or sea into the porous bottom or floor layer whereby material suspended in the water or transported along the bed settles on the floor or bottom. The reduction of the hydraulic pressure is obtained by pumping water from underground drain tubes or other drainage devices extending along and adjacent to the coastline. The method may be used for coast protection and reclamation of land.