generate questions: The Rhine-Meuse Delta is a tidal delta, shaped not only by the sedimentation of the rivers, but also by tidal currents. This meant that high tide formed a serious risk because strong tidal currents could tear huge areas of land into the sea. Before the construction of the Delta Works, tidal influence was palpable up to Nijmegen, and even today, after the regulatory action of the Delta Works, the tide acts far inland. At the Waal, for example, the most landward tidal influence can be detected between Brakel and Zaltbommel.
What type of Delta is the Rhine-Meuse? {sep_token} Besides rivers, what shapes the sedimentation of the rivers? {sep_token} What does a high tide risk near lands? {sep_token} Between Brakel and what other city can the most landward tidal influence be detected?