A means of alleviating or preventing flooding in geographic areas which are normally drained by slow moving water in ditches, rivers, bayous or other waterways of relatively shallow slope by using a water thrusting means to add kinetic energy and therefore velocity to a portion of the water, mixing the portion back in the main body of water in a downstream direction to increase the average velocity downstream of the main body of water, and thereby move water away from the flooding area to a remote area more quickly than would occur naturally.