The Reversing Falls is a series of rapids on the Saint John River, located just west of downtown of Saint John, in New Brunswick, in Canada. Here the river runs through a narrow gorge before emptying into the Bay of Fundy. The tremendous rise and fall of the tides of the Bay of Fundy causes the ‘falls’ to reverse the direction of flow with each incoming tide.
As the bay tides begin to rise, they slow the course of the river and finally stop the river's flow completely. This short period of complete calm is called slack tide and is the only time that the boats are able to navigate the falls. Shortly after this slack tide, the bay tides become higher than the river, which begins to flow upstream. As the bay tides continue to rise, the reverse flow gradually increases and the rapids begin to form, reaching their peak at high tide. The effect of this reversal is felt upstream as far as Fredericton, more than 80 miles inland. At this point, tidal waters reach 14 ft higher than the river.
After high tide, the bay tides begin to fall and the upstream flow of the river gradually lowers until the bay tides fall to the level of the river—once again resulting in another slack tide. The river then resumes its normal course and begins to flow back out of the bay. The bay tides continue to fall below the level of the river until at low tide the rapids are again at their peak, flowing down stream.