A knick point is a sudden break or irregularity in the gradient along the long profile of a river. Some knick points are sharply defined, for example waterfalls, whereas others are barely noticeable. Although a number of factors can cause such features to occur, they are most attributed to rejuvenation.
When a river is rejuvenated, adjustment to the new base level starts at the sea and gradually works its way up the river's course. The river gains renewed cutting power (in the form of vertical erosion), which encourages it to adust its long profile. In this sense the knick point is where the old long profile joins the new. The knick point recedes upstream at a rate which is dependent on the resistance of the rocks, and may linger at a relatively hard outcrop. It can be difficult to determine whether a waterfall occurs due to the variability in rock type or to rejuvenation. Headward erosion upstream may mean that a waterfall cuts back through the valley towards its source until the long profile eventually adjusts to its new energy equilibrium.
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