It sweeps and rolls sand, gravel and polished stones downstream, along the floor of the stream. Where a stream is following a straight course the slower boundary layer along the floor of the stream is also following the same straight course. The primary flow (the vortex) might be expected to sweep the solid particles to the perimeter of the bowl or cup, but instead the secondary flow along the floor of the bowl or cup sweeps the particles toward the center. The secondary flow will quickly sweep the solid particles into a neat pile in the center of the bowl or cup. Set the water in circular motion with a hand or spoon. Partly fill a circular bowl or cup with water and sprinkle a little sand, rice or sugar into the water. This movement of the boundary layer is capable of sweeping and rolling loose particles including sand, gravel, small stones and other submerged objects along the floor of the stream toward the point bar. ( Tropical cyclones, tornadoes, and the spinning motion of water as it escapes down a drain are all visible examples of vortex flow.) In the case of water flowing around a bend in a stream the secondary flow in the boundary layer along the floor of the stream does not flow parallel to the banks of the stream but flows partly across the floor of the stream toward the inside of the stream (where the radius of curvature is smallest). In vortex flow the speed of the fluid is fastest where the radius of the flow is smallest, and slowest where the radius is greatest. Point bar at a river meander: the Cirque de la Madeleine in the Gorges de l'Ardèche, France.Īny fluid, including water in a stream, can only flow around a bend in vortex flow. Point bars are formed as the secondary flow of the stream sweeps and rolls sand, gravel and small stones laterally across the floor of the stream and up the shallow sloping floor of the point bar. However, camping on a point bar can be dangerous as a flash flood that raises the stream level by as little as a few inches (centimetres) can overwhelm a campsite in moments.Ī point bar is an area of deposition where as a cut bank is an area of erosion. Due to their near flat topography and the fact that the water speed is slow in the shallows of the point bar they are popular rest stops for boaters and rafters. ![]() Since they are low-lying, they are often overtaken by floods and can accumulate driftwood and other debris during times of high water levels. ![]() ![]() They also have a very gentle slope and an elevation very close to water level. Point bars are composed of sediment that is well sorted and typically reflects the overall capacity of the stream. They are crescent-shaped and located on the inside of a stream bend, being very similar to, though often smaller than, towheads, or river islands. Point bars are found in abundance in mature or meandering streams. Cut bank erosion and point bar deposition as seen on the Powder River in Montana.Ī point bar is a depositional feature made of alluvium that accumulates on the inside bend of streams and rivers below the slip-off slope.
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