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Erosion – 21.2. Water Erosion. Erosion – process by which weathered material is transported. Common agents of erosion – gravity, wind, glaciers, running water. Stream Erosion. Water is constantly changing from one form to another through the water cycle Rivers flow into oceans
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Erosion – 21.2 Water Erosion
Erosion – process by which weathered material is transported • Common agents of erosion – gravity, wind, glaciers, running water
Stream Erosion • Water is constantly changing from one form to another through the water cycle • Rivers flow into oceans • Evaporates back to vapor in atmosphere • Falls on land as precipitation • All this movement – has the energy to carry and move sediment • Sediments is REMOVED from one location and DEPOSITED at another location
Parts of a River System • Main River • Tributaries – feeder streams that flow into main stream • Meanders – winding pattern of curves • Flood Plains - part of the valley floor that can be covered by water during a flood
Parts of a River • Channel – relatively narrow depression that a stream follows as it flows downhill • Banks – edges of a stream channel above water level • Stream Bed – part of channel that is below the water
Stream Load – material carried by a stream Suspended Load – velocity of stream keeps them from sinking Bed Load – larger, coarser materials- move by sliding and jumping along the bed Dissolved Load – mineral matter that has been dissolved and transported in solution
How much a river can carry depends on how much water and how fast it is moving. Headwaters – steep gradient, so has high velocity causing rapid channel erosion Mouth – gradient becomes flatter, velocity decreases, has less erosive power
Rivers with low gradients tend to have more bends • As river slows down, less energy is available to erode the stream bed • More energy is directed at the banks • Erosion around the bends and curves in meanders
Meanders can become so curved – form a loop or an oxbow lake
Stream Deposition • As velocity decreases the stream can’t carry as much sediment – so some sediment gets deposited • Can deposit sediment on land or in water
River Delta • As stream enters a large body of water such as an ocean or lake, velocity decreases suddenly – load is deposited in triangular pattern – called a Delta
Alluvial Fan • As stream descends slopes of mountains or hills and reaches a flat plain – speed suddenly decreases. • Stream deposits some of its load on the level plain at the base of the slope • Fan shaped deposit – Alluvial Fan
Flood Plain Deposits • As stream floods and spreads out – loses velocity and deposits sediments on the flood plains
Wave Erosion • Power of waves striking rock on shoreline – can sometimes shake ground as much as a small earthquake. • Force of waves break off pieces of rock and throw pieces back against shore. • Abrasion – reduces the rocks to pebbles and sand grains. • Usually takes place during storms • Also have chemical weathering due to salt content of sea water
Longshore Currents Transportation of sand along shoreline Will keep moving until shoreline changes direction
Does the stream below have a relatively steep gradient or a shallow gradient?
Does the stream below have a relatively steep gradient or a shallow gradient?
Do the following pictures show examples of stream erosion or stream deposition?
Do the following pictures show examples of stream erosion or stream deposition?