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14.1: Erosion by Streams

  • Page ID
    5563
  • What's different about these landscapes?

    Both of these rivers run through Yellowstone National Park. The Firehole River is a tributary of the Madison. In this photo, it's flowing over flat ground. The Yellowstone River on the right is cascading over Yellowstone Falls. Which river is doing more erosion? In what direction is the stream eroding?

    Erosion by Surface Water

    Water that flows over Earth’s surface includes runoff, streams, and rivers. All these types of flowing water can cause erosion and deposition.

    Erosion by Runoff

    When a lot of rain falls in a short period of time, much of the water is unable to soak into the ground. Instead, it runs over the land. Gravity causes the water to flow from higher to lower ground. As the runoff flows, it may pick up loose bits of soil and sand.

    Runoff causes more erosion if the land is bare. Plants help hold the soil in place. The runoff water pictured below (Figure below) is brown because it eroded soil from a bare, sloping field. Can you find evidence of erosion by runoff where you live? What should you look for?

    Runoff has eroded small channels through this bare field

    Runoff has eroded small channels through this bare field.

    Much of the material eroded by runoff is carried into bodies of water, such as streams, rivers, ponds, lakes, or oceans. Runoff is an important cause of erosion. That’s because it occurs over so much of Earth’s surface.

    Erosion by Streams

    Streams erode sediment from their banks. They pick up and transport sediments.

    A stream in the desert erodes the cliff face

    A stream in the desert rushes past its banks. The power of the water erodes the cliff face.

    As a stream erodes its banks, it creates a V-shaped valley (Figure above). This contrasts with the U-shaped valleys created by glaciers.

    Erosion and Water Speed

    Erosion by a stream depends on the velocity of the water. Fast water erodes more material than slow water. Eventually, the water deposits the materials. As water slows, larger particles are deposited first. As the water slows even more, smaller particles are deposited. The graph pictured below (Figure below) shows how water velocity and particle size influence erosion and deposition.

    Graph of how particle size and water velocity affect erosion and deposition

    Flowing water erodes or deposits particles depending on how fast the water is moving. It also depends on how big the particles are.

    Erosion in the Mountains

    Streams often start in mountains, where the land is very steep (Figure below). A mountain stream flows very quickly because of the steep slope. This causes a lot of erosion and very little deposition. The rapidly falling water digs down into the stream bed and makes it deeper. It carves a narrow, V-shaped channel.

    Stream flowing over a waterfall

    This mountain stream is in Whitney Portal in the Sierra Nevada of California. The slope is so steep that water cascades down in a waterfall.

    How Waterfalls Form

    Mountain streams may erode waterfalls. A waterfall forms where a stream flows from an area of harder to softer rock (Figure below). The water erodes the softer rock faster than the harder rock. This causes the stream bed to drop down, like a step. This creates a waterfall. As erosion continues, the waterfall gradually moves upstream.

    Diagram of how a waterfall forms

    How a waterfall forms and moves. Why does a waterfall keep moving upstream?

    Erosion by Slow-Flowing Rivers

    Streams eventually run onto flatter ground. Rivers flowing over gentle slopes erode the sides of their channels more than the bottom. Large curves, called meanders, form because of erosion and deposition by the moving water. The curves are called meanders because they slowly “wander,” or meander, over the land. Below, you can see how this happens (Figure below).

    Diagram of how meanders form and move

    Meanders form because water erodes the outside of curves and deposits eroded material on the inside. Over time, the curves shift position.

    As meanders erode from side to side, they create a floodplain. This is a broad, flat area on both sides of a river. Eventually, a meander may become cut off from the rest of the river. This forms an oxbow lake (Figure below).

    On oxbow lake along a river

    An oxbow lake forms in the Mackenzie River Delta, Canada.

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    Further Reading

    Deposition by Streams

    Summary

    • Faster water carries more and larger sediment.
    • Streams erode their banks to create V-shaped valleys.
    • A river on flat ground meanders. When a meander is cut off it may become an oxbow lake.
    • A floodplain is where the extra water goes when the river is in flood.

    Review

    1. Where along a meander does a river erode its banks? Where does it deposit sediment? Why?
    2. How does a waterfall form?
    3. How does stream erosion in the high mountains differ from that on flatter ground?
    4. How does erosion by runoff differ from stream erosion?
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