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EROSION & DEPOSITION (teach)
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EROSION & DEPOSITION (teach)

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  • 1. Erosion and Deposition
    By Moira Whitehouse PhD
  • 2. In the last presentation we examined weathering. Now we will move to the concepts of erosion and deposition.
    They will be considered these two together because it is hard to separate them; one follows the other.
  • 3. Erosion—the movement of rocks and sediment from one place to another. The main agents are:
    1. Water
    3. Ice
    4. Gravity
    2. Wind
    Deposition—the dropping of sediment and/or rocks in another place follows weathering and erosion. Deposition occurs when:
    1. Water carrying the sediment slows down.
    2. The wind carries the sediment dies down.
    3. The glacier carrying the sediment melts.
  • 4. Here we see the processes acting of weathering, erosion and deposition working together.
    Gravity
    Deposition
  • 5. Agents of erosion: water.
  • 6. Water is the main agent of erosion.
    Running water carries weathered pieces of rock from one location to another.
    It can carry big pieces of rock as well as smaller rock pieces and soil.
    It can also weather rock at the same time as it is eroding it (carrying it away).
  • 7. Rock is worn away (weathered) at the same time that is carried away (eroded) by fast moving water.
    Rocks hit one another causing them to break.
  • 8. Fast moving water can move (erode) very large rocks transporting them downhill along with smaller rocks.
    http://www.flickr.comHamed Saber
    http://www.flickr.com Diego
  • 9. A slow moving river carries mainly pebbles, sand, silt and clay (sediment). The slower water cannot carry bigger rocks.
    http://www.flickr.com traveling lunas
    http://www.flickr.comwatchsmart
  • 10. As soon as the rushing water slows down, the larger pieces of weathered material it had been carrying is deposited.
    Photo courtesy daneen_vol of Flickr under Creative Commons license
  • 11. As can be seen by this diagram, as the water slows down, first the larger pieces fall out. And then as it flows slower and slower, smaller and smaller pieces are deposited.
  • 12. Soil and pebbles may be carried for a great distance as sediments in the river. As we said before, a river carrying a lot of sediment looks muddy. Shown here, sediments are being deposited at the mouth of a river in Lake Genoa.
    Wikipedia Commons
  • 13. http://www.arthursclipart.org/
  • 14. When sediments (gravel and soil) are deposited at the mouth of a river, a delta may be formed. It becomes a fertile area for to grow crops such as rice.
  • 15. Sediment deposited at the mouth of a river also may build a sandy beach.
  • 16. Sediment deposited at the mouth of a river also may build a sandy beach.
    • Some of the sediment carried by a river is deposited immediately at the mouth of the river.
    • Most of the sediment is suspended in sea water and is carried along the coast by the longshore current, a stream of water flowing parallel to the beach. This current is created by waves breaking at an angle to shore. 
  • 17.
  • 18. Agents of erosion: Wind
  • 19. Wind, the second agent of erosion.
    Wind picks up small pieces of rock or soil and transports them from their source to another location where they are deposited.
    http://www.flickr.com nukeit1
  • 20. When the wind blows in the desert, sand is continuously deposited in a different places. When the
    wind
    stops
    blowing,
    new sand
    dunes
    may have
    been
    formed.
  • 21. In this section we see will see mesas, buttes, arches, canyons and and other strange rock formations that were created through both weathering and erosion.
    The wind’s remarkable ability to sculpt such odd and beautiful landforms is explained by the hardness of the rock involved. Some rocks are softer and weather faster than others.
  • 22. Plateau with mesas, butte and gully
    http://www.flickr.com/
    puroticorico
  • 23. Photo of a mesa—this is what is left of the plateau
    that made up this entire landform before weathering
    and erosion carried much of it away.
    http://pics4learning.com/
  • 24. Photo of buttes
    What could the red line be depicting?
    http://pics4learning.com/
  • 25. Photo of arch
    Why was the middle of the arch
    eroded away and not the supporting sides?.
    Photo courtesy of USGS
  • 26. The difference in hardness of the rock composing the “cap” and the rock below the cap explains why the under rock weathered faster than the cap itself.
    a hoodoo.
    http://pics4learning.com/
  • 27. Here we can see that the weathering and erosion from these boulders is filling in the area beneath them.
  • 28. Over hundreds, maybe thousands of years,
    it could have happened something like this.
  • 29. On their way to the sea, some rivers wind across plateaus, carving deep valleys and taking sediment down stream with them.
    Once the valley walls become exposed, these rocks are further weathered by the wind, rain and changing temperatures.
    Over millions of year, these valleys can become giant, majestic chasms called canyons.
    The Grand Canyon is just such a canyon, it is continually being carved by the Colorado River.
  • 30. The Grand Canyon
    http://www.pdphoto.org
  • 31. Palo Duro Canyon
    Wikipedia commons
  • 32. In summary:
    How a delta and some beaches are formed through weathering, erosion and deposition.
  • 33. The river carries the sediment (tiny pieces of weathered rock including soil) downstream away from the canyon.
    This is called erosion.
    Whenever the river slows down, some of the sediment is deposited on the river bottom.
    The sediment that the river is able to carry to a lake or ocean is deposited at the mouth of the river and may form a delta or beach.