| Erosion |
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| TEKS: conservation Grade 3: 112.5.b11A Grade 4: 112.6.b1B Actually, the b1B in most grade levels addresses conservation Renewable/nonrenewable/inexhaustible resources – some address conservation and human impacts Grade 1: 112.3.b10 A-C Grade 3: 112.5.b11A Grade 5: 112.7.b11C Grade 7: 112.23.b14C (desertification, deforestation, urban sprawl/development, ...) Grade 8: 112.24.b14C (desertification, deforestation, urban sprawl/development, ...) Env Sys: 112.44c4E (desertification, deforestation, urban sprawl/development, ...), 5C |
TEKS: erosion
takes time: Grade 4: 112.6.b10A Grade 5: 112.7.b11A&C Grade 5: 112.7.b12A Grade 6: 112.22.b14A Grade 7: 112.23.b8A (kinetic energy related to erosion) Grade 7: 112.23.b14 A-C Grade 8: 112.24.b12A rock cycle Grade 8: 112.24.b14 A&C Int Phys Chem: 112.42c8A |
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![]() Black Sunday: April 14, 1935, Pampa, TX. Wind erosion was a terrible problem in the Great Plains of the United States in the 1930's during the Dust Bowl, and again in the drought of the 1950's. (Larger picture) |
Wind erosion is still a problem at times in some areas in the
Great Plains, as can be seen in these photos. These were taken near
Olney, TX circa 1998. (These trees did not grow with their roots out of
the ground!) This result of erosion is called pedestaling.![]() ![]() These were taken in various places in the Texas and Oklahoma Panhandles between 1994 and 2005. |
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| Though
wind erosion will always occur, it will probably never be as bad in the
United States as it was during the Dust Bowl because farmers are using
better technology to protect the soil. Even a small amount of residues
(leftover
plant parts) on the soil surface helps reduce erosion. Wind erosion was
not as severe in the "Filthy Fifties" due to the use of irrigation and
better management practices. However, wind erosion like this is currently a problem in Western China, and in the Sahel and Sahara regions of Africa. Link to story about April 2001 China dust storm |
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| Water can wash soil away, leaving rills (the small
finger-like areas
just larger than the pen), or it can wash away gullies that may be
deeper
and wider than a car. (Larger picture) (More on rills) Water can also wash off a thin layer from the soil surface. This type of erosion is difficult to detect. |
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When water washes soil out of one place, it leaves it
somewhere else.
The sand bar in this field was deposited after a thunderstorm that
created
runoff and erosion upslope. (Larger
picture) |
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| Soil that has no vegetation (plants) to protect it is the
most vulnerable
to both wind and water erosion. Soil was eroded out of the field on the
left,
and carried into the ditch beside the road. Some of the soil was left
in
the ditch after the runoff subsided. (Larger picture) |
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(Larger picture) |
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(Larger picture) |
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(Larger picture) |
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| Updated
06-27-2008. Copyright 2005. Clay
Robinson, Ph.D., as to
all resources: Materials may not be reproduced without Dr. Robinson's
written consent. Students are prohibited from selling (or being paid
for taking) notes or webpages during this course to or by any person or
commercial firm without the express written permission of the developer
of these pages. |
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