|
Breaking Up is Hard to Do |
| It's spring. You are going up the canyon with
your family as you've done many times before; and all of you know this road.
Its twists and turns provide treasured glimpses of the beauty of nature
when suddenly - bonk! bumpity-bump! bonk! Your nature trek becomes a dodge-the-pothole
challenge. The road has been changed; attacked by weathering and erosion.
During the winter, water penetrated the road's surface. It froze and expanded,
creating cracks. More water got into the cracks and it froze, making the
cracks wider. Melting snow carried particles of road away. What remains
is a changed surface, and not for the better. Earth's surface is also constantly
changing. Weathering breaks rocks into smaller pieces. Erosion
carries the pieces away. Together these forces slowly wear down Earth's
surface. The main agent of weathering and erosion is running water. |
Living
Agents of Change
Living things can also weather and erode rock. Plants
have roots as you know. The roots can force themselves between rocks.
As the plant grows, the roots grow, forcing rocks apart. This is called
root pry.
Do it!
- Take a walk around your neighborhood.
- Look for signs of plant weathering. Describe what
you observe.
- If you have a camera. Take pictures of the evidence
that plants have caused sidewalks, roads or even playgrounds to weather.
Do it again!
- At home and with parent permission, you will use a frosted pastry
such as a Zingers® or Ho Ho’s® for
this activity.
- You will also need toothpicks.
- With a friend, begin inserting toothpicks into the
pastry, applying a bit of upward pressure.
- What changes in the pastry do you observe, what happens
to the frosting?
Analysis:
- How is the pastry like a structure affected by plant weathering?
- How are the toothpicks like plant roots?
|
Animals
can physically break rock down and move particles away. Marmots scratch
and move material while digging dens. Ants haul pebbles. We humans skip
rocks across the lake. |
Remember the cracks made by the roots? When
winter comes water will penetrate those cracks just like it did the road
surface. The water will freeze, widening the cracks and breaking the rock.
Spring's thaw will carry particles away. Gusty winds hit the rock's surface,
picking up tiny particles. These particles blow about, not unlike a sandblaster,
wearing down even more of the surface. |
|
|
|
|
Get the plug-ins:
, and
(The QuickTime plug-in is needed to play sounds and movies correctly.)
Want to share photos of you or your friends doing this activity? Send
in an e-mail with the
following information: the title of the activity, the URL (Internet
address), and your name. Remember that no pictures can be used which
show any student faces or has a student name.
|
|