These classroom activities will help students understand 4 types of weather processes: wind, running water, plant growth, and freezing water.
Worksheets for each student
Activity 1 Materials
Activity 2 Materials
- 16 oz. paper cups
- Colored Chalk
Activity 3 Materials
- Plastic bottle with lid
- Small pieces of sandstone (about 3 pieces per bottle)
Activity 4 Materials
- 16 oz. paper cups
- Bean seeds
- Plaster of Paris
- Paper towels
- Small plastic bags
- Clay (the soil kind)
- Bill Nye Video, Erosion. The "Rocks and Soil" episode also has a very good
segment on weathering.
- Dirt: Secrets in the Soil: The first segment after the introduction talks about
how long it takes to form a layer of topsoil. After the words "Nitty-gritty," there
is a five-minute segment that specifically talks about how rocks are broken
down by water, roots, and chemicals.
Background for Teachers
Soils form over millions of years from parent material that is broken down by weathering from wind, water, temperature, chemical changes, and living organisms. Over time, glaciers move over the land and grind rocks together, rubbing off particles of all sizes. By day, rocks are warmed by the sun and expand, while at night the rocks cool and contract.
Over time, enough expansion and contraction cause rock particles to chip off. In cold temperatures water in the cracks of rocks freezes and expands, causing the rocks to break into smaller pieces. Plant roots will grow into "soft" rock and cause them to break. Water and wind wear away at rocks carrying tiny bits of rock along until they get trapped by soil.
Many rocks are broken apart by lichens. Lichens are tiny crusty, coral-like plants (green, orange, gray, etc.) that live on rocks. These tiny plants secrete an acid that dissolves some minerals and breaks down the rock. Decaying plants and animals are organic matter. Organic matter is also acidic. When water and organic matter mix, they form a slightly acidic solution that breaks down rocks in soil That is why soils in the eastern United States are more acidic than the soils in the West. They contain more organic matter.
Organic matter is good for plants. It keeps topsoil in its place, keeps soil particles together, retains soil moisture, and speeds up soil formation. It takes between 100 and 500 years for just one inch of topsoil to form, depending on the type of rocks and climate.
Intended Learning Outcomes
1. Use a Science Process and Thinking Skills
Pre-Assessment/Invitation to Learn
Ask the students to consider thee questions: Which is stronger, a plant or rock? Is water stronger than a rock? Would you expect water to damage or break apart large rocks?
Students should draw diagrams illustrating each of the following types of weathering processes. Some of these will occur over a period of days and weeks. They should draw and label a series of diagrams to show the progression of weathering.
Activity 1 - Wind as an agent of weathering
- Give groups of students a cup half-filled with salt and a colored piece of chalk. Have them take turns stirring the colored chalk through the salt.
- Two things will happen: the salt will be colored and the chalk piece will wear away. Relate this to wind blowing sand on rocks and wearing them away like the formations seen southern Utah. (Instead of wind blowing sand against Arches, tell them the chalk represents Arches and they are moving Arches through the sand.)
Activity 2 - Running water as an agent of weathering
- Compare river rocks with sharp-edged rocks. Rub two pieces of sandstone together and notice the pile of sand that collects.
- Fill the plastic bottle 3/4 full of water.
- Drop in three or four small pieces of sandstone.
- Make sure the top is screwed on tightly. Have students observe the clean, clear water, and the shape of the rocks.
- Shake bottle vigorously for three minutes.
- Examine water. Take stones out. Observe the weathering (rounded edges).
Activity 3 - Plant growth as an agent of weathering
- Explain that Plaster of Paris hardens and will represent rocks in this demonstration. Mix the Plaster of Paris quite well and pour into a disposable 16 oz. cup. "Plant" several bean seeds in the wet mix so that some are covered and are just below the surface and the others are resting on the surface (about half submerged).
- Assign a student to keep a wet folded paper towel on top of the cup. It must be moistened every day. (Soaking the seeds ahead of time will hasten their growth.)
- Ask students to predict what will happen to the seeds. Record predictions and subsequent observations in their science log.
- Over the course of two to three weeks you will see the seeds sprout. As they do, small fragments or flakes of the Plaster of Paris will break away. These flakes represent rock flakes broken away from large rocks as plants take root and grow on them.
Activity 4 - Freezing water as an agent of weathering
- Wet a chunk of clay about the size of a grapefruit. Roll it into a ball.
- Place the ball in a plastic bag and put it in the freezer. Leave it overnight.
- Next day, removed the clay from the freezer. Its surface should be slightly cracked and broken. Ask students to record their observations.
- Wet the clay again, taking care not to close up the cracks that have been formed. Put it back into the freezer for another night.
- On the following day, take it out and have students observe what has happened to the cracks. Measure the cracks. You could repeat this process several more times, watching the cracks widen. Discuss how this relates to the breaking down of rocks on a larger scale. Compare this to autumn rains filling cracks in the rocks (and sidewalks) then freezing during the winter.
- Measure the length of objects to the nearest 1/4 inch. (Standard IV, Objective 2)
- Use the different colored salts to make “sand” paintings. Gather baby food jars
and pour layers of different colored salts to make colored “sand” jars. Fill
completely and don’t shake. (Standard I, Objective 1)
- Another way to show weathering by acid - Place a piece of limestone in a small
jar. Cover with clear vinegar. Have students observe the “fizzing.” Explain
that the calcite in the limestone is reacting with the weak acid of the vinegar.
Together they create carbon dioxide gas that is released through the bubbles.
This action breaks down some rocks. For added interests, let the fizzing continue
over night. Pour some of the spent vinegar into an evaporation dish (petri dish
or flat lid). Let the liquid evaporate and look at the calcite crystals that form.
Examine the limestone for pitting caused by the acid. (ILOs 1, 3, 4)
Homework & Family Connections
Find examples of weathering around the home and on trips. Make a photo album
showing examples of all types of weathering.
Take a tour around the school grounds to look for evidence of weathering.
Show pictures and categorize types of weathering illustrated.