Suggested use of 2 Hour Class Day: -15 min set-up -15 min introduction -4 Centers, 20 min. each -15 min conclusion Introduction Please keep an eye on the “drying” sand bin in the ELF closet. Stir often to facilitate drying – if you’re there for lunch, a doc appt., or otherwise, go give the sand a stir!! 1 ELF Erosion April 1, 2013 Focus: The landscape continually changes over time due to forces of weathering and erosion by water (e.g., rain, rivers, groundwater, waves), wind, gravity, ice, and organic activities of animals, plants and humans. Opening Question: What is erosion, and how does it shape the landscape? The slide show provides an effective opening. The CD and script (K-2 and 3-6th versions) are in the ELF intro/conclusion bin. If necessary: please arrange laptop loan with the LMC prior to your ELF date. Remember to hit “pause” when first slide cues. Prior to or instead of the slide show, you might choose to discuss a few of the following concepts: Ask the students if any of them have run water into their sandbox. What happened to the sand? Show them a picture of the Grand Canyon and of a gully in the mud bank. Could both these features be formed the same way? Ask how these features were formed (running water). Could the Grand Canyon really have formed by water carrying away sand and pebbles? What are other examples of weathering and erosion by water? Ocean waves erode the shore. Caves form when underground water dissolves limestone. What about frozen water? Giant masses of packed snow and ice called glaciers grind away land to form valleys and lakes. What other forces cause erosion? Wind? (Important in dry climates like deserts, it “sandblasts” rocks.) Gravity? (avalanches, landslides) Plants? (Roots crack open rocks.) Do animals contribute to erosion? How do human activities affect erosion? When soil, sand, and rocks are eroded from one location, where do the materials end up? You can connect this unit with the previous unit on rocks by showing a rock cycle diagram and discussing how weathering and erosion fit into the rock cycle. Since rocks and soil are constantly eroded, why are there still mountains? Why doesn’t all land erode away and end up in the sea? (Mountains are formed by uplift of molten material from inside the earth.) What can prevent erosion? Can people prevent erosion? Why might you want to prevent erosion? A fun way to distinguish weathering, erosion and deposition are with the phrase “break, take and make.” Weathering breaks down rock to sediment, erosion takes it away, and deposition makes new landforms. ELF Intro Bin: Five puppets This puppet show follows Ricky Rock and Billy Boulder as they experience different kinds Sheet for stage of changes through weathering and erosion. There are six speaking parts; one is a voice with no puppet. One puppeteer could do both Ricky and Tiny Ricky, and another could do Spray bottle both Billy and Tiny Billy (using higher voices for the tiny versions). Puppet Show Afterwards, review with students the forces of erosion identified in the show: glaciers, gravity, rain, rivers, human activity (tree cutting), wind, and waves. 2 Centers – there are SIX centers, you only have time for FOUR. Center 1: Shaping the Land/Blowing in the Wind Shaping the Land Objective: To identify examples of weathering and erosion and their causes. Show pictures of land changed by erosion. The photos show features formed by various agents of weathering and erosion: wind, moving water (ocean, rivers, runoff), gravity, as well as the effects of animal and human activities on erosion. Have the students discuss each photo: how the processes of erosion affected these landforms. Each photo has a key on the back. Point out how the landforms caused by wind erosion relate to the previous experiment. Several forces may work together – there are no real wrong answers. Use photos from books, such as Shaping the Earth – Erosion by Downs and Erosion by Rutten, to supplement this activity. If time permits, you might review the laminated articles. If you do not wish to use the photos for this center, you may want to use them in the closing or as examples of erosion in another center (Center 2?). Blowing in the Wind Objective: To explore the effects of wind eroding the landscape. If there is sand in the plastic tub, pour it into another container. Place a few small items in the tub (penny, bell, etc) and then pour in about an inch of dry sand. Cover the pan with the plexi-glass and give each student a straw. Ask the students what will happen to the sand if they blow the sand using the straw. Have the students take turns to insert a flexible drinking straw, bent at nearly 90 degrees, through the hole in the plexi-glass and blow the sand. Encourage them to move the straw around in different directions, noticing places where sand builds or gets hollowed out. Students should not share straws. Where might this type of erosion occur? Ask what will happen if the surface of the sand is moistened with water. Then, remove the plexi-glass and let them use a spray bottle to dampen the sand lightly (3-4 sprays). Replace the cover and let the children try to blow the sand again. What happens differently this time? Afterward, ask them in what environment is wind most effective as an agent of erosion? Discuss how wind affects deserts, sand dunes, and beaches. Discuss why wind might cause more erosion in a desert that in a jungle. Can wind wear down rocks? Discuss how wind picks up sand and “blasts” rocks, wearing them away like a sandblaster. This is called “abrasion.” After each group, pour out the damp sand into the drying bin and replace with dry sand. When all rotations are completed, leave the sand in the plastic tub to dry. Center 1 Bin Soda Straws Plastic tub DRY Sand Plexi-glass w holes Spray bottle Misc. small items to bury in sand Container for damp sand Laminated photos Laminated Formation of a Sand Dune Laminated Chemical Weathering Laminated Chemical vs. Physical Weathering Books: Sand Dunes by Bannan; Sand on the Move by Gallant; Sand by Prager. Please keep an eye on the “drying” sand bin in the ELF closet. Stir often to facilitate drying – if you’re there lunch, a doc appt., or otherwise, go give the sand a stir!! 3 Center 2: Erosion Hunt ELF Center 2 Bin Laminated Objective: To discover signs of erosion and weathering on the school grounds. “Erosion” drawings Especially for the first rotation, you might begin by showing the group erosion photos from Laminated: the laminated sheets or from the books.. erosion web Laminated: Then take the students outside to look for effects of erosion and weathering around the Weathering and school grounds. Good examples may be found near drains and at the edges of black tops. Erosion Venn Look on the hill south of the school between playgrounds and directly behind the school Diagram (on the side down the stairs) for signs of water runoff, human impacts, and the role plants Maps of school play. What is the effect of fences? Look for worn pathways in the dirt, erosion around Clipboards downspouts, crumbling edges of blacktops, chipped paint, and cracked concrete. Also look for rust – caused by oxidation, a form of chemical weathering. Discuss possible agents weathering the different sites. Where is the eroded material going? Look for signs Classroom of deposition, around downspouts and below runoff features. What could be done to slow Pencils or prevent the erosion they see? What has been done? (Gravel, netting, terraces, Paper (optional) retaining walls, sealant in cracks, concrete gutters, diverters below downspouts). How does gravel affect erosion? Grass and trees? You might find potholes on the adjacent road or parking lot. Discuss the weathering impact of repeated freezing and thawing of water that seeps in to cracks in roads or rocks (freeze wedging). Discuss how plants, animals, and people affect erosion. Then discuss how erosion affects the plants and animals that live in the area. What can be done to slow down or prevent erosion on the school grounds? Ask the students to describe specific erosion sites, discuss whether something should be done to prevent further erosion, and if so, what ideas do they have? With younger students, simply explore the grounds, discussing the features that are found. Allow them to sketch the erosion features on paper, if they wish. For older students, hand out clipboards and the maps of the school grounds. Have students mark the locations where erosion is taking place, noting what forces are at work (e.g., water runoff) with different symbols of their own design, including a key to their symbols. Alternatively, kids could write or sketch their ideas for erosion control at Mitchell. 4 Center 3: Splash Objective: To discover the power of raindrops on the earth. This is a floor space center. Begin by asking how raindrops might cause erosion. Since each raindrop is small, can it contribute significantly to erosion? What about the combined effects of heavy rains over time? What might rain do to loose top soil? Explain that this center will involve experiments to show how raindrops cause weathering and erosion on materials representing different soil types (flour, sand and gravel for fine to course soil types). Set the plastic table cloth on the floor and then set down one of the blue plates with waxed paper on it. Place only a spoonful of flour in the center of the sheet on the waxed paper. The flour represents dry, fine soil. Ask for predictions of what will happen when a drop of water (simulated raindrop) hits the flour. For younger kids, you might prompt ideas (will the flour puff up? Will it scatter? How far do you think some will move?). Review the predictions and the process with the group. Then, have one student stand, holding the baby bottle or eyedropper at waist height over the plate, and gently squeeze out ONE drop of water so it falls onto the flour. What happens? Then, ask the student to hold the bottle or dropper at head height and squeeze out another drop. How are the results different? Ask the students for their observations and use the laminated data sheet to record your findings. Did their predictions match the results? Older students might measure the distance of the spatter from the flour pile for each attempt and later graph the results. Is waist height and head height going to be the same for each student? How might that change the results? Depending on the size of your group, and the time you have, let students take turns conducting the flour experiment, then place just a spoonful of sand on fresh waxed paper on a second blue plate. How might the sand react differently from the flour when hit with a raindrop? Collect predictions and then repeat the process of squeezing a water drop from waist height and head height onto the soil. Lastly, use the gravel, taking predictions and repeating the test process. Once the experiments are completed, ask students for their conclusions about the effects of raindrops falling from the sky on loose soil. Will the rate and duration of rain impact the results? Will the composition of the soil matter? Rainwater causes weathering when it hits the surface soil and it carries away soil once it rains enough for there to be “runoff” from the rain (flooding and river action erodes land). Start with a spoonful of dry flour, sand, and gravel for each rotation. Please use only a spoonful of each “soil type” for each test. When finished, please use paper towels to wipe dry the garbage bag, blue plates, eye dropper, and baby bottle before returning them to the Center 3 box. If time permits, review the laminated handouts about water erosion: “Which is stronger: Rocks or Water?” “Rivers: Water is Powerful” and/or “The Outside Story.” Center 3 Bin Plastic spoon Baby bottle, mini bottles and eyedroppers 3 blue plates Waxed paper Plastic table cloth Containers of flour, sand, and gravel Laminated Handouts Laminated data sheet for observations as a group Classroom Paper towels Water 5 Center 4: Slipping Soil Objective: To experiment with various landscape designs to limit or control erosion. Tell students that they will examine the impact of water runoff on top soil and try to come up with solutions to help reduce the effects of erosion. Prepare the erosion table so it contains a thin layer of packed sand and forms a slope. Fill the table with sand only to the shallowest tier. Be sure drain spout is at the bottom. Place plastic hose in empty pail on floor to drain. (use rags from home to prop up the table and make a slope). The steepest slope will be at the high end of the table and taper off so the sand stops 10-12 inches from the lower end of the table. The exposed lower end needs to be clear of sand (it depicts a clear stream bed). Tell the children that the slope represents a bare hillside on which all trees have been cut, with a clear stream running at the base of the hill. Briefly summarize “clear cutting” logging and disruption of vegetation for construction. Show some photos of landslides from Landslides, Slumps and Creep by Goodwin. Ask for predictions about what will happen to the bare slope when rainwater runs down it? Then, slowly sprinkle water from the top of the slope using a watering can. Ask for observations about what happened to the bare slope and to the stream below it as a result of the water runoff. Point out the quantity of sediment in the “stream” for later comparison. What will happen eventually if nothing is done to limit the effects of this erosion? How would animals be impacted if this were a real slope? Now, explain that students must develop and put in place a plan to reduce the extent of erosion. Ask them about control methods they have seen in their neighborhoods or in the mountains. Show photos of erosion control methods from the books Soil and/or Erosion both by D. Stille. Use the following sorts of questions to help them formulate their erosion control plan (show them the materials they have to work with): How can the soil be held in place? What could be added to absorb the water rather than let it run off into the stream? What might divert the water flow? Center 4 Box wood twigs, rocks, twigs, plastic netting, sponges, greenery, etc Watering cans Pail for drain Plastic tablecloth Trowels Shovels ELF Storage area Erosion table Sand in bucket – wet sand Classroom Water Paper Towels Volunteer Old “wash-thedog” type towels for clean-up Once students have decided on a plan, let them use the nets, greenery, sponges, fabric, etc. to implement it. Then, let them test their plan by sprinkling water down the top of the slope. Ask for observations as the water moves down the slope and comparisons of the amount of sediment that reaches the “stream” versus the amount that occurred prior to implementing the plan. At the end, talk about the importance of erosion control on ecosystems, and discuss matters like the importance of staying on marked hiking trails rather than cutting across switchbacks, which can contribute to erosion. For each rotation, build the slope back up and clear space for the stream. Add a thin layer of dry top-sand (smooth with trowel). When rotations are complete, please dry off all materials before placing in Center 4 box. Please pour sediment water from pail outside. Empty erosion table and dry for next use. Replace sand in the bucket (NOT BIN) to dry for later use. Centers 5 and 6 involve aspects of weathering. Weathering is the breakdown of rock (break), while erosion is the transport of the products (take). The two types of weathering are chemical and mechanical (or physical) weathering. Chemical weathering involves decomposition (acidic rain or groundwater, oxidation, lichen). Mechanical weathering involves physical forces that fracture rocks (water freezing and thawing in small cracks, growth of mineral crystals in cracks, abrasion from wind, crashing waves, and prying action of plant roots). Ultimately, weathering processes results in the creation of soil. The forces of chemical weathering and mechanical weathering often work in combination to break down rocks and form soil. 6 Center 5: Shake, Rattle, and Roll / Frozen Erosion Objective: To examine the weathering effects of abrasion on rock. Shake, Rattle, and Roll This center examines mechanical weathering through the impact of water and abrasion on rocks. Ask students to fill both lidded containers with pieces of rock to the line marked ROCK. Next, have them fill both containers with water to the line marked WATER. Screw both lids on tightly and set aside the container marked DON’T SHAKE. Now, pass around the container marked SHAKE, and have each child take a turn shaking it at least 20 times. Keep track of the total number of times it is shaken, with 100 shakes as a minimum. Pour the water from both containers into separate clear cups and compare the water from the container that was shaken to the water from the container that was not shaken. Is the color of the water different? Why? Why are there fine particles floating in the water from the SHAKE container? Where did they come from? Where might a similar process occur in nature? Perhaps the “DON’T SHAKE” jar represents a calm lake, while the “SHAKE” jar represents a river or a beach, where rocks are jostled against each other. Center 5 Bin 2 lidded jars: one marked SHAKE and one marked DON’T SHAKE Clear cups Water pitcher Pieces of sandstone River rocks Beach glass Venn diagrams and charts of chemical vs. physical erosion Coffee filters Let the students pour the contents of the two jars through the filters to compare the amounts of sediment. If you don’t use coffee filters, you might set the clear cups aside so the sediment in them can settle during other rotations. At the end of the unit, the coordinator may wish to use these to point out how the sediment has been deposited in the bottom of the cups. Empty the wet rocks onto a paper towel between rotations. When finished, please dry off the rocks and spread on paper towel to dry more before next use. Next, pass around some smooth river rocks and beach glass from the ocean for the children to feel and observe. Do you think these pieces were always smooth? How did they get this way? How did our experiment help us to determine this? Frozen Erosion FROZEN EROSION Center 5 Bin Scratch rock Gloves Books: Glaciers (by George), Glaciers (by Brimner), Glaciers (by Walker) Spread an old towel on a table. Let each student use an ice cube with gravel imbedded as a ‘glacier’ to scrape the scratch rock (moving one direction). Please use one ice cube per Volunteer: student. Ask them to imagine how this scraping might work with huge rocks over ten Cooler to keep thousand years. Look through the books, and show the students pictures of terrain that ice cubes cold has been shaped by the passage of glaciers. Old towel Note: Bring a small cooler to keep the ice cold. Remember to bring in ice with gravel imbedded in it. Ice cubes w/ pebbles frozen inside Explain that glaciers are nature’s bulldozers and that ice has an adhesive grip, which you can feel if you touch cold ice with damp hands. Because of this grip, rocks are “plucked” up by glaciers as they move, and these rocks give glaciers tremendous powers of erosion. Like a giant file, the flowing rocks and ice grate against the underlying terrain. Large bowlshaped hollows, called cirques, are formed. When two glaciers occupy valleys that lie side by side, they produce a sharp, jagged ridge called an arête. Glaciers slide along because their bottom layers may begin to melt, or creep due to friction of adjacent crystal layers. 7 Center 6: The Hole Story Objective: To learn about caves and discover how they are formed. The process of forming caves in soluble rock is very slow. It begins with rain water falling through the air and picking up carbon dioxide. Then, as the rain water soaks into the soil, it picks up more carbon dioxide that is being given off by the decaying vegetation in the soil. The combination of water and carbon dioxide forms carbonic acid, which is similar to the fizz in a coke. Over thousands of years as the carbonic acid seeps through the cracks and crevices of soluble rock (such as limestone, dolomite, gypsum or marble), cavities and channels are formed creating underground rooms and chambers. When carbonic acid seeps through limestone, it absorbs the calcium carbonate out of the limestone (remind students of the “fizz” test with vinegar that they performed on limestone rocks during the “Rocks & Minerals” unit). This dissolved mineral is dripped into the cave where the carbon dioxide is then released. Without the carbon dioxide, the water can no longer carry the minerals, so they are deposited as tiny crystals. Sometimes calcite (or another soluble mineral) is deposited as the drips hang from the ceiling of the cave, forming a stalactite. As they drop to the cave floor, they deposit more minerals and build up stalagmites. Beads of moisture sometimes deposit minerals on the cave walls in rough-looking clusters called cave coral. Alternatively, water flowing slowly down the walls or across an incline in the cave form smooth-looking formations known as flowstone. Mineral formations can take many different shapes, depending on the way the water comes into the cave. Guide the students to make a model of a cave being formed: (students could work in pairs or as individuals) 1. 2. 3. 4. Place 12 sugar cubes close together on a tray, forming a rectangle (4 x 3 cubes). [one layer of sugar cubes seems to work better than stacking them] Make a pancake out of clay that is larger than the sugar cube rectangle. Place the clay over the cubes and press down the 2 side edges so that they attach to the plastic plate. Leave the front and back open for water flow. Place the tray into a tub resting on the edge so that it is tilted. Slowly squeeze a baby bottle of water in a stream that runs into the sugar cube ‘rock’. (use about 1/3 of a bottle per cave) After a few minutes, check to see if the ‘rock’ is being eroded, and if a cave is being formed. Use a flashlight to explore inside. If all the ‘rock’ has dissolved, try again with a little less water. If very little ‘rock’ has dissolved, try again with a little more water. Think about what might happen if there were rock that was very hard to dissolve mixed in with the rock that is easier to dissolve. If we did the experiment again making small cubes of clay the same size as the sugar cubes, and mixing them among the sugar cubes, what do you think would happen? Maybe do this with older students, if time permits. Share some pictures of caves with the students, looking at the formations. Center 6 Bin Sugar cubes Plastic plates Modeling clay Flashlights Baby bottles Measuring cup Books: Cave by Knapp; Caves by Brimner; Caves by Walker Classroom Water Paper towels CleanUp is monumentally important with this center. Rinse the sugar off the clay and pat dry with paper towels. Let us know if you are running low on supplies: MitchellELF@ gmail.com 8 Wrap-up Options Slide Show: If you opted for puppet show only for your opening, use the slide show as a visually powerful closing. Sharing Circle: Have the kids sit on the floor, forming a circle. Let them pass around the SHAKE jar or scratch rock from Center 5 (or some other erosion symbol) and pass it along, as each student who holds it completes the sentence: “Something interesting about erosion is ______” or “I learned that erosion _______.” Read a Book: Earthsteps, A Rock’s Journey through Time by Spickert, Erosion by Rutten, or The Sun, the Wind, and the Rain by Peters. Erosion Snack Anyone? – Some kind of cookie or brownie covered loosely with powered or granulated sugar, which the kids could use their straws to blow off (wind erode) before eating? Please keep an eye on the “drying” sand bin in the ELF closet. Stir often to facilitate drying – if you’re there for lunch, a doc appt., or otherwise, go give the sand a stir!! Books In addition to those books listed above for use with specific centers, the following books are available: Earthsteps, A Rock’s Journey through Time (Spickert) Erosion (Riley) Learning About Rocks, Weathering, and Erosion with Graphic Organizers (Estigarribia) The Sun, the Wind, and the Rain (Peters) Valleys and Canyons (Brimner) Materials For your classroom session, you may need: 1. Puppet stage 2. Intro/Conclusion bin 3. Center 1 bin 4. Drying Sand bin 5. Center 2 bin 6. Center 3 bin 7. Center 4 bin 8. Erosion table 9. Center 5 bin 10. Center 6 bin You will need the center boxes for only those centers that your class will conduct. THE THREE KEYS TO THIS UNIT ARE TOWELS, TARPS, AND TAKING CARE TO LEAVE MATERIALS IN GOOD CONDITION FOR THE NEXT CLASS. HAVE FUN!
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