Lesson 1 What Are Weathering and Erosion? Fast Fact Rising Seas The Giant's Causeway, in Ireland, is made of basalt, which can form fiveor six-sided columns as it cools and shrinks. The sea is wearing away these cliffs. In the Investigate, you'll get an up-close look at one way rock breaks down. Shake Things Up Materials 6 medium-sized rocks 2 pieces of chalk empty clear plastic juice container with lid (2 qts) Procedure 1. Make a model of the way rocks break down in nature. Add two pieces of chalk to the container. 2. Place six rocks in the container. 3. Put the lid on the container. 4. Shake the container so that the rocks and chalk rub against each other. Do this for several minutes. You can take turns with your lab partner. Draw Conclusions 1. Compare the ways the rocks and chalk looked at the start and at the end of the investigation. 2. Inquiry Skill Scientists often infer the reasons for an investigation's results. Why do you think some of the materials in the container broke down faster than other materials? How do you think this relates to rocks in nature? Investigate Further First, weigh the chalk that is left after the investigation. Then, add water to the container and repeat the test. Compare the mass of the chalk before and after the water. What conclusion can you draw? 197 Reading in Science VOCABULARY weathering p. 198 erosion p. 202 SCIENCE CONCEPTS how weathering affects rock how erosion affects rock READING FOCUS SKILL CAUSE AND EFFECT Look for the causes of weathering. Weathering Have you ever seen a weed growing through a crack in a sidewalk? Maybe you've seen a statue with its features worn away. These are examples of weathering. Weathering is the breaking down of rock on Earth's surface into smaller pieces. Weathering helps shape landforms. It also helps make soil. There are two types of weathering. One type of weathering physically breaks rock into smaller pieces. The other type of weathering changes the chemical makeup of rock. This softens and weakens the rock, helping water wear it away. Water causes most weathering. It can break down some rock by itself. For example, water can wear away rock salt, calcite, and limestone. Sinkholes are the result of weathering. They form when water slowly dissolves underground rock. ---see pictures Water can help wear away bits of surface rock. A chemical change has turned the surface of this rock brown. Iron oxide, or rust, breaks down the outer layer of some kinds of rock. 198 Some rocks break down when oxygen combines with minerals in them. This often happens in rocks that have iron. When iron mixes with oxygen, iron oxide, or rust, forms. Rust makes it easier for other processes to weather the rock. CAUSE AND EFFECT What is the effect of weathering? Science Up Close Formation of a Sinkhole 1. Rain soaks into the ground. The rainwater dissolves limestone rock under the surface. Water carries away the dissolved rock. A small opening forms. 2. The opening in the rock becomes larger as time passes. 3. Rock and soil that covered the underground opening cave in. A sinkhole forms on the surface. Do you think this process happens quickly or slowly? Explain. ---see picture This 15-story-deep sinkhole formed in Florida in 1994. It formed in an area where large amounts of minerals were taken out of the ground. For more links and activities, go to www.hspscience.com 199 Weathering by Other Processes Physical weathering doesn't change the rock chemically. It breaks rock down through physical processes. Water, ice, living things, and wind are causes of this type of weathering. You see the results of this weathering around you each day. It can cause cracks in sidewalks and potholes in streets. Rain enters cracks in rock and cement. If the water freezes into ice, it expands. The ice cracks and breaks rock around it. Stones in streams are also a sign of weathering. These stones were broken from larger pieces of rock. As they tumble against each other, they break down even more. Large ocean waves weather coastlines. Waves smash into the bottom of a cliff. The rock that the waves hit cracks and breaks. In time, rock at the top of the cliff falls into the sea. Even temperature changes can weather rock. Rock expands when it heats up. It contracts when it cools. Repeated heating and cooling can 200 weaken some rock. The rock can then crack or break. Living things can cause weathering. You have probably seen plants grow through cracks in rocks. The roots wedge into the rocks, splitting the rock around them as they grow. Animals can cause weathering, too. When animals dig in soil, they move rocks closer to Earth's surface. Then rainwater can reach them more easily. Wind also causes weathering. Wind picks up bits of rock and soil and throws them against other rocks. This chips away the rocks' surface bit by bit. ---see pictures pg. 200 Pounding waves force air into cracks. This helps split the rock. Water also carries sediment. This scrapes rock as sandpaper scrapes wood. Waves hit cliffs like this with great force. Thousands of tons of water smash into coastal rocks during storms. ---see pictures pg. 201 Running water carries sediment. The sediment scrapes against itself and against rocks in the streambed as the water moves. Scraping and bumping against each other in a moving stream gives these rocks rounded edges. CAUSE AND EFFECT How does ice cause weathering? Insta-Lab Observe Weathering Use a large rock or brick to press down on a handful of rock salt. What happens to the rock salt? What kind of weathering does this model? 201 Erosion What happens after weathering breaks down rock into sediment? Erosion takes over. Erosion is the process of moving sediment. Water can cause erosion. Rivers carry sediment downstream. They drop it on their banks or at their mouths. Ocean waves pick up sediment and leave it on the shore as sand. Wind erosion is most common in deserts. With few plants to hold sediment in place, wind picks it up easily. Wind stacks sand into huge mounds called sand dunes. Glaciers are important causes of erosion. As these giant sheets of ice move, they scrape the ground. They pick up rocks and soil. During the last Ice Age, huge glaciers covered large parts of what is now the northern United States. As glaciers moved over land, they helped shape the plains and other landforms we see today. When the glaciers melted, they formed lakes. They left behind huge ridges of sediment and large amounts of water. CAUSE AND EFFECT What are the main causes of erosion? Math in Science Interpret Data What is the largest type of sediment? What is the smallest? Which would erosion affect more, boulders and cobbles or silt and clay? Why is that? ---see chart Water that washes over areas of bare soil can create gullies. Planting vegetation can help prevent this type of soil erosion. This photo shows one river flowing into another. Soil washes into rivers from areas along its banks. One of these rivers is carrying much more sediment than the other. The sediment has turned parts of the water brown. ---see pictures 202 Reading Review 1. CAUSE AND EFFECT Copy and complete the graphic organizer below. ---see chart 2. SUMMARIZE Summarize the lesson section on physical weathering. 3. DRAW CONCLUSIONS The Colorado River flows through the bottom of the Grand Canyon. Does the river cause weathering or erosion? Explain. 4. VOCABULARY Make a crossword puzzle using the vocabulary for the three lessons in this chapter. Test Prep 5. Critical Thinking You see a marble sign. Its letters are too worn to read. What caused this? 6. Which of these doesn't cause weathering? A. wind B. magma C. water D. plants Writing Narrative Writing Write the story of a grain of sediment that has been weathered from a mountain, carried to the sea by a river, and left on a beach. Write from the sediment's point of view. Math Solve Problems A farmer plants of his land with trees to stop erosion. If he plants trees on 525 hectares, how much land does he have? Show your work. Social Studies Famous Features Research a famous natural feature, such as a canyon, mountain, or rock formation. Explain how it formed. Draw a map that shows where the feature is located. Share with the class what you find. For more links and activities, go to www.hspscience.com 203