Relative Age Dating By Nancy Volk Law of Superposition One of the fundamental laws of archaeology is the Law of Superposition. The law states that sedimentary layers are deposited in a time sequence, with the oldest on the bottom and the youngest on the top. Weathering and Erosion When a rock layer is not parallel and smooth but appears irregular (see the interface between layers C and D), then erosion and weathering occurred and like a big eraser removed part of the history of the rock layer. We compare the rock layers to other areas to try and find clues to the missing evidence. The rock layers below show this abnormality. VOCABULARY Anticlines Faults Folds Igneous Law of Superposition Sedimentary Synclines HELPFUL TERMS Absolute age dating Fractures Lava Magma Monocline Relative age dating We still know the youngest to the oldest. What is the order? Sequence What type of rock creates layers? What About Igneous Rocks? When an igneous activity comes into play in an area with sedimentary rock layers it can push through the cracks of layers making interesting formations. When an igneous activity occurs it is always younger than the rocks it moves, flows through or erupts over. Think about this and see if this makes sense! Inside This Packet Relative Age Dating 1 New York State Standards 1 Activity: Layers 2 Demonstration/Activity: Rock Layers 3 Paper Block Printouts 4-7 New York State Standards Middle School Activity Standard 1: Analysis, Inquiry, and Design What is the order of oldest to youngest rock layers? Earth Science - Prior Module 4 Middle School Standard 4: Physical Setting Key idea 2.1c, 2.1f, 2.1g, 2.1h, 2.1i, 2.2a, 2.2c, 2.2g Page 1 Demonstration: Age Dating MATERIALS NEEDED Canning jar and lid Food coloring Modeling clay Scissors Tape Wax paper What to do: 1. Take the glass canning jar and fill it about 1/3 full of sediments that are multi-sized particles. 2. Fill the remainder of the jar with water. Cover tightly and add electrical tape around the perimeter of the lid area to add more security. 3. Shake vigorously. 4. Allow the sediments in the jar to settle for several days. Notice what occurs to the sediments as they are deposited. 5. The students should be able to see layers of sediments settling out from the stirred water. Discuss how this happens in locations on earth in streams, ponds, lakes and oceans. Students should be able to: Identify layers of deposition Describe the relative ages of sedimentary layers Earth Science - Prior Module 4 Middle School Page 2 Demonstration/Activity: Rock Layers MATERIALS NEEDED Modeling dough (recipe provided) Plastic knife Wax paper Using modeling dough (recipe provided below) add three different colors to make three different rock layers. Have students roll out three different layers and place them on top of one another. Have them create anticlines, synclines and describe how they made these. Have them discuss how this is like the forces in the earth causing rock layers to bend and fold. They can explore ideas about faults with the use of a plastic knife as well. Have the students work with the modeling dough on top of wax paper for easy cleaning. Paper block printouts Tape Modeling Dough Recipe 1 cup flour 1. Mix flour, salt and oil, and slowly add the water. 1/2 cup salt 2. Cook over medium heat, stirring until dough becomes stiff. 1 cup water 3. Turn out onto wax paper and let cool. 2 tablespoons oil 4. Knead the modeling dough with your hands until of proper consistency. 2 tablespoons cream of tartar Students should be able to: 5. Divide the recipe into three portions coloring each one a different color. Explain the Law of Superposition_ Explain the difference between sedimentary and igneous rock layers After explaining the notes to the students, have them cut out the perimeter of the paper block printouts provided. Using tape, put the blocks together to show a 3D form of rock layers cut out of a piece of land. 1. Ask the students to identify the youngest and oldest rock layer in each block. 2. They should be able to share why they chose these. 3. They should be able to explain any abnormalities in the layers. 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