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STeLLA Focus on Student Learning: Elementary Students’ Ideas about Earth’s Changing Surface Connie J. Hvidsten & Elaine V. Howes NARST Conference Rio Grande, Puerto Rico April 9, 2013 Context of the Study • Creating a STeLLA videocase • How videocases are used in STeLLA Professional Development STeLLA Videocase • • • • • • Earth’s changing surface Two fourth-grade classrooms Six lesson unit Classroom video Teacher interviews Two interviews with three students from each class • Student work Theoretical Framework • Constructivism/Conceptual Change If students construct new knowledge using knowledge they already have, what’s the stuff they already have that they can use? Hammer & van Zee, 2006, p. 15 • Developing Learning Progressions If mastery of a core idea in a science discipline is the ultimate educational destination, then well-designed learning progressions provide a map of the routes that can be taken to reach that destination. NGSS Framework, 2012, p. 11 Research Questions • What causal mechanisms do these students invoke to explain Earth's surface changes over time? • In what ways did these students’ ideas change in these STeLLA classrooms? Methods • Interview approach – STeLLA questioning strategies – Multiple representations • Interview analysis (Delamont, 2002, Erickson, 2012) – Look for recurrent patterns and contrary instances to patterns – Compare and revise patterns and contrary instances – Carry out multiple iterations – Construct generalizations based in these data and analysis Learning Goals 1. Earth’s surface has recognizable features/landforms, and these landforms are constantly changing. 2. Some of the processes that change Earth’s surface result in the tearing down of surface landforms. Erosion is one process that tears down landforms by transporting weathered earth materials from one place to another over time by wind and water. 3. Some of the processes that change Earth’s surface result in the building up of surface landforms. These processes include deposition of sediments, volcanic activity, and crustal uplift. 4. At any given point in time, Earth’s surface is going up in some places and wearing down in others. It can happen quickly in some places and slowly in others. Findings: Prior to Instruction • Generally, Earth’s surface landforms are permanent. • Any changes in Earth’s surface due to earthquakes or volcanoes. • It is hot inside of the Earth (water, fire, volcanoes). • Rocks break down because they get “old” and “weak.” • No mention of the influence of water on changes to Earth’s surface. • No mention of plate movement. 9 Findings: Intermediate Constructions • Rocks can get smaller through weathering – Local vs. global • Plate movement adopted as the causal mechanism for all changes in landforms – Small scale landforms – Formation of individual mountains associated with plate movement – Plate movement explains decrease in elevation of mountain ranges Marta: Plate movement explains everything Marta: [When plates come together] they build mountains. And when they come apart they don’t build mountains. They shrink the mountains. Interviewer: So you’re also saying that when the mountains could be built up like this [pushing the plates together to represent collision and mountain building], and then … what happens when the plates start pulling away? Marta: It makes the mountain flat. Greg: Holding two ideas at once Interviewer: Are there any other things that might cause these mountains to become flatter besides the plates moving apart? Greg: Oh, yeah, the snow, like how I said ice can, if it gets inside a rock can get make it like explode, and like if it gets snowing and ice keeps getting in rocks, rocks might keep exploding and fall down and the mountain might get smaller and smaller. Nathan: Adopting new ideas Interviewer: Can you show me using the arrows and these foam pads how plates move? Nathan: The plates are connected kind of, and if they move this way [moving away from each other, creating a gap between them] it will create a canyon … that will open up the Earth and it might spread out magma over the surface and that will create another crust…but if it connects to each other, goes toward each other [moving the arrows to point toward each other] it will collide and hit each other and go up. And that’s kind of like a mountain and that will kind of form a mountain. Findings: Adopting Science Ideas • Each type of plate movement results in different types of surface features. • The movement of tectonic plates results in the formation of volcanic and non-volcanic mountains and causes earthquakes. • The processes of weathering and erosion can break rocks apart and move them to different places in a localized way. Implications All research on student conceptions of science is motivated by the belief that a better understanding of student conceptions – both in general and for specific domains – is essential for designing instruction. Sherin, Krakowski & Lee, 2011, p. 195 • Reinforces the notion that teachers’ use of STeLLA strategies in classroom settings (as distinct from interviews) contributes to students’ conceptual understanding. • Intermediate conceptual constructions can be thought of as helpful steps along a learning progression building deep scientific understanding.