Students master how continental drift and plate tectonics reshape Earth's landscape over geological time. Through solving fossil distribution mysteries across continents or investigating whale bones in desert locations, reconstructing Pangaea using fossil and geologic data creating "before and after" maps showing continental positions, and designing modern equipment measuring plate movement gathering data proving plates still shift today, students analyze evidence for plate motion.
- Lesson 1

Solve: Whale Valley + Fossil Mystery
Lystrosaurus bones found on three separate continents—Africa, India, and Antarctica! The Triassic Park guide calls it impossible—how can one creature's fossils be distributed so widely? Students follow Mosa as she time-travels beneath oceans and across Earth's surface, discovering Earth's structure: inner core, outer core, mantle, and crust. The crust is broken into tectonic plates floating on the mantle's hot, slowly moving magma (convection currents). Millions of years ago, these continents were connected in the supercontinent Pangaea. As plates drifted apart, Lystrosaurus fossils separated—continental drift explains the distribution!
- Lesson 2

Make: Use Evidence from Plant and Animal Fossils to Prove Tectonic Plate Motion
Act as an archaeological team reconstructing Pangaea! Students analyze fossil evidence (Lystrosaurus in Africa/India/Antarctica, Mesosaurus in Africa/South America, Glossopteris fern across southern continents, Cynognathus in South Africa/South America) and continental shapes. They cut out continent pieces, use logic and evidence to position landforms as they appeared 200 million years ago, construct a Pangaea "before" map by tracing continents in their connected supercontinent formation, create an "after" map showing current positions, then photograph or create stop-motion animations showing continental drift over time. Present findings explaining plate tectonics theory based on fossil distribution.
- Lesson 3

Engineer: Engineer a Device to Detect Plate Movement
Design modern equipment answering the question: Are Earth's plates still moving? Students research current plate movement measurement technologies (GPS sensors tracking millimeter shifts? Seismographs detecting earthquakes at plate boundaries? Satellite imaging monitoring continental drift? Laser ranging systems? Ocean floor mapping equipment?), then engineer their own data-gathering devices. They create technical diagrams or 3D prototypes showing how their equipment measures plate motion, calculates movement rates, or detects boundary interactions. Presentations explain how collected data proves plates continue moving today—typically 2-10 centimeters per year.








