
Science • 30 • 1 students • Created with AI following Aligned with Australian Curriculum (F-10)
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This is lesson 1 of 20 in the unit "Exploring Earth and Space". Lesson Title: Introduction to Earth Systems Lesson Description: Investigate the structure of the Earth, including geological layers and their composition.
Students begin the unit by investigating Earth’s structure as a system. They model how different geological layers differ in composition and use evidence-based reasoning to connect Earth systems to tectonic activity studied later in the unit.
0–5 min · Hook (think–pair–share). Teacher shows a simple diagram of Earth layers and asks: “If we can’t drill to the centre, how do scientists know what’s inside Earth?” Students answer individually, then discuss with a partner.
5–12 min · Direct teaching (Earth structure overview). Teacher explains the four main layers, focusing on what each layer is thought to be made of, and why conditions change with depth (temperature, density). Students complete a guided Earth-layers notes sheet: label, then write one key feature per layer.
12–20 min · Model investigation (evidence reasoning). Teacher provides a “layer cake” model kit: different-coloured discs or clay/plasticine for crust, mantle, outer core, inner core plus a simple temperature/density prompt card (e.g. “denser materials go deeper” and “hotter materials closer to inner core”). Students predict where each model material should sit, then assemble a cut-and-compare model to check whether their ordering matches the teacher’s evidence-based pattern.
20–26 min · Micro inquiry (hypothesis test). Teacher displays an investigable question: “Does increasing depth in Earth models correspond to increasing density and temperature?” Students state a hypothesis, then justify it using their model observations and the evidence idea discussed earlier.
26–30 min · Exit ticket (formative check). Teacher collects an exit ticket: (a) label the layers on a blank diagram, and (b) write one sentence explaining the best piece of evidence scientists use when direct observation is impossible.
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