Lesson 3
Detailed Teacher Guidance
Lesson purpose and approach: This lesson develops a connected understanding of the Moon by moving from familiar observation to scientific explanation. Begin with what learners can see from Earth, then use models and diagrams to explain the Moon’s formation, surface and influence on Earth. Keep explanations visual and cumulative: introduce one idea at a time, revisit key vocabulary aloud, and regularly ask learners to explain a concept in their own words rather than simply recall a definition.
Suggested teacher narration: Emphasise that the Moon is a rocky, nearly spherical natural satellite whose appearance is shaped by impacts and ancient volcanism. When teaching synchronous rotation, physically rotate a ball once while moving it around a central object so that the same face remains pointed inward. During the Giant Impact sequence, distinguish clearly between evidence, scientific modelling and direct observation. For surface features, contrast the darker basaltic maria with the older, brighter and more heavily cratered highlands. During the tides section, explain that gravity produces two tidal bulges and that local tide times are also affected by coastlines, water depth and the shape of ocean basins.
• Common misconception: the far side is permanently dark. Response: explain that both sides receive sunlight; “far side” means the side that normally faces away from Earth.
• Common misconception: maria contain water. Response: link their dark colour to solidified basaltic lava and explain that the name is historical.
• Common misconception: the Moon does not rotate. Response: use the ball-and-orbit model to show that one rotation per orbit keeps the same side facing Earth.
• Common misconception: tides are caused only on the side nearest the Moon. Response: point out the two bulges and have learners identify when a location experiences high and low tide as Earth rotates.
Assessment and responsive teaching: Use short hinge questions after each main phase. Ask learners to justify why we see the same lunar face, order the stages of the Giant Impact Theory, identify an unfamiliar surface feature from its appearance, and compare spring with neap tides. Listen for accurate use of “rotation”, “orbit”, “impact”, “maria”, “highlands” and “tidal bulge”. If several learners give the same incorrect answer, pause for a second model or worked example before moving on. Use the exit task to decide whether the next lesson should begin with retrieval practice on Moon formation, surface features or gravitational effects.















