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ScienceVolcanoes & EarthquakesAges 11–12

How Tectonic Plates Move

Understand that convection currents in the molten mantle drive the movement of rigid tectonic plates; distinguish between convergent (collision/subduction), divergent (spreading ridges), and transform (sliding) plate boundaries; explain why volcanoes, earthquakes, and mountain chains cluster at boundaries; introduce the Wilson cycle of supercontinent assembly and breakup

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“If your child looks at a world map showing where volcanoes and earthquakes happen, can they explain why these events follow specific ring-shaped patterns rather than occurring randomly around the globe?”

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  1. Activity. Understand that convection currents in the molten mantle drive the movement of rigid tectonic plates; distinguish between convergent (collision/subduction), divergent (spreading ridges), and transform (sliding) plate boundaries; explain why volcanoes, earthquakes, and mountain chains cluster at boundaries; introduce the Wilson cycle of supercontinent assembly and breakup

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If your child looks at a world map showing where volcanoes and earthquakes happen, can they explain why these events follow specific ring-shaped patterns rather than occurring randomly around the globe?

Understand that convection currents in the molten mantle drive the movement of rigid tectonic plates; distinguish between convergent (collision/subduction), divergent (spreading ridges), and transform (sliding) plate boundaries; explain why volcanoes, earthquakes, and mountain chains cluster at boundaries; introduce the Wilson cycle of supercontinent assembly and breakup

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“If your child looks at a world map showing where volcanoes and earthquakes happen, can they explain why these events follow specific ring-shaped patterns rather than occurring randomly around the globe?”

Curriculum record

Type
Conceptual
Subject
Science
Domain
Volcanoes & Earthquakes
Age range
Ages 11–12