Journey to Earth's Hidden Layers
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Journey to Earth's Hidden Layers
Exploring the Structure of Our Planet Year 10 Earth Science New Zealand Curriculum
WALT: We Are Learning To
Identify and describe the four main layers of Earth Explain the physical properties of each layer Understand how scientists study Earth's interior Connect Earth's layers to geological processes
What's Beneath Our Feet?
Think about digging the deepest hole possible What do you think you would find? How hot do you think it gets inside Earth? Discussion: Share your predictions with a partner
Earth's Layer Discovery Timeline
The Crust: Our Rocky Foundation
Thinnest layer - like the skin of an apple Continental crust: 30-70km thick Oceanic crust: 5-10km thick Made of solid rock - granite and basalt Temperature: 0°C to 1000°C
Crust Comparison
{"left":"Continental Crust: Thicker (30-70km)\nOceanic Crust: Thinner (5-10km)\nContinental: Made of granite\nOceanic: Made of basalt","right":"Continental: Less dense\nOceanic: More dense\nContinental: Older rocks\nOceanic: Younger rocks"}
The Mantle: Earth's Hot Middle Layer
Largest layer - 84% of Earth's volume 2900km thick Made of hot, dense rock (peridotite) Temperature: 1000°C to 3700°C Mostly solid but can flow very slowly
Mantle Convection Activity
Materials: Colored water, heat source, clear container Observe how heated water rises and cooler water sinks Draw what you observe Connect this to mantle rock movement Extension: Research how this drives plate tectonics
The Outer Core: Liquid Metal Layer
2200km thick liquid layer Made of iron and nickel Temperature: 3700°C to 5000°C Creates Earth's magnetic field Liquid due to extreme heat
The Inner Core: Earth's Solid Heart
Despite temperatures of 5000°C to 6000°C, the inner core is SOLID due to extreme pressure 1200km radius sphere of iron and nickel Pressure is so intense it forces atoms together
Journey Complete: Earth's Hidden Layers Revealed
Crust: Thin, solid, rocky foundation Mantle: Thick, hot, slowly flowing rock Outer Core: Liquid iron creating magnetic field Inner Core: Solid iron under extreme pressure Each layer has unique properties and functions