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Earth’s Structure and Materials
Table of Contents
Earth’s Interior
Convection and the Mantle
Classifying Rocks
Igneous and Metamorphic Rock
Sedimentary Rocks
The Rock Cycle
Earth’s Interior
Waves
Paths of ocean waves change when the waves reach an island.
Earth’s Interior
Earth’s Crust
The circle graph shows the composition of Earth’s crust.
Earth’s Interior
Mantle Piece
Earth’s mantle is nearly 3,000 kilometers thick. The rigid lithosphere rests
on the softer material of the asthenosphere.
Order of Earth’s Layers
• Crust
• Mantle (lithosphere which includes
crust and asthenosphere)
• Outer Core
• Inner Core
Earth’s Interior
Temperature Inside Earth
The graph shows how temperatures change between
Earth’s surface and the core. ***Can you read this graph?
Convection and the Mantle
How does a Lava Lamp Model Convection Currents?
Mantle Convection
Heat from the core and the
mantle itself causes
convection currents in the
mantle.
Classifying Rocks
Rock Origins
Rocks are classified by the way they formed.
Sedimentary Rocks
How Sedimentary Rock Forms
Sedimentary rocks form through a series of
processes over millions of years.
Sedimentary Rocks
What is the proper sequence of the terms in the word bank that will show
how mountains can change into sedimentary rock?
The Rock Cycle
The Rock Cycle
Through melting,
weathering and erosion,
and heat and pressure, the
rock cycle constantly
changes rocks from one
type into another type.
The Rock Cycle
Patterns in the Rock
Cycle: Surface Events
All of the paths of the rock
cycle result from only a few
surface and subsurface
processes. What words
belong in the empty boxes
in the graphic organizer?
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