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1/13/17
THE INTERIOR
STRUCTURE OF EARTH
Objective: I will model the interior structure of
Earth based on both chemical and physical
composition.
PAGE 49
Earth’s Interior
• can be divided two ways:
• chemical composition- what elements
make up each layer
• physical composition- what state of matter
the layer is
Chemical Composition
• crust:
• made up mostly of silicates (silicon +
oxygen)
• two types:
• oceanic- thinner, more dense
• continental- thicker, less dense
Chemical Composition
• mantle:
• composed of silicates, but also aluminum,
magnesium, and iron
• more dense than the crust
• core:
• composed of iron and nickel
• most dense layer
Physical Composition
• Lithosphere:
• solid outer layer of Earth
• crust + the upper mantle
• Asthenosphere:
• has characteristics of a solid and a liquid
• plasticity- the ability of a solid to flow
• Mesosphere:
• Solid mantle rock below asthenosphere
Physical Composition
• Outer Core:
• very dense liquid iron and nickel
• flowing metals generate Earth’s magnetic
field
• Inner Core:
• solid iron and nickel due to extreme pressure
Output Activity (Page 48)
• You have two options:
1) Illustrate the diagram of Earth’s interior
• May use Figure 2 from page 28 in your textbook or find your own
diagram on the iPad
• Label your diagram with both the chemical and physical layers
2) Create a graphic organizer to organize the information from
your notes about Earth’s interior
• Concept map
• Venn diagram
• T-chart