Earth's Layers
Evidence & Tools
Seismic Waves
Convection
Magnetic Field
100

What are Earth’s three compositional layers?

Crust, mantle, core

100

Name one direct way scientists study Earth’s interior

Drilling, lava from volcanic activity

100

What causes seismic waves to form?

Energy released by earthquakes

100

What causes convection?

Differences in temperature and density

100

Which structural layer creates Earth’s magnetic field?

The liquid outer core

200

What is the difference between compositional and structural layers?

Compositional = what the layer is made of. 

Structural = how the layer behaves physically.

200

Name two indirect methods we use to study Earth’s interior

Seismic waves, gravity measurements, meteorites, lab experiments

200

What type of wave cannot move through liquids?

S-waves

200

In which layer does rock convection occur?

The mantle (especially the asthenosphere).

200

Which metal is mainly responsible for generating Earth’s magnetic field?

Iron

300

Which structural layer is soft, hot, and able to flow: lithosphere or asthenosphere?

Asthenosphere

300

Why are meteorites useful for studying Earth’s composition?

They preserve materials from the early solar system similar to Earth’s original makeup

300

Why do P-waves and S-waves change speed as they move deeper into Earth?

They speed up or slow down based on density and state of matter.

300

Explain why cool mantle rock sinks and warm mantle rock rises.

Cooler rock is denser; warmer rock expands and becomes less dense.

300

How does the inner core help the outer core make the magnetic field?

The inner core’s heat powers convection in the outer core, which keeps the liquid metal moving and generating the field.

400

Name the discontinuity between the crust and the mantle.

The Mohorovičić Discontinuity (Moho)

400

Why is drilling limited for studying Earth’s deep interior?

Too hot, too much pressure, and too expensive to drill very deep

400

Describe the difference between how P-waves and S-waves move.

P-waves compress and expand (like a slinky). S-waves move material up and down (like a rope)

400

Why does convection in the outer core happen much faster than convection in the mantle?

The outer core is liquid metal, which moves easily, while the mantle is solid rock that flows very slowly.

400

Why is the motion of the outer core’s liquid iron necessary for keeping Earth’s magnetic field going?

Because the flowing metal constantly moves electric charges, which creates an electric current.

500

Explain why the outer core is liquid and the inner core is solid even though the inner core is hotter

The pressure in the inner core is so high that atoms cannot move freely, so iron solidifies despite high temperatures.

500

Explain how multiple types of evidence (seismic, gravity, labs, meteorites) work together to build Earth models

Each gives incomplete information, but combining them allows cross-checking and more accurate inferences

500

Why do seismic waves bend (refract) when they enter layers with different densities?

Because the change in material causes a change in wave speed, which forces the wave path to bend.

500

How does convection deep inside Earth affect the surface?

The rising and sinking of mantle material pushes and pulls on the tectonic plates, causing them to move.

500

If Earth’s magnetic field began weakening, what is one effect scientists might expect to see on Earth’s surface or near-Earth space?

More charged particles reaching Earth (stronger auroras, potential satellite or power grid issues) because the magnetic field would block less solar wind.