Heat Transfer
Density & Convection

Earth Layers
Convection Lab
Plates & Earth Changes
Final Jepordy
100

What type of heat transfer occurs through direct contact?

Conduction

100

What happens to the density of material when it is heated?

It becomes less dense.

100

What is Earth’s thin, rigid outer layer?

Crust

100

What happened to the warm red-colored water in the lab?

It rose.

100

What is Earth’s crust broken into?

Tectonic plates

100

Explain the complete cause-and-effect chain from Earth’s internal heat to changes at Earth’s surface.

Earth’s internal heat creates temperature differences. Those temperature differences create density differences. Warm mantle material rises and cooler material sinks, producing convection currents. Mantle movement can help move tectonic plates, and plate movement can create mountains, volcanoes, ridges, trenches, and earthquakes.

200

What type of heat transfer moves thermal energy through the movement of material?

Convection

200

What happens to warm, less-dense material?

It rises

200

What is the thick layer beneath the crust?

Mantle

200

What happened to the cooler water near the ice?

It sank.

200

About how fast do most tectonic plates move?

A few centimeters per year

300

In which layer of Earth is convection especially important?

The mantle

300

What happens to cool, denser material?

It sinks.

300

Which layer is made of liquid metal?

Outer Core

300

Why did the warm water rise?

It became less dense than the surrounding water.

300

Mantle convection can help cause what major Earth process?

Tectonic plate movement

400

Name one source of Earth’s internal heat.

Heat left over from Earth’s formation or radioactive decay


400

What is a convection current?

A continuous circular movement caused by warm material rising and cool material sinking.

400

Which layer is Earth’s hot, solid center?

inner core

400

Why did the cooler water near the ice sink?

It became denser than the surrounding water.

400

Name two features or events that plate movement can create.

mountains, volcanoes, ocean ridges, deep-ocean trenches, earthquakes

500

Explain why heat moves from deeper inside Earth toward the surface.

Heat moves from hotter regions toward cooler regions because of temperature differences.

500

Explain how temperature differences create a convection current.

Heating makes material less dense so it rises. Cooling makes material denser so it sinks, creating continuous circulation.


500

Is the mantle a giant ocean of liquid magma? Explain.

No. The mantle is mostly solid rock that can slowly deform and flow over very long periods of time.

500

How did the lab model mantle convection inside Earth?

The warm water rose and the cool water sank, creating a circular current similar to the slow movement of mantle material.

500

Why can plate movement create major changes even though plates move only a few centimeters per year?

Small movements add up over millions of years and can create large changes to Earth’s surface.

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