Convection Currents and Earth's Layers

Convection Currents and Earth's Layers

Assessment

Interactive Video

Science

6th - 7th Grade

Hard

Created by

Patricia Brown

FREE Resource

The video introduces sixth graders to Topic 7, focusing on minerals and rocks in the geosphere. It covers Earth's interior, including vocabulary terms like seismic waves, crust, mantle, outer core, and inner core. The lesson check questions guide students through understanding Earth's layers and the evidence geologists use to study them. The video explains convection currents in the mantle, how they cause material and energy movement, and compares rock properties in different mantle layers.

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10 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the primary focus of topic 7 in the lesson?

Minerals and rocks in the geosphere

The biosphere

The hydrosphere

The atmosphere

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Which of the following is NOT a layer of the Earth?

Crust

Atmosphere

Mantle

Outer core

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What type of evidence do geologists use to learn about Earth's interior?

Both direct and indirect evidence

Indirect evidence from seismic waves

None of the above

Direct evidence from rock samples

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

How do geologists obtain direct evidence about Earth's interior?

By drilling deep into the Earth

By observing the Earth's surface

Through rock samples brought to the surface by volcanoes

By studying seismic waves

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What would happen to convection currents if Earth's interior cooled down?

They would speed up

They would stop

They would reverse direction

They would remain unchanged

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What drives the process of convection currents in the mantle?

Earthquakes

Magnetic fields

Wind

Density differences due to temperature variations

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

How does the density of materials affect convection currents?

Density has no effect

Less dense materials rise and more dense materials sink

More dense materials rise

Less dense materials sink

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