Layers of the Atmosphere

Layers of the Atmosphere

6th Grade

22 Qs

quiz-placeholder

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Layers of the Atmosphere

Layers of the Atmosphere

Assessment

Quiz

Science

6th Grade

Medium

NGSS
MS-ESS2-6, MS-ESS2-5, MS-LS2-1

+1

Standards-aligned

Created by

Darrian Bennett

Used 481+ times

FREE Resource

22 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

The atmosphere is divided into 4 main layers. Each layer has unique physical properties. Which is true about the Stratosphere?

Weather occurs here.

The Stratosphere is below the Troposphere.

The Stratosphere has the Ozone layer with a 3-atom molecule of oxygen.

The Space Shuttle flies in this layer.

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What layer is between the Stratosphere and Thermosphere?


Troposphere

Exosphere

Mesosphere

Ozone layer

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

The gases that make up the Earth’s atmosphere are commonly called air. What percentage of the air is made up of nitrogen?

1%

21%

78%

99%

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What happens in the Mesosphere?

Man can fly in this layer.

There are just a few clouds in this layer.

Meteors can be seen.

Satellites revolve around the Earth in this layer.

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Which layer has many clouds and is where weather occurs?

Mesosphere

Thermosphere

Stratosphere

Troposphere

Tags

NGSS.MS-ESS2-5

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Which layer is the hottest and has the ionosphere which is the component that makes the Aurora Borealis or Northern Lights?

Stratosphere

Thermosphere

Troposphere

Mesosphere

Tags

NGSS.MS-ESS2-6

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What happens to density in the atmosphere the higher you go in altitude?

Density decreases the higher you go in altitude.

Density increases the higher you go in altitude.

Density stays the same no matter how high you go in the atmosphere.

Density increases and decreases, going back and forth, as you go higher in altitude.

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