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Mystery Science: The Birth of Rocks Unit Review

Authored by Tina Mosier

Science

4th Grade

NGSS covered

Used 562+ times

Mystery Science:  The Birth of Rocks Unit Review
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17 questions

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1.

MULTIPLE SELECT QUESTION

45 sec • 1 pt

Where do you have to live to make it more likely for a volcano to pop up in your backyard? (Choose 2)

near a volcano

in the Ring of Fire

in the middle of the ocean

near Carmi

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Where is the Ring of Fire located?

along the edge of the Pacific Ocean

along the edge of the Atlantic Ocean

along the edge of the Mexican Ocean

along the shores of the Ohio River

Tags

NGSS.4-ESS2-2

3.

MULTIPLE CHOICE QUESTION

45 sec • 1 pt

Will a mountain last forever?

Yes, a mountain will last forever. It is made of solid rock.

No, a mountain won't last forever. Thunder and lightning can make it crumble.

Yes, a mountain will last forever. Rocks can never break apart.

No, a mountain won't last forever. Ice wedging and root wedging break rock apart.

Tags

NGSS.4-ESS2-1

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What shape does the Ring of Fire make?

a square pattern

a circular or horseshoe pattern

a triangular pattern

no pattern

Tags

NGSS.4-ESS2-2

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Where are most of the of the volcanoes in the world?

in California

in Hawaii

in the Ring of Fire

in Mexico

Tags

NGSS.4-ESS2-2

6.

MULTIPLE CHOICE QUESTION

1 min • 1 pt

Why do cone volcanoes explode?

They have thin lava that releases the air bubbles.

They have thick lava that releases the air bubbles.

They have thick lava that traps the bubbles and creates pressure, causing an explosion.

They have thin lava that traps the bubbles and creates pressure, causing an explosion.

7.

MULTIPLE CHOICE QUESTION

45 sec • 1 pt

Why do shield volcanoes flow gently?

Their thick lava lets the bubbles out freely.

Their thin lava traps the bubbles and explodes.

Their thick lava traps the bubbles and explodes.

Their thin lava lets the bubbles out freely.

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