Exploring the Rock Cycle Process

Exploring the Rock Cycle Process

Assessment

Interactive Video

Science

6th - 10th Grade

Medium

NGSS
MS-ESS2-1, MS-PS1-5, MS-ESS2-3

Standards-aligned

Created by

Sophia Harris

Used 71+ times

FREE Resource

Standards-aligned

NGSS.MS-ESS2-1
,
NGSS.MS-PS1-5
,
NGSS.MS-ESS2-3
The video explains the three types of rocks: sedimentary, igneous, and metamorphic, and introduces the rock cycle, a process where older rocks transform into new ones. It details how rocks can melt into magma or break into sediments, and how these materials form new rocks through processes like compaction, cementation, and cooling. The video emphasizes visualizing the rock cycle to enhance understanding and concludes with tips for learning the cycle effectively.

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10 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What are the three types of rocks discussed in the video?

Igneous, Metamorphic, and Fossil

Sedimentary, Fossil, and Metamorphic

Sedimentary, Igneous, and Metamorphic

Sedimentary, Igneous, and Fossil

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

According to the law of conservation of matter, what can matter not do?

Be measured

Be seen or touched

Change form

Be created or destroyed

Tags

NGSS.MS-PS1-5

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

How are new rocks formed from older rocks?

By evaporating

By freezing

By breaking apart or melting

By growing

Tags

NGSS.MS-ESS2-3

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the process of making younger rocks from older rocks called?

The nitrogen cycle

The carbon cycle

The water cycle

The rock cycle

Tags

NGSS.MS-ESS2-1

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is magma?

Cold liquid rock

Solid rock

Tiny pieces of rock

Hot liquid rock

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What process turns rocks into sediments?

Freezing

Compaction and cementation

Melting

Weathering and erosion

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

How do sedimentary rocks form?

By weathering and erosion

By melting of rocks

By cooling of magma

Through compaction and cementation of sediments

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