The Rock Cycle Journey Through Earth’s Dynamic Processes

The Rock Cycle Journey Through Earth’s Dynamic Processes

Assessment

Interactive Video

Science, Biology, Geography

4th - 5th Grade

Hard

Created by

Patricia Brown

FREE Resource

The video tutorial 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 tutorial emphasizes visualizing the rock cycle to understand the transformation processes better.

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10 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

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

Granite, Basalt, Limestone

Quartz, Feldspar, Mica

Sedimentary, Igneous, Metamorphic

Sandstone, Shale, Marble

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

According to the video, how are new rocks formed?

By crystallization of minerals

Through volcanic eruptions

From older rocks breaking apart or melting

By combining minerals

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is magma as described in the video?

Solid rock

Hot liquid rock

Compressed sediments

Cooled lava

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the process called when rocks turn into sediments?

Melting

Weathering and erosion

Compaction

Cementation

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Which rock type can transform into magma?

Only igneous rocks

Only sedimentary rocks

Only metamorphic rocks

All three rock types

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

How do sedimentary rocks form according to the video?

By compaction and cementation of sediments

By crystallization of minerals

Through melting and cooling

From volcanic activity

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What process is responsible for the formation of igneous rocks?

Heat and pressure

Erosion and weathering

Cooling of magma

Compaction of sediments

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