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Weathering and Erosion Processes

Authored by Wayground Content

English

11th Grade

Used 1+ times

Weathering and Erosion Processes
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13 questions

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1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Rocks do not last forever.

Rocks can last for millions of years without breaking down.

Rocks eventually break down and do not last forever.

Rocks are indestructible and will last indefinitely.

Rocks only break down under extreme conditions.

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Weathering process.

Weathering involves root-wedging and ice-wedging.

Weathering is the process of soil formation.

Weathering is caused solely by human activities.

Weathering only occurs in tropical climates.

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Repeated expansion and contraction.

This process causes further cracks until the rock breaks apart.

This process leads to the formation of new minerals.

This process results in the rock becoming more compact.

This process causes the rock to become smoother.

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Mountains start as solid rock.

Mountains begin as solid rock but break into smaller pieces over time.

Mountains are formed from ice and snow.

Mountains are created by volcanic activity only.

Mountains are made entirely of sand and gravel.

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Characteristics of rocks at the top of mountains

Rocks at the tops of mountains are smooth.

Rocks at the tops of mountains are jagged.

Rocks at the tops of mountains are round.

Rocks at the tops of mountains are soft.

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Cracks widen with freezing water.

As water freezes, cracks get wider and rocks break.

Water expands when it freezes, causing cracks to close.

Freezing water has no effect on cracks in rocks.

Cracks remain the same size regardless of temperature.

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Characteristics of rocks at the bottom of mountains

Rocks at the bottom of mountains are sharp and jagged.

Rocks at the bottom of mountains are flat and smooth.

Rocks at the bottom of mountains are rounded.

Rocks at the bottom of mountains are large and blocky.

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