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Earth and Space ScienceEarth and Space Science114 views·Updated May 23, 2026·4 pages

Understanding Weathering and Erosion in Earth Science

user profile picture
Miranda M.@scarmira1

Weathering and erosion are powerful processes that shape our planet's... Show more

1
of 4
Weathering & Erosion Review Sheet

Physical Weathering- the breakdown of rock into smaller
pieces with NO CHANGE in the chemical composition

Types of Weathering

Ever wonder why rocks break down over time? It happens through two main processes. Physical weathering breaks rocks into smaller pieces without changing what they're made of. Chemical weathering actually changes the minerals or chemicals in the rock as it breaks down.

Physical weathering happens faster in colder places with less rain. Look for signs like animal activity, abrasion (when rocks scrape against each other), plant roots growing into cracks, and frost action (when water freezes and expands in rock cracks). Another cool example is exfoliation, where rocks peel in sheets due to temperature changes.

Chemical weathering thrives in hot, wet environments. It includes processes like carbonation (when carbon dioxide dissolves in rainwater to form weak acid), acid rain, organic decay from plants, and oxidation (when oxygen and iron combine to form rust).

💡 Both physical and chemical weathering require moisture to work! Without some water, these processes slow down dramatically.

2
of 4
Weathering & Erosion Review Sheet

Physical Weathering- the breakdown of rock into smaller
pieces with NO CHANGE in the chemical composition

Factors Affecting Weathering & Erosion Basics

The speed of weathering depends on three key things. First, rocks with more surface area weather faster because more of the rock is exposed. Second, higher temperatures usually speed up weathering. Third, a rock's mineral composition matters—softer rocks weather much faster than harder ones.

Once rocks break down, erosion takes over! Erosion is simply the movement of weathered particles from one place to another. There are four main erosional agents that do this work: glaciers, gravity, water, and wind.

Glaciers and gravity create unsorted deposits with different-sized particles all mixed together. When glaciers move, they can leave scratches called striations on rocks. Water and wind create sorted deposits where particles are similar in size and shape. Water makes rocks smoother and rounder, while wind carries sand and dust.

🏞️ You can tell if a valley was formed by a stream or a glacier by its shape! Stream valleys are V-shaped, while glacier valleys are U-shaped.

3
of 4
Weathering & Erosion Review Sheet

Physical Weathering- the breakdown of rock into smaller
pieces with NO CHANGE in the chemical composition

Beach Erosion & Groins

Beaches are constantly changing due to wave action. When waves and currents move in the same direction along a shoreline, they can carry sand away, causing beach erosion.

To protect beaches, people sometimes build structures called groins that extend from the shore into the water. These structures trap sand on one side, widening the beach in that area.

However, groins have consequences! While they build up sand on one side (the side facing the direction waves are coming from), they can cause increased erosion on the opposite side. This happens because the groin blocks the natural movement of sand along the shoreline.

🌊 Beach protection structures might help one area but can harm another area! Engineers have to carefully consider the entire coastline when planning these structures.

4
of 4
Weathering & Erosion Review Sheet

Physical Weathering- the breakdown of rock into smaller
pieces with NO CHANGE in the chemical composition

Deposition & Final Review

Deposition is the final stage of erosion when materials are dropped off in new locations. This happens when wind or water slows down and can't carry particles anymore. Larger, rounder, heavier particles drop first, while smaller, flatter, lighter ones deposit last.

Streams deposit sediments at their mouths, creating deltas where they enter larger bodies of water. Deposition can happen in two ways: horizontal sorting (where larger sediments deposit before smaller ones) and vertical sorting (where bigger elements settle to the bottom).

Remember the big differences between erosional forces! Glaciers create U-shaped valleys and unsorted deposits. They can leave erratics (boulders) far from their source. Streams form V-shaped valleys and become curvier (meandering) as they age. Gravity causes landslides with angular rocks, while wind forms sand dunes.

🧠 Quick test: If you see rounded, smooth rocks all similar in size, they were probably transported by water. If you see rocks of many different sizes all mixed together, a glacier likely carried them!

We thought you’d never ask...

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Our AI companion is specifically built for the needs of students. Based on the millions of content pieces we have on the platform we can provide truly meaningful and relevant answers to students. But its not only about answers, the companion is even more about guiding students through their daily learning challenges, with personalised study plans, quizzes or content pieces in the chat and 100% personalisation based on the students skills and developments.

Where can I download the Knowunity app?

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Is Knowunity really free of charge?

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Earth and Space ScienceEarth and Space Science114 views·Updated May 23, 2026·4 pages

Understanding Weathering and Erosion in Earth Science

user profile picture
Miranda M.@scarmira1

Weathering and erosion are powerful processes that shape our planet's surface. These natural forces break down rocks and move the resulting fragments, creating everything from valleys to beaches. Understanding how weathering and erosion work will help you make sense of... Show more

1
of 4
Weathering & Erosion Review Sheet

Physical Weathering- the breakdown of rock into smaller
pieces with NO CHANGE in the chemical composition

Sign up to see the content. It's free!

  • Access to all documents
  • Improve your grades
  • Join milions of students

Types of Weathering

Ever wonder why rocks break down over time? It happens through two main processes. Physical weathering breaks rocks into smaller pieces without changing what they're made of. Chemical weathering actually changes the minerals or chemicals in the rock as it breaks down.

Physical weathering happens faster in colder places with less rain. Look for signs like animal activity, abrasion (when rocks scrape against each other), plant roots growing into cracks, and frost action (when water freezes and expands in rock cracks). Another cool example is exfoliation, where rocks peel in sheets due to temperature changes.

Chemical weathering thrives in hot, wet environments. It includes processes like carbonation (when carbon dioxide dissolves in rainwater to form weak acid), acid rain, organic decay from plants, and oxidation (when oxygen and iron combine to form rust).

💡 Both physical and chemical weathering require moisture to work! Without some water, these processes slow down dramatically.

2
of 4
Weathering & Erosion Review Sheet

Physical Weathering- the breakdown of rock into smaller
pieces with NO CHANGE in the chemical composition

Sign up to see the content. It's free!

  • Access to all documents
  • Improve your grades
  • Join milions of students

Factors Affecting Weathering & Erosion Basics

The speed of weathering depends on three key things. First, rocks with more surface area weather faster because more of the rock is exposed. Second, higher temperatures usually speed up weathering. Third, a rock's mineral composition matters—softer rocks weather much faster than harder ones.

Once rocks break down, erosion takes over! Erosion is simply the movement of weathered particles from one place to another. There are four main erosional agents that do this work: glaciers, gravity, water, and wind.

Glaciers and gravity create unsorted deposits with different-sized particles all mixed together. When glaciers move, they can leave scratches called striations on rocks. Water and wind create sorted deposits where particles are similar in size and shape. Water makes rocks smoother and rounder, while wind carries sand and dust.

🏞️ You can tell if a valley was formed by a stream or a glacier by its shape! Stream valleys are V-shaped, while glacier valleys are U-shaped.

3
of 4
Weathering & Erosion Review Sheet

Physical Weathering- the breakdown of rock into smaller
pieces with NO CHANGE in the chemical composition

Sign up to see the content. It's free!

  • Access to all documents
  • Improve your grades
  • Join milions of students

Beach Erosion & Groins

Beaches are constantly changing due to wave action. When waves and currents move in the same direction along a shoreline, they can carry sand away, causing beach erosion.

To protect beaches, people sometimes build structures called groins that extend from the shore into the water. These structures trap sand on one side, widening the beach in that area.

However, groins have consequences! While they build up sand on one side (the side facing the direction waves are coming from), they can cause increased erosion on the opposite side. This happens because the groin blocks the natural movement of sand along the shoreline.

🌊 Beach protection structures might help one area but can harm another area! Engineers have to carefully consider the entire coastline when planning these structures.

4
of 4
Weathering & Erosion Review Sheet

Physical Weathering- the breakdown of rock into smaller
pieces with NO CHANGE in the chemical composition

Sign up to see the content. It's free!

  • Access to all documents
  • Improve your grades
  • Join milions of students

Deposition & Final Review

Deposition is the final stage of erosion when materials are dropped off in new locations. This happens when wind or water slows down and can't carry particles anymore. Larger, rounder, heavier particles drop first, while smaller, flatter, lighter ones deposit last.

Streams deposit sediments at their mouths, creating deltas where they enter larger bodies of water. Deposition can happen in two ways: horizontal sorting (where larger sediments deposit before smaller ones) and vertical sorting (where bigger elements settle to the bottom).

Remember the big differences between erosional forces! Glaciers create U-shaped valleys and unsorted deposits. They can leave erratics (boulders) far from their source. Streams form V-shaped valleys and become curvier (meandering) as they age. Gravity causes landslides with angular rocks, while wind forms sand dunes.

🧠 Quick test: If you see rounded, smooth rocks all similar in size, they were probably transported by water. If you see rocks of many different sizes all mixed together, a glacier likely carried them!

We thought you’d never ask...

What is the Knowunity AI companion?

Our AI companion is specifically built for the needs of students. Based on the millions of content pieces we have on the platform we can provide truly meaningful and relevant answers to students. But its not only about answers, the companion is even more about guiding students through their daily learning challenges, with personalised study plans, quizzes or content pieces in the chat and 100% personalisation based on the students skills and developments.

Where can I download the Knowunity app?

You can download the app in the Google Play Store and in the Apple App Store.

Is Knowunity really free of charge?

That's right! Enjoy free access to study content, connect with fellow students, and get instant help – all at your fingertips.

Most popular content in Earth and Space Science

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Origins and Dynamics of the Columbian Exchange

Analyze the ecological and economic motivations behind the initial transfer of goods, people, and diseases between the Old and New Worlds.

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Introduction to Early Cultural Interactions

Analyze the initial social and religious encounters between Europeans, Africans, and Indigenous peoples in the colonial Americas.

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Origins of Ancient River Civilizations

Analyze the environmental factors and technological innovations that led to the rise of early states in Mesopotamia, Egypt, and the Indus Valley.

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Analyze the economic, religious, and political factors that drove European powers to the Americas during the 15th and 16th centuries.

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Practice identifying the essential elements including carbon, nitrogen, phosphorus, and sulfur that compose biological macromolecules.

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Explore the fundamental economic and social structures of the Spanish colonial system, focusing on the encomienda and the casta social hierarchy.

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Can't find what you're looking for? Explore other subjects.

Students love us — and so will you.

4.6/5App Store
4.7/5Google Play

The app is very easy to use and well designed. I have found everything I was looking for so far and have been able to learn a lot from the presentations! I will definitely use the app for a class assignment! And of course it also helps a lot as an inspiration.

Stefan SiOS user

This app is really great. There are so many study notes and help [...]. My problem subject is French, for example, and the app has so many options for help. Thanks to this app, I have improved my French. I would recommend it to anyone.

Samantha KlichAndroid user

Wow, I am really amazed. I just tried the app because I've seen it advertised many times and was absolutely stunned. This app is THE HELP you want for school and above all, it offers so many things, such as workouts and fact sheets, which have been VERY helpful to me personally.

AnnaiOS user