Observe Weathering Effects — Make observations that show...

SECTION 1

How People Learned About Weathering

Have you ever noticed a crumbly old statue or a rock with a hole worn right through it? People have wondered about these things for thousands of years. Long ago, most people thought rocks stayed the same forever. But curious observers noticed something important: rocks change over time. The process that breaks rocks apart or wears them away is called weathering.

1700s

James Hutton Studies Rocks

A Scottish scientist named James Hutton noticed that rain, wind, and rivers slowly broke down rocks. He realized Earth's surface changes little by little over a very long time.

1830s

Charles Lyell Writes About Earth Changes

Lyell wrote books explaining that the same forces we see today — rain, frost, and flowing water — have been shaping Earth for millions of years.

1900s

Scientists Study Different Types of Weathering

Scientists began grouping weathering into types: physical (breaking apart), chemical (changing what rocks are made of), and biological (caused by living things).

Today

Observing Weathering Everywhere

Now scientists and students observe weathering all around them — from cracked sidewalks to rounded river rocks — and use these observations to understand how Earth keeps changing.

So here is the big question this lesson will help you answer: What clues can we observe that show weathering is changing rocks and land? Let's find out!

SECTION 2

What Is Weathering? Core Ideas

Weathering is the breaking down or wearing away of rocks and land on Earth's surface. It happens slowly, sometimes over hundreds or thousands of years. Weathering is different from erosion (the moving of broken pieces to a new place). Weathering breaks the rock; erosion carries the pieces away.

Physical Weathering

Rocks break into smaller pieces, but the pieces are still made of the same material. Freezing water, plant roots, and temperature changes can crack rocks apart.

Chemical Weathering

The rock actually changes into something new. Rainwater (which is slightly acidic) can dissolve minerals in rock, creating soft, crumbly surfaces or even caves.

Biological Weathering

Living things cause weathering too! Tree roots push into cracks and widen them. Lichens (tiny plant-like organisms) release acids that eat away at rock surfaces.

Observable Evidence

You can see weathering by looking for cracks, rounded edges, pits, color changes, crumbling surfaces, and sand or soil around rocks.

✦ KEY TAKEAWAY

Think of weathering like what happens to a sugar cube when you drip water on it. The water slowly dissolves the sugar and makes the cube crumble. In the same way, water, wind, ice, and living things slowly break down rocks. It just takes much, much longer!

SECTION 3

See Weathering in Action

The diagram below shows three main types of weathering and what they look like. Notice how each type leaves different clues on the rock.

This diagram shows three columns. Physical weathering cracks rocks and rounds their edges. Chemical weathering changes the rock's color and creates pits. Biological weathering happens when roots, lichens, and animals break rock apart.

Look at the diagram above. Each column shows one type of weathering and the clues it leaves behind. When you go outside, you can look for these same clues on rocks, sidewalks, buildings, and hillsides. Rounded river stones are a sign of physical weathering. Orange rust stains on a rock are a sign of chemical weathering. A tree root splitting a sidewalk is a sign of biological weathering.

SECTION 4

How Weathering Works Step by Step

The Freeze-Thaw Cycle (Ice Wedging)

One of the most powerful forms of physical weathering is called ice wedging (also called the freeze-thaw cycle). Here is how it works. Water seeps into tiny cracks in a rock. When the temperature drops below freezing (0 °C or 32 °F), the water turns to ice. Ice takes up more space than liquid water. This pushes the crack open wider. When it warms up, the ice melts and more water flows in. This cycle repeats over and over, making the crack bigger and bigger until the rock splits apart!

This step-by-step diagram shows how ice wedging works. Water enters a crack, freezes and expands, and eventually splits the rock apart.

How Chemical Weathering Works

Rainwater picks up a tiny bit of carbon dioxide from the air. This makes it slightly acidic (like very, very weak lemon juice). When this acidic water lands on certain rocks — especially limestone — it slowly dissolves the rock. Over thousands of years, this can carve out caves, create sinkholes, and leave pits on the surface of rocks.

How Biological Weathering Works

Living things can be powerful weathering agents! A tiny seed lands in a crack. As the plant grows, its roots push deeper and wider, forcing the crack open. Animals that dig burrows move soil and break apart rock underground. Even tiny organisms like lichens and moss release acids that slowly eat into the rock beneath them.

SECTION 5

Clues That Show Weathering Is Happening

Scientists observe evidence — clues that tell them weathering is at work. You can look for these clues too! The table below shows common signs of weathering and what type they belong to.

Observable evidence of weathering

What You See (Evidence)	Type of Weathering	Where You Might Find It
Cracks or splits in rock	Physical	Mountain cliffs, boulders, sidewalks
Smooth, rounded stones	Physical	Riverbeds, beaches
Orange or brown rust stains	Chemical	Rocks with iron minerals
Pits, holes, or soft crumbly areas	Chemical	Limestone buildings, statues
Tree roots lifting or cracking rock	Biological	Sidewalks, trails, rocky hillsides
Moss or lichens growing on rock	Biological	Old walls, gravestones, forest rocks
Sand or small rock chips at base of a cliff	Physical	Cliff bases, canyon floors

🔍 TRY THIS!

Go outside and look at rocks, walls, sidewalks, or old buildings near your home or school. Can you spot any of these clues? Take a photo or draw a picture and label what type of weathering you think caused it!

SECTION 6

Observing and Identifying Weathering

Let's practice making observations like a scientist! Imagine you are on a nature walk and you see a large boulder sitting next to a stream. Let's figure out what kind of weathering is happening.

Nature Walk Observation

Step 1 — Look Closely at the RockYou notice the boulder has smooth, rounded edges. There are no sharp corners. The side facing the stream is especially smooth.

Step 2 — Look for Color ChangesPart of the rock has orange-brown patches. This looks like rust. Rust forms when iron in a rock reacts with water and oxygen.

Step 3 — Look for Living ThingsYou spot patches of green and gray lichen growing on the top of the rock. A small tree root has grown into a crack on one side.

Step 4 — Identify the Types of WeatheringNow match your observations to weathering types. Smooth, rounded edges → physical weathering from water rubbing against the rock. Orange rust stains → chemical weathering from water and oxygen reacting with iron. Lichen and tree roots → biological weathering from living things breaking down the rock.

This single boulder shows all three types of weathering happening at the same time!

Step 5 — Record Your ObservationsA good scientist writes down what they see. You could draw the boulder and label each clue. You might also write: "I observed physical, chemical, and biological weathering on a streamside boulder."

SECTION 7

Comparing the Three Types of Weathering

The three types of weathering are different, but they often work together. The table below helps you compare them side by side.

Comparing three types of weathering

Feature	Physical Weathering	Chemical Weathering	Biological Weathering
What happens?	Rock breaks into smaller pieces	Rock changes into new materials	Living things crack or dissolve rock
Does the rock's material change?	No — same rock, just smaller	Yes — minerals change into new substances	Can be either
Main causes	Ice, wind, water, temperature	Acid rain, oxygen, water	Roots, animals, lichens, moss
Observable clues	Cracks, rounded edges, rock chips	Rust, pits, soft crumbly spots	Roots in cracks, lichen patches
Speed	Can be fast (landslide) or slow	Usually very slow	Usually slow

✦ KEY TAKEAWAY

Think of the three types of weathering like three teammates working together on a demolition crew. Physical weathering is the team member with the hammer who cracks things apart. Chemical weathering is like the team member who uses a special spray to dissolve glue holding bricks together. Biological weathering is like tiny helpers (roots and lichens) that sneak into cracks and push from the inside. Together, they slowly take down even the biggest rocks!

SECTION 8

Weathering, Erosion, and the Big Picture

Weathering is just one part of how Earth's surface changes. After weathering breaks rock into smaller pieces, erosion carries those pieces to new places. Then deposition drops the pieces in a new spot. Together, these three processes shape mountains, carve valleys, create beaches, and build deltas.

How weathering connects to erosion and deposition

Process	What It Does	Example
Weathering	Breaks rock into smaller pieces (stays in place)	A boulder cracks from freezing water
Erosion	Moves rock pieces to a new location	A river carries sand downstream
Deposition	Drops the pieces in a new spot	Sand piles up to form a beach

In later grades, you will learn more about how these processes create landforms like canyons, sea cliffs, and sand dunes. You will also explore how humans can speed up or slow down weathering and erosion. For now, remember that weathering is the first step in Earth's never-ending process of reshaping its surface.

SECTION 9

Practice Problems

PROBLEM 1 — CONCEPTUAL

What is weathering, and how is it different from erosion?

PROBLEM 2 — BASIC CALCULATION

A student collects three rocks from a riverbed and three rocks from a mountaintop. The river rocks are smooth and round. The mountain rocks are rough and jagged. Which set of rocks shows more weathering, and what type is it?

PROBLEM 3 — INTERMEDIATE

Maria notices that an old limestone gravestone from the year 1850 has words that are hard to read because the surface looks soft and pitted. A granite gravestone from the same year still has clear, sharp letters. Why do you think the limestone gravestone weathered more?

PROBLEM 4 — APPLIED

Imagine you are a park ranger. You notice that the trails on a steep hillside are getting wider and more crumbly every year. Tree roots are sticking out of the ground, and there are small piles of rock chips at the base of a cliff nearby. List at least two types of weathering you see evidence of, and explain what you could do to protect the trail.

PROBLEM 5 — CRITICAL THINKING

A scientist compares two identical rocks. One was left outside in a cold, wet climate (lots of rain and freezing temperatures). The other was kept in a dry, warm desert. After 50 years, the cold-wet rock is cracked and crumbly, while the desert rock looks almost the same. Using what you know about weathering, explain why the cold-wet rock changed more. Think about at least two types of weathering.

SUMMARY

Lesson Summary

Weathering is the breaking down of rocks and land on Earth's surface. There are three main types. Physical weathering breaks rock into smaller pieces without changing what it is made of — caused by ice wedging, wind, water, and temperature changes. Chemical weathering changes rock into new substances through reactions with water, oxygen, and acids. Biological weathering is caused by living things like roots, lichens, and burrowing animals.

You can observe evidence of weathering by looking for cracks, smooth rounded edges, rust stains, pits, crumbly surfaces, and roots growing in rock. Weathering is different from erosion (which moves pieces) and deposition (which drops pieces in a new place). Together, these processes are always reshaping Earth's surface, slowly but surely.