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Weathering

Interactive passage with audio narration, comprehension questions, and printable PDF.

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Format: Interactive (Online), Printable (PDF)
Grades: 5678
Subjects: scienceela
Standards: MS-ESS2-1
Languages: English, Spanish

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What's included

Reading passage

Reading comprehension

Audio narration

With word word highlighting

Comprehension quiz

Auto-graded

Writing activity

Open-ended response

Glossary & flashcards

Vocabulary practice

Differentiated version

Adapted for varied levels

Spanish translation

Bilingual support

About this reader

This comprehensive science reading passage for grades 6-8 focuses on the concept of weathering, aligning with NGSS standard MS-ESS2-1. Students will learn how weathering breaks down rocks at or near Earth's surface through mechanical (physical) and chemical processes. The passage explores the mechanisms of frost wedging, root growth, oxidation, and other causes, with real-world examples and data. Connections to soil formation and landscape change are highlighted, along with environmental implications. The resource includes a glossary, simplified and Spanish versions, a quiz, writing activities, and graphic organizers, making it ideal for diverse learners. The passage is audio integrated for accessibility. Keywords include weathering, earth science, rock cycle, and NGSS MS-ESS2-1, ensuring alignment with middle school science standards and supporting cross-curricular connections.

Written by Workybooks TeamPublished by Workybooks

Sample passage and quiz content

CONTENT PREVIEW

chemical-weathering-2 — Diagram of the chemical weathering process

Weathering is the process that breaks down rock at or near Earth’s surface, shaping our planet’s landscapes over time. Unlike erosion, which moves rock and sediment, weathering only changes the rock where it sits. Understanding weathering helps scientists explain how mountains become hills, how soil forms, and why ancient monuments crumble.

Mechanisms of Weathering
There are two main types of weathering: mechanical (or physical) and chemical weathering. Mechanical weathering breaks rock into smaller pieces without changing its chemical composition. For example, frost wedging happens when water seeps into cracks in rocks, freezes, and expands, forcing the rock apart. Plant roots can also grow into cracks, slowly prying rocks apart as they widen. Other mechanical processes include abrasion (rocks grinding against each other), thermal expansion and contraction (rocks expanding and shrinking with temperature changes), and salt crystallization (salt crystals growing and pushing rocks apart).
Chemical weathering, in contrast, changes the minerals inside the rock through chemical reactions. One common type is oxidation, where oxygen reacts with iron in rocks to form rust. Carbonation occurs when carbon dioxide from air or soil mixes with water to form a weak acid, which can dissolve rocks like limestone. Hydrolysis is another process, where water reacts with minerals to create new substances and weaken the rock.

Factors Affecting Weathering Rates
Several factors influence how quickly rocks weather. Climate plays a major role: mechanical weathering is more common in cold or dry climates, while chemical weathering is faster in warm, wet areas. The type of rock also matters. Some rocks, like granite, are resistant to weathering, while others, like limestone, break down more easily. Surface area is important too; smaller pieces of rock have more exposed surfaces and weather faster. Finally, time is a key factor—weathering is a slow process that can take thousands or millions of years to change landscapes.

Impacts and Importance
Weathering is a critical part of the rock cycle. It produces sediment that can be moved by erosion and deposited elsewhere, eventually forming new rocks. Weathering also creates the mineral particles and nutrients that make up soil, supporting plant life and agriculture. Human activity, such as pollution, can speed up chemical weathering, as seen with acid rain damaging buildings and statues. By studying weathering, scientists can better protect ancient structures and understand how Earth’s surface evolves.

Interesting Fact: Some ancient Egyptian monuments have survived for thousands of years because the dry desert climate slows down both mechanical and chemical weathering.

What is weathering?

The process that breaks down rocks at or near Earth's surfaceThe movement of rocks and sediment from one place to anotherThe process of forming mountainsThe movement of water in rivers

Which of these is an example of mechanical weathering?

Frost wedgingOxidationCarbonationHydrolysis

What does chemical weathering do to rocks?

It changes the minerals in the rockIt moves the rocks to a new placeIt forms new mountainsIt leaves rocks unchanged

Which process involves oxygen reacting with iron to form rust?

OxidationFrost wedgingAbrasionSalt crystallization

In the passage, what is meant by 'surface area' and why does it matter for weathering?

The amount of exposed rock, which affects how quickly it weathersThe color of the rock's surfaceThe location of the rock on Earth's surfaceThe amount of soil covering the rock

What is one effect of human activity on weathering, according to the passage?

Pollution speeds up chemical weathering, such as acid rain damaging buildingsHuman activity slows down all weatheringHumans stop the rock cyclePeople create new rocks from scratch

Which statement best summarizes the importance of weathering in the rock cycle?

Weathering produces sediment, which helps form new rocks and soilWeathering only affects old mountainsWeathering removes soil from Earth's surfaceWeathering does not affect landscapes

Which is a TRUE statement based on the passage?

Weathering helps form soil and sedimentWeathering is the same as erosion

True or False: Mechanical weathering changes the chemical composition of rocks.

TrueFalse

True or False: Chemical weathering is faster in warm, wet climates.

TrueFalse