Introducing KNOVA — A free reading app with curriculum-aligned passages on History & Science for Grades 3-8Learn More →

Sedimentary Rocks — Reading Comprehension

No ratings yet

Premium Resource

Grades

Standards

MS-ESS2-1
MS-ESS2-3
MS-ESS3-1

Rate this resource

Send Feedback / Report an Issue

About This Reader

This comprehensive middle school science passage introduces students to sedimentary rocks, detailing their step-by-step formation through weathering, erosion, deposition, compaction, and cementation. Students learn about the three main categories—clastic, chemical, and organic—along with examples like sandstone, limestone, and coal. The passage explores the features of sedimentary rocks, such as layering (strata), fossils, ripple marks, and mud cracks, explaining how these clues help scientists reconstruct ancient environments and understand Earth's history. Real-world applications, including the role of sedimentary rocks in storing fossil fuels and aquifers, are highlighted. The resource is fully aligned with NGSS standards MS-ESS2-1, MS-ESS2-3, and MS-ESS3-1. It includes a glossary, Spanish translation, differentiated reading version, comprehension quiz, writing prompts, and graphic organizers. Audio integration supports diverse learners. This resource is ideal for grades 6–8 earth science instruction and seamlessly fits into curriculum units focused on Earth's systems, history, and resources.

CONTENT PREVIEW

Sedimentary rocks are one of the three main types of rocks found on Earth. These rocks are crucial for understanding how our planet has changed over millions of years. Scientists study sedimentary rocks to investigate the environments of the past, uncover fossil evidence, and find important resources. The formation and features of sedimentary rocks are closely linked to Earth’s systems and cycles.

How Sedimentary Rocks Form

The formation of sedimentary rocks involves several connected processes. First, existing rocks are broken down into smaller pieces by weathering, which can be caused by wind, water, temperature changes, or chemical reactions. These particles, called sediments, are then carried away by erosion. Rivers, glaciers, and wind transport sediments across the land. When the energy of moving water or wind decreases, sediments settle and build up in layers through deposition. Over time, the weight of more layers presses the lower sediments together, a process called compaction. Minerals dissolved in water fill the spaces and glue sediments together, a process named cementation. This entire sequence can take thousands to millions of years and results in solid sedimentary rock.

Types and Features of Sedimentary Rocks

Sedimentary rocks are classified into three main categories. Clastic sedimentary rocks form from fragments of other rocks. Examples include shale (made from clay), sandstone (sand-sized grains), and conglomerate (rounded pebbles). Chemical sedimentary rocks develop when minerals precipitate from water, such as rock salt and some types of limestone. Organic or bioclastic sedimentary rocks are made from the remains of once-living things, like coal, fossil limestone, and chalk. Sedimentary rocks often have visible layers called strata, where each layer represents a different period of deposition. They may also contain fossils, ripple marks, and mud cracks—features that provide clues to ancient environments and the conditions in which the rocks formed.

Importance and Applications

Sedimentary rocks are essential to science and society. Fossils found in these rocks help scientists reconstruct the history of life and major environmental changes. The arrangement and features of strata allow geologists to interpret events like floods, droughts, or shifts in climate. Many natural resources, such as fossil fuels (coal, oil, and natural gas), are found in sedimentary rocks. Aquifers, which store freshwater underground, often occur in porous sedimentary rocks. By studying sedimentary rocks, scientists gain insight into Earth’s past, manage resources, and protect the environment.

Sedimentary rocks are more than just piles of old mud or sand. They are dynamic records of Earth’s story and vital to our daily lives. Their study connects geology, biology, chemistry, and environmental science, illustrating how Earth’s processes are interconnected.

Interesting Fact: Some sedimentary rock layers contain fossils that are over 500 million years old, giving us a direct window into ancient life on Earth.

Which of the following best describes the process of weathering?

Breaking down rocks into smaller pieces by wind, water, or other forcesThe movement of sediments from one place to anotherThe gluing together of sediments by mineralsThe settling of sediments in layers

What comes immediately after deposition in the formation of sedimentary rocks?

WeatheringCementationCompactionErosion

Which type of sedimentary rock is made from fragments of other rocks?

ClasticChemicalOrganicIgneous

What is a key feature of sedimentary rocks that helps scientists interpret ancient environments?

Volcanic ashStrata or rock layersCrystalsLava flows

What is the meaning of the word 'cementation' as used in the passage?

Breaking rocks into smaller piecesThe gluing together of sediments by mineralsThe movement of sedimentsThe layering of sediments

In the passage, what does 'organic' sedimentary rock mean?

Formed from minerals in waterMade from fragments of other rocksFormed from remains of once-living thingsCreated by volcanic eruptions

Why are sedimentary rocks important to scientists? (Choose the best answer.)

They are used for making jewelryThey show changes in Earth's surface and historyThey are only found in desertsThey are the hardest rocks