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Stratigraphy: Reading Earth's Layered History — Reading Comprehension

Grades
5
6
7
8
Standards
MS-ESS2-1
MS-PS1-2
RST.6-8.3
PRINT+DIGITAL RESOURCE
This learning resource is available in interactive and printable formats. The interactive worksshet can be played online and assigned to students. The Printable PDF version can be downloaded and printed for completion by hand.
ABOUT THIS READER
This passage explains stratigraphy as the study of rock layers to interpret Earth's history. Aligned with NGSS MS-ESS1-4 (Earth's history) and ESS2-3 (Earth's systems), it covers key principles like the Law of Superposition and Original Horizontality. The text details lithostratigraphy, biostratigraphy (fossil-based dating), and applications in paleontology/resource exploration. Examples include trilobite fossils and oil-bearing strata. Meets CCSS.ELA-LITERACY.RST.6-8.2 for analyzing scientific concepts and supports curriculum standards about geological time and sedimentary processes.
Publisher: Workybooks
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Written by:Workybooks Team
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Illustrated by:

Stratigraphy is the study of rock layers (strata. and their sequence to interpret Earth’s geological history. By analyzing these layers, scientists uncover clues about past environments, climate changes, and life forms.

 

Key Principles

  1. Law of Superposition: In undisturbed layers, the oldest rocks are at the bottom, and the youngest are on top.
  2. Original Horizontality: Sedimentary layers form horizontally; tilted or folded layers indicate later geological forces.
  3. Cross-Cutting Relationships: Features like faults or igneous intrusions are younger than the layers they cut through.

 

Types of Stratigraphy

●       Lithostratigraphy: Focuses on rock types and physical layers.

●       Biostratigraphy: Uses fossils to date and correlate layers (e.g., dinosaur bones in specific strata..

●       Chronostratigraphy: Examines rock ages using radiometric dating.

 

Applications

●       Fossil Discovery: Reveals evolutionary timelines (e.g., trilobites in Paleozoic layers).

●       Resource Exploration: Helps locate oil, coal, or groundwater by identifying rock sequences.

●       Climate Studies: Ancient soil layers (paleosols) show past climate conditions.

 

Stratigraphy is essential for understanding Earth’s timeline, from mountain formation to mass extinctions. It bridges geology, paleontology, and archaeology, helping decode our planet’s 4.6-billion-year story.

 

Fun Fact: The principle of superposition in stratigraphy (younger layers on top of older ones) was first described in the 1600s by Nicolas Steno, who began his career not as a geologist but as a royal physician! His observations of shark teeth and rock layers laid the foundation for modern geological dating, nearly 200 years before Darwin proposed his theory of evolution.

What does stratigraphy study?

Ocean currentsRock layers and their sequenceAtmospheric pressureVolcanic eruptions

Which principle states that older rocks lie beneath younger ones?

Cross-cutting relationshipsOriginal horizontalityLaw of superpositionUniformitarianism

What does biostratigraphy use for dating?

Mineral compositionFossilsMagnetic fieldsWater content

How do tilted rock layers form?

Original deposition at an angleLater geological forcesVolcanic activityErosion by wind

Which field benefits from stratigraphy?

AstronomyPaleontologyMeteorologyRobotics

What reveals past climates in stratigraphy?

Igneous intrusionsPaleosols (ancient soils)Granite layersOcean salts

Which layer would be youngest?

A basalt intrusion cutting through shaleLimestone below sandstoneFossils in deep bedrockTilted sedimentary layers

Why is stratigraphy vital for oil exploration?

It identifies rock sequences holding oilIt measures earthquake activityIt tracks weather patternsIt studies plant photosynthesis

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