Transform Plate Boundaries: Earth's Sliding Plates — Passage

Grades
5
6
7
8
Standards
MS-ESS2-3
RI.6.1
RI.7.4
RI.8.2
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 NGSS aligned nformational passage examines transform plate boundaries where tectonic plates slide horizontally past each other, creating fault lines like California's San Andreas Fault. It explains strike-slip motion, earthquake formation, and human impacts through historical examples (1906 San Francisco quake). The text details how scientists monitor fault movement using GPS and lasers while addressing NGSS Earth Science standards about plate interactions. Key terms include fault gouge, seismic waves, and plate velocity (5 cm/year). The passage connects to MS-ESS2-2 (Earth's surface processes) and supports reading standards for analyzing technical texts about natural hazards.
Publisher: Workybooks
|
Written by:Workybooks Team
|
Illustrated by:

Beneath our feet, Earth’s tectonic plates are constantly moving—not just colliding or pulling apart, but also grinding sideways past each other at transform boundaries. These sliding boundaries create some of the world’s most famous fault lines, where earthquakes reshape landscapes and challenge human communities.

 

How Transform Boundaries Work

 

Unlike convergent or divergent boundaries, transform boundaries don’t create or destroy crust. Instead, two plates slide horizontally in opposite directions, building up tremendous stress along jagged fault lines. When this stress suddenly releases—SNAP!—an earthquake strikes.

 

The San Andreas Fault: A Living Laboratory

 

The San Andreas Fault in California is the world’s most famous transform boundary. Here, the Pacific Plate slides northward past the North American Plate at about 5 cm per year—the speed your fingernails grow. Over millions of years, this motion has shifted rocks hundreds of miles and created a landscape of cracked valleys and offset streams.

 

Did You Know?


Parts of California west of the fault (including Los Angeles) are slowly moving toward Alaska, while the rest of the state stays put! In 20 million years, L.A. could be a suburb of San Francisco.

 

Earthquakes and Human Impact

 

Because plates don’t slide smoothly, they often get “stuck” for years—even centuries—before suddenly lurching forward. The result? Devastating quakes like:

●       1906 San Francisco earthquake (7.9 magnitude, 3,000 deaths)

●       1989 Loma Prieta earthquake (collapsed freeways, World Series interruption)

Today, scientists monitor fault lines with lasers and GPS, but predicting earthquakes remains nearly impossible.

 

Transform Boundaries Worldwide

 

While the San Andreas gets the spotlight, other transform boundaries exist:

●       Alpine Fault (New Zealand): Where the Pacific and Australian Plates scrape past each other.

●       North Anatolian Fault (Turkey): Caused a deadly 7.4 quake in 1999.

 

Fun Fact: Did you know the San Andreas Fault is so visible from space that astronauts use it as a landmark? This giant scar on Earth’s surface stretches 1,200 km (745 miles)—longer than the entire state of California!

What is the primary movement at transform plate boundaries?

Plates collidePlates pull apartPlates slide past each otherPlates sink into the mantle

Which famous fault is an example of a transform boundary?

Mariana TrenchSan Andreas FaultMid-Atlantic RidgeHimalayan Frontal Fault

How fast are the Pacific and North American Plates moving along the San Andreas Fault?

1 cm per year5 cm per year20 cm per year1 meter per year

What natural hazard is MOST common at transform boundaries?

VolcanoesEarthquakesTsunamisLandslides

Why do earthquakes occur at transform boundaries?

Magma rises to the surfacePlates get stuck and suddenly release energyNew crust is formedMountains are eroded

What will likely happen to Los Angeles in millions of years due to the San Andreas Fault?

It will sink into the oceanIt will move closer to San FranciscoIt will become a volcanoIt will stay in the same place

Which tool do scientists use to monitor fault movement today?

TelescopesBarometersGPS and lasersWeather balloons

Which of these is NOT a transform boundary?

North Anatolian Fault (Turkey)Alpine Fault (New Zealand)Mariana Trench (Pacific Ocean)San Andreas Fault (USA)

Related Content

interactive | printable worksheet on CCSS MS-ESS3.C,RI.6.1,RI.7.4,RI.8.2 - The Dust Bowl Disaster - thumbnail
The Dust Bowl Disaster
The Dust Bowl was an environmental disaster in the 1930s. Farmers had removed too much grass to plan...
MS-ESS3.CRI.6.1RI.7.4RI.8.2
interactive | printable worksheet on CCSS MS-ESS2-3,RI.6.1,RI.7.4,RI.8.2 - Divergent Plate Boundary: Where Earth's Crust Pulls Apart - thumbnail
Divergent Plate Boundary: Where Earth's Crust Pulls Apart
This science passage explains how divergent plate boundaries form where Earth's crust pulls apart, c...
MS-ESS2-3RI.6.1RI.7.4RI.8.2
interactive | printable worksheet on CCSS MS-ESS2-3,RI.6.1,RI.7.4,RI.8.2 - Convergent Boundary: When Earth's Plates Collide - thumbnail
Convergent Boundary: When Earth's Plates Collide
This science passage describes three types of convergent plate boundaries (oceanic-continental, ocea...
MS-ESS2-3RI.6.1RI.7.4RI.8.2
interactive | printable worksheet on CCSS MS-ESS2-3,RI.6.1,RI.7.4,RI.8.2 - Types of Plate Boundaries - thumbnail
Types of Plate Boundaries
This science passage explores how geologists use rock formations, fossil distributions, and seafloor...
MS-ESS2-3RI.6.1RI.7.4RI.8.2
interactive | printable worksheet on CCSS MS-ESS2-3,RI.6.1,RI.7.4,RI.8.2 - How Are Metamorphic Rocks Formed? - thumbnail
How Are Metamorphic Rocks Formed?
This science passage explains how metamorphic rocks form through metamorphism, detailing the effects...
MS-ESS2-3RI.6.1RI.7.4RI.8.2
interactive | printable worksheet on CCSS MS-ESS2-3,RI.6.1,RI.7.4,RI.8.2 - What Type of Plate Boundary Is the San Andreas Fault? - thumbnail
What Type of Plate Boundary Is the San Andreas Fault?
This explanatory passage examines the San Andreas Fault as a transform plate boundary where the Paci...
MS-ESS2-3RI.6.1RI.7.4RI.8.2
interactive | printable worksheet on CCSS MS-ESS2-3,RI.6.1,RI.7.4,RI.8.2 - How Are Igneous Rocks Formed? - thumbnail
How Are Igneous Rocks Formed?
This science passage explains the complete formation process of igneous rocks, covering both intrusi...
MS-ESS2-3RI.6.1RI.7.4RI.8.2
interactive | printable worksheet on CCSS MS-ESS2-3,RI.6.1,RI.7.4,RI.8.2 - Intrusive Igneous Rocks: Formation and Features - thumbnail
Intrusive Igneous Rocks: Formation and Features
This passage explains the formation of intrusive igneous rocks through slow cooling of magma beneath...
MS-ESS2-3RI.6.1RI.7.4RI.8.2
interactive | printable worksheet on CCSS MS-ESS2-3,RI.6.1,RI.7.4,RI.8.2 - Extrusive Igneous Rocks: Formation and Features - thumbnail
Extrusive Igneous Rocks: Formation and Features
This educational passage describes extrusive igneous rock formation through rapid cooling of lava on...
MS-ESS2-3RI.6.1RI.7.4RI.8.2
interactive | printable worksheet on CCSS MS-ESS2-3,RI.6.1,RI.7.4,RI.8.2 - Type of Mountain Ranges Formed at Convergent Plate Boundaries - thumbnail
Type of Mountain Ranges Formed at Convergent Plate Boundaries
This passage explains how Earth's tallest mountain ranges form at convergent plate boundaries. It de...
MS-ESS2-3RI.6.1RI.7.4RI.8.2
interactive | printable worksheet on CCSS MS-ESS3-2,MS-ESS2-3,RST.6-8.2 - Kīlauea Volcano: Hawaii’s Ever-Changing Landscape - thumbnail
Kīlauea Volcano: Hawaii’s Ever-Changing Landscape
This passage details Kīlauea's volcanic history and status, aligned with NGSS MS-ESS3-2 (natural haz...
MS-ESS3-2MS-ESS2-3RST.6-8.2
interactive | printable worksheet on CCSS MS-ESS3-2,MS-ESS2-3,RST.6-8.2 - All About Seismometers - thumbnail
All About Seismometers
This informational science passage explores seismometers and their role in measuring earthquakes, de...
MS-ESS3-2MS-ESS2-3RST.6-8.2
interactive | printable worksheet on CCSS MS-ESS2-3,MS-ESS3-2,RST.6-8.4 - What Is the Difference Between Magma and Lava? - thumbnail
What Is the Difference Between Magma and Lava?
This educational reading passage explains the critical difference between magma and molten rock bene...
MS-ESS2-3MS-ESS3-2RST.6-8.4
interactive | printable worksheet on CCSS MS-ESS2-3,MS-ESS3-2,RST.6-8.4 - Obsidian: The Natural Glass Rock - thumbnail
Obsidian: The Natural Glass Rock
This science reading passage explores obsidian, a volcanic glass that forms when lava cools so rapid...
MS-ESS2-3MS-ESS3-2RST.6-8.4
Copyright © 2025 Workybooks. Made with ♥ in California.