ShakeAlert: Discover Plate Boundaries Through Ground Motion and Deformation Open

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Tectonic plates are constantly moving, and GPS instruments anchored to the ground help measure these motions over time. Scientists use GPS data to identify plate boundaries, deformation zones, and earthquake hazards, with regions showing rapid changes in movement being at higher seismic risk. 

This triad of activities helps learners explore and interpret authentic GPS data to understand plate motion in the western U.S. and Alaska:

In this 5-Minute Activity, learners use hand movements to demonstrate different tectonic plate boundary types and understand how ground motion varies in speed and direction. After learning about vectors, they apply this knowledge to real-world plate motion scenarios, interpreting tectonic movements as measured by GPS instruments.

In this 20-minute Activity, learners work in pairs to create vectors using a compass rose to understand how vectors represent direction and speed. They then explore GPS vector ground motion maps or the GPS Velocity Viewer to observe areas where ground motion is consistent and areas where speed and direction vary, helping them analyze tectonic plate boundary movements.

In this 50-Minute Activity, learners explore GPS data to analyze how the western U.S. is moving, identifying regions where tectonic plates interact and deformation builds up, leading to earthquakes. Through data jigsawing and role-playing geoscience careers, they investigate the relationships between earthquakes, volcanoes, plate movement, topography, and hazards, concluding with an introduction to the ShakeAlert Earthquake Early Warning System.

This activity sequence not only builds data interpretation skills but also introduces careers in geodesy, seismology, and volcanology. Understanding plate motion and ground deformation is crucial, as over 143 million people in the U.S. are at risk from earthquakes. Tools like ShakeAlert, which integrates GPS data, enhance hazard preparedness by detecting and quickly warning about earthquakes.

Objectives:

Learners will be able to:

  • Analyze and describe plate motion as represented as vectors.
  • Interpret ground motion vector maps and use hand movements to demonstrate motion along tectonic plate boundaries.
  • Correlate GPS vectors on a map with plate tectonic boundary types.
  • Make a claim based on evidence about which locations are most likely to have earthquakes in the future.
What would you do with seconds to prepare for earthquake shaking? With even a few seconds, the ShakeAlert® Earthquake Early Warning can save lives and reduce injuries by alerting people that an earthquake may cause shaking near you as it triggers automated actions.
Animation Novice
This set of hands-on activities helps students investigate ground deformation and earthquake hazards in the Pacific Northwest using physical models, real-world data, and map analysis. A brief demonstration with a compression spring illustrates how the subduction of the Juan de Fuca plate beneath the North American plate causes varying motion across the region. In longer activities, students measure compression, analyze GPS vector maps, and identify seismic hazard zones. By interpreting real-world data, students develop a deeper understanding of tectonic forces and connect these concepts to earthquake preparedness strategies.
Activities Novice
Are you looking for all of the ShakeAlert® related activities? Find all available activities at this site!
Activities Novice
ShakeAlert (www.shakealert.org) is an experimental earthquake early warning system (EEW) being tested in the seismically vulnerable West Coast of the United States. This animation shows how ShakeAlert worked for the Napa earthquake, and how it could work for a large M7.8 hypothetical earthquake in Southern California.
Animation Novice
This new animation (2020) describes the ShakeAlert Earthquake Early Warning app: How it works, why we should have it. Made in collaboration with governmental agencies and universities on the West Coast.
Animation Novice
The ShakeAlert® Earthquake Early Warning system uses over two thousand seismometers and GPS sensors to detect earthquakes rapidly and alert people in the affected areas.
Animation Novice
Ground deformation occurs both at plate boundaries and within plates, such as the Basin and Range Province in Nevada, Utah, and California, where extension and rifting can be measured using GPS data. This triad of activities helps learners explore deformation through hands-on modeling with marble tongs, kinesthetic demonstrations of extensional motion, and quantitative analysis of GPS vectors and earthquake hazard maps. Understanding these processes is crucial, as over 143 million people in the U.S. face earthquake risks, and tools like ShakeAlert use GPS data to provide early warnings that can help reduce damage and save lives.
Activities Novice
Tectonic plates are constantly moving, and GPS instruments help scientists measure this motion, identifying plate boundaries, deformation zones, and earthquake hazards, with rapidly changing regions being at higher seismic risk. This triad of activities engages learners in exploring authentic GPS data, using hand movements to model plate boundaries, creating vectors to analyze motion, and examining real-world GPS data to study deformation and earthquake risks in the western U.S. and Alaska. By interpreting data, role-playing geoscience careers, and learning about ShakeAlert, learners develop key skills in seismology, geodesy, and hazard preparedness while understanding the risks earthquakes pose to over 143 million people in the U.S.
Activities Novice
ShakeAlert® Earthquake Early Warning gets even better by using GPS technology for better estimation of major earthquakes
Animation Novice

Related Activitiess

This set of hands-on activities helps students investigate ground deformation and earthquake hazards in the Pacific Northwest using physical models, real-world data, and map analysis. A brief demonstration with a compression spring illustrates how the subduction of the Juan de Fuca plate beneath the North American plate causes varying motion across the region. In longer activities, students measure compression, analyze GPS vector maps, and identify seismic hazard zones. By interpreting real-world data, students develop a deeper understanding of tectonic forces and connect these concepts to earthquake preparedness strategies.

Activities Novice

Ground deformation occurs both at plate boundaries and within plates, such as the Basin and Range Province in Nevada, Utah, and California, where extension and rifting can be measured using GPS data. This triad of activities helps learners explore deformation through hands-on modeling with marble tongs, kinesthetic demonstrations of extensional motion, and quantitative analysis of GPS vectors and earthquake hazard maps. Understanding these processes is crucial, as over 143 million people in the U.S. face earthquake risks, and tools like ShakeAlert use GPS data to provide early warnings that can help reduce damage and save lives.

Activities Novice

In this activity, learners explore ground deformation at and near plate boundaries using hand and body motions, data from GPS and maps. In the 5-minute activity, learners explore the concept of vectors by kinesthetically enacting ground movement using their body and hand movements. In the 20-minute activity, learners model GPS ground motion in different regions and connect deformation to earthquake hazards. In the 45-minute activity learners distinguish between different boundary types by measuring the vectors within tectonic plates and identify regions with higher earthquake hazards, comparing their findings to earthquake shaking potential maps.

Activities Novice

Related Animations

GPS can record the movement of the leading edge of the overlying continental plate in a subduction zone. The plates are locked and the overlying plate is forced back. When friction is overcome and strain is released, the GPS receiver will snap back toward its original position. 

Animation Novice

Subduction zones show that there are 3 distinct areas of movement in the overlying plate:

  1. constant movement above the locked leading edge,
  2. see-saw pattern of back-&-forth movement above a zone that alternately locks then slips, and
  3. no movement far inland above the deeper part of the diving oceanic plate.
Animation Novice

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