Analyzing Plate Motion Using EarthScope GPS Data
Description
In this chapter, users access GPS data from the Plate Boundary Observatory (PBO); they analyze the data in a spreadsheet to measure the motion of GPS stations in the Pacific Northwest. From their analyses, users generate and map annual velocity vectors of GPS stations. Finally, they explore patterns in the direction and length of velocity vectors on the map to understand tectonic motion and surface deformation associated with the subduction of the Juan de Fuca plate under the North American plate.
From an easy-to-use map interface, users access information about GPS stations and the data they collect. They learn about the network of GPS monuments and how position data collected at these sites are analyzed to reveal plate motion. The activity provides complete instructions for calculating north-south and east-west velocity vectors for a GPS station and combining them to produce a vector that represents the annual horizontal motion of the station. Users plot velocity vectors on a map and examine the pattern of direction and lengths. With first-hand experience in producing and mapping station velocity vectors, users are better prepared to use the patterns of velocity vectors and earthquake distributions to interpret regional geology.
EarthScope comprises three observatories:
- The Plate Boundary Observatory (PBO) is installed and maintained by UNAVCO with funding from NSF and NASA. The PBO provides data for study of surface deformation caused by the interactions between tectonic plates. Data come from a network of high precision Global Positioning System (GPS) monuments, borehole strainmeters, and tiltmeters throughout the western United States.
- The USArray is installed and maintained by the Incorporated Research Institutions for Seismology (IRIS). This project collects data from a transportable array of seismometers. The seismometers are sited in a 70-km grid to collect data for 24 months at time. After two years, the seismometers are removed and set up in another grid in a new region of the U.S.
- The San Andreas Fault Observatory at Depth (SAFOD) is installed and operated by Stanford University. SAFOD drilled across the San Andreas fault in Parkfield, California and collected a core of rock material from a depth of 2.3 miles below Earth's surface.
The data from these three observatories are unparalleled in terms of scope and resolution, and they are providing a detailed picture of North America. For more information about EarthScope, visit www.earthscope.org . Development of this EET chapter was funded by NSF grant EAR-637157 to UNAVCO.
This chapter is part of the Earth Exploration Toolbook. Each chapter provides teachers and/or students with direct practice for using scientific tools to analyze Earth science data. Students should begin on the Case Study page.
The EET web site collects no personally identifying information and so is compliant with the Children's Online Privacy Protection Act. The site is constructed with tools that attempt to ensure the broadest possible accessibility in line with section 508 and w3c guidelines.





