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Exploring Plate Motion and Deformation in California Using GPS Time Series Plots Shelley Olds, UNAVCO Andy Newman, Georgia Institute of Technology. Parts of Activity. Part I: Analyze real time-series data of two GPS stations to determine plate tectonic motion
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Exploring Plate Motion and Deformation in California Using GPS Time Series Plots Shelley Olds, UNAVCO Andy Newman, Georgia Institute of Technology
Parts of Activity • Part I: Analyze real time-series data of two GPS stations to determine plate tectonic motion • Part II. Investigate deformation at two GPS stations in California
Processed Data SBCC GPS STATION • Located near Mission Viejo, CA • Position data collected every 30 seconds • One position estimatedeveloped for each day • North • East • Vertical
Position time series plot • Time series plot shows the GPS station’s change in position over time • X-axis: • Date of the measurement • In 10ths of year or months • Y-axis: • North (N/S) • East (E/W) • Height (up/down) (sometimes called Vertical) • In millimeters
Units of measurement • X Axis • Typically in 10ths of year • Y Axis • Usually millimeters (but always check)
In Your Packet: Station Homepages • Station name/location • Latitude / longitude • Elevation • More information: • Area map – w/ nearby stations • Link to data (Excel readable format)
Part I Instructions • Work in pairs to complete the table (pg 2-3) • One person: BEMT GPS Station • One person: SBCC GPS Station • Required GPS station information is on pgs 4-5 • Get together with your partner • Plot the north-south and east-west velocity vectors on graph paper • Determine the magnitude and direction of the resulting velocity vector • Plot this vector on the map of southern California. • Answer the questions on pg 3 Vectors on next slide
Velocity of plates • BEMT • 5.0 N • -5.4 E • -2.1 V • SBCC • 26.8 N • -26.8 E • -3.9 V BEMT SBCC
CAND: • Lat: 35.94 • Long: -120.43 • CARH • Lat: 35.89 • Long: -120.43 CAND CARH
Anyone have a calculator • How much slip on the fault occurred during the event using the CAND time series plot? • ~ 75 mm south and ~ 60 mm east resulting in 96 mm combined slip to the southeast • Describe how the CAND GPS station’s position changed: • During the earthquake. • After the earthquake. • What was the magnitude* of the Parkfield earthquake based on the slip that you calculated? Sudden change in position to SE… Continued SE until ~Jan 2005, then resumed NW movement M = log10(D) + 6.32 0.9 where M = magnitude D= average slip in meters [1000 mm = 1 meter] M = log10(.096) + 6.32 0.9 M = 5.9 (according to the USGS, the Parkfield earthquake was a magnitude 6.0 Mw)
Reoccurring Earthquakes • ~96 mm total slip • Plate moving ~22mm/yr at Parkfield • How long should it take to build enough strain energy to generate an earthquake with a similar magnitude? • 96mm / 22 mm per year = ~4.4 years Area map of Parkfield: USGS Red = epicenters of mainshock and aftershocks within one month of event. Yellow = Epicenters of earthquakes from 1973-2006.
Reoccurring Earthquakes • Observed frequency of M6 earthquakes during the 20th century? • ~every 20 years • Predicted frequency: • 96mm / 22 mm per year = ~4.4 years • Why are these numbers different? • smaller earthquakes release some of the strain, • interaction with nearby faults, etc.
Extension: Explore other GPS sites • Compare the slip at 4 – 6 more sites. • Choose sites increasingly further away from epicenter… • MNMC • CAND & CARH • MASW • LOWS, CRBT … • (check the installation dates)
Data for Educators Website http://www.unavco.org/edu_outreach/data.html
Teaching Tips / Errors • What teaching tips to implement this lesson? • What sources of error would your students have?
Questions? Contact info: Shelley Olds olds unavco.org 303-381-7496