Unit 5: 2014 South Napa Earthquake and GPS strain part of GPS, Strain, and Earthquakes
Phil Resor, Wesleyan University
The 2014 South Napa earthquake was the first large earthquake (Mag 6) to occur within the Plate Boundary Observatory GPS network (now Network of the Americas- NOTA) since installation. It provides an excellent ...

Unit 6: Applying GPS strain and earthquake hazard analyses to different regions part of GPS, Strain, and Earthquakes
Vince Cronin, Baylor University (Vince_Cronin@baylor.edu) Phil Resor, Wesleyan University (presor@wesleyan.edu)
Students select their own set of three stations in an area of interest to them, conduct a strain analysis of the area between the stations, and tie the findings to regional tectonics and societal impacts in a 5–7 ...

Unit 1: Earthquake! part of GPS, Strain, and Earthquakes
Vince Cronin, Baylor University (Vince_Cronin@baylor.edu) Phil Resor, Wesleyan University (presor@wesleyan.edu)
In this opening unit, students develop the societal context for understanding earthquake hazards using as a case study the 2011 Tohoku, Japan, earthquake. It starts with a short homework "scavenger hunt" ...

Unit 3: Geodetic survey of a fault scarp part of Analyzing High Resolution Topography with TLS and SfM
Bruce Douglas (Indiana University) Nicholas Pinter (University of California Davis) Nathan Niemi (University of Michigan) J. Ramon Arrowsmith (Arizona State University) Kate Shervais (UNAVCO) Chris Crosby (EarthScope)
In this unit, students will design a survey (TLS and/or SfM) of a fault scarp. After conducting the survey in the field, students will analyze the data to identify the number and magnitude of possible fault ...

Unit 2: Identifying faulting styles, rates and histories through analysis of geomorphic characteristics (Lidar) part of Imaging Active Tectonics
Bruce Douglas, Indiana University-Bloomington; Gareth Funning, University of California-Riverside
Can active faults be identified remotely, based upon their appearance in the landscape? How can the geomorphic features associated with active faults be used to classify and quantify fault movement? In this unit, ...

Unit 1: "If an earthquake happens in the desert and no one lives there, should we care about it?" [How are human-made infrastructure lifelines affected by earthquakes?] part of Imaging Active Tectonics
Bruce Douglas, Indiana University-Bloomington; Gareth Funning, University of California-Riverside
This unit initiates a discussion about the importance of recognizing faults in relation to modern societal infrastructure. Students consider the types of infrastructure necessary to support a modern lifestyle, ...

Unit 5: How do earthquakes affect society? part of Imaging Active Tectonics
Bruce Douglas, Indiana University-Bloomington; Gareth Funning, University of California-Riverside
Unit 5 is a final exercise that can start during a lab period and carry over into work outside of the lab time. The project report will test students' abilities to synthesize and apply knowledge related to ...

Unit 4: The phenomenology of earthquakes from InSAR data part of Imaging Active Tectonics
Bruce Douglas, Indiana University-Bloomington; Gareth Funning, University of California-Riverside
How are different types of earthquakes represented in InSAR data? How can we obtain detailed information on the earthquake source from InSAR data? How well can we resolve those details? In this unit, students ...

Unit 3: How to see an earthquake from space (InSAR) part of Imaging Active Tectonics
Bruce Douglas, Indiana University-Bloomington; Gareth Funning, University of California-Riverside
How can we tell what style of faulting was responsible for a particular earthquake? Especially in cases where there is limited instrumentation in a region, or where geologists have difficulty accessing the affected ...

How do Faults Slip: Earthquakes versus Episodic Tremor and Slip part of Deep Earth:Activities
Mike Brudzinski, Miami University-Oxford
A comparison of earthquakes and episodic tremor and slip using GPS and seismic data to illustrate how faults slip.