Topographic differencing: Earthquake along the Wasatch fault part of Teaching Activities
Chelsea Scott, Arizona State University at the Tempe Campus
After a big earthquake happens people ask, 'Where did the earthquake occur? How big was it? What type of fault was activated?' We designed an undergraduate laboratory exercise in which students learn how ...

Unit 1: Slip-sliding away: case study landslides in Italy and Peru part of Surface Process Hazards
Sarah Hall, College of the Atlantic; Becca Walker, Mt. San Antonio College
How have mass-wasting events affected communities, and what lessons have we learned from these natural disasters that might help us mitigate future hazards? In this unit, students answer these questions by being ...

Unit 5: Summative assessment project part of Analyzing High Resolution Topography with TLS and SfM
Bruce Douglas (Indiana University) Chris Crosby (EarthScope Consortium) Kate Shervais (UNAVCO)
Unit 5 is the summative assessment for the module. This final exercise takes eight to ten hours. The exercise evaluates students' developed skills in survey design, execution of a geodetic survey, and simple ...

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 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 ...

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 ...

Global Topography and Tectonic Plates part of Structural Geology and Tectonics:Structure, Geophysics, and Tectonics 2012:Activities
David Greene, Denison University
The goal of this activity is to investigate global topographic and tectonic features, especially the tectonic plates and their boundaries. Using a double-page size digital topographic map of the Earth that includes ...

Cracked, Bumpy and Beautiful: Earth's Surface part of Earth and Space Science:Summer 2010:Activities
Lisa Alexander
Using a variety or resources, students will plot the locations of mountain ranges,volcanoes and major earthquakes on a class map. Students will then hypothesize what may be creating concentrated areas of these ...

Recognizing and mapping faults using lidar and field data part of Structural Geology and Tectonics:Structure, Geophysics, and Tectonics 2012:Activities
Anne Egger, Central Washington University
In this activity, students create a geologic map and cross-section of the Fish Springs cinder cone and surrounding area in the Owens Valley, CA, using a high-resolution DEM developed from airborne lidar data as a ...