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Subject: Structural Geology
- 20 matches General/Other
- Folds/Faults/Ductile Shear Zones
- Microstructures, Deformation Mechanisms, Fabrics
- Stress/Strain/Strain Analysis
- Rheology/Behavior of Materials
- Modeling Structural Processes
- Regional Structural/Tectonic Activity
- Geophysics and Structural Geology Earthquakes/Seismic Reflection Profiling
- Structural Visualizations Maps/Air Photos/Images/Cross Sections/Projections
Results 1 - 10 of 98 matches
Geologic Puzzles: Morrison Formation part of Starting Point-Teaching Entry Level Geoscience:Interactive Lectures:Examples
Heather Macdonald, College of William and Mary
Images of faulted strata, tilted turbidites, and beach rocks bring the field into the classroom, giving students practice in doing what geoscientists do. These images are examples of geologic puzzles. -
Evolution of Normal Fault Systems During Progressive Deformation part of Activities
Bob Burger, Smith College
This activity is based on QuickTime movies and color digital photographs derived from sandbox experiments that produce normal faults in a variety of boundary conditions following experiments developed by Ken ...
Using THEMIS Images of Mars Graben in a Structural Geology Course part of Cutting Edge:Discoveries from Mars:Activities
Barb Tewksbury, Hamilton College
Students use Mars THEMIS images of normal faults to learn to recognize features of normal faults systems that are typically obscured on Earth by erosion and/or deposition and to calculate displacement and estimate ...
Did it Rain on Mars? Analysis of Valley Networks on Mars in an Intro Geo Course part of Cutting Edge:Discoveries from Mars:Activities
Barb Tewksbury, Hamilton College
Students investigate the question of whether it might have rained on Mars by doing an activity based on an article by Hynek and Phillips (2003). Students do a simple drainage basin analysis based on Hynek and ...
What is Magnitude? Earthquake Magnitude By Analogy part of Cutting Edge:Geophysics:Workshop 07:Geophysics Activities
Scott White, University of South Carolina-Columbia
Understanding magnitude scales by analogy to distance. Students use distance as a proxy for understanding how the logarithmic earthquake magnitude scale works. Very simple class or lab exercise for introductory ...
Where is that chunk of crust going? part of Cutting Edge:Introductory Courses:Activities
Vince Cronin, Baylor University
I introduce students to GPS, frames of reference, and the permanent GPS stations in the EarthScope Plate Boundary Observatory (PBO) in class, and obtain near-real-time data for two stations from UNAVCO. We use ...
Emergent Models in Google Earth part of Cutting Edge:Introductory Courses:Activities
Declan De Paor, Old Dominion University
This is one sample of a set of emergent models we are developing for use with Google Earth. Students use the Google Earth time-slider to lift 3D models of the subsurface into view. They can substitute their own ...
How do Faults Slip: Earthquakes versus Episodic Tremor and Slip part of Cutting Edge: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.
Aerial photo interpretation and mapping - Bayou Meda anticline, Arkansas part of Cutting Edge:Geoscience in the Field:Activities
Jamey Jones, University of Arkansas at Little Rock
Multi-day project using aerial photography and field observation to map and interpret a megascopic anticline/syncline pair exposed in the Ouachita Mountains of central Arkansas. This exercise involves two classroom ...
Determining Earthquake Recurrence Intervals from Trench Logs part of Rates and Time:GSA Activity Posters
Patricia H. Cashman
Trench logs of the San Andreas Fault at Pallett Creek, CA are the data base for a lab or homework assignment that teaches about relative dating, radiometric dating, fault recurrence intervals and the reasons for uncertainty in predicting geologic phenomena. Students are given a trench log that includes several fault strands and dated stratigraphic horizons. They estimate the times of faulting based on bracketing ages of faulted and unfaulted strata. They compile a table with the faulting events from the trench log and additional events recognized in nearby trenches, then calculate maximum, minimum and average earthquake recurrence intervals for the San Andreas Fault in this area. They conclude by making their own prediction for the timing of the next earthquake.