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Subject: Structural Geology Show all Subject: Structural Geology
Results 1 - 10 of 61 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. -
Mid-level spreadsheeting and complex modeling of real-world scarp evolution part of Quantitative Skills:Activity Collection
William Locke, Montana State University-Bozeman
This exercise is a second or familiarization exercise in spreadsheeting, but is also a mathematical model for slope evolution. It uses the concept of "erosivity" (generally, the relative ratio of driving and resisting forces) and slope angle to reshape an initial topography. Finally, it asks the students themselves to come up with a real-world situation worth modeling.
Guided Reading of Scientific Journal Articles part of Cutting Edge:Structural Geology:Activities
Carol Ormand, Carleton College
This is a sequence of assignments for my Structural Geology course that guides students through the process of critically reading and analyzing scientific journal articles. For each article, I outline the general ...
Recognizing and mapping faults using lidar and field data part of Cutting Edge:Structural Geology: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 ...
Creating Custom Map Images of Earth and Other Worlds part of Earth Exploration Toolbook:Jules
LuAnn Dahlman; Lou Estey, UNAVCO
DATA: Planetary images and geodesy data. TOOL: UNAVCO's Jules Verne Voyager Map Server. SUMMARY: Generate maps of Earth or any of 19 other planets and moons. Save and import images into presentations or reports.
Maps, Folds, Stereonets, and Simple Fabric Analysis part of Cutting Edge:Structural Geology:Activities
John Weber, Grand Valley State University
This analysis involves analyzing structures shown on beautiful, rich, detailed, and well-prepared outcrop bedrock geology of a real region. Students construct a number of stereonets step-by-step, and the map-scale ...
Borehole analysis using stereographic projection part of Cutting Edge:Structural Geology:Activities
Eric Nelson, Colorado School of Mines
Advanced stereonet project using unoriented core structural data. The project gives practice in plotting small circles and in rotations. -
Evolution of Normal Fault Systems During Progressive Deformation part of Cutting Edge:Structural Geology: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 ...
Tectonics of Fiction part of Structure, Geophysics, and Tectonics 2012:Activities
Kyle Fredrick, California University of Pennsylvania
This writing project of our Tectonics course is assigned at the start of the semester and due near the end. It is a group project that encourages creativity, cooperation, and synthesis of an entire ...
Determining Earthquake Recurrence Intervals from Trench Logs part of Rates and Time:GSA Activity Posters
Patricia Cashman, University of Nevada-Reno
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.