Teaching Activities
These teaching activities have been submitted by participants in Cutting Edge workshops and all have to do with Structural Geology, Geophysics, and/or Tectonics. You can narrow the view by using the free-text search box as well as by selecting terms from the list on the right. This will allow you to see a particular slice through the collection.
Subject: Geology
- 40 matches General/Other
- Economic Geology 2 matches
- Environmental Geology 7 matches
- Geochemistry 21 matches
- Geomorphology 33 matches
- Geophysics 290 matches
- Historical Geology 16 matches
- Igneous and Metamorphic Petrology 68 matches
- Mineralogy 11 matches
- Sedimentary Geology 24 matches
- Structural Geology 242 matches
- Tectonics 291 matches
Results 1 - 10 of 668 matches
Getting started with Structure from Motion (SfM) photogrammetry
Beth Pratt-Sitaula, EarthScope
Structure from Motion (SfM) photogrammetry method uses overlapping images to create a 3D point cloud of an object or landscape. It can be applied to everything from fault scarps to landslides to topography. This ...
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Measuring Ground Motion with GPS: How GPS Works
Shelley E Olds, EarthScope Consortium; Daniel Zietlow, UNAVCO; David Thesanga, Alexander Dawson School
With printouts of typical GPS velocity vectors found near different tectonic boundaries and models of a GPS station, demonstrate how GPS work to measure ground motion.GPS velocity vectors point in the direction that a GPS station moves as the ground it is anchored to moves. The length of a velocity vector corresponds to the rate of motion. GPS velocity vectors thus provide useful information for how Earth's crust deforms in different tectonic settings.
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Measuring Plate Motion with GPS: Iceland | Lessons on Plate Tectonics
Roger Groom, Mt. Tabor Middle School; Cate Fox-Lent, UNAVCO; Shelley E Olds, EarthScope Consortium; Nancy West, Quarter Dome Consulting; David Thesenga, Front Range Community College
This lesson teaches middle and high school students to understand the architecture of GPS—from satellites to research quality stations on the ground. This is done with physical models and a presentation. Then students learn to interpret data for the station's position through time ("time series plots"). Students represent time series data as velocity vectors and add the vectors to create a total horizontal velocity vector. They apply their skills to discover that the Mid-Atlantic Ridge is rifting Iceland. They cement and expand their understanding of GPS data with an abstraction using cars and maps. Finally, they explore GPS vectors in the context of global plate tectonics.
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Working with Point Clouds in CloudCompare and Classifying with CANUPO
Sharon Bywater-Reyes, University of Northern Colorado
This exercise will walk you through 1) basic operations and use in CloudCompare, and 2) use of an Open-Source plugin in CloudCompare called CANUPO (http://nicolas.brodu.net/en/recherche/canupo/) that allows for ...
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Exploring California's Plate Motion and Deformation with GPS | Lessons on Plate Tectonics
Roger Groom, Mt. Tabor Middle School; Andy Newman, Georgia Institute of Technology; Shelley E Olds, EarthScope Consortium; Cate Fox-Lent, UNAVCO; Nancy West, Quarter Dome Consulting; David Thesenga, Front Range Community College
Students analyze data to study the motion of the Pacific and North American tectonic plates. From GPS data, students detect relative motion between the plates in the San Andreas fault zone--with and without earthquakes. To get to that discovery, they use physical models to understand the architecture of GPS, from satellites to sensitive stations on the ground. They learn to interpret time series data collected by stations (in the spreading regime of Iceland), to cast data as horizontal north-south and east-west vectors, and to add those vectors head-to-tail.Students then apply their skills and understanding to data in the context of the strike-slip fault zone of a transform plate boundary. They interpret time series plots from an earthquake in Parkfield, CA to calculate the resulting slip on the fault and (optionally) the earthquake's magnitude.
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Sandy Hollow Virtual Field Geology Exercise
Andrew Laskowski, Montana State University; Devon A. Orme, Montana State University-Bozeman
This is a Google Earth based virtual field exercise focused on Sandy Hollow, near Block Mountain and McCartney Mountain in southwest Montana. This is a classic field locality in the Montana portion of the Sevier ...
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Geology of Yosemite Valley
Nicolas Barth, University of California-Riverside
This is a four-part module designed to be flexible in duration and student grade-level. (1) Geology of Yosemite Valley Virtual Field Trip. A 43-stop web-based Google Earth tour with embedded views, hyperlinked ...
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Magnetometry at home: a hands-on survey with your smartphone
Charly Bank, University of Toronto
Using a free app downloaded to their smartphone or tablet device students engage in collecting magnetic field data. Students have to design and document a survey, and are encouraged to do simple quality control. ...
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Karst Hydrogeology: A virtual field introduction using Google Earth and GIS
Rachel Bosch, Northern Kentucky University
Students will have the opportunity to select and virtually explore the hydrogeology and geomorphology of a karst landscape using Google Earth, lidar data-sourced DEM(s) and geologic maps, and GIS software (QGIS) ...
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Pinpointing Location with GPS Demonstration: How GPS Works (Part 2)
Shelley E Olds, EarthScope Consortium; Daniel Zietlow, UNAVCO; David Thesenga, Alexander Dawson School
Using string, bubble gum, and a model of a GPS station, demonstrate how GPS work to pinpoint a location on Earth.Precisely knowing a location on Earth is useful because our Earth's surface is constantly changing from earthquakes, volcanic eruptions, tectonic plate motion, landslides, and more. Thus, scientists can use positions determined with GPS to study all these Earth processes.
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