AP/IB/Honors Geoscience Activity Browse
Resource Type: Activities Show all Resource Type: Activities
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- Cutting Edge 337 matches
- Earth Exploration Toolbook 34 matches
- EarthLabs 2 matches
- EarthLabs for Educators 39 matches
- Geoscience in Two-year Colleges 7 matches
- Integrate 6 matches
- Integrating Research and Education 3 matches
- MARGINS Data in the Classroom 14 matches
- NAGT 12 matches
- Pedagogy in Action 6 matches
- Quantitative Skills 49 matches
- SISL 1 match
- Starting Point-Teaching Entry Level Geoscience 424 matches
- Teacher Preparation 4 matches
Results 1 - 20 of 938 matches
The Sleeping Mountain part of Starting Point-Teaching Entry Level Geoscience:Role Playing:Examples
In this role-playing scenario, students represent townspeople whose lives and livelihoods are endangered by an active volcano which may or may not erupt in the near future. -
Geologic Puzzles: Morrison Formation part of Starting Point-Teaching Entry Level Geoscience:Interactive Lectures:Examples
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. -
Is Greenland Melting? part of Earth Exploration Toolbook:GreenlandMelt
DATA: Thickness, velocity, and annual melt extents of the Greenland ice sheet TOOL: My World GIS SUMMARY: Explore map layers to examine annual melting and long-term changes of Greenland's ice sheet.
How Fast Do Materials Weather? part of Starting Point-Teaching Entry Level Geoscience:Interactive Lectures:Examples
A think-pair-share activity in which students calculate weathering rates from tombstone weathering data. -
Carbon Dioxide Exercise part of Starting Point-Teaching Entry Level Geoscience:Interactive Lectures:Examples
Students work in groups, plotting carbon dioxide concentrations over time on overheads and estimating the rate of change over five years. -
Being P-Waves and S-Waves part of Starting Point-Teaching Entry Level Geoscience:Role Playing:Examples
Teach students about P-waves and S-waves by having them model them with their own bodies. -
Whose Fault Is It Anyway? part of Starting Point-Teaching Entry Level Geoscience:Games:Examples
This game has students simulate the propagation of P and S waves after an earthquake and to use the lag between these to determine where in the simulation the earthquake occurred. -
Analyzing the Antarctic Ozone Hole part of Earth Exploration Toolbook:Analyzing the Antarctic Ozone Hole
DATA: Total Ozone Mapping Spectrometer (TOMS) Images. TOOLS: ImageJ, Spreadsheet. SUMMARY: Animate and explore 10 years of Southern Hemisphere ozone images. Then measure and graph the area of the ozone hole over time.
Back-of-the-Envelope Calculations: Weight of Gold part of Quantitative Skills:Activity Collection
Question Let's suppose that you have a shoe box full of water (the box is waterproof, of course). The shoe box weighs about 9 kg (19.8 pounds). Suppose you emptied the box and filled it completely with rock ...
Evolution of Normal Fault Systems During Progressive Deformation part of Cutting Edge:Structural Geology:Activities
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 ...
Directed Discovery of Crystal Structures part of Integrating Research and Education:Crystallography:Directed Discovery of Crystal Structures
David Mogk and Kent Ratajeski Department of Earth Sciences, Montana State University, Bozeman, MT Published Jan. 25, 2005 Description This contribution is modified from a published exercise "Directed ...
Runaway Greenhouse Effect Exercise part of Starting Point-Teaching Entry Level Geoscience:Role Playing:Examples
This site has a collection of role-playing exercises that provide the students with equations and data to use in collaborative problem-solving. -
Two streams, two stories... How Humans Alter Floods and Streams part of Quantitative Skills:Activity Collection
An activity/lab where students determine the changes in 100-year flood determinations for 2 streams over time.
2004 Asian Earthquake and Tsunami Disaster Project part of Starting Point-Teaching Entry Level Geoscience:Cooperative Learning:Examples
Students are employees of a unit of the United Nations responsible for coordinating disaster relief after a major disaster (the 2004 Asian Earthquake and Tsunami) occurs. The agency needs to understand the ...
Directed Discovery of Crystal Structures part of Cutting Edge:Mineralogy:Activities
This online exercise uses a "discovery-based" approach and the latest online crystallographic information and visualization software to teach the spatial relationships and crystal-chemical rules that ...
Pathogenic Microorganisms in Water part of Cutting Edge:Hydrogeology:Activities
This activity introduces students to sampling and testing for microorganisms in different water sources. It also tests iodine tablets to kill coliform bacteria which interest many students. The activity utilizes ...
Mineral Classification Exercise part of Cutting Edge:Mineralogy:Activities
This exercise gets students thinking about mineral classification and the properties that are most useful for classifying and identifying minerals.
Igneous Rock Compositions and Plate Tectonics part of Cutting Edge:Petrology:Teaching Examples
In this exercise, students use whole-rock major- and trace-element compositions of igneous rocks from a variety of tectonic settings and locations to explore the importance of plate setting in determining magma ...
Creating Custom Map Images of Earth and Other Worlds part of Earth Exploration Toolbook:Jules
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.
Mass Balance and Mineral Reactions part of Cutting Edge:Petrology:Teaching Examples
This is a short exercise to make sure that students understand mass balance and how the different starting assemblages may lead to different results after metamorphism. It is quick but not trivial.