AP/IB/Honors Geoscience Activity Browse
Resource Type: Activities
- ACM Pedagogic Resources 6 matches
- CLEAN 1 match
- Curriculum for the Bioregion 46 matches
- Cutting Edge 873 matches
- Earth Exploration Toolbook 34 matches
- EarthLabs 2 matches
- EarthLabs for Educators 45 matches
- Geoscience in Two-year Colleges 9 matches
- Integrate 50 matches
- Integrating Research and Education 3 matches
- Keyah Math 2 matches
- MARGINS Data in the Classroom 26 matches
- NAGT 77 matches
- Pedagogy in Action 51 matches
- Quantitative Skills 87 matches
- SISL 12 matches
- Starting Point-Teaching Entry Level Geoscience 524 matches
- Teacher Preparation 8 matches
- Visualizing the Liberal Arts 2 matches
Results 41 - 60 of 1858 matches
Determining Earthquake Recurrence Intervals from Trench Logs part of Rates and Time:GSA Activity Posters
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.
Roping Geologic Time part of Rates and Time:GSA Activity Posters
After having talked about the geologic time scale, I ask for two volunteers from the class to hold a rope that is 50 feet long. I say that one end is the beginning of the Earth (4.6 billion years ago), and the other is today. I then give out 16 clothes pins and ask various students to put a cloths pin on the 'time line' at various 'geologic events'. Throughout the activity I have a quiz going on where the students calculate percentages of Earth History for major geologic events, and compare it to their own ages. On their time scale, the dinosaurs died only about two 'months' ago! The exercise is very effective at letting them get a sense of how long geologic time is, and how 'recently' some major geologic events happened when you consider a time scale that is the age of the earth.
The Evolution of Earth through Time part of Cutting Edge:Rates and Time:Teaching Activities
This activity is designed for large freshman courses (>200 students) and is used in-class. The activity requires a short (15 minute) overview of Earth history before students have the opportunity to work through ...
Hierarchical Alignment of Timelines part of Cutting Edge:Rates and Time:Teaching Activities
In the hierarchical alignment activity students progressively and hierarchically align scale information to a spatial linear representation. The progressive alignment of scales may alleviate the conceptual ...
Aerial photo interpretation and mapping - Bayou Meda anticline, Arkansas part of Cutting Edge:Geoscience in the Field:Activities
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 ...
How Many Is A Million? part of Cutting Edge:Rates and Time:Visualizations with Teaching Notes
Roger Steinberg, Department of Natural Sciences, Del Mar College Description To help students visualize the immensity of geologic time, or even the immensity of just one million years, I have created a very large ...
A Cross-Section and Geologic History from Field Data Collected by Second Year Students in the St Francois Mountains of Missouri part of Cutting Edge:Geoscience in the Field:Activities
This field activity takes place during a 3-day field trip to St Francois Mountains, Missouri. Students use their field data to construct a cross-section through a portion of the field area.
Field Trip to Enfield Glen, NY Finger Lakes Region part of Cutting Edge:Geoscience in the Field:Activities
This is a 2.5 hour field trip in which students search through strata of the Upper Devonian Catskill Delta for paleocurrent indicators that allow them to infer paleogeographic differences between Devonian and ...
Depositional Environments and Geologic History Labs part of Cutting Edge:Rates and Time:Teaching Activities
This is a pair of labs that incrementally prepare students to interpret the geologic history of a rock sequence. The first lab introduces students to depositional environments and fossils. The second lab presents a ...
Building Blocks part of Cutting Edge:Environmental Geology:Activities
In association with rock and mineral ID tables, this lab introduces students to basic rocks and minerals via grouping and comparison, rather than as individual samples. I use this lab in my environmental geology ...
Global Earthquakes: Teaching about Earthquakes with Data and 3D Visualizations part of Cutting Edge:Visualization:Examples
In this series of visualizations and accompanying activities, students visualize the distribution and magnitude of earthquakes and explore their distribution at plate boundaries. Earthquakes are visualized on a 3D ...
Visualizing Global Earthquakes Where and Why do Earthquakes Occur? part of Cutting Edge:Visualization:Examples
In this activity students visualize the distribution and magnitude of earthquakes at and below the surface of Earth and how their distribution is related to plate boundaries. Earthquakes are visualized on a 3D ...
Visualizing Earthquakes at Divergent Plate Margins part of Cutting Edge:Visualization:Examples
In this activity students visualize the distribution and magnitude of earthquakes at divergent plate boundaries. Earthquakes are visualized on a 3D globe, making it easy to see their distribution within ...
Marine Oxygen Isotopes and Changes in Global Ice Volume part of Cutting Edge:Climate Change:Activities
Students explore marine oxygen-isotope data from cores collected by the Ocean Drilling Program. The activity gives students access to real paleoclimate data, develops their skills in organizing and graphing data, ...
The Non-linearity of Environmental Change: A coral reef model part of Cutting Edge:Environmental Geology:Activities
This is an exercise that is used in an undergraduate, non-major course titled "Coral Reefs: Biology, Geology & Policy". The course uses this popular environment as a proxy for environmental decline ...
Case Study: Zhouqu, China Landslide part of Cutting Edge:Environmental Geology:Activities
This is a 'citizen science' research project where students to apply their knowledge of landslide processes in an investigation of the natural and anthropogenic causes of a real-world landslide ...
Recognizing and mapping faults using lidar and field data part of Cutting Edge:Structural Geology:Structure, Geophysics, and Tectonics 2012:Activities
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 ...
Half Life Model part of Starting Point-Teaching Entry Level Geoscience:Interactive Lecture Demonstrations:Examples
While working in groups to facilitate peer tutoring, students manipulate a hands-on, physical model to better comprehend the nature of half life. Students use the model to simulate the decay of radionuclides. The ...
Paleotempestology Lab part of Cutting Edge:Introductory Courses:Activities
Paleotempestology Lab: this lab activity is designed to help students gain experience in relative and absolute dating techniques as well as a sense of how scientific investigations proceed.
Where is that chunk of crust going? part of Cutting Edge:Introductory Courses:Activities
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 ...