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Results 11 - 20 of 1123 matches
Geologic Mapping Exercise part of Cutting Edge:Early Career:Previous Workshops:Workshop 2010:Teaching Activities
This exercise is designed to simulate some of the mapping aspects of a basic geological investigation. This mock geological investigation is a good wrap-up exercise because it incorporates a variety of geological ...
Observing Streams & Rivers in Google Earth part of Cutting Edge:Early Career:Previous Workshops:Workshop 2010:Teaching Activities
Students are asked to observe fluvial features on both Earth and Mars in satellite images via Google Earth (as well as online panoramas) and explore processes of erosion and deposition and the relationship of ...
Topographic Maps part of Cutting Edge:Career Development:Pursuing an Academic Career 2010:Teaching Activities
This geology lab is designed to teach students the basic skills needed to read, construct, and interpret topographic maps. The goal of this lab is to help students build direct connections between the topography ...
Comparing Carbon Calculators part of Teaching with Data:Examples
Carbon calculators, no matter how well intended as tools to help measure energy footprints, tend to be black boxes and can produce wildly different results, depending on the calculations used to weigh various ...
Accessing Streamflow Data via the Worldwide Web part of Cutting Edge:Geodesy:Activities
The objectives of this exercise are to (a) use the worldwide web to access hydrologic data, and (b) compare precipitation/runoff characteristics in different regions of the USA.
M & M Decay part of Cutting Edge:Rates and Time:Teaching Activities
This is a simulation of radioactive decay which illustrates what a half-life is and explains some of the challenges involved with radiometric dating. Pennies or other cheap coins can be substituted for M&Ms if ...
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 ...