I use an "engaging question" on the first day of class in all of my courses. This activity is designed to be both engaging and central to all of the course content. That is, the activity is designed around questions that we can keep coming back to, over and over, after each learning unit. This approach not only provides a unifying focus for the course, but it also provides an opportunity to model critical thinking as we revisit the question each time with a different perspective. For the Dynamic Earth and Global Change (the Physical Geology course at Macalester) I chose a question about climate change. The activity starts with two graphs (plots of surface temperature and atmosphere CO2 composition for the past 1,000 years). Students are asked to describe the graphs, interpret the graphs, make some predictions, and explain the graphs using basic earth science processes.

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This hands-on lesson introduces students to the engineering design process. It connects to the story The Three Billy Goats Gruff. Students will use the design process to create a bridge that will keep the Billy Goats Gruff safe and complete the Engineering Design Process Journal.

Students are introduced to the engineering design process within the context of reading Dr. Seuss’s book, Bartholomew and the Oobleck. To do so, students study a sample of aloe vera gel (representing the oobleck) in lab groups. After analyzing the substance, they use the engineering design process to develop and test other substances in order to make it easier for rain to wash away the oobleck. Students must work within a set of constraints outlined within the Seuss book and throughout the activity and use only substances available within the context of the plot. Students also take into consideration the financial and environmental costs associated with each substance.

Students use a recipe to prepare a hydrogel gummy snack, which has a similar consistency to that found in a Haribo® gummy product. They must convert the juice and gelatin-based recipe from US customary units to metric units with dimensional analysis conversion. After unit conversion, teams are given different gelatin quantities and design their gummy snacks. Once the candies have solidified, student groups compare the gummy snacks are for viscosity and taste. After a taste test, teams reflect on their experiment and brainstorm ways to iterate a better gummy recipe.

To complete this activity, students can follow the instructions and the tutorial in the Environmental Health Risk Inventory website. In doing this, they will gain an understanding of how to use on-line tools and databases as well as the processes of compiling an environmental health risk inventory for a specific locale. In the activity, students will address the question: "how healthy is your neighborhood?" Students will address anthropogenic and naturally-occurring health risks in their hometown or neighborhood by using data collected from online mapping tools and databases. Students will also complete a reflective summary based on the data that they collect.

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An activity designed to enable the students to access the impact of oil-development on environment in Alaska. Students will draw conclusion based on various data and reading various views.

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Earthquakes in western Washington and Oregon are to be expected -- the region lies in the Cascadia Subduction Zone. Offshore, the Juan de Fuca tectonic plate subducts under the North American plate, from northern California to British Columbia. The region, however, also experiences exotic seismicity -- Episodic Tremor and Slip (ETS).In this lesson, your students study seismic and GPS data from the region to recognize a pattern in which unusual tremors--with no surface earthquakes--coincide with jumps of GPS stations. This is ETS. Students model ductile and brittle behavior of the crust with lasagna noodles to understand how properties of materials depend on physical conditions. Finally, they assemble their knowledge of the data and models into an understanding of ETS in subduction zones and its relevance to the millions of residents in Cascadia.

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This short video and interactive assessment activity is designed to teach fifth graders about estimating the measure of objects by image: feet or inches?.

This lesson unit is intended to help you assess how well students are able to: solve simple problems involving ratio and direct proportion; choose an appropriate sampling method; and collect discrete data and record them using a frequency table.

On July 4th, 1997, Mars Pathfinder landed at the mouth of Ares Vallis, a large channel that drains into the Chryse Planitia basin. While there remains a great deal to debate about the origin of the channels, one of the leading hypotheses at present is the idea that these features are the result of catastrophic flooding. If this is correct, then the plains where Pathfinder landed may be rich in debris eroded out of the Martian highlands across which the Ares Vallis channel passes, providing a golden combination -- a relatively safe landing site which still provides access to a wide variety of different rock types. [If you would like to learn more about the many Pathfinder results, explore the April, 1999 and January, 2000 issues of the journal Journal of Geophysical Research -- Planets (the green one) in the library.]

For the sake of this lab assignment you will hypothesize that the Ares Vallis and associated deposits were indeed produced by catastrophic flooding, and will use the information at your disposal to learn all you can about the putative flooding event.

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Simple budgets may be used to estimate the exchange of water in embayments that capitalize on the concept of steady state and conservation principals. This is especially true for bays that experience a significant exchange of freshwater. This exchange of freshwater may reduce the average salt concentration in the bay compared to seawater if it involves addition of freshwater from rivers, R, and/or precipitation, P. Alternatively, it may increase the average salt concentration in the bay compared to seawater if there is relatively little river input and high evaporation, E. Since freshwater input changes the salt concentration in the bay, and salt is a conservative material, it is possible to combine two steady state budgets for a bay, one for salt and one for water, to solve for the magnitude of the water flows that enter and exit the bay mouth.
Students will make actual calculations for the inflow and outflow of water to Puget Sound, Washington and the Mediterranean Sea and compare them to actual measured values.

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Description here.

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In this computer lab, students use satellite imagery, daylength information, and phytoplankton physiology models to calculate annual primary production for an assigned ocean region.

Satellite data is obtained from the NASA Earth Observation website. Students use the analysis tool to determine chlorophyll concentration and sea surface temperature. They also receive a day-length calculator and are asked to model light transmission through the water column. Using step-by-step instructions and proviede equations relating phytoplankton physiology to irradiance and temperature students calculate carbon uptake at discreet locations in the water column. The second half of the exercise involves scaling up to the entire water column, region, and season. Students present their work to the class and evaluate their result using scientific literature. Differences between regions are then discussed by the class.

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This short video and interactive assessment activity is designed to teach fifth graders about estimating the measure of items by description: inches, feet, or yards?.

This module introduces students to the fundamental principles and uses of electrical resistivity, with a focus on an environmental application. Students explore the characteristics and environmental setting of Harrier Meadow, a saltmarsh just outside of New York City. They investigate the relationship between electrical resistivity and physical properties of the soil in the marsh. Students also discover how variations in survey configuration parameters control investigation depth (how far into the ground the signals sense) and spatial resolution (what size objects can be detected). Finally, students learn about and then perform geophysical inversion, which is the process of estimating the geophysical properties of the subsurface from geophysical observations. In the final unit of the module, students evaluate the extent to which the geophysical dataset and direct physical measurements support the hypothesis, introduced in Unit 1, accounting for the distribution of Pickleweed in Harrier Meadow.
This module is intended to require approximately 2-3 weeks of class time. Teaching material includes PowerPoints that may be used in lectures or provided for self-guided learning, exercises, and handouts that ask students to synthesize what they learn from the exercises. In addition, multiple choice and short answer questions can be given to students as homework, on quizzes, or on exams.

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Many papers by Ken McClay and colleagues have established the value of scale-model experiments in understanding the evolution and geometries of extensional fault systems (e.g. T. Dooley and K.R. McClay, 1997, Analogue modeling of pull-apart basins: American Association of Petroleum Geologists Bulletin, v. 81, no.11, p. 1804 -- 1826).

There are few resources available that help students visualize the dynamic nature of faulting, especially the complex interplay of faults during growth and evolution of a fault system. Such an understanding is critical, however, if students are to think meaningfully about fault geometries and what they imply.

Conducting scale-model experiments in a class setting is useful, but very time-consuming, difficult for all students to see well, and very temporary, except for the end product. Accordingly, taking a cue from a movie produced by Ken McClay, I constructed a deformation apparatus, conducted and filmed several experiments conducted by McClay, and then produced QuickTime movies of the experiments. This approach makes it possible for students to observe an experiment in a minute or two that took 30-45 minutes to produce and to view the experiment repeatedly, so as to become very familiar with all that is taking place.

Individual frames from the movie provide a template on which students can identify the sequence of fault development, rotation of features, and cessation of motion on some faults as they become inactive. Requiring students to document their observations, establish a chronological sequence of events, and explain in writing what happens during the experiment results in an increased awareness of the faulting process.

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In this exercise, students process LiDAR data for the Hamilton College campus area to determine accurate elevations of wellheads of sampling wells on campus. Students use both GPS readings and orthophotos to determine wellhead locations and combine those with water levels, casing heights, and wellhead elevations to interpolate a groundwater surface under the campus and portray the groundwater in ArcScene. They also learn how to use Model Builder. You might also be interested in our Full GIS course with links to all assignments. You might also be interested in our webinar for the NYS GIS Association on A Simple Example of Working with LiDAR using ArcGIS and 3D Analyst.

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Ice core data allow students to explore a number of patterns while learning that researchers need to gather and interpret evidence to understand Earth's past. Students will explore core data collected in Western Greenland that document a few decades of Earth's atmosphere. Students are challenged to identify patterns and then use those patterns and background information to answer a few key questions. The data include measurements of temperature, dust, and atmospheric gases.
Downloadable files are provided for those who intend to run the activity in person. For those running the activity with an online or virtual class, a separate page includes all of the necessary information for students to complete the activity, including an interactive graph and background readings. Support videos are provided.

Students learn far more from doing than from viewing. By seeing relationships that they have developed themselves, by diagraming those relationships themselves, students learn far more than merely reading over what someone else has done. It is argued that especially for the dynamic problems encountered in environmental and resource economics, Excel has a comparative advantage as a learning aid. We develop a simple, flexible Excel assignment to illustrate the Brander and Taylor (1998) model of the Easter Island economy. Brander and Taylor argue that on Easter Island a crucial natural resource, the island's palm forest, was an open-access (res nullius) resource, leading to over harvesting and eventual societal collapse. Brander and Taylor's simple model showing the interaction of human population with a renewable resource, a forest, mimics what is known about the human population and forest from archaeological evidence.

The open access institutional protection of renewable resources is illustrated by a simple diagram of population and resource stock over centuries, a model much like ordinary predator-prey models in biology. Variations on the basic Brander and Taylor model, such as changes in propoerty rights institutions and/or changes in technology, based on published work in the literature, can be explored and compared to the original Brander and Taylor results of boom and eventual collapse.

Brander, J.A. and M.S. Taylor (1998). The simple economics of Easter Island: A Ricardo -- Malthus model of renewable resource use. American Economic Review

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In this activity, students use real water chemistry data and descriptive statistics in Excel to examine primary productivity in an urban estuary of the Salish Sea. They will consider how actual data do or do not support expected annual trends.