Unit 3: Codorus Creek Case Study: Measuring and Interpreting Seismic Refraction Data part of Measuring Depth to Bedrock Using Seismic Refraction
Using seismic refraction data in a case study for urban renewal. Andy Parsekian, University of Wyoming, aparseki@uwyo.edu Download a ZIP file of this Unit
This unit presents an applied case study example and the associated concepts related to designing a seismic survey and analyzing the data. It discusses parts of the instrument and presents practical experience ...

Career Portfolio part of E-STEM:Field Course:ESTEM-PD Activities
Sarah R. Hall, College of the Atlantic Calla Schmidt, University of San Francisco Becca Walker, Mt. San Antonio College
This activity is an opportunity for students to document their interaction with environmental professionals with whom they interact during and after their environmental field course. Each career portfolio entry ...

Tectonic Plates Life Cycle Drag and Drop part of IODP School of Rock 2020:Teaching Activities
Beverly Owens, Cleveland Early College High School; Molly Ludwick, Kings Mountain Middle School
This activity will allow students to manipulate Google slide textboxes to explore different features of tectonic plates and their interactions.

Unit 1: Introducing Shallow Seismology to Explore Our Subsurface Environment part of Measuring Depth to Bedrock Using Seismic Refraction
Introduction to the importance and relevance of geophysics. Andy Parsekian, University of Wyoming, aparseki@uwyo.edu Download a ZIP file of this Unit
This introductory unit is designed to provide a standalone introduction to geophysical imaging of the shallow subsurface, motivate students to become invested in the topic, provide career context for these ...

Unit 2.6: Is heat always a dead end, or can it do something useful too? part of TIDeS:TIDeS Teaching Materials:Physical Science
Sandra Penny, Russell Sage College, and Natalie Bursztyn, University of Montana
Students focus on some thermodynamic aspects of energy: Heat, heat engines, and the second law of thermodynamics. We have already laid the groundwork for these concepts in Unit 2.3 (Energy Types and ...

Unit 2.4: Power part of TIDeS:TIDeS Teaching Materials:Physical Science
Sandra Penny, Russell Sage College
In this unit, students explore the relationship between energy and power when they design an experiment to measure and calculate their maximum power output by running up a staircase at a fast, medium, and slow ...

Unit 4.3 Nature and machine: implementation of forces part of TIDeS:TIDeS Teaching Materials:Physical Science
Natalie Bursztyn, University of Montana
How do forces cause Earth's crust to collide and divide? Students plan, design, and construct a model of plate tectonics to further develop a concept that they began to investigate back in Unit 3. Then, ...

Unit 4.4 Unit synthesis and lesson plan part of TIDeS:TIDeS Teaching Materials:Physical Science
Natalie Bursztyn, University of Montana
In this final unit for the course, students apply their understanding of motion and forces concepts to: 1. Create an NGSS lesson plan for an activity that they have completed in Unit 4; and 2. Conduct analyses of ...

Unit 1: What Is Ground-Penetrating Radar? part of Forensic Geophysics Using Ground Penetrating Radar
Sarah Kruse, University of South Florida, skruse@usf.edu Christine Downs, University of South Florida, christinemdowns1@gmail.com Download a ZIP file of this Unit
This unit introduces the concepts behind ground-penetrating radar (GPR) through a comparison to medical imaging, building on what students may already know or be familiar with. The concepts are then extended to ...

Unit 2: What does GPR data look like? part of Forensic Geophysics Using Ground Penetrating Radar
Sarah Kruse, University of South Florida, skruse@usf.edu Christine Downs, University of South Florida, christinemdowns1@gmail.com Download a ZIP file of this Unit
GPR imaging is more complex than is portrayed in the media. This unit describes what the GPR response for a buried object looks like. This is a distorted image of the object itself. Nevertheless, the response we do ...