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 ...

Earth's Magnetic Field CogSketch geoscience worksheet part of Introductory Courses:Activities
Bridget Garnier, Blue Valley School
Sketching activity that uses a sketch-understanding program, CogSketch. To draw attention to the changes in magnetic inclination with latitude on Earth, students move, rotate, and match packages of "rock" ...

Unit 2: How Seismic Waves Travel Through the Ground part of Measuring Depth to Bedrock Using Seismic Refraction
Basic concepts in refraction seismology. Andy Parsekian, University of Wyoming, aparseki@uwyo.edu Download a ZIP file of this Unit
This unit presents core underlying principles needed to understand refraction seismology concepts including refraction of rays, types of seismic waves, interpreting information about subsurface materials from ...

A Daily Dose of MATLAB for College Freshmen part of Teaching Computation with MATLAB:MATLAB Workshop 2020:Activities
Frederik J Simons, Princeton University
Teaching first-year college students, with my colleague Adam Maloof, as part of a research-oriented "Freshman Seminar" involves teaching students MATLAB -- from scratch to proficiency. Rather than sharing ...

Geologic Time Calculations part of Quantitative Skills:Activity Collection
Francisco San Juan, Elizabeth City State University
Radiometric age determination using parent/daughter composition and a radiometric decay curve.

A short lecture on evaluation of Complex integrations for Geophysics part of Teaching Activities
Avradip Ghosh, University of Houston-University Park
In Geophysics, we heavily use Fourier/Laplace, or inverse Fourier/Laplace transforms in all branches. Anyone who has tried to evaluate them using pen and paper (especially an inverse Fourier/Laplace transform) ...