Trans-California Seismic Profile Analysis
Magali Billen
, U. C. Davis, Department of Geology
Summary
Homework assignment focused on identifying seismic arrivals and
determining layer thickness and velocity using real-world data from a
published article.
Context
Audience
Upper division, elective course in the theory and analysis of exploration geophysics methods.
Designed for a geophysics course
Designed for a geophysics course
Skills and concepts that students must have mastered
Students need to have been introduced to travel-time diagrams, the the
travel-time curves from reflected, refracted and direct waves. Although
the students are encouraged to use MATLAB for the plotting and analysis,
the assignment can be done on graph paper.
How the activity is situated in the course
One in a series of homework assignments on seismic reflection and refraction
methods.
Goals
Content/concepts goals for this activity
Interpreting seismic travel-time data for crustal-scale velocity and layer
structure.
Higher order thinking skills goals for this activity
Synthesis of understanding of different travel-time relationships.
Interpretation of results in terms of earth structure.
Interpretation of results in terms of earth structure.
Other skills goals for this activity
It is expected that students will have to seek out the information
needed to answer the interpretive question on the web or in books from
lower division geology courses.
Description of the activity/assignment
Homework assignment asks the students to analyze data from a refraction profile
across California. The data is presented in a table together with the abstract
and map figure scanned from a 1970s article in which the was published and
analyzed. The assignment requires the student to plot the data, determine
line-fits to the three arrivals, identify the arrivals as the direct,
reflected or refracted arrival and then to determine the layer velocities.
The final question asks the student to consider the velocities and layer
thickness and determine what boundary in the continental crust the refracted
waves come from.
Determining whether students have met the goals
Students have met the goals of the assignment if they correctly identify the
arrivals, determine the layer velocities and the layer thickness. For the
interpretation question, the response needs to explain why they have
made the conclusions based on the results of their analysis.
More information about assessment tools and techniques.Download teaching materials and tips
- Activity Description/Assignment (Acrobat (PDF) 559kB Jul5 07)
- Solution Set (Acrobat (PDF) 594kB Jul5 07)
Other Materials
Supporting references/URLs
The data set included in the homework assignment is from the article
published in:
Cardier D. S., A. Qamar, and T. V. McEvilly, Trans-California Seismic Profile-Pahute Mesa to San Francisco Bay, Bulletin of the Seismological Society of America, v. 60, no. 6, pp 1829-1846, 1970.




