For the Instructor
These student materials complement the Coastal Processes, Hazards and Society Instructor Materials. If you would like your students to have access to the student materials, we suggest you either point them at the Student Version which omits the framing pages with information designed for faculty (and this box). Or you can download these pages in several formats that you can include in your course website or local Learning Managment System. Learn more about using, modifying, and sharing InTeGrate teaching materials.Case Study 1: 2004 Sumatran Earthquake
The Boxing Day 2004 Earthquake: A Holiday's Worst Nightmare
In order to explore what a tsunami is and how tsunamis are formed, we will use the 2004 Sumatran Tsunami to illustrate exactly how earthquake events can produce such destructive outcomes. You will rely on topics covered in Unit 1 (modules 2 and 3) to help understand the plate tectonics responsible for earthquake activity, but we will use the USGS's Pacific Coastal and Marine Science Center's website to explore the specific geologic details that gave rise to the tsunami. The day after Christmas (December 26, 2004), a large magnitude earthquake occurred just west of the island of Sumatra along a subduction boundary between two tectonic plates. The date couldn't be worse for such an event to occur, with thousands of people on holiday in the region and with very few people working in government offices, it was a recipe for disaster. Tourists from all over the world were vacationing in seaside resorts in Thailand, Indonesia, India, and elsewhere. Unplugged as they were, it was next to impossible to inform them or the residents of the region of the impending hazard once the earthquake and tsunami were detected. The result was that over 150,000 people lost their lives. But how? Let's take some time and work through a series of questions whose answers can be found on the website.
Credit: USGS: Tsunamis and Earthquakes