Introducing Mountain Building, Obduction & Tsunamis
"No matter how sophisticated you may be, a large granite mountain cannot be denied—it speaks in silence to the very core of your being."
—Ansel Adams, The Spirit of the Mountains
Old, cold sea floor goes down subduction zones beneath warmer sea floor or continent, but what happens when a high-floating continent or island arc tries to go down a trench under another continent or island arc?
The answer is obduction, a BIG collision. The Great Smokies, Mt. Nittany near Penn State's University Park campus, and all of the Appalachians were formed by just such a collision when Africa and Europe hit the Americas, causing a long, thin slab of crust to become a short, thick one by folding and thrust-faulting. Higher mountains have deeper roots (for the same reason that toy boats can float in less water than aircraft carriers, and the iceberg that sank the Titanic stuck farther down in the water than did the ice cubes in the drinks on deck). When erosion lowers a mountain range, the root floats up, bringing metamorphic rocks to the surface that have been "cooked" by heat and pressure deep within the Earth.
Before we go any further, take a look at the following short video introduction by Dr. Anandakrishnan...
And....a Word About Tsunamis
Pull-apart, slide-past, push-together obduction and push-together subduction plate boundaries plus hot-spots make earthquakes, volcanoes, and steep slopes that can landslide. If any of these happen underwater, great waves called tsunamis can be generated, with catastrophic consequences. Fortunately, warning systems can be devised to reduce the loss of life, and building with a little foresight can reduce property damage. We'll be looking into these as we wrap up our multi-week exploration of Plate Tectonics and Mountain Building.
- Differentiate between the three basic tectonic styles: pull-apart, push-together, and slide past
- Identify which plate tectonics created various mountain ridges
- Understand how various types of obduction zones work to create geologic formations
- Visually identify various types of rocks
What to do for Unit 4?
You will have one week to complete Unit 4. See the course calendar for specific due dates.
As you work your way through the online materials for Unit 4, you will encounter a video lecture, several vTrips, some animated diagrams (called GeoMations and GeoClips), additional reading assignments, a practice quiz, a "RockOn" quiz, and a "StudentsSpeak" Survey. The chart below provides an overview of the requirements for this unit.
|REQUIREMENTS||SUBMITTED FOR GRADING?|
|Read/view all of the Instructional Materials for Unit 4:||No, but you will be tested on the material found in the textbook.|
|Take the Unit 4 "RockOn" quiz||Yes, this is the fourth of 12 end-of-unit RockOn quizzes and is worth 4.5% of your total grade.|
|Continue working on Exercise #2: Geology is All Around You||Yes, this is the second of 6 Exercises and is worth 5% of your total grade.|
|Complete the "StudentsSpeak #5" survey||Yes, this is the fifth of 12 weekly surveys and is worth 1% of your total grade.|
If you have any questions, please feel free to email "All Teachers" and "All Teaching Assistants" through Canvas conversations.
On the following pages, you will find all of the information you need to successfully complete Unit 4, including the online textbook, a video lecture, several vTrips and animations, and two overview presentations.
Students who register for this Penn State course gain access to assignment and instructor feedback, and earn academic credit. Information about registering for this course is available from the Office of the University Registrar.