Answers to questions: The hidden half - seafloor spreading.

How do we peer into the watery depths? What are the types of data we can pull together to understand the geology of the oceanic basins?

Notice how dependent much of this is on technology. This is big project science.

Course materials for Plate Tectonics, GEOL 3700, University of Nebraska at Omaha. Instructor: H. D. Maher Jr., copyright. This material may be used for non-profit educational purposes with appropriate attribution of authorship. Otherwise please contact author.