Textbook
Syllabus
| Geological Sciences 146. Plate Tectonics | |||
| The theory of
Plate Tectonics states that the Earth's outermost layer is fragmented into
a dozen or more large and small plates that are moving relative to one
another as they ride atop hotter, more mobile material. The theory developed
from the hypothesis that continents on opposite sides of the Atlantic Ocean
had drifted apart (‘Continental drifting’). Fossil Earth’s magnetic field
in rocks, volcanoes and earthquakes provide the evidence. Development of
the theory allows to better understanding mountain building, distribution
of fossil remains, the origin of features on the ocean floor, and much
more. The course involves three hours of weekly meeting time and selected
reading material. No background in Earth Science is necessary. Evaluation
is based on class participation, three exams, a series of student presentations
on selected topics and written essays on the same subject.
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| Lectures: T, Th 1-2:30 pm, 3540 CCL | |||
| Jmpares@umich.edu | |||
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