Princeton University

The benefits of including research experiences in the pedagogy of graduate and undergraduate education are diverse and lasting. Therefore, I treat all of my classes, even freshman seminar and core undergraduate geology courses, as research endeavors. I divide my courses into four overlapping skill sets that I hope to impart to students through experiential learning. First, students develop the ability to make keen observations of the natural world, and to translate observational data into salient questions about how Earth works. Second, students learn to distill these questions into a manageable group of hypotheses that can be tested with additional observations or analysis.  Third, students apply quantitative computational methods to extract more information from their data. And fourth, students learn to communicate their discoveries with publication quality text and illustrations.

EARTH'S ENVIRONMENTS AND ANCIENT CIVILIZATIONS
Professors: Adam C. Maloof and Frederik J. Simons
In this Freshman Seminar, you will combine eld observations of the natural world with mathematics,
physics, chemistry and computer science in order to answer questions like: Why are mountains
high? Why are some landscapes wetter, drier, smoother, or more jagged than others? How does
environmental change alter the course of civilization, and how do civilizations modify their environment?
In the classroom, through problem sets, and on campus excursions, you will gain practical
experience collecting geological and geophysical data in geographic context, and analyzing these.

EARTH'S CHANGING SURFACE AND CLIMATE [ST]
Professors: Adam C. Maloof and Frederik J. Simons
The surface of Earth today, an amalgamation of mountain ranges, basins, and the hydrosphere, records an integrated history of processes that act on a range of time scales spanning 17 orders of magnitude. The central question treated in this Freshman Seminar is: How does Earth's surface evolve in response to internal (e.g., tectonic and magmatic), surficial (e.g., weather, climate, and anthropogenic effects) and external (e.g., extraterrestrial) forcing? The seminar provides students with practical experience making geological and geophysical observations, and in particular, focuses on quantitative analysis of observables such as topography, gravity and weather. The classroom seminar is complimented by a mandatory week-long field trip to the Western United States. During this trip, students will develop research projects that involve geological and geophysical mapping of the interplay between recent volcanic explosion craters, changing climate, and anthropogenic demands on water resources in the Mono Lake region. All costs of the fall break trip are covered by the University. [student course evaluations]

SEDIMENTOLOGY
Professor: Adam C. Maloof
This course presents a treatment of the physical processes that shape Earth's surface, such as solar radiation, deformation of the solid Earth, and the flow of water (vapor, liquid, and solid) under the influence of gravity. In particular, the generation, transport, and preservation of sediment are studied as diagnostic tools to link processes with the geologic records of Earth history and modern environmental change [Taught: SPRING 2012, T Th 1:30-2:50 pm, Guyot Hall 155]. [student course evaluations]

STRUCTURAL GEOLOGY
Professors: Adam C. Maloof and B. Schoene
An introduction to the physics and geometry of brittle and ductile deformation in Earth’s crust. We consider deformation at scales from atomic to continental, in the context of mountain building, rifting, and the origin of topography. Weekend Field Trips: Kentucky, Pennsylvania, New Jersey, New York. [student course evaluations]

TOPICS IN EARTH HISTORY
Professor: Adam C. Maloof
This seminar examines the history of global change on Earth. Topics include the relationship between paleogeography, sea level and climate, the character and geometry of Earth's ancient magnetic field, the evolution of Earth's spin vector, the interpretation of global sea level variability, the deconvolution of periodic and stochastic forcing in sedimentary records, and the large-scale events and processes that affected global change and the evolution of life.