GEO382

This course explores deformation of the earth from the micro- to regional scale. We will examine concepts of stress and strain to investigate the formation of geologic structures, such as faults, folds, and fabrics. We will use geometric analysis of structures, geologic maps, cross-sections, and geologic field data to interpret the deformational history of a region within a plate tectonic context. This course will address questions such as "why do some rocks fold and others fracture?", "What controls the location and scale of faults?", and "How do mountain belts form?" This course must be taken concurrently with GEO-383. Prerequisite: GEO-110 or ENV/GEO-120 and one additional Geology course, or permission of the instructor. Fall semester.

Even Years