Spring 2025 Teaching
16:460:506:01: Structure and Formation of Terrestrial Planets
The solid Earth has an internal structure that consists of well-organized lithological and chemical parts that have been identified by geochemical, seismological, and petrological observations. Many of the chemical and physical characteristics of the Earth’s interior are also expected to exist within other terrestrial planets. This course will review the current understanding of planetary formation, planetary compositions, processes shaping planetary interiors and observations reflecting their structure, and hypotheses of planetary evolution in the Solar System. This course is open to undergraduate students and graduate students. If you have not completed the course prerequisites, please contact me and Professor Bermingham.