Earth history, as a scientific topic, encompasses the reconstruction and analysis of the planet’s physical, chemical, and biological evolution from its formation ~4.54 billion years ago to the present. It integrates evidence from stratigraphy, geochronology, paleontology, geochemistry, and tectonics to delineate major intervals (eons, eras, periods, epochs) and events, such as crust formation, supercontinent cycles, ocean–atmosphere evolution, biotic radiations, and mass extinctions. Research in earth history focuses on quantifying rates and magnitudes of processes (e.g., plate motions, climate shifts, biogeochemical cycles) and constraining cause–effect relationships that link Earth’s interior, surface environments, and biosphere through deep time.