Scientists study the Earth's history by examining rocks and dating them. The geological time scale divides Earth's lifetime into eras based on layers of rock and fossils. Relative dating involves placing rocks in proper sequence, while radiometric dating uses radioactive decay to determine ages. The oldest fossils date to around 3.8 billion years ago. Major periods include the Paleozoic, Mesozoic, and Cenozoic eras. Mass extinctions occurred, like at the end of the Permian, possibly due to asteroid impact. Humans have significantly impacted geology through pollution, deforestation, and species extinction.