This document discusses key concepts in geology including the difference between a timeline and timescale, relative and absolute dating, fossils, index fossils, rock layers, and unconformities. It explains that timelines show events in order while timescales assign numerical ages. Relative dating compares rock layers while absolute dating assigns numerical ages. Most fossils are preserved in sedimentary rock. Index fossils found in specific rock layers worldwide can help correlate rock sequences. The oldest rock layers are on the bottom according to the law of superposition, though layers can be disturbed by folding, faulting, or volcanic intrusions creating unconformities.