Geology is the study of Earth's rocks and materials. Nicholas Steno developed ideas in the 1600s about how rocks and fossils form using the analogy of shark teeth resembling stones found in rocks. These ideas formed the basis for relative dating techniques. Relative dating determines the order events occurred in by applying principles like superposition, original horizontality, lateral continuity, cross-cutting relationships, inclusions, and faunal succession to analyze rock layers and fossils. Earth's age was originally calculated to be between 10-100 million years but is now estimated at 4.6 billion years based on radioactive dating techniques.