Dendrochronology
Dendrochronology is the scientific method of dating past events and environmental changes by analyzing the patterns of tree growth rings. Since trees typically produce one ring per year whose width and characteristics reflect the climatic and environmental conditions during that growing season, these rings form a distinct chronological record. By cross-dating the unique ring patterns among numerous trees, including ancient wood from archaeological sites or geological deposits, researchers can construct continuous timelines stretching back thousands of years, providing invaluable data for forestry management, climate change studies, and dating historical events.
- Introduction to Dendrochronology
- Definition and Scope
- Historical Development
- Fundamental Scientific Principles