| Paleo Slide Set: Tree Rings: Ancient Chronicles of Environmental Change |
| Keet Seel Ruins, Navajo National Monument, Arizona | |
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The father of dendrochronology is widely acknowledged to be A.E. Douglass, who came to Arizona at the turn of the 20th century as an astronomer interested in sunspots and climate. A pioneer in
the study of the relationships between tree growth, climate, and solar cycles, he was also instrumental in developing dendrochronology as a method to date archaeological remains. By matching the ring patterns in wood from roof beams and around door and
window openings with the patterns in a dated tree-ring chronology derived from living trees, he and others were able to date many of the Anasazi ruins in the southwestern United States. The Anasazi ruin Keet Seel was built around AD 1250. The Anasazi
are believed to be the ancestors of the modern Pueblo Indians of northern Arizona and New Mexico. They inhabited parts of Colorado, Utah, Arizona, and New Mexico from about AD 900-1300. During this time, they built many cliff dwellings and
multi-storied towns in the canyon country of the southwestern U.S., of which Keet Seel is one example.
Photo Credits: Peter Brown Rocky Mountain Tree-Ring Research, Ft. Collins, CO |
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