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Dendrochronology

Published online by Cambridge University Press:  26 May 2015

Extract

During the first years of this century an astronomer, Dr A. E. Douglass, started a series of examinations of the annual increment in trees just south of Flagstaff, Arizona, to see if the cyclical nature of sun-spot appearances was reflected in tree growth, through their influence on climate. He found that there was a rather high correlation between tree growth and sun-spots in the living trees he examined. In order to extend his studies into the past—beyond the 500 years recorded by living trees—he collected material taken from beams in the old Spanish Missions that dot the southwestern United States. He had found that it was possible to identify certain characteristic sequences of tree-ring widths with certain years, and thus project into the past his chart of tree growth from timbers cut at an unknown past date. In doing so he discovered a technique that has founded a new branch of science—dendrochronology.

Type
Research Article
Copyright
Copyright © Antiquity Publications Ltd 1937

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References

A Selected Bibliography

Brown, F.M.America’s Yesterday, J.B. Lippincott Company, 1937. Appendix I contains the only available compilation of all the important dates derived by dendrochronologists, to December 1936.Google Scholar
Douglass, A.E..–The Secret of the Southwest solved by Talkative Tree-Rings, National Geographic Magazine, 1929, LVI, 745–50.Google Scholar
Douglass, A.E..–Dating Pueblo Bonito and other Ruins of the Southwest, Pueblo Bonito Series no. I, 1935, National Geographic Society, Washington, D.C. Google Scholar
Hawley, F.M..–The significance of dated prehistory of Chetro Ketl, Chaco Canyon, New Mexico, University of New Mexico Bulletin, Monograph Series, vol. I, no. I, 1936, Albuquerque, New Mexico.Google Scholar
Macgregor, J..–Dating the Eruption of Sunset Crater, Arizona, American Antiquity, 1936, vol. II, 1526.Google Scholar
The Tree Ring Bulletin, 1934 to date, Flagstaff, Arizona. A small journal devoted solely to the study of dendrochronology.Google Scholar