Archaeometry
Radiocarbon Dating
Radiocarbon dating allows archeologists to date materials, formed between 300 and 40-50,000 years ago, that contain organic carbon. Carbon 14 is a naturally occurring radioisotope of ordinary carbon (carbon-12) that is created in the upper atmosphere when carbon-12 is bombarded by cosmic rays. On Earth, living organisms metabolize carbon 14 in the same percentage that it exists in the atmosphere. Once the plant or animal dies, however, the carbon-14 atoms began to decay at a known rate. Consequently, the age of a carbon-containing specimen such as charcoal, wood, shells, bone, antlers, peat, and sediments with organic matter, can be determined. One of the first applications of this technique was to assign a date to the beginning of the postglacial period of about 10,000 years ago.
Resources
Books
Daniel, Glyn, ed. The Illustrated Encyclopedia of Archeology. New York: Thomas Y. Crowell: 1977.
Fagan, Brian M., ed. The Oxford Companion to Archeology. New York: Oxford University Press, 1996.
Maloney, Norah. The Young Oxford Book of Archeology. New York: Oxford University Press, 1997.
Sullivan, George. Discover Archeology: An Introduction to the Tools and Techniques of Archeological Fieldwork. Garden City, NY: Doubleday & Company, 1980.
Periodicals
Fowler, M.J. "Satellite Remote Sensing and Archaeology." Archaeology Prospection 9, no. 2 (2002): 55-70.
Randall Frost
Additional topics
Science EncyclopediaScience & Philosophy: Anticolonialism in Southeast Asia - Categories And Features Of Anticolonialism to Ascorbic acidArchaeometry - Archaeomagnetic And Paleomagnetic Dating, Dendrochronology, Fission-track Dating, Lithics, Luminescence Dating, Metals Analysis