How Old Is It? The Story of Dating in ArcheaologySchoenwetter, James
Science
How Old Is It? The Story of Dating in Archeaology
Schoenwetter, James
Archaeological dating; Dendrochronology; Radiocarbon dating
The absolute clock utilized most widely in archaeology is the historical
record. Men have used calendars for a long time, and have often left
records with written dates. On tombstones at a site in old Virginia, on
the pedestals of statues and other monuments from classical Greece and
Rome, on the walls of the tombs of Egyptian kings, dates are clearly
inscribed which can be related to the sites dug into by the
archaeologists. These dates must often be recalculated in terms of the
Christian calendar which we use. Most calendars in use in the
Mediterranean, the Near East and China during classical antiquity have
been successfully correlated with the one we use today, and a date
inscribed or noted on such sites can be considered in our own terms.
Other calendars, such as those developed in the ancient cultures of the
Maya on the Yucatan Peninsula, have yet to be accurately correlated with
our own. Such calendars can be used on their own terms of course, and a
site which has an inscription in the Mayan calendar is known to be so
many years older or younger than another one with a different date in
that calendar. We speak of such a situation as a _floating chronology_.
That is, the sequence of events and the number of years which separate
them are known, but the dates of those events in absolute time are
unknown.
[Illustration: (uncaptioned)]
Tree rings afford another kind of absolute clock, the _dendrological_
method. Each year a tree adds a growth ring. Depending on the amount of
water the tree has available to it for cell growth, the ring will be
wider or narrower. Certain trees whose water requirements are high live
near streams or other places where their roots can tap a constant supply
of water. Such trees, referred to as _complacent_, have annual rings
which are all of about the same width. Other _sensitive_ trees live in
places where they must depend almost wholly on rainfall for their water
supply, as on the slopes of hills or in the clefts of rocks. Such trees
have annual rings which vary in width depending upon the amount of rain
they receive. In any given area, especially in arid and semiarid
regions, some years have more rainfall than others. The sensitive trees
will produce wider rings during years when there is more rainfall and
narrower rings in years when there is less. Often there are periods of a
decade or so when all of the sensitive trees will produce the same
pattern of ring growth; for example, three years of narrow rings, one
year of wide, two more of narrow and three more of wide. Such a pattern
is called a _signature_.
Public-domain text, read in full here on John Shaqi.
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