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LAVA FLOW TRAIL STOP 11

Dating the eruption


Ponderosa pines growing on the slopes of a cinder cone .

How can we find out when Sunset Crater erupted? One way is to ask a tree. Each year, a living tree adds a new layer of wood in a ring around the trunk. The better the growing conditions, the wider the ring. In times of drought, climate change, or disturbance - fire, flood, or a volcanic eruption - little tree growth takes place, and rings are very narrow.

 

We can count the number of tree rings to learn the age of a tree. And we can compare patterns of wide and narrow rings in different trees and stumps to learn the actual dates they grew. This process is called dendrochronology.

To find trees that grew at the time of the Sunset Crater eruption, scientists looked at Wupatki, about 20 miles away. Wupatki Pueblo was a thriving community after the eruption. Roof beams used in some of its rooms revealed several narrow, dark rings, indicating a period of stunted growth in the years 1064 and 1065. Perhaps there was a severe drought or other disturbance during these years, or those narrow rings may indicate volcanic activity at Sunset Crater.

As new dating technologies become available, we may learn more about the timing of this eruption and others in the vicinity.

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This site is a cooperative endeavor of the
US Geological Survey Western Earth Surface Processes Team
and the National Park Service.

This page was last updated on 8/16/2006.