In this graph, the y-axis refers to the radiocarbon ages of midden macrofossils at Chaco Canyon. The bars represent the number of middens from a given 250-year age range that either do or do not
contain evidence of piņon pine at the study site. The arrival of piņon pine from its glacial refugium in central New Mexico is clearly visible after 9000 14C yr. BP. Piņon is found in all of the middens dated between 9,000 and 1,000 14C yr. BP, at
which point piņon again drops out of the midden record. It is probably not a coincidence that piņon, used intensively as a fuelwood by the Anasazi, dropped out of the paleoecological record during the height of Anasazi activity in the Chaco Canyon
Although climatic change could partially explain the abandonment of Chaco Canyon by the Anasazi about 800 years ago, the resident population probably exceeded local carrying capacity even in times of optimal weather. An extensive road
network connected Chaco with procurement areas of outlying communities, but resources close at hand were fully exploited, (Betancourt and Van Devender ). These findings have led researchers to speculate that, depletion of fuelwood and other local
resources probably intensified the reliance on commodity imports from peripheral communities, (Betancourt and Van Devender ).
Indeed, by 1030 A.D., the people of Chaco were forced to rely on logging expeditions to distant mountain ranges,
sometimes 100 km from home but more typically 30-40 km away, to gather spruce and Douglas fir to use as architectural timbers and fuelwood. In the next century, perhaps seeking refuge from the political and economic instability that resource depletion
engendered, the people of Pueblo Bonito abandoned the canyon entirely, moving out to the northern Rio Grande and elsewhere, where their descendants live on in several of the Pueblo and Hopi Indian villages of New Mexico and Arizona.
U. S. Geological Survey
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