CHACO CANYON’S ANOMALOUS GEOMORPHIC AND CULTURAL HISTORIES—POSSIBLE CONNECTIONS
Chaco Canyons geomorphic development is anomalous in its region, and was governed by base levels at the junction of Chaco and Escavada Washes, apparently by a transitory eolian (+masonry?) dam. So how were Chacos unique culture and anomalous geomorphology related? The relation precedes the Bonito channel, for the Chacoan culture was already unique by the mid-AD 800s, when multi-story greathouses first appeared. The Chaco unit of Hall, now thought to represent about AD 1-920?, and into which the Bonito channel is cut, has the answers.
The Chaco unit forms much of the valley floor, which is perched above Escavada Wash behind the eolian dune at the junction. Floodplain deposits predominate except at the downvalley end, where a delta grew over playa-lake deposits. Multiple thick (but poor) soils are present on the unit. Thus the pioneers choice of Chaco Canyon was a choice of some combination of an aggrading system that permitted ak chin farming at all side-tributary junctions, the main-valley part of the system where floodplain farming could be conducted in large areas, and/or something useful about the playa-lake itself.
Force, E. R., Vivian, R. G., Windes, T.C., and Dean, J. S., 2002, Relation of "Bonito" paleochannels and base-level variations to Anasazi occupation, Chaco Canyon, New Mexico: Arizona State Museum Arch. Series 194, 49 p.