A Synthesis of the Prehistory of the Central Little Colorado Valley, Arizona
George J. Gumerman, S. Alan Skinner
Abstract
George J. Gumerman, S. Alan Skinner
Abstract
Abstract Recent excavation by the Museum of Northern Arizona has provided a basis for a review of the prehistory of the poorly known region of the central Little Colorado basin of northeastern Arizona. A regional sequence of considerable complexity is established beginning with a Clovis-Folsom horizon and culminating in Pueblo IV (see Table 1). An amalgam of Anasazi and Mogollon traditions with a dominant Kayenta base is apparent as early as Basketmaker III. The introduction of Little Colorado White ware, beginning about A.D. 1075, signals the beginning of the Winslow branch, a distinguishable regional Anasazi variant, lasting until the abandonment of much of this desert region in the mid-13th century. The archaeological distinctiveness of the region is apparently due to its location between the Anasazi and Mogollon area and the necessary adaptations to the arid, basin environment.
OpenAlex reports 20 citations for this work. Citation counts describe recorded attention and do not establish research quality.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
Abstract Recent excavation by the Museum of Northern Arizona has provided a basis for a review of the prehistory of the poorly known region of the central Little Colorado basin of northeastern Arizona. A regional sequence of considerable complexity is established beginning with a Clovis-Folsom horizon and culminating in Pueblo IV (see Table 1). An amalgam of Anasazi and Mogollon traditions with a dominant Kayenta base is apparent as early as Basketmaker III. The introduction of Little Colorado White ware, beginning about A.D. 1075, signals the beginning of the Winslow branch, a distinguishable regional Anasazi variant, lasting until the abandonment of much of this desert region in the mid-13th century. The archaeological distinctiveness of the region is apparently due to its location between the Anasazi and Mogollon area and the necessary adaptations to the arid, basin environment.
Key concepts: Prehistory, Archaeology, Excavation, Geography, Structural basin, White (mutation), Arid, Geology