The history of archaeological research in the Flagstaff area since 1851 is reviewed. The thesis of this study is that critical analysis of archaeological history can yield significant insights into both the process and the products of archaeological research. These insights in turn may lead to conclusions about the general nature of intellectual disputes and transitions in archaeology, and the validity of particular reconstructions and explanations of prehistoric behavior. The history of archaeological research in the Flagstaff area is broken into nine major divisions, each of which is separated by a significant intellectual or institutional transition. Particular attention is devoted to historical analysis of the period immediately before World War II, when the fundamental concepts and methods of Flagstaff archaeology were developed by Harold Colton and his associates at the Museum of Northern Arizona (MNA). These developments took place during a remarkably prolific period of archaeological investigation designed to disclose a prehistoric sequence of occupation conceived by MNA workers as "one grand history" of the Hopi people. It is argued, on the basis of the historical review, that Flagstaff archaeology, in its specific examples, indeed reveals much about the nature of intellectual disputes and transitions in American archaeology, and demonstrates that knowledge of the prehistoric past can indeed be cumulative. The study concludes with specific recommendations for improving such knowledge in the Flagstaff area, particularly for the issues of chronology and ceramic taxonomy.

Using cluster analysis, a total of 605 vents in San Francisco Volcanic Field are studied over an area of approximately 5000km2. Application of alignment analysis techniques, including the two-point azimuth analysis and Hough transform analysis, demonstrates that cinder cones are aligned along common orientations within larger clusters. These alignments consist of 9-10 cinder cones, are 20-38 km long, and are regional features. The vent alignments indicate the presence of geological features along which magma ascended more readily than elsewhere. The NE-trending Mesa Butte and Oak Creek Canyon-Doney fault systems seem to control the intermediate to silicic centers which are on the intersection of these fault systems with Cataract Creek fault system and affect the development of cinder cone alignments. Geological maps and geophysical surveys indicate that most vent alignments are parallel or subparallel to these large scale fault systems. This suggests that vent alignment patterns are controlled by regional structures.