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'the Archaic and early Ute, or that they were occupied on an episodic basis by specialized task groups, such as might be expected from the rr^ormative (Fremont and Anasazi) Cultures, who transported procured resources to a residential bases located elsewhere. ?iowever, it is known that groups from both the aforementioned r^^ormative Cultures practiced a broad based foraging strategy implying a pattern of transhumance may not be distinguishable between them and the Archaic/Ute. The sites were found mainly in the pinyon/juniper vegetated areas along the mesa edges and similarly vegetated drainage bottoms on the mesa top. The term "site", if defined as a "discrete activity area", may not properly be used for those large, usually sparse, distributions of cultural materials because of the complicated overlapping of the detritus of (possibly) several cultural groups, and the natural depositional and post-depositional processes. The cultural materials of at least SMN3760 and SMN3761 were probably continuous, but are subdivided because of disturbance by historical occupants and for topographic reasons. It is apparent that concentrations within the two site may represent discrete activity areas from diverse cultural/temporal periods. Testing is required to interpret the finds. • It is clear from the mapping currently completed that specialized activity areas can be identified. The information drawn from this site-based perspective may allow archaeologists to differentiate the nature of the activities that took place at residential campsites verses limited activity sites and to make inferences about the settlement/subsistence patterns of the Archaic, Formative and early Utes in this region. By defining a set of characteristics that identify these cultural phenomenon, archaeologists will be able to recognize it in diverse environmental or site-based contexts although some elements may be absent. Most of the sites apparently have little or no depth of cultural fill due to their location on rocky ground surfaces that are characterized as having low, water permeability and rapid runoff. In most cases, mapping, photographing, and surface collecting of the diagnostics will preserve the essential data from the sites. Testing of the hearth features will provide some additional information, but most are surficial and will not yield carbon samples. Localities within a few of the sites have potential for depth of cultural fill and selective testing of those areas should be conducted. If significant depth of cultural fill is encountered, the • sites should be subject to additional excavation within the 19