These two sites share the characteristics of being located on lateral moraines that parallel the east-west direction of the Molinos drainage. Lithic scatters associated with large blocks of tuff that serve as small rock shelters are the principal features of these sites. A broken (longitudinally snapped) Middle Archaic 3e projectile point [A03-539.25] was found in one of these moraine sites; interestingly this point was made of andesite and was the only non-obsidian artifact found in this cluster of sites. A Late Archaic 3f obsidian point was also found in this area. Corral features and ceramics were identified here as well, indicating that the sites are multicomponent.
Figure 6-10. Lithic scatters are associated with shelter provided by large boulders located along moraines [A03-539]. One surveyor that is visible in blue provides scale.
The occupation of these sites was likely related to the use of resources in the upper Quebrada de los Molinos valley, although the moraines are not an obvious place for site locations. The sloping moraines are far from level and there is little open space between boulder, however the sites are probably located on these moraines due to factors that include insolation on these north-west trending moraines, the availability of water descending from Maymeja and the flanks of Hornillo, and the shelter offered by the large boulders.