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Sugg. 25-02
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leucocephala), scattered Lantana (Lantana camara)bushes, other introduced shrubs and various <br /> desiccated grasses. This groundcover has been kept under control by the cattle that presently <br /> graze the area, and the understory is relatively open,limiting the need for clearance during the <br /> survey and greatly assisted the recording of sites. <br /> The present inventory survey identified a total of 62 archaeological sites located throughout the <br /> survey property. Each site was assigned a temporary field number (e.g. T-001) for easy <br /> identification. Once all of the information collected during the survey has been compiled and <br /> reviewed, a list of sites and their descriptions will be submitted to the Hawaii State Historic <br /> Preservation Division(SHPD) which will assign them more permanent State Inventory of <br /> Historic Places (SIHP) site numbers. During the course of fieldwork,the location of each site <br /> was mapped using a hand held global positioning system(GPS). The resulting map of site <br /> distribution is shown in Figure 3. Each site was then documented and photographed. Several <br /> of the more significant sites were mapped in detail. <br /> The weathered pahoehoe lave flow that forms the southern portion of the project area was found <br /> to be extensively modified by the construction of modified outcrops, stone mounds,rough stone <br /> edged and soil filled terraces, and other minor features. Most of the modified outcrops and <br /> mounds may have served as clearance piles. Loose stones,collected off the ground surface, <br /> appear to have been piled atop exposed areas of lava outcrop to clear the surrounding soil. <br /> These open soil areas would then have been used for the planting of crops. The various <br /> mounds and modified outcrops found within this southern area may also have been used as <br /> planting features. Vine crops such as `uala (sweet potato,Ipomoea batatas) and Uhl (yam, <br /> Dioscorea spp.) may have been grown within them. Occasionally,rough alignments of stones <br /> have been placed along the down slope edge of soil pockets creating small soil terraces. These <br /> alignments probably served as retaining walls to better catch and hold the soil. Another <br /> characteristic of this area is the presence of concentrations of battering marks which are present <br /> on some patches of exposed bedrock. These areas of concentrated battering likely represent <br /> locations at which some processing activity,possibly related to agriculture,took place. What <br /> that activity may have been is uncertain. <br /> Modified outcrops,mounds, soil terraces and other apparently agricultural features are spread <br /> throughout the full extent of the pahoehoe lave flow within the boundaries of the project area, <br /> though they are less abundant toward the south where the soil is thinner. Given the density of <br /> these features and the lack of any recognizable divisions within this dryland field system,the <br /> entire complex was assigned a single field number (T-040). During the 2001 archaeological <br /> inventory survey for the adjacent Mamalahoa Bypass Road (Robbins et al. 2001), similar <br /> agricultural features resting within the ahupua`a of Kuamo`o were assigned State Inventory of <br /> Historic Places site number 21244. Features resting within the ahupua`a of Ma`ihi 2 were <br /> assigned site number 21243. Only a small portion of the agricultural features present within the <br /> current 59.40 acre study area extend into Ma`ihi 2. For this reason, and so as not to arbitrarily <br /> divide what is obviously a single continuous archaeological landscape,the entire modified <br /> pahoehoe lave flow will be assigned SIHP site number 21244. <br /> The open soil area that forms the northern portion of the survey area,though not so extensively <br /> modified as the southern portion,was most probably also used for crop cultivation. The soil <br /> here is relatively free of bedrock outcropping and the extensive clearance of surface stone so <br /> evident at Site 21244 would not have been necessary. <br /> Page 3 <br />
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