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June 1 - 3 , 1978 - University of Hawaii at Manoa

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Presence-absence trait analysis further defined these<br />

classes in functional terms. Because <strong>of</strong> their small size, shape,<br />

and virtual absence <strong>of</strong> other distinctive <strong>at</strong>tributes, Class I<br />

structures are inferred to be for the storage <strong>of</strong> tools and<br />

m<strong>at</strong>erials, or possibly for such produce as yams and sweet<br />

pot<strong>at</strong>oes. Class I1 fe<strong>at</strong>ures are the ordinary dwellings <strong>of</strong> indi-<br />

vidual households. Class 111 enclosures also appear to be ordi-<br />

nary dwellings. Although these enclosures are r<strong>at</strong>her large when<br />

compared to other habit<strong>at</strong>iqn fe<strong>at</strong>ures in the study area, none<br />

approach the usual size range or structural complexity to<br />

indic<strong>at</strong>e more specialized fe<strong>at</strong>ures, such as men's hoyses.<br />

A fourth class <strong>of</strong> habit<strong>at</strong>ion fe<strong>at</strong>ure is defined from the<br />

trait analysis. These are distinguished by the presence <strong>of</strong> sc<strong>at</strong>-<br />

tered midden and large mounds <strong>of</strong> burned coral associ<strong>at</strong>ed with<br />

open, elev<strong>at</strong>ed floors. Class IV fe<strong>at</strong>ures are therefore inferred<br />

to bs cooking areas using surface imu, or ovens, although oven<br />

pits may be found under the raised floors.<br />

Extensive disturbances in the study area hive left few prob-<br />

able clusters intact. Of the remaining examples, one cluster<br />

especially, includes seven Class I storage fe<strong>at</strong>ures, six Class I1<br />

dwellings, and five Class IV cooking fe<strong>at</strong>ures in two separ<strong>at</strong>e<br />

areas within the cluster (Fig. 3). The habit<strong>at</strong>ion fe<strong>at</strong>ures are<br />

associ<strong>at</strong>ed with structurally modified sinkholes and clearings <strong>of</strong><br />

soil-humus deposits--both inferred to be garden areas, and with<br />

other unmodified sinkholes used as refuse dumps. The entire<br />

cluster is situ<strong>at</strong>ed on a slight rise <strong>of</strong> limestone outcropping<br />

immedi<strong>at</strong>ely adjacent to an area <strong>of</strong> surface drainage. Despite<br />

considerable evidence for surface run<strong>of</strong>f, the rel<strong>at</strong>ively minor<br />

difference in elev<strong>at</strong>ion does not seem sufficient to explain this<br />

loc<strong>at</strong>ion as a direct response to flooding alone. Wh<strong>at</strong> is <strong>of</strong><br />

interest is th<strong>at</strong> shallow, but numerous pockets <strong>of</strong> silt are found<br />

in these drainages. The proximity <strong>of</strong> the habit<strong>at</strong>ion area to the<br />

accumul<strong>at</strong>ed sediments suggests th<strong>at</strong> the drainages were also uti-<br />

lized. This may have been for additional gardening, or perhaps<br />

as a source <strong>of</strong> alluvial m<strong>at</strong>erials for use in mulched garden pits<br />

(sinkholes) .<br />

The one fe<strong>at</strong>ure conspicuously missing from this cluster is<br />

the Class 111 enclosure. Although a Class 11 or several Class I<br />

fe<strong>at</strong>ures may be loc<strong>at</strong>ed nearby, the larger enclosures are in fact<br />

quite dispersed throughout the study area without any apparent<br />

p<strong>at</strong>tern to their loc<strong>at</strong>ion. It is possible th<strong>at</strong> these enclosures<br />

are the residences for individual households, and th<strong>at</strong> the<br />

"clusters" may have functioned as communal foci for a larger<br />

settlement group. If so, then the whole n<strong>at</strong>ure <strong>of</strong> the residence<br />

group in terms <strong>of</strong> sp<strong>at</strong>ial distribution may require rethinking.<br />

Altern<strong>at</strong>ively, the Class I11 enclosures may not be contem-<br />

poraneous with the fe<strong>at</strong>ure clusters, and their distribution may<br />

reflect changes occurring in the settlement <strong>of</strong> the area. Trait<br />

analysis suggests th<strong>at</strong> Class I11 fe<strong>at</strong>ures are either very l<strong>at</strong>e<br />

prehistoric, or wholly historic phenomena. Although precontact<br />

d<strong>at</strong>es <strong>of</strong> A.D. 1666k41 and 1743+41 were obtained from one such<br />

enclosure tested by the Bishop Museum (Sinoto 1976: 87), the

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