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