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

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

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In 1823 Ellis described five dryland agricul tural field<br />

systems on Hawai'i where sweet pot<strong>at</strong>o was the primary cultigen<br />

(Newman 1970: 114-115). These were loc<strong>at</strong>ed in leeward North<br />

Kohala, in Kona between Kailua and Ka'awaloa, <strong>at</strong> Wai'ohinu and<br />

Kapapala in Ka'u, and near Kamaili in Puna. Two <strong>of</strong> these areas<br />

have been investig<strong>at</strong>ed archaeologically: the North Kohala system<br />

<strong>at</strong> Lapakahi (Newman 1970; Rosendahl 1972; Tuggle & Griffin 1973)<br />

and the Kona system <strong>at</strong> Kealakekua (Soehren & Newman 1968; Newman<br />

1970: 123-137). Research in Makaha Valley, O'ahu (Green, in<br />

press) and Halawa Valley, Moloka'i (Kirch 1975) provide addi-<br />

tional d<strong>at</strong>a on dryland cultiv<strong>at</strong>ion in prehistoric Hawai'i.<br />

The earliest indirect evidence in Hawai' i for sweet pot<strong>at</strong>o<br />

cultiv<strong>at</strong>ion is from Makaha Valley. Field shelters d<strong>at</strong>ed <strong>at</strong> 1100<br />

to 1300 A.D. were found in str<strong>at</strong>igraphic associ<strong>at</strong>ion with evi-<br />

dence for swiddening (slash and burn agriculture) (Green 1970:<br />

101). It is assumed th<strong>at</strong> these fields were used for either sweet<br />

pot<strong>at</strong>o or dry taro cultiv<strong>at</strong>ion. This initial swidden agriculture<br />

was followed by more permanent inland pondfield systems with<br />

associ<strong>at</strong>ed dryland farming (Green, in press). In Halawa Valley,<br />

geological and malacological evidence suggest a sequence <strong>of</strong><br />

forest burning resulting in slope instability and erosion by<br />

1200 A.D. Based on this d<strong>at</strong>a, in conjunction with the cultural<br />

remains, Kirch (1975: 175-176) suggests th<strong>at</strong> swiddening was prob-<br />

ably a major agricultural activity in the valley from the d<strong>at</strong>e <strong>of</strong><br />

initial settlement (ca. 650 A.D.) onward. It was concluded th<strong>at</strong><br />

a quantit<strong>at</strong>ive shift in rel<strong>at</strong>ive emphasis from swidden to pond-<br />

field cultiv<strong>at</strong>ion gradually took place. The extensive field<br />

system <strong>at</strong> Lapakahi d<strong>at</strong>es from the l<strong>at</strong>e 1400's to historic con-<br />

tact. It is in this area th<strong>at</strong> the first direct evidence <strong>of</strong> sweet<br />

pot<strong>at</strong>o was found. Carbonized sweet pot<strong>at</strong>o tuber fragments were<br />

excav<strong>at</strong>ed from a field shelter in upland Lapakahi with associ<strong>at</strong>ed<br />

d<strong>at</strong>es ranging from 1425 to 1725 A.D. (Rosendahl & Yen 1971;<br />

Rosendahl 1972). Less directly, some coastal Lapakahi sites d<strong>at</strong>e<br />

to about 1300 A.D. (Tuggle & Griffin 1973: 58) and - may indic<strong>at</strong>e<br />

the initial stages <strong>of</strong> sweet pot<strong>at</strong>o cultiv<strong>at</strong>ion. Sweet pot<strong>at</strong>o<br />

tuber skin has also been tent<strong>at</strong>ively identified from one <strong>of</strong> the<br />

Mauna Kea Adze Quarry rockshelters (B.P. Bishop Museum, current<br />

analysis). Only one radiocarbon d<strong>at</strong>e has been obtained for the<br />

rockshelter, 1492 A.D. (corrected), and the identified m<strong>at</strong>erial<br />

is from a layer th<strong>at</strong> is str<strong>at</strong>igraphically more recent, but<br />

definitely prehistoric.<br />

Recent research has led some archaeologists to hypothesize a<br />

prehistoric expansion <strong>of</strong> permanent settlement into the dry lee-<br />

ward areas <strong>of</strong> Hawai'i beginning as early as 1000 to 1100 A.D.<br />

(Cordy <strong>1978</strong>). It is suggested th<strong>at</strong> this settlement was accom-<br />

panied by inland agricultural expansion and substantial popula-<br />

tion increase, as exhibited by the extensive remains <strong>of</strong> dryland<br />

field systems and numerous coastal habit<strong>at</strong>ion sites. There were<br />

also certain social developments th<strong>at</strong> took place which resulted<br />

in the form<strong>at</strong>ion <strong>of</strong> complex ranked societies during the l<strong>at</strong>e<br />

1400's (Hommon 1976). This is in part documented by the appear-<br />

ance <strong>of</strong> large house sites and heiau (temples) which represent<br />

social str<strong>at</strong>ific<strong>at</strong>ion. The areas affected are notably those in<br />

which the sweet pot<strong>at</strong>o would be the most productive crop. It is

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