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Chapter I Intro & Objectives - SPREP

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PHOENIX ISLANDS PROTECTED AREA MANAGEMENT PLAN<br />

<strong>Chapter</strong> III. Background, 2. Human Activities<br />

Draft 1 March 2007<br />

Pearthree and Di Piazza (2003) examined archaeological items (fish hooks, basalt flakes,<br />

basalt cores, chisels, and abraders) from Manra and compared them with similar items from<br />

the Pacific. They concluded that the Manra items were similar to those found in eastern<br />

Polynesia. Charcoal samples from ancient fires were carbon dated to the 12 th and 13 th<br />

century A.D. These finding suggested a period of explosive migration in eastern Polynesia.<br />

Di Piazza and Pearthree (2004) noted that Orona and Manra were examples of Polynesian<br />

colonisation in the 13 th century. The reasons for abandonment were examined by Di Piazza<br />

and Pearthree (2004). They speculate that initially the population flourished with virgin<br />

resources. As local resources were depleted, resources were obtained from adjacent islands.<br />

Once these resources were depleted, coupled with the effects of drought, settlements had to<br />

be abandoned.<br />

MCKEAN<br />

In 1924, the Whitney South Sea Expedition found ancient stone structures on Orona (Hull),<br />

Abariringa (Canton) as well as Manra (Sydney), but none on other Phoenix Islands<br />

(MacGregor n.d.).<br />

Bryan (1934) reported that there was no sign of human occupation of McKean.<br />

On the western side of the island was the ruin of a large building with a coral slab wall 2.1 m<br />

(7 ft) high (Hydrographic Office 1940; Hydrographer of the Navy 1969).<br />

Bryan (1941 and 1942) reported that there was a trough-like depression on the north side of<br />

McKean. It was about 146 m (160 yards) long with steep sides. It appeared to have been dug<br />

and faced by human hands. No insights were provided regarding the origin of this walled<br />

depression.<br />

15

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