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A RCTIC CIRCULA NO. I Notes on a trip in l6-foot ... - The Arctic Circle

A RCTIC CIRCULA NO. I Notes on a trip in l6-foot ... - The Arctic Circle

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VGL. XV No" 2 THE A<str<strong>on</strong>g>RCTIC</str<strong>on</strong>g> <str<strong>on</strong>g>CIRCULA</str<strong>on</strong>g>IT z6<br />

<strong>The</strong> rather high ratio of Dorset to Thule artifacts <strong>in</strong> the collecti<strong>on</strong>e<br />

made by dt.A.nglure is general support for the dat<strong>in</strong>g of the<br />

petrogtyphs. <strong>The</strong> absence of Dorset tools <strong>in</strong> the small artifact eample<br />

fro<strong>in</strong> Cikertaaluk Island itself is likely forhritous. A high ratio of<br />

Dorset to Thule artifacts was also noted dur<strong>in</strong>g a survey that visited<br />

Sugluk, Ivugivik, and rv, ansel Island <strong>in</strong> L957, 1958, and 1959 (Taylort<br />

1958, 1959, 1960), <strong>The</strong> samples of Ungava artifacts that came to the<br />

Natioaal viugeurn between tJre wars show a similar ratio. This is not<br />

surpris<strong>in</strong>g s<strong>in</strong>ce Dorset culture Eskimoe occupied the Ungava coagt<br />

for a much l<strong>on</strong>ger tirne than their Thule culhrre successor6.<br />

<strong>The</strong> site s<br />

Tuperpvilajllak. This site, roughly 8 miles southeasterly frorn<br />

tbe \4 akeharn Bay settlernent, i; <strong>on</strong> the n::i-Land n"crth sh.ore of Joy<br />

Bay. Near tJre pregent surnrTrer camp stand some ? semi-subterranean<br />

house ru<strong>in</strong>s. DrAnglure saw no whaleb<strong>on</strong>e, did not recall eee<strong>in</strong>g eatranee<br />

passages to the houses, and guessed the elevati<strong>on</strong> of the site to be 20<br />

metres above present aea level. This suggests a Dorset eite; the artifact<br />

sample described below c<strong>on</strong>firms that suggesti<strong>on</strong> for all the specimens<br />

are llorset types, n<strong>on</strong>e are Thule, and <strong>on</strong>ly a few have parallels<br />

<strong>in</strong> pre-Dorset sites, A. rnuliiple sidenotched ground slate end blade<br />

provides a weak h<strong>in</strong>t of an early Dorset occupati<strong>on</strong>, but the low frequency<br />

of ground slate <strong>in</strong> this srnall sample does not support i:!ri.,s. <strong>The</strong> f<strong>in</strong>egra<strong>in</strong>ed<br />

black quartzite, the black cherty quartzite rnaterialr tJre triangular,<br />

stemmed, and sidenotched chipped end blade forms, and the two<br />

end scraper forms recall the Dorset sarnple from the Imaha siter about<br />

l25 miles to the southeast <strong>in</strong> Fayne Bay (Laughl<strong>in</strong> and Taylor' 1960).<br />

C,kiivik I, <strong>The</strong>re were four ma<strong>in</strong> sites <strong>on</strong> Ckiivik Island, just<br />

east of Tffifrkadlak. <strong>The</strong> positi<strong>on</strong>s of these sites given <strong>in</strong> the text<br />

below corne from a quick sketch prepared by drAnglure prior to his<br />

deparhrre for France. A comparis<strong>on</strong> of this sketch vrith tlre 1950<br />

editi<strong>on</strong> of the Topographical Surveyts eight mile to <strong>on</strong>e <strong>in</strong>ch sheet, Vr akeham<br />

Bay N.lv. 60 l7Z, suggests that drAnglurers directi<strong>on</strong>s are 90 degrees too<br />

far to the east. Okiivik IV may be <strong>on</strong> tJre nortJr side of Tuttle Po<strong>in</strong>t at the<br />

southeastern corner of the island with Ckiivik I at the west end of the

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