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Crossing the Borders: New Methods and Techniques in the Study of Archaeological Materials from the Caribbean

by Corrine L. Hoffman, et. al.

by Corrine L. Hoffman, et. al.

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Table 4.1. Description <strong>of</strong> Chert <strong>and</strong> Fl<strong>in</strong>t Sources <strong>in</strong> <strong>the</strong> Nor<strong>the</strong>astern Antilles, Included <strong>in</strong> This <strong>Study</strong>.<br />

Isl<strong>and</strong> Source locality<br />

Geological<br />

sett<strong>in</strong>g<br />

Type <strong>of</strong><br />

(orig<strong>in</strong>al)<br />

host-rock<br />

Type <strong>of</strong><br />

occurrence Description<br />

Antigua Long Isl<strong>and</strong> (LI) Antigua Formation Limestone primary,<br />

secondary,<br />

tertiary<br />

Major ®<strong>in</strong>t occurrence on small isl<strong>and</strong> <strong>of</strong>f<br />

Antigua’s nor<strong>the</strong>rn coast. Fl<strong>in</strong>t is scattered along<br />

<strong>the</strong> islet’s nor<strong>the</strong>rn shore <strong>and</strong> at surface scatters<br />

on large portions <strong>of</strong> <strong>the</strong> isl<strong>and</strong>.<br />

Little Cove (LC) Antigua Formation Limestone primary,<br />

secondary<br />

Limestone section <strong>and</strong> cobble beach along<br />

Antigua’s eastern coast. Fl<strong>in</strong>t can be found on <strong>the</strong><br />

cobble beach <strong>and</strong> <strong>in</strong> limestone sections.<br />

Soldier Po<strong>in</strong>t (SP) Antigua Formation Limestone primary,<br />

secondary<br />

Extended rock po<strong>in</strong>t along Antigua’s northwestern<br />

coast. Fl<strong>in</strong>t can be found with<strong>in</strong> limestone <strong>of</strong><br />

this rock po<strong>in</strong>t as well as at both cobble beaches<br />

enclos<strong>in</strong>g it.<br />

Blackman’s Po<strong>in</strong>t<br />

(BP)<br />

Antigua Formation Limestone secondary,<br />

tertiary<br />

Exclusive secondary occurrence <strong>of</strong> ®<strong>in</strong>t at <strong>the</strong><br />

Blackman’s Po<strong>in</strong>t pen<strong>in</strong>sula along Antigua’s<br />

nor<strong>the</strong>rn shore. Fl<strong>in</strong>t can be found scattered on<br />

<strong>the</strong> surface <strong>and</strong> along an eroded coastl<strong>in</strong>e.<br />

Coconut Hall<br />

(CH)<br />

Antigua Formation Limestone secondary,<br />

tertiary<br />

Exclusive secondary occurrence <strong>of</strong> <strong>in</strong>l<strong>and</strong> scatters<br />

<strong>of</strong> ®<strong>in</strong>t at Coconut Hall along Antigua’s nor<strong>the</strong>rn<br />

coast.<br />

Shirley Heights<br />

(SH)<br />

Basal Volcanic Suite Tuff primary,<br />

secondary<br />

Chert boulders are exposed at <strong>the</strong> ®anks <strong>of</strong><br />

Shirley Heights <strong>in</strong> <strong>the</strong> sou<strong>the</strong>astern part <strong>of</strong> Antigua,<br />

surrounded by secondary surface scatters.<br />

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