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Sample Sites<br />

CHAPTER 4<br />

RESULTS<br />

A total <strong>of</strong> twenty-nine sites were investigated on St. Vincent Isl<strong>and</strong>. Of <strong>the</strong>se twenty-nine<br />

sites, eight were dated using Optically Stimulated Luminescence (OSL). Figure 4.1 shows <strong>the</strong><br />

location <strong>of</strong> <strong>the</strong> samples collected over <strong>the</strong> course <strong>of</strong> this investigation <strong>and</strong> indicates which were<br />

vibracores <strong>and</strong> which were trenches. Each sampling site is briefly described below. Note: All<br />

coordinates are UTM Zone 16 (NAD 83). Table 4.1 lists all sample site numbers <strong>and</strong> sample<br />

locations.<br />

Beach ridge type is related to environmental conditions. The identification <strong>of</strong> beach ridge<br />

type is, <strong>the</strong>refore, important. Taylor <strong>and</strong> Stone (1996) <strong>and</strong> Tanner (1995) discuss <strong>the</strong> multiple<br />

origins <strong>of</strong> beach ridges, noting that morphology alone does not distinguish swash-built ridges<br />

from aeolian or storm-deposited ridges. However, internal structure is diagnostic. Beach ridge<br />

internal structure is difficult to observe <strong>and</strong> measure. This problem is in large part solved by <strong>the</strong><br />

excavation <strong>of</strong> trenches. In this investigation, trenches enabled direct observation <strong>of</strong> <strong>the</strong> basal<br />

deposits <strong>of</strong> former shoreline ridges, <strong>and</strong>, <strong>the</strong>refore, enabled sampling <strong>of</strong> only <strong>the</strong> wave-deposited<br />

portions <strong>of</strong> complex beach ridges that include aeolian deposition on <strong>the</strong>ir surface. In <strong>the</strong> ridges<br />

trenched, those that have visible bedding surfaces reveal a wave-built structure, with some<br />

aeolian decoration <strong>and</strong> no evidence <strong>of</strong> storm influence (i.e., <strong>the</strong> ridges exhibit seaward-dipping<br />

units throughout <strong>the</strong> ridge strata). This supports <strong>the</strong> swash-built hypo<strong>the</strong>sis for beach ridge<br />

formation, proposed by Stapor (1973, 1975), Stapor et al. (1991) <strong>and</strong> Tanner (1995), <strong>and</strong> serves<br />

as good evidence that each ridge represents a former shoreline position. By collecting samples<br />

from <strong>the</strong> exposed walls <strong>of</strong> trenches it was also possible to avoid collecting samples from areas<br />

that had been affected by bioturbation. An example <strong>of</strong> a typical trench is shown in Figure 4.2. A<br />

total <strong>of</strong> 18 trenches were excavated. Sample sites are described below. All information relevant<br />

to each site is presented in Table 4.1.<br />

SVI 001<br />

This site, located within ridge set A, is referred to as <strong>the</strong> “Paradise Point Site”. It is <strong>the</strong><br />

location <strong>of</strong> <strong>the</strong> complex midden site described in chapter 3. This site was first visited on July 23,<br />

56

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