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Surface <strong>and</strong> Subsurface Morphology <strong>of</strong> <strong>the</strong> Beach Ridge Plain<br />

A summary <strong>of</strong> <strong>the</strong> characteristics <strong>of</strong> each beach ridge set, including average ridge crest<br />

elevation, average swale elevation, ridge orientation, direction <strong>of</strong> ridge splay <strong>and</strong> width <strong>of</strong> each<br />

beach ridge set at its widest point, is shown in Table 4.2.<br />

Topographic Survey Results<br />

A leveling pr<strong>of</strong>ile was conducted along a north-south transect across <strong>the</strong> isl<strong>and</strong>, following<br />

Road 4. This line crossed <strong>the</strong> trend <strong>of</strong> most <strong>of</strong> <strong>the</strong> beach ridge sets. The goal <strong>of</strong> <strong>the</strong> survey was<br />

to accurately measure <strong>the</strong> elevations <strong>of</strong> individual beach ridge crests <strong>and</strong> swales <strong>and</strong> <strong>the</strong> mean<br />

elevation <strong>of</strong> ridge sets. The location <strong>of</strong> <strong>the</strong> topographic survey line conducted across St. Vincent<br />

Isl<strong>and</strong> is shown in Figure 4.23. As discussed in Chapter 3, a benchmark was set at each sample<br />

location. The elevations <strong>of</strong> <strong>the</strong>se benchmarks were measured as part <strong>of</strong> <strong>the</strong> topographic survey.<br />

Figure 4.24 shows <strong>the</strong> result <strong>of</strong> <strong>the</strong> topographic survey. Table 4.3 shows <strong>the</strong> measured elevations<br />

<strong>of</strong> each benchmark. The blue line represents <strong>the</strong> survey conducted by Stapor as part <strong>of</strong> his<br />

dissertation work in 1973. The red line represents <strong>the</strong> survey conducted Stapor <strong>and</strong> Tanner<br />

(1977). The red line represents <strong>the</strong> survey conducted during this investigation. The two<br />

independent surveys are in reasonably good agreement. The green line represents <strong>the</strong> elevation<br />

<strong>of</strong> <strong>the</strong> road, which was also determined as part <strong>of</strong> this investigation. Since <strong>the</strong> road cuts through<br />

<strong>the</strong> high ridges, it mutes <strong>the</strong> natural topography. The boundaries between <strong>the</strong> ridge sets<br />

intersected by this transect have been superimposed on Figure 4.24, in addition to <strong>the</strong> locations<br />

<strong>of</strong> all samples that were collected along Road 4.<br />

Several features are apparent in Figure 4.24:<br />

1) The pr<strong>of</strong>ile obtained during this study closely agrees with <strong>the</strong> pr<strong>of</strong>ile obtained by<br />

Stapor <strong>and</strong> Tanner (1977). However, one beach ridge within set K has been eroded in<br />

<strong>the</strong> time elapsed between <strong>the</strong> current study <strong>and</strong> <strong>the</strong> Stapor <strong>and</strong> Tanner (1977) study.<br />

2) Set K has one ridge with an elevation <strong>of</strong> 3.8 m.<br />

3) The average elevation <strong>of</strong> <strong>the</strong> ridges in ridge set G is 2.4 m. Within this set <strong>the</strong>re are<br />

two high ridges (containing sample sites SVI 009 <strong>and</strong> SVI 023) with elevations <strong>of</strong> 4.4<br />

63

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