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barrier island status report - Coastal Protection and Restoration ...

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Figure 31. Barrier <strong>isl<strong>and</strong></strong> average gulf-side shoreline change rates pre-restoration (1884-2005)<br />

<strong>and</strong> post-restoration (2005-2010/2011). Projects constructed (<strong>and</strong> years) are also listed in the<br />

data table.<br />

4.4.1 East Gr<strong>and</strong> Terre<br />

East Gr<strong>and</strong>e Terre Isl<strong>and</strong> is part of the original Gr<strong>and</strong> Terre Isl<strong>and</strong> which has divided into East<br />

<strong>and</strong> West Gr<strong>and</strong> Terre Isl<strong>and</strong>s separated by Pass Abel. This <strong>isl<strong>and</strong></strong> was restored in 2010 through<br />

the construction of the East Gr<strong>and</strong> Terre Isl<strong>and</strong> <strong>Restoration</strong> Project (BA-30) by the CPRA with<br />

funding from the <strong>Coastal</strong> Impact Assistance Program (CPE, 2011). The East Gr<strong>and</strong> Terre Isl<strong>and</strong><br />

<strong>Restoration</strong> Project was part of the original East <strong>and</strong> West Gr<strong>and</strong> Terre Isl<strong>and</strong> <strong>Restoration</strong> Project<br />

which was cooperatively designed <strong>and</strong> engineered by the CPRA <strong>and</strong> National Marine Fisheries<br />

Service through the CWPPRA program.<br />

Presented in Figure 32 are the average shoreline change rates for East Gr<strong>and</strong> Terre. The prerestoration<br />

erosion rates ranged from -38.9 ft/yr (BICM short-term) to -48.3 ft/yr (BICM longterm)<br />

noting the BICM historical average was on the same order of magnitude equal to -41.7<br />

ft/yr. East Gr<strong>and</strong> Terre has experienced breaching throughout the long-term <strong>and</strong> short-term<br />

intervals. The <strong>isl<strong>and</strong></strong> experienced net accretion in the near-term interval (+85.9 ft/yr on average)<br />

noting this period included the recently completed restoration project. The new historical<br />

average, equal to -34.7 ft/yr, is less than the BICM time period averages. Thus restoration of the<br />

<strong>isl<strong>and</strong></strong>‟s geomorphic form <strong>and</strong> function offset a significant percentage of the erosion experienced<br />

in the short-term period, returning the historical erosion rate to less than pre-restoration rates.<br />

40 | P a g e

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