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Bogue Banks Beach - Carteret County Shore Protection Office

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Final Report <strong>Bogue</strong> <strong>Banks</strong> <strong>Beach</strong> & Nearshore Mapping Program<br />

Periodic Survey Evaluation<br />

Accretion<br />

Erosion<br />

Volume Change (cy/ft)<br />

80<br />

60<br />

40<br />

20<br />

0<br />

-20<br />

-40<br />

-60<br />

-80<br />

-100<br />

-120<br />

Beaufort Inlet Unit Volume Change<br />

South North<br />

112 113 114 115 116<br />

B<br />

Transect Number<br />

Volume Change Above MHW Volume Change Above -5 ft Volume Change Above -12 ft<br />

Volume Change Above -20 ft Volume Change Above -30 ft<br />

Figure 16. Beaufort Inlet Unit Volume Change (2010 - 2011)<br />

5.4.8. Bear Island<br />

Bear Island contains 18 transects spaced 1000 ft apart. A summary of average shoreline and<br />

volume changes between summer 2010 and spring 2011 for the Bear Island region are presented<br />

in Table 22.<br />

Reach<br />

Length<br />

Table 22. Average <strong>Shore</strong>line and Volume Change for Bear Island<br />

avg<br />

shoreline<br />

change @<br />

MHW<br />

avg volume<br />

change<br />

above +1.1<br />

ft NAVD<br />

cumulative<br />

volume<br />

change<br />

above +1.1<br />

ft NAVD<br />

avg volume<br />

change<br />

above -5 ft<br />

NAVD<br />

cumulative<br />

volume<br />

change<br />

above -5 ft<br />

NAVD<br />

avg volume<br />

change<br />

above -12 ft<br />

NAVD<br />

cumulative<br />

volume<br />

change<br />

above -12 ft<br />

Bear Island appears to have been very stable over the past year, showing a slight accretion of<br />

shoreline position and gains in the volume of sand. Upon looking at the volume change plots in<br />

Appendix B and profile plots in Appendix C, it is apparent that the large offshore gain at<br />

Transect 1 accounts for much of the volume gain above -20 ft NAVD88 and -30 ft NAVD88.<br />

Most importantly, there was a volumetric gain of approximately 167,000 cy above -12 ft<br />

NAVD88, which was only slightly influenced by the large offshore gain at Transect 1 since most<br />

of the gain occurred below -12 ft NAVD88. Volume gain near <strong>Bogue</strong> Inlet was also evident in<br />

the previous survey evaluation. It is possible that the dynamic movements of <strong>Bogue</strong> Inlet are<br />

responsible for the accretion seen at the eastern end of Bear Island. It is thought that the channel<br />

has been naturally realigning to the east of its current position, causing the ebb shoal material to<br />

November 2011 30<br />

NAVD<br />

avg volume<br />

change<br />

above -20 ft<br />

NAVD<br />

cumulative<br />

volume<br />

change<br />

above -20 ft<br />

NAVD<br />

avg volume<br />

change<br />

above -30 ft<br />

NAVD<br />

cumulative<br />

volume<br />

change<br />

above -30 ft<br />

NAVD<br />

Reach (Profiles) ft ft cy/ft cy cy/ft cy cy/ft cy cy/ft cy cy/ft cy<br />

Bear Island (1-18) 16,500 22.3 3.2 53,005 7.5 123,382 10.1 167,132 8.4 137,875 6.1 100,963

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