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It was obvious that migration of the North Carolina barrier islands would, in time, undermine this historic structure Dr Orrin H Pilkey, a Duke University geologist and noted authority on the Outer Banks, stated many times that the attempts to save the lighthouse in place are doomed On May 19, 1985, a Cape Hatteras Shoreline Erosion Workshop was held at Buxton, North Carolina Participants included representatives from the National Park Service, North Carolina State University, the University of Virginia, the Army Corps of Engineers, and the North Carolina Department of Natural Resources and Community Development The purpose of the workshop was to review the patterns and frequency of ocean shoreline changes in the vicinity of the Cape Hatteras Lighthouse Regardless of the database or study used, it was clear to the participants that the long-term change in this shoreline is characterized by erosion.



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Einc(r) = eiiki 'r (3.2.5)

Substituting (3.2.5) and (3.2.4) into (3.2.2) and using the momentum representation of T, we have (3.2.6)





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than 100 percent gain. It took three years to get there, but as the arrow indicates, the QQQ came within pennies of the retracement point, at which time it eased away. You may have noticed in the dialog box that the Fibonacci retracements do not end at 100 percent. They can go on to higher ratio levels, such as 161.8 percent, 261.8 percent, and higher. So not only can these retracement levels guide you in terms of price action between the two extremes of the reference line, but also they can give you guidance as to how high or low a price may move outside those extremes. The stock graph shown in Figure 13.16 provides a tting example of this. The graph encompasses the time range 1985 to 2006, a period of more than two decades. The retracement was drawn based on points in 1985 (the low) and 1991 (the high). From 1987 through 1999 there are many instances just a few of which are highlighted where the retracement levels have been obeyed. What s more interesting is what happens when the price breaks above the 100 percent level. There are three times when the stock paused and

dr'.Le-ik.Lor'.L+ikz!(r'.L)

(1.1.4)

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x [e( -kz)e(-k z ) + h( -kz)h( -k z )] . a(r'.L)

Equation (1.1.4) is the extended boundary condition and can be used to solve for the surface field a(r'.L). Since n x H is tangential to the surface, we also have the condition

n(r'.L) . a(r'.L) = 0

(1.1.5)

_' ) _ (' of(r'.L) a z(r 1- - x ox'

This erosion trend appears to be consistent with changes reported for most of the mid-Atlantic coast They concluded that causes were a combination of longterm sea level rise, storms, and both manmade and natural reduction in sediment supply The erosion of the beach was documented by reviewing 18 publications dealing with the quanti cation of erosion and accretion The information reviewed was based on aerial photographs and bathymetric charts for a period of 100 years Shoreline erosion is a manifestation of the whole island changing shape and position Migration of the Barrier Islands is a well-documented natural condition caused by the forces of waves, tides, and wind As the Barrier Islands roll over themselves in tank-tread fashion, nature maintains the dynamic equilibrium of the beaches through unceasing trade-offs of material, energy, topology, and the rising sea level.

of(r'.L)) . _ (_' ) oy' a1- r1-

FIGURE 13.16 Fibonacci levels beyond 100 percent can be an invaluable predictive tool, as illustrated here.

(1.1.6)

After the surface field is evaluated, the scattered field is, for z > fmax, using the plane wave representation of Green's function in equation (2.1.20) of Volume 1.

[e(kz)e(k z) +h(kz)h(kz)] a(r'..L)

(1.1.7)

Equation (1.1.7) shows that the scattered wave consists of a spectrum of plane waves. The incident wave, on the other hand, as represented by (1.1.1), consists of a plane wave in a single direction. Equations (1.1.4) through (1.1.7) are exact. We shall solve (1.1.4) and (1.1.7) by the perturbation method to the second order. A higher-order solution can be calculated in a similar manner with more complicated algebra. To solve for the surface fields, the perturbation method makes use of series expansions. Let

(1.1.8)

e ik.f(r~) =

For thousands of years, the traditional methods of protecting shorelines have centered around stabilizing the natural system The construction of marine.

(1.1.9)

a~O)(r~) = 0

consolidated, and in each of those three instances it matches the retracement level perfectly. Thus, the retracements are not only able to provide interpolation between two extremes, they are also able to extrapolate to price levels that haven t even been experienced by a stock yet. This obviously doubles the power and value of a well-placed Fibonacci retracement object.

(1.1.10)

(m)(-, ) _ (A of(r~) az r..L - x ox'

+ y of(r~)) A oy'

(1111)

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