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Academicians do make assumptions about the price distribution of underlying assets For instance, we may expect that volatility (the square root of variance) during a short time interval is proportional to the square root of the time interval (Hull 1997) This is the power 1 2 Other evidence (Mandelbrot 2004) shows that the power can be between 1 2 and 1 This is useful for finding more realistic VaR (value at risk) estimations But wait, if one suggests a stochastic process driven by random variables of known distributions, then other observable characteristics such as trend lines, price patterns, and moving averages values are all deduced from this information and can be simulated For instance, the probability that two moving averages with different calculation periods will cross becomes quite certain, as will the probability that the price will penetrate some trend channel line.



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Elements of technical analysis, which sometimes causing skepticism among academicians, can be a natural consequence of the same stochastic processes applied by academicians This idea can be used for navigating bridges between what is often considered, two opposing worlds For instance, if one selects the price behavior of geometric Brownian motion dP/P = m dt + s dz, which has been mentioned in previous chapters, then it is clearly possible to simulate and observe whether certain trendlines and support and resistance lines appear and with what frequency For practical applications, this process is considered too simple and more realistic models should be selected (Mandelbrot 2004) It is interesting to read how those traders with many years of experience describe trends and volatility (Williams 2000): I doubt that anyone fully understood how the markets work until the mid-1980s.





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Sure, we knew about trend; about overbought and oversold markets; about a few patterns, seasonal influences, fundamentals, and the like But we really did not know what caused trend or, more correctly put, how it began and ended We do now [ ] Trends.

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transport of heat within the mantle wedge (England & Wilkins, 2004). Thus, many of the fundamental differences between crustal accretion in backarc and midocean ridge settings can be explained by the structure and dynamics of ow in the upper mantle wedge. However, it is important to realize that, in addition to processes related to subduction, it is probable that some backarc basins are in uenced by the speci c con gurations of plate boundaries in their vicinity. An example of this may be the North Fiji basin where the backarc spreading direction is oriented at unusually low angles (10 30 ) to the trend of the arc. Schellart et al. (2002) suggested that this unusual spreading direction could be related to an asymmetric opening of the basin and to collisional processes occurring along the plate boundary. The evolution of the Woodlark Rift (Section 7.8.2) also is strongly in uenced by local boundary conditions, including rheological weaknesses in the lithosphere. Variability in the structure and magmatic characteristics of backarc basins also is common in continental settings. Along the western margin of South America, for example, a series of extensional basins formed during a period of Mesozoic extension above a long-lived subduction zone (Fig. 9.34) (Section 10.2.1). In most of these basins, extension and backarc rifting

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