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Templates are composed of two types of regions: locked and editable. Every element on the Web page template falls into one category or the other. When a template is first created, all the areas are locked. Part of the process of defining a template is to designate and name the editable regions. Then, when a document is created from that template, the editable regions are the only ones that can be modified. Naturally, templates can be altered to mark additional editable areas or to relock editable areas. Moreover, you can detach a document created from a template at any point and edit anything in the document you cannot, however, reattach the document to the template without losing newly inserted content. On the other hand, a document based on one template can be changed to a completely different look but with the same content, if another template with identical editable regions is applied. Dreamweaver ships with a tutorial that illustrates the power of templates. The tutorial, found in the Dreamweaver/Tutorial folder, is based on an example Web site for a travel company called Compass. Previewing the site in a browser shows that all the sample pages for the different trips in the Destinations section are basically the same only the destination title, description, and Flash movie vary. The layout, background, and navigation controls are identical on every page. Each of these pages was created from the template page shown in Figure 32-1. Notice the highlighting surrounding certain areas; in a template, the editable regions are highlighted, and the locked areas are not. A tab further identifies each editable region to make it easier to add the right content in the right area.

is shorter After trying a number of possibilities, the route SBACEFDG may be arrived at, which gives a total distance of 12 even though all cities have been visited To verify that this is indeed the shortest route, other routes have to be tried, but now there is a benchmark of 12 which can be used to stop further examination of particular routes if the distance is 12 or more and G has not been reached The solution to this task is reached quickly, but now imagine that there is a real-life labelled map containing 100 or more cities and distances, with many different ways of getting from one city to another.

q = 510t 1/2 for t 55 Ma and q = 48 + 96exp( t/36) for t > 55 Ma. The variation of heat ow with age predicted by all three thermal models is illustrated in Fig. 6.9b and compared to observed heat ow values. It will be noted that observed values for younger lithosphere have not been plotted. This is because there are large variations in the heat ux measured in young oceanic crust (Fig. 6.4). The values obtained are typically less than those predicted by the models and there is now thought to be good reason for this. In particular, there is a large scatter in heat ow magnitude near the crests of ocean ridges. Thermal lows tend to occur in at- oored valleys and highs within areas of rugged topography (Lister, 1980).

Multiplying Equation 5.4 through by hfg and subtracting the result from Equation 5.2 results in the sensible heat balance for the heat exchanger experiencing both heat and mass transfer: Ta T Ma Do (T - Tf ) = -ua a t l r a c pa Aaf a An energy balance for the water side will be: r w Awf c pw Dl i.e.: Tw T hi Di (T - Tt ) = uw w r w c pw Awf w t l where: rw = density of water (kg m-3) Aw = the equivalent free ow area on the water side (m2) Tw T = r w uw Awf c pw Dl w - hi Di Dl(Tw - Tt ) t l

The output of this puts statement is: