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Another way to use e-communities is through the chat rooms. Become familiar with the various e-community chat rooms where your customers go, so you can try to interest some of those audiences in coming to your party. If people are regularly logging on to WebMD and spending time there, how can Genzyme attract them to its party Try sharing information in the chat areas, or the bulletin boards, or posting questions. Or participate in the e-community s blog to raise

Figure 8.9 (a) Map of the south-central coast of Fiordland and (b,c) line drawings of seismic re ection pro les showing active faults, strike-slip basins, and other physiographic features along the southern segment of the Alpine Fault (images provided by P. Barnes and modi ed from Barnes et al., 2005, with permission from the Geological Society of America). Map location shown in Fig. 8.2a. Pro le (b) shows the subsiding part of the Dagg Basin, pro le (c) the uplifting part. Pro le locations are shown in (a). Solid faults are active, dashed faults are inactive. Labeled re ections are unconformities.

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In year four, the index will be the extended year-end price of $271,875 divided by the extended beginning-of-year price of $261,000, or 104.2%. We then derive the new cumulative index by multiplying the preceding year s cumulative index of 112.4% by the year four index of 104.2%, resulting in a new cumulative index of 117.1%. By dividing year four s extended year-end inventory of $271,875 by this cumulative index, we arrive at inventory priced at base year costs of $232,173. We then subtract the preexisting base year inventory valuation for all previous layers of $176,157 from this amount to arrive at the base year valuation of the year four inventory layer, which is $56,016. Finally, we multiply the $56,016 by the cumulative index in year four of 117.1% to arrive at an inventory valuation for the year four layer of $62,575. At this point, the inventory layers and associated cumulative indexes are as follows:

Identi cation trees have been used extensively in industry and academia and are perhaps the most widely applied arti cial intelligence technique covered in this book. This success is largely attributable to the ef ciency

5. Desolder the five thick leads holding the blue power on/off reset switch connector. Use a screwdriver to pry and lift the connector off. 6. Flip the board over to the parts side. See all those orange things that look like little frogs all over the board Those are capacitors, and you can carefully bend them over to make everything thinner (Figure 6-4). Tilt them over with your fingers try to keep their leads from touching any other metal, however. Looking at the board from the side, nothing should be much higher than the white controller connectors.

have been interpreted as being derived by the fractional crystallization of olivine from a primary magma originating at relatively shallow mantle depths of 65 100 km The calc-alkaline and alkaline series are encountered in more mature subduction zones, and appear to re ect magmas generated at depths greater than those that result in tholeiitic rocks Calc-alkaline magmas, represented by andesite and basaltic andesite, are the most abundant of the volcanic series Alkaline magmas exhibit the lowest abundance in island arcs and are more common in continental rifts and intraplate environments (Section 742) Some island arcs exhibit spatial patterns in the distribution of the volcanic series In the Japanese island arc system, for example, a compositional trend of tholeiite/ calc-alkaline/alkaline volcanic rocks is apparent with increasing distance from the trench.

Once you and your client are in the ConnectNow online meeting, choose Share My Computer Screen to display your Dreamweaver or other screen. You ll have an option to chat, enter notes, or even annotate the screen with arrows, text, or highlighted regions as shown in Figure 3-34. You can also incorporate a webcam and/or microphone, if you have them available.

This trend may re ect magmas derived from increasingly greater depths and/or differences in the degree of partial melting (Gill, 1981) A low degree of partial melting tends to concentrate alkalis and other incompatible elements into the small melt fraction (Winter, 2001), and could lead to an increase in alkalinity away from the trench due to a greater depth of melting or a decrease in the availability of water However, there are many exceptions to this pattern in other arcs, indicating that differences in local conditions strongly in uence magma compositions The Izu-Bonin Mariana arc system (Fig 91), for example, shows compositional trends along the axis of the arc From 35 N to 25 N latitude, volcanoes that form part of the Izu and Bonin arc segments are dominated by low and medium potassium rock suites (Fig 924).