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n a world accustomed to being entertained by moving images 50 feet high, it s hard to understand why people are thrilled to see a grainy, jerky, quarter-screen sized video on a Web page. And in truth, it s the promise of video on the Web, not the current state of it, that has folks excited. Many of the industry s major players, including Microsoft and Apple, are spending big bucks to bring that promise a little closer to reality. QuickTime and RealVideo are the most popular formats on the Web, and both are cross-platform. Video can be downloaded to the user and then automatically played with a helper application, or it can be streamed to the user so that it plays while it s downloading. This chapter looks at the many different methods for incorporating video whether you re downloading an MPEG file or streaming a RealVideo movie into your Web pages through Dreamweaver.

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As with any plugin, your Web server has to have the correct MIME types set before Shockwave files can be properly served to your users. If your Web page plays Shockwave and Flash movies locally, but not remotely, chances are good that the correct MIME types need to be added. The system administrator generally handles configuring MIME types. The system administrator needs to know the following information to correctly configure the MIME types:

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large-offset normal faults may evolve from high-angle faults by exural rotation (Section 7.6.4). As the hanging wall is removed by slip on the fault, the footwall is mechanically unloaded and results in isostatic uplift and doming (Buck, 1988; Wernicke & Axen, 1988). The doming can rotate the normal fault to gentler dips and lead to the formation of new high-angle faults. The variety of Cenozoic fault patterns that typify the Basin and Range is illustrated in Fig. 7.14, which shows a segment of the eastern Great Basin in Utah and eastern Nevada (Niemi et al., 2004). The 350 km long Wasatch Fault Zone is composed of multiple segments with the largest displaying dips ranging from 35 to 70 to the west. Its subsurface geometry is not well constrained but it probably penetrates at least through the upper crust. The Sevier Desert Detachment Fault dips 12 to the west and can be traced continuously on seismic re ection pro les to a depth of at least 12 15 km (Fig. 7.14b). The range-bounding Spring Valley and Egan Range faults penetrate to at least 20 km depth and possibly through the entire 30 km thickness of the crust at angles of 30 . The Snake Range Detachment also dips 30 through most of the upper crust. Large-magnitude extension along the Snake Range (Miller et al., 1999) and Sevier Desert (Stockli et al., 2001) detachment faults began in Early Miocene time and Late Oligocene or Early Miocene time, respectively. In most areas, high-angle normal faults are superimposed on these older structures.

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8. Enter your Check out name and then put your email address in the Email address field. The username and email address are displayed for checked-out files. 9. To circumvent automatic logon to the WebDAV database when connecting in Dreamweaver and cause Dreamweaver to prompt you for a password every time deselect the Save option. 10. If you want to automatically check out a file when opening it from the Files panel, select the Check Out Files When Opening option. When this option is enabled, double-clicking a file in the Local Files view (or selecting it and then choosing File Open Selection) automatically performs the checkout procedure. 11. Click OK to close the Site Definition dialog box. 12. Click Done to close the Manage Sites dialog box.

In this example, the word "Art is underlined and colored. When it is clicked, the browser links to the URL http: //www.vbs.com/Books/Art.html as specified by the HREF attribute. Recall that in the URL, "http" stands for the hypertext transfer protocol; "www .vbs .com" is the server name; "Books is the directory; and, "Art .html" is the HTML file. We can also set up an email link with the <A> tag. It is widely supported by most browsers such as Netscape and Internet Explorer. For example, we can set up the following email link for customers to send emails to the Webmaster of our VBS: