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Syntax the rules governing the formation of statements in a programming language is important regardless of which language your pages employ. Earlier browsers tended to be more relaxed about following the syntactical rules of HTML, but as standardization becomes increasingly important, browsers and businesses are following suit. Certain languages, such as XML, require the code to be proper or it just won t work. To ensure that a page is correctly written, the page should be validated. The Web offers numerous validation services most notably the one run by the W3C at http:// validator.w3.org but you don t need to leave Dreamweaver to validate your pages ever again. With Dreamweaver s Validation feature you can check a single page or an entire site. After it is checked, the resulting errors and warnings, if any, can be stored in an XML file for future output. Any error can be double-clicked to go right to the offending element for immediate correction. As with other Dreamweaver-style reports, the Validation feature resides in the Results panel, as shown in Figure 6-37. To display the Validation panel, choose Window Results and click the Validation tab. Controls for the Validation panel are found along the left, and the panel is divided into three sections: File, which lists the file being referenced; Line, which lists the line number on which the error can be found; and Description, which contains a brief overview of the problem. Clicking the Validate button the green triangle in the left margin of the Validation tab shown in Figure 6-37 unveils a menu of options:

Need a quick way to add a parent tag to a selection Choose Wrap Tag and you can easily enter the desired outer element, along with any desired attributes and values. Press Enter (Return) to confirm your choices and the parent tag code is inserted.

Financial Assets: Mortgages held for sale Loans held for sale Loans, net Nonmarketable equity investments (cost method) Total Difference Financial Liabilities: Deposits Long-term debt Total Difference Net Difference

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With seerer key encryption the sender and the receiver both use the same key to lock and unlock the message The key is known only to these parties In contrast, with public kej) encryption [291 2971 each user has two unique keys, a public key and a private one You distribute your public key to correspondents and they use this key to encrypt messages they send to you Messages encrypted with your public key can only be decrypted with your private key so that as long as this key remains secret no one else can read your incoming messages You can similarly encrypt outgoing messages with your correspondent s public key so that they can decode them with their own private key Your private key can also be used to encrypt any message you [298].

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The recipient can decrypt the signature with send as a digital sigrzatz~i-e your public key to verify your identity and the authenticity of the message The power of digital signatures is that they detect even very slight changes to a message If someone alters a comma to a full stop in the transmitted message (data) or introduces a virus then the signature will no longer verify..

Proof Existence: Given an element j3 E G F ( q m ) ,write down the ( m 1 ) elements 1, j3, P 2 , . . . , ,B" which are elements of G F ( q m ) . Since G F ( q m )is a vector space of dimension m over G F ( q ) ,these m 1 elements must be linearly dependent. Hence there exist coefficients ai E G F ( q )suchthatao+alj3+. . .+ampm= 0; theseare the coefficients of a polynomial f ( x ) = Ey!oa i d which has j3 as the root. (It is straightforwardto make this polynomial monic.) This also shows that the degree of f ( x ) 5 m. Uniqueness: Supposethat there are two minimal polynomials of j3, which are normalized to be monic; call them f ( x ) and g ( x ) . These must both have the same degree. Then there is a polynomial r ( x )having deg(r(x)) < deg(f(x)) such that

(Fig. 7.4b). Inside the rift, earthquake clusters parallel faults and volcanic centers in a series of 20 km wide, right-stepping zones of magmatism (Fig. 7.4c). Up to 80% of the total extensional strain is localized within these magmatic segments (Bilham et al.,

P(Aj ) P(B|Aj )

, W j ,aj) =

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