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Understanding Character Encodings 135 Special Characters 136 En and Em Spaces and Dashes 137 Copyright and Trademark Symbols 138 Currency Symbols 138 Real Quotation Marks 139 Arrows 140 Accented Characters 140 Greek and Mathematical Characters 142 Other Useful Entities 146 Summary 148.

40. ye x z 2 42. Project. The first formula follows from [( g)x, ( g)y, ( g)z] [ x g, y g, z g] [ gx, gy, gz].

its discoverer(s), and earthquakes on it extend from near the surface, beneath the forearc region, down to a maximum depth of about 670 km Figure 95 shows a section through the Tonga Kermadec island arc system with earthquake foci projected on to a vertical plane parallel to the direction of underthrusting The foci can be seen to occur at progressively greater depths with increasing distance from the site of underthrusting at the Tonga Trench Further information on the nature of the Benioff zone was obtained from a study of the body wave amplitudes from deep earthquakes (Fig 96) Seismic arrivals at the volcanic islands of the arc, such as Tonga, were found to be of far greater amplitude than those recorded to the front or rear of the arc at stations such as Raratonga and Fiji.

The design of the Java security package is quite complex, caused in part by a desire to solve all problems from the ground up and in part by a desire to make the JVM and its

Authorization headers in HTTP/l.O, respectively. However, the Proxy-Authentication and Proxy-Authorization headers are used on a hop-by-hop basis. Better support for data compression: HTTP/1.1 provides better support for data compression. In particular, a web client can specify the encoding method such as the compression scheme(s)that idare supported and preferred by using the Accept-Encodingheader. * Better support for language(s): In H ITP/l.l, a web client can specify the language(s) that idare acceptable and preferred. Support for content integrity: In HTTP/1.1, content integrity can be supported by the Content-MDS header. Additional request methods: Four additional request methods are added as described in Table 2.10. However, they are less commonly-used than the GET, POST, and HEAD request methods.

The differences in amplitude are usually described quantitatively in terms of the Q-factor, the inverse of the speci c attenuation factor, and in general the higher the Q-factor the stronger the rock High Q travel paths give rise to little attenuation, and vice versa Seismic waves traveling up the length of the seismic zone appear to pass through a region of high Q (about 1000), while those traveling to lateral recorders pass through a more normal region of low Q (about 150) The Benioff zone thus appears to de ne the top of a high Q zone about 100 km thick The Benioff zone had originally been interpreted as a large thrust fault between different crustal provinces The seismic data allowed a new interpretation to be made in terms of a high Q belt of Paci c lithosphere underthrust into the mantle.

1999; Ebinger & Casey, 2001). The largest earthquakes typically occur along or near major border faults, although the seismicity data indicate that the border faults are mostly aseismic. Earthquakes are concentrated around volcanoes and ssures at depths of

0, the critical point is an unstable node. 3 ] 3 i]T and [1 i]T,

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This interpretation was re ned by Barazangi & Isacks (1971), by the use of a local seismometer network in the region of the Tonga arc (Fig 97) In addition to the previous results, a zone of very high attenuation.

images folder: ../images/.

(c) Temperature (10 Myr)

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1. Choose Text List Definition List or click the Definition List button in the Text category of the Insert panel. 2. Type the definition term and press Enter (Return) when you are finished. Dreamweaver indents the next line. 3. Type the definition data and press Enter (Return) when you are finished. 4. Repeat steps 2 and 3 until you have finished your definition list. 5. Press Enter (Return) twice to stop entering definition list items.