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Since Netscape Navigator 2.0, Web designers have been able to use background images and color. Thanks to CSS Background attributes, designers can now use background images and color with increased control. Whereas traditional HTML background images are restricted to a single image for the entire browser window, CSS backgrounds can be specified for a single paragraph or any other CSS selector. (To set a background for the entire page, apply the style to the <body> tag.) Moreover, instead of an image automatically tiling to fill the browser window, CSS backgrounds can be made to tile horizontally, vertically, or not at all (see Figure 7-16). You can even position the image relative to the selected element. The latest versions of browsers support the CSS Background attributes shown in Figure 7-17 and described in Table 7-2.
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Figure 1.3 Wegener s reconstruction of the continents (Pangea), with paleoclimatic indicators, and paleopoles and equator for (a) Carboniferous and (b) Permian time. I, ice; C, coal; S, salt; G, gypsum; D, desert sandstone; hatched areas, arid zones (modi ed from Wegener, 1929, reproduced from Hallam, 1973a, p. 19, by permission of Oxford University Press).
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Mitra, S. et al. (2006) Variation of Rayleigh wave group velocity dispersion and seismic heterogeneity of the Indian crust and uppermost mantle. Geophys. J. Int. 164, 88 98. Miyashiro, A. (1961) Evolution of metamorphic belts. J. Petrol. 2, 277 311. Miyashiro, A. (1972) Metamorphism and related magmatism in plate tectonics. Am. J. Sci. 272, 629 56. Miyashiro, A. (1973) Paired and unpaired metamorphic belts. Tectonophysics 17, 241 54. Mohr, P.A. & Zanettin, B. (1988) The Ethiopian ood basalt province. In MacDougall, J.D. (ed.) Continental Flood Basalts, pp. 63 110. Kluwer Academic Publishers, Dordrecht, Netherlands. Mohriak, W.U. & Rosendahl, B.R. (2003) Transform zones in the South Atlantic rifted continental margins. In Storti, F., Holdsworth, R.E. & Salvini, F. (eds) Intraplate Strike-slip Deformation Belts. Spec. Pub. geol. Soc. Lond. 210, 211 28. M ller, A. et al. (1995) Evidence for a 2 Ga subduction zone: eclogites in the Usagarian belt of Tanzania, Geology 23, 1067 70. Molnar, P. & Chen, W.-P. (1982) Seismicity and mountain building. In Hs , K.G. (ed.) Mountain Building Processes, pp. 41 57. Academic Press, London. Molnar, P. & Tapponnier, P. (1975) Cenozoic tectonics of Asia: effects of a continental collision. Science 189, 419 26. Molnar, P., Freedman, D. & Shih, J.S.F. (1979) Lengths of intermediate and deep seismic zones and temperatures in downgoing slabs of lithosphere. Geophys. J. Roy. astr. Soc. 56, 41 54. Molnar, P., England, P. & Martinod, J. (1993), Mantle dynamics, uplift of the Tibetan Plateau, and the Indian monsoon. Rev. Geophys. 31, 357 96. Montelli, R. et al. (2004a) Finite-frequency tomography reveals a variety of plumes in the mantle. Science 303, 338 43. Montelli, R. et al. (2004b) Global P and PP traveltime tomography: rays versus waves. Geophys. J. Int. 158, 637 54. Mont si, L.G.J. & Zuber, M.T. (2002) A uni ed description of localization for application to large-scale tectonics. J. geophys. Res. 107, 2045, doi:10.1029/2001JB000465. Mont si, L.G.J. & Zuber, M.T. (2003) Spacing of faults at the scale of the lithosphere and localization instability: 1. Theory. J. geophys. Res. 108, 2110, doi:10.1029/2002JB001923. Montgomery, D.R., Balco, G. & Willett, S.D. (2001) Climate, tectonics, and the morphology of the Andes. Geology, 29, 579 82. Moody, J.D. (1973) Petroleum exploration aspects of wrench fault tectonics. Am. Assoc. Pet. Geol. 57, 449 76. Mooney, W.D., Laske, G. & Masters, T.G. (1998) CRUST 5.1: a global crustal model at 5 5 . J. geophys. Res. 103, 727 47. Moore, G.F. et al. (2001) New insights into deformation and uid ow processes in the Nankai Trough accretionary prism: results of Ocean Drilling Program Leg 190. Geochem. Geophys. Geosyst. 2, doi:10.1029/2001GC000166. Moore, G.F. et al. (2005) Legs 190 and 196 synthesis: deformation and uid ow processes in the Nankai Trough accretionary prism. In Mikada, H. et al. (eds) Proceedings of the Ocean Drilling Program. Scienti c Results. 190/196, pp. 1 26. College Station, Texas.
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Figure 1.2 Total storage capacity compared.
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Web servers should not assume that all users will conduct accesses from within the confines of a known Web browser. A malicious user can generate any valid HTTP stream to the Web server for processing, and assumptions of input validity because of checks within the browser (say, through data validation checks implemented in JavaScript) might be risky. Using JavaScript to perform data validation improves user response because the user gets immediate feedback about malformed data within a form before it is actually sent to the server. The server should duplicate all data validation checks, however, and add additional checks against maliciously formed user input. Also do not depend on security implemented through the hidden variables in HTML forms. These variables are visible in the HTML source and can be easily modified before being sent to the Web server.
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