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1. Choose Favorites from the Insert panel menu or tab. 2. Right-click (Control+click) and choose Customize Favorites from the context menu. You can actually perform the same action from any category/tab of the Insert panel to open the Customize Favorite Objects dialog box. 3. In the Customize Favorite Objects dialog, select the category holding the object you want to display in the Favorites category from the drop-down list under Available Objects. The All category displays every available object, sorted by category. If you know what category your object is in, it s quicker to select that category from the list.

The three-dimensional velocity structure of the upper mantle beneath rifts can be ascertained using teleseismic travel-time delays and seismic tomography. Davis & Slack (2002) modeled these types of data from beneath the Kenya Dome using two Gaussian surfaces that separate undulating layers of different velocities (Plate 7.2 between pp. 244 and 245). An upper layer (mesh surface) peaks at the Moho beneath the rift valley and has a velocity contrast of 6.8% relative to 8 km s 1 mantle. A lower layer (grayscale surface) peaks at about 70 km depth and has a 11.5% contrast extending to a depth of about 170 km. This model, which is in good agreement with the results of seismic refraction studies, shows a domal upper mantle structure with sides that dip away from the center of the Kenya Rift. The authors suggested that this structure results from the separation of upwelling asthenosphere into currents that impinge on the base of the lithosphere and form a low velocity, low density zone of melting between 70 and 170 km depth. Park & Nyblade (2006) used teleseismic P-wave travel times to image the upper mantle beneath the

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P1: JYS WY022-11

/ / Return the price of an item public double getItemPrice(int cindex)

ehold Figure 10-1, the Super Nintendo Portable you can build by hand!

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Site root relative addresses are indicated with a leading forward slash. For example:

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Finally, we will add a validate() implementation to MyForm:

Fi (0)TW,i, L (n) - SPast,W,i,0 (n) + (ho + hW,i, 0, Rad - hWR,i,0,G - hWR,i,0,Sky )To(n) + hWR,i,0,G TG (n) + hWR,i,0,Sky TSky(n) + a W,i,0 IT,i (n) Ei (0) + ho + hW,i,0,Rad (2.104) Fi (0)TW, i, 0 (n) + SPast,W, i,L (n) + hi, i Ti (n) + qW, i,L,Sol (n) + qW, i,L,Rad,W (n) + qW, i,L,Rad,Int (n) Gi (0) + hi, i

i #/

where p is pressure; Su ,Su ,Su are momentum source terms in the x,y,z directions respectivex y z ly; m and r are the viscosity and density of air respectively. Comparing Equations 3.16 3.18 with the general form of Equation 3.14, a more compact form of the momentum equations emerges: r Du x p = Su + m 2 u x x Dt x (3.19)

Then you obtain (valid in the whole disk and thus in the semidisk) u(r, ) 16.

Rule 3:

A typo can make a significant impression. Not many things are more embarrassing than showing a new Web site to a client and having that client point out a spelling error. Dreamweaver includes an easy-to-use Spell Checker to help you avoid such awkward moments. I make it a practice to spell-check every Web page before it s posted online. You start the process by choosing Text Check Spelling or you can press the keyboard shortcut Shift+F7. This sequence opens the Check Spelling dialog box, as seen in Figure 9-4.

Steps to compute p1 = -X- (-ET-~A Operation x1 = A m x2 = T-lxi ~3 = -Ex2 x4 = Cm x5 = x3 +a pi = -X- x5 Operation x1 = A m x6 = PPl XI = xi XI p2 = T- (x7)

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