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Before you can successfully include a Shockwave file, you need to know one small bit of information the dimensions of your movie. Dreamweaver automatically reads the dimensions of your Flash file when you use the Insert Flash Movie object. Unfortunately, if you re incorporating a Shockwave movie, you still need to enter the dimensions by hand in the Shockwave Property Inspector. To check the width and height of your movie in Director, load your file and then choose Modify Movie Properties to open the Movie Properties dialog box.

Variations in intracrustal seismic re ectivity also suggest the presence of igneous intrusions directly below the rift valley (Fig 75b) Gravity data provide additional evidence that the crustal structure of rift zones is permanently modi ed by magmatism that occurs both prior to and during rifting In Ethiopia and Kenya, two longwavelength (>1000 km) negative Bouguer gravity anomalies coincide with two major 2 km high topographic uplifts: the Ethiopian Plateau and the Kenya Dome, which forms part of the East African Plateau (Figs 72, 76a) The highest parts of the Ethiopian Plateau are more than 3 km high This great height results from the eruption of a large volume of continental ood basalts (Section 74) between 45 and 22 Ma, with the majority of volcanism coinciding with the opening of the Red Sea and Gulf of Aden at 30 Ma (Wolfenden et al, 2005).

The single unfocused testBean method is now cleaned up to be six separate test methods. The test code is much easier to follow and is more focused on the particular aspect that is being tested. The names of the test methods are also more descriptive. This is a good time to bring up TestDecorators in Cactus. Keep in mind that a typical implementation of a JUnit test decorator in your Cactus tests will be run on the client side, not on the server side. This means that any access to a local EJB interface will fail because the test starts in a different JVM. In order to use test decorators they must interact with remote interfaces. You can accomplish this in several different ways. Placing a session fa ade is a popular way to provide a remote interface to the underlying entities. The typical problem with this approach, however, is that the session then needs specific methods to support testing. An alternative approach is to deploy your entities twice, once under their local interfaces and once with remote interfaces when doing testing. Placing remote interfaces over your entities is a maintenance burden so it is not without cost. Using the session fa ade is the recommended approach.

The negative gravity anomalies re ect the presence of anomalously low density upper mantle and elevated geotherms (Tessema & Antoine, 2004) In each zone, the rift valleys display short-wavelength positive Bouguer gravity anomalies (Fig 76b) that re ect the presence of cooled, dense ma c intrusions (Tiberi et al, 2005)..

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