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Bob receives the message, finds the first portion, and decrypts it with his private key to obtain the session key. He then uses the session key to decrypt the message and digital signature. Next, Bob takes Alice s public key and uses it to decrypt the hash value that was encrypted with Alice s private key. (Remember that, to make sure no one modified the key, Alice encrypted the hash with her private key; Bob uses Alice s public key to retrieve the original hash value to be sure that no one modified it in transit.) Bob would then run the message he decrypted through the same hash and compare the two hashes. If the hashes match, not only can Bob prove that Alice sent the message, but he also knows the message was unaltered in transit. This example shows how you would typically use all three types of crypto symmetric, asymmetric, and hash to achieve all of the goals of secure communication.

unlikely to engulf the unsuspecting pedestrian above knee-depth. Deeper quicksands can be more hazardous, and people have certainly drowned in some of these. The problem is that, although quicksands are more buoyant than open water, they are also more viscous. This has the unfortunate consequence that instinctive efforts to tread water (as one would in a swimming pool) can actually lead to deeper immersion, as the viscous sediment/water mixture offers frictional resistance to the rapid raising of the hands towards the surface. By lling your lungs with air and resisting the temptation to move arms and legs, it is possible to oat to the surface of the quicksand, whence rescue ought to be possible. In the case of most coastal quicksands, the real danger arises from the hindrance to rapid walking, thus entrapping struggling travelers in the path of a rising tide. 8.2.3 Subsidence Natural subsidence is a widespread consequence of the collapse of subsurface voids, which in turn owe their existence to the erosive action of groundwaters.iii The largest-scale and most widespread instances of this genre of subsidence are found in karst terrains, where groundwaters have dissolved limestone, gypsum and other soluble rocks. Closed depressions in the ground surface are abundant in most karst terrains; indeed they are so widespread that they have been proposed as the diagnostic feature of karst terrains (Ford and Williams 1989). These closed depressions are known by a variety of names, including sinkholes, iv potholes, and shakeholes. The preferred term in karst science circles is doline. While all dolines share in common the basic form of a surface depression, this uniformity belies a wide range of origins (Ford and Williams 1989):

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11321 Forward Generation of ATs Each AT de ned in the CDM written in the ERM language will result in a new eld being de ned inside a record type The HDM uses pointers rather than PKs and FKs; therefore, it is quite similar to the NDM for many of the AT mapping issues and considerations The rules and restrictions available to the HDM are as complete as those in the NDM, but otherwise the NDM data item and HDM eld are fairly similar 11322 Forward Generation of RTs Only one-to-many RTs can be directly represented in the HDM, and these must form a tree in order to make a hierarchy When the data being captured by the CDM is not particularly hierarchical, we will be forced to generate several hierarchies and use VLTs to connect the record types found in different hierarchies.

Figure 18.15 is a reference con guration for traf c and congestion control on a B-ISDN/ ATM network.

Sub MsgBoxHelp() Msg = Do you want to exit now Buttons = vbQuestion + vbYesNo + vbMsgBoxHelpButton HelpFile = ThisWorkbook.Path & \AppHelp.hlp ContextID = 1002 Ans = MsgBox(Msg, Buttons, , HelpFile, ContextID) If Ans = vbYes Then Call CloseDown End Sub

Similarly, VLTs must be used for all nonbinary or many-to-many RTs 11323 Forward Generation of ETs Each ET in the CDM will result in a new record type in the HDM with new elds de ned for each AT contained in the ET Otherwise, the situation is very similar to that considered in the NDM with respect to the identi cation issues and ET avors, except that the location of the record type in the hierarchy affects the existence and lifetime In other words, whenever a parent record type instance is deleted, all of its associated child record type instances are also deleted VLTs reduce the impact of this situation, but this restriction greatly affects the decision process for determining which ET should be generated as the parent record type of another.

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In some cases, this restriction is compatible with the de nition of Weak ETs, but that is not always the case 11324 Forward Generation of ITs ITs de ned in the CDM written in the ERM language can be used to de ne the hierarchies of record types and link types in the HDM The generation is straightforward, with only a single technique namely, generating a record type for the Super ET and each Sub ET and then generating one link type for each IT connection between Super ET and Sub ET Fields are generated in the corresponding record types Both the Total and Partial participation avors are supported, as well as the Disjoint and Overlapping participation avors but no direct support for enforcing these avors is provided.

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