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The following fault styles and physiographic features characterize the surface and upper crust of continental transforms and major continental strike-slip faults: 1 Linear fault scarps and laterally offset surface features. Large continental strike-slip faults typically display linear scarps and troughs that result from the differential erosion of juxtaposed material and the erosion of fault gouge (Allen, 1981). Surface features along active or recently active fault traces may be displaced laterally due to the strike-slip motion. The age and magnitude of these offsets provide an important means of determining slip rates. In New Zealand, for example, the Alpine Fault is marked by a nearly continuous, linear fault trace that extends across the South Island for a distance of 850 km (Fig. 8.2). Glacial moraines, rivers, valleys, lake shores, and other topographic features are offset laterally across the fault (Fig. 8.4), suggesting late Pleistocene slip rates of 21 24 mm a 1 (Sutherland et al., 2006). Vertical motion between parallel fault segments also is common and may create areas of localized uplift and subsidence that are expressed as pressure ridges and sag ponds, respectively (Sylvester, 1988). 2 Step-overs, push-ups, and pull-apart basins. Most large strike-slip faults are composed of multiple fault segments. Where one active segment terminates in proximity to another sub-parallel segment, motion is transferred across the intervening gap, resulting in zones of localized extension or contraction (Fig. 8.5a). In these step-overs, the initial geometry and sense of slip on the adjacent faults control whether the area separating them is extended or shortened (Dooley & McClay, 1997; McClay & Bonora, 2001). Normal faults and extensional troughs called pull-apart basins characterize step-overs where the intervening region is thrown into tension. Thrust faults, folds, and topographic uplifts known as push-ups form where the intervening region is compressed. In these



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Biometric identi cation will be used more and more to identify the person as the true and correct user. Today, the US immigration authorities scan thumbs and eyes to identify non-US citizens visiting the United States, and there are also some companies that require biometric identi cation for entrance to their premises and access to their computer systems. The aviation companies have discussed using ngerprint scanning for access to the ight deck, but they are also aware that a terrorist would be prepared to cut off a nger in order to gain access. Therefore, the scanning also needs to take into account that the nger is attached to a body; that is, by checking blood circulation. Discuss potential problems for each of the following types of biometric identi cation that is, the things that can go wrong for a normal user in a normal company: r r r r ngerprint scanning retina recognition voice recognition face recognition





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