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Where plate boundaries occur within continental lithosphere, deformation is spread out over a much larger area than the plate boundary itself. In the case of the San Andreas fault continental transform, many earthquakes occur away from the plate boundary and are related to strains developed within the broader zone of deformation caused by major irregularities in the fault trace(e.g. the “Big bend” region). The Northridge earthquake was associated with movement on a blind thrust within such a zone. Another example is the strongly oblique convergent plate boundary between the Arabian and Eurasian plates where it runs through the northwestern part of the Zagros mountains.

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The authors (with the permission of the airlines) carried a specially instrumented laptop on board 37 passenger flights in the US. On each flight they noted at least one case of a passenger making a cellular phone call, including a few during the critcal take-off and landing phases.
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