b) The pilot has no assurance of the accuracy of the GPS position. When the Receiver Autonomous Integrity Monitoring (RAIM) capability is lost in-flight, it means that the GPS receiver is no longer able to perform integrity checks on the GPS signals it receives.
RAIM is an important feature that ensures the accuracy and reliability of GPS positioning information. Therefore, without RAIM capability, the pilot cannot have assurance of the accuracy of the GPS position.
Option a, stating that the pilot may still rely on GPS derived altitude for vertical information, is incorrect because the loss of RAIM affects the overall accuracy and reliability of the GPS position, not just the vertical information.
Option c, stating that GPS position is reliable provided at least three GPS satellites are available, is also incorrect. While it is generally true that a minimum of three satellites is required for GPS positioning, the loss of RAIM compromises the ability to ensure the integrity of the received GPS signals, leading to potential inaccuracies and unreliability in the GPS position.
In summary, when RAIM capability is lost in-flight, the pilot cannot rely on the accuracy of the GPS position and must seek alternative means of navigation or rely on other available navigation aids for accurate positioning information.
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can the same fault be classified as both a strike-slip and a transform fault?
Yes, a fault can be classified as both a strike-slip and a transform fault. This is because the two terms are not mutually exclusive and can overlap.
A strike-slip fault is a type of fault in which the blocks of rock on either side of the fault move horizontally past each other. On the other hand, a transform fault is a type of fault in which two tectonic plates slide past each other in a horizontal motion. In both types of faults, there is horizontal movement occurring along the fault line.
In some cases, a fault may exhibit both strike-slip and transform characteristics, depending on the specific location and the tectonic forces at work. For example, the San Andreas Fault in California is classified as a strike-slip fault, but it also has transform properties as it separates the North American and Pacific plates.
Similarly, the Anatolian Fault in Turkey is classified as both a strike-slip and a transform fault as it separates the Eurasian and Arabian plates. Therefore, it is possible for a fault to be classified as both a strike-slip and a transform fault, as these terms describe different aspects of the same phenomenon of horizontal movement along a fault line.
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