B most likely:) hope this helps
Answer:
Here a struggle caused by the <em>Gulf of execution:</em>
While using Booking website, I want to book a hostel and I am logged in with my account. I think that because I am logged in, I need to only click the button book, put in some the details of my arrival and confirm booking. But for some reason system asks me to type in my email and name again though I am logged in. From my perspective as a user it should not happen because it takes unnecessary extra step from me.
Here a struggle caused by the <em>Gulf of evaluation:</em>
While using the Booking website I search a hostel in Singapore and it is nicely shows me how far a particular hostel is from the city center (for example 2 kilometers). Meanwhile, when I open a page of this hostel I do not see the information anymore. I have to click at the location, select arbitrary location in the city center on the map and only then will I see the distance between hostel and that location. As a user, I experience a huge gulf in evaluation that forces me to take a numerous extra steps.
The president is removed from office and the vice president takes over.
Explanation:
Satellite image of the Piqiang Fault, a northwest trending left-lateral strike-slip fault in the Taklamakan Desert south of the Tian Shan Mountains, China (40.3°N, 77.7°E)
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In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within the Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as subduction zones or transform faults.[1] Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep.[2]
A fault plane is the plane that represents the fracture surface of a fault. A fault trace or fault line is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault.[3][4]
A fault zone is a cluster of parallel faults.[5][6] However, the term is also used for the zone of crushed rock along a single fault.[7] Prolonged motion along closely spaced faults can blur the distinction, as the rock between the faults is converted to fault-bound lenses of rock and then progressively crushed.[8]
YW
