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NEW QUESTION: 1
Which of the following are contained in the SMP/E CSI?
A. PTF Elements
B. Element descriptions
C. APAR Elements
D. User Elements
Answer: B
NEW QUESTION: 2
Suppose that the probability of A is 0.80 and the probability of B is 0.60, if A and B are independent events, what is the probability of A or B?
A. 0.80
B. 0.92
C. 0.48
Answer: B
Explanation:
Since A and B are independent events P(A) = P(A|B) = 0.8 and P(AB) = P(A|B)
P(B) = 0.80 x 0.60 = 0.48, so P(A or B) = P(A) + P(B) - P(AB) = 0.80+0.60-0.48=0.92.
NEW QUESTION: 3
Examine this FortiGate configuration:
How does the FortiGate handle web proxy traffic coming from the IP address 10.2.1.200 that requires authorization?
A. It always authorizes the traffic without requiring authentication.
B. It authenticates the traffic using the authentication scheme SCHEME2.
C. It authenticates the traffic using the authentication scheme SCHEME1.
D. It drops the traffic.
Answer: C
NEW QUESTION: 4
Big earthquakes are naturally occurring events well outside the powers of humans to create or stop. An
earthquake is caused by a sudden slip on a fault. Stresses in the earth's outer layer push the side of the
fault together. The friction across the surface of the fault holds the rocks together so they do not slip
immediately when pushed sideways. Eventually enough stress builds up and the rocks slip suddenly,
releasing energy in waves that travel through the rock to cause the shaking that we feel during an
earthquake. Earthquakes typically originate several tens of miles below the surface of the earth. It takes
many years--decades to centuries--to build up enough stress to make a large earthquake, and the fault
may be tens to hundreds of miles long. The scale and force necessary to produce earthquakes are well
beyond our daily lives. Likewise, people cannot prevent earthquakes from happening or stop them once
they've started--giant nuclear explosions at shallow depths, like those in some movies, won't actually stop
an earthquake.
The two most important variables affecting earthquake damage are the intensity of ground shaking cased
by the quake and the quality of the engineering of structures in the region. The level of shaking, in turn, is
controlled by the proximity of the earthquake source to the affected region and the types of rocks that
seismic waves pass through en route (particularly those at or near the ground surface). Generally, the
bigger and closer the earthquake, the stronger the shaking. But there have been large earthquakes with
very little damage either because they caused little shaking or because the buildings were built to
withstand that shaking. In other cases, moderate earthquakes have caused significant damage either
because the shaking was locally amplified or more likely because the structures were poorly engineered.
You can conclude from this passage that
A. scientists understand a great deal about the origins of earthquakes but are powerless to stop them
B. all earthquakes are equally dangerous
C. there are steps that people can take to prevent or at least mitigate earthquakes
D. very little is known about earthquakes
E. earthquakes occur all over the world
Answer: A
Explanation:
Choices A, B, and D cannot be correct. Choice D is contradicted by information in the passage. Thus, the
only possible correct response is choice E.