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NEW QUESTION: 1
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.
This passage was most likely written to
A. explain some basic facts about the causes and effects of earthquakes
B. reassure people who are considering moving into regions prone to earthquakes that they will be safe
from harm
C. describe the damage that earthquakes can cause and the reason for varying degrees of damage
D. teach people the methods they need to alleviate earthquake damage
E. persuade people to allocate more funding to earthquake research
Answer: A
Explanation:
Using process of elimination, choices B and C are directly contradicted by information in the text. Choice
D is never mentioned. The second half of choice E is correct, but not the first half. Thus, the only possible
correct response is choice A.

NEW QUESTION: 2
A customer deploys a new WLAN that has 60 APs and 10 SSIDs. The customer uses a 40-MHz channel design for a 5-GHz WLAN that supports 10 nonoverlapping channels. The customer uses a mandatory Basic rate of 12 Mbps on the 5-GHz WLAN and 6 Mbps on the 2.4-GHz WLAN. After the deployment, the customer discovers that the 2.40-GHz frequency band is almost completely unusable and that the 5-GHz frequency is degraded. Which two options are possible ways to resolve the issues? (Choose two.)
A. Decrease the Beacon interval from 100 to 50 ms.
B. Change Channel Width to 20 MHz for the 5-GHz radio.
C. Increase the Beacon interval from 100 to 200 ms.
D. Reduce the number of SSIDs to four or less.
E. Set the mandatory Basic rate to 18 Mbps on 5 GHz and 24 Mbps on 2.4 GHz for the RF profile.
Answer: B,D

NEW QUESTION: 3
Which option is one way to mitigate asymmetric routing on an active/active firewall setup for TCP-based connections?
A. disabling asr-group commands on interfaces that are likely to receive asymmetric traffic
B. performing packet captures
C. replacing them with redundant routers and allowing load balancing
D. disabling stateful TCP checks
Answer: D