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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. describe the damage that earthquakes can cause and the reason for varying degrees of damage
B. explain some basic facts about the causes and effects of earthquakes
C. reassure people who are considering moving into regions prone to earthquakes that they will be safe
from harm
D. persuade people to allocate more funding to earthquake research
E. teach people the methods they need to all eviate earthquake damage
Answer: B
Explanation:
Explanation/Reference:
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
When protecting an organization's IT systems, which of the following is normally the next line of defense after the network firewall has been compromised?
A. Personal firewall
B. Virtual local area network (VLAN) configuration
C. Antivirus programs
D. Intrusion detection system (IDS)
Answer: D
Explanation:
Explanation/Reference:
Explanation:
An intrusion detection system (IDS) would be the next line of defense after the firewall. It would detect anomalies in the network/server activity and try to detect the perpetrator. Antivirus programs, personal firewalls and VI_AN configurations would be later in the line of defense.

NEW QUESTION: 3
Refer to the exhibits.
Exhibit 1

Exhibit 2

An Aruba solution supports a WLAN that uses WPA2-Enterprise security. Exhibit 1 shows the AAA policy for the WLAN. Users are supposed to be assigned to different roles after authentication. Network administrators test a connection with the employee user account. Exhibit 2 shows the status for the client after this test.
What is a possible reason for the issue shown in Exhibit 2?
A. The RADIUS server is not correctly set up to send a user role for the employee account.
B. MAC authentication is enabled on the WLAN, and the test device does not have an authorized address.
C. The shared key configured for the ClearPass server is incorrect.
D. The administrators entered the wrong password for the employee account.
Answer: A