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NEW QUESTION: 1
2つのサイトにはそれぞれ1つのWANエッジがあります。各WANエッジには、制限が設定されていない2つのパブリックTLOCがあります。
TLOC間の完全な到達可能性があります。各エッジルーターでいくつのデータトンネルが形成されますか？
A. 0
B. 1
C. 2
D. 3
Answer: A

NEW QUESTION: 2
Your network contains an Active Directory domain named contoso.com.
All domain controllers run
Windows Server 2012.
In a remote site, a support technician installs a server named DC10 that runs Windows Server 2012. DC10
is currently a member of a workgroup.
You plan to promote DC10 to a read-only domain controller (RODC).
You need to ensure that a user named Contoso/User1 can promote DC10 to a RODC in the contoso.com
domain.
The solution must minimize the number of permissions assigned to User1.
What should you do?
A. From Active Directory Administrative Center, modify the security settings of the Domain Controllers organizational unit (OU).
B. Join DC10 to the domain.
Modify the properties of the DC10 computer account
C. From Active Directory Administrative Center, pre-create an RODC computer account.
D. Join DC10 to the domain.
Run dsmod and specify the /server switch
Answer: C
Explanation:
A staged read only domain controller (RODC) installation works in two discrete phases:
1.Staging an unoccupied computer account
2.Attaching an RODC to that account during promotion

http://technet.microsoft.com/en-us/library/jj574152.aspx

NEW QUESTION: 3
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.
The amount of shaking during an earthquake is determined by
A. how soon people take action to stop the earthquake
B. how close the epicenter of the earthquake is to the area
C. the duration of the quake
D. how well the offices and homes have been built in the region
E. the amount of damage
Answer: B
Explanation:
Explanation/Reference:
Explanation:
The answer is directly stated: "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).