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NEW QUESTION: 1
アプリケーションの作成中に会社間消去の追跡オプションを有効にする主な機能は何ですか？
A. アプリケーションに会社間データを含めることができます。
B. 連結ディメンションの消去メンバーを有効にします
C. プロセスは、データソースごとに合計消去値を分離します。
D. アプリケーションが会社間消去を実行できるようにします
Answer: C

NEW QUESTION: 2
Hotspot Question
You have a base class named Tree with a friend property named color and a protected property named NumberOfLeaves.
In the same project, you also have a class named Person.
For each of the following statements, select Yes if the statement is true.
Otherwise, select No. Each correct selection is worth one point.

Answer:
Explanation:

NEW QUESTION: 3

A. E
B. D
C. CSV
D. DATA
E. C
Answer: A,D
Explanation:

It slices, it dices, and it cleans your floors! Well, the Data Deduplication feature doesn't do everything in this version. It is only available in certain Windows Server 2012 editions and has some limitations. Deduplication was built for NTFS data volumes and it does not support boot or system drives and cannot be used with Cluster Shared Volumes (CSV). We don't support deduplicating live VMs or running SQL databases. See how to determine which volumes are candidates for deduplication on Technet. http://blogs.technet.com/b/filecab/archive/2012/05/21/introduction-to-data-deduplication-inwindowsserver-2012.aspx http://blogs.technet.com/b/uspartner_ts2team/archive/2012/10/08/data-deduplication-inwindows-server-2012.aspx

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