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NEW QUESTION: 1

A. Option B
B. Option A
C. Option D
D. Option C
Answer: C
Explanation:
References: https://support.office.com/en-us/article/Share-SharePoint-files-or-folders-in- Office-365-1fe37332-0f9a-4719-970e-d2578da4941c

NEW QUESTION: 2
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. the duration of the quake
B. the amount of damage
C. how well the offices and homes have been built in the region
D. how soon people take action to stop the earthquake
E. how close the epicenter of the earthquake is to the area
Answer: E
Explanation:
Explanation/Reference:
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 seismicwaves pass through en route
(particularly those at or near the ground surface).

NEW QUESTION: 3

Refer to the exhibit. An engineer must add a subnet for a new office that will add 20 users to the network.
Which IPv4 network and subnet mask combination does the engineer assign to minimize wasting addresses?
A. 10.10.225.32 255.255.255.224
B. 10.10.225.48 255.255.255.240
C. 10.10.225.32 255.255.255.240
D. 10.10.225.48 255.255.255.224
Answer: A

NEW QUESTION: 4
質問のドラッグアンドドロップ
サイト間VPNを使用してAzureに接続する予定のオンプレミスネットワークがあります。
Azureには、アドレス空間を使用するVNet1という名前のAzure仮想ネットワークがあります
10.0.0.0/16。 VNet1には、10.0.0.0 / 24のアドレススペースを使用するSubnet1という名前のサブネットが含まれています。
Azureへのサイト間VPNを作成する必要があります。
どの4つのアクションを順番に実行する必要がありますか？回答するには、適切なアクションをアクションのリストから回答エリアに移動し、正しい順序に並べます。
注：回答の選択肢の複数の順序が正しいです。選択した正しい注文のいずれかのクレジットを受け取ります。

Answer:
Explanation:

Explanation:
注：回答の選択肢の複数の順序が正しいです。
ローカルゲートウェイ（オンプレミスルーターを表す論理オブジェクト）の作成は、ステップ1、ステップ2、またはステップ3で実行できます。他の3つのステップは、ゲートウェイサブネットを作成してからVPNゲートウェイを作成し、VPNを作成するために順番に実行する必要があります接続。 VPN接続は、VPNゲートウェイとローカルゲートウェイ間の接続です。