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NEW QUESTION: 1
Which set of actions does a network engineer perform to set the IPv6 address of a DHCP relay server at the VLAN interface level?
A. Enter the VLAN interface configuration mode, enable IPv6 DHCP relay, and define the IPv6 address of a DHCP relay server
B. Enter the global configuration mode, enable IPv6 DHCP relay from interface configuration mode and define the IPv6 address of a DHCP relay server
C. Enter the global configuration mode and enable the IPv6 DHCP relay
D. Enter the VLAN interface configuration mode and define the IPv6 address of a DHCP relay server
Answer: A
Explanation:
Explanation: You can accept DHCP requests from clients on the associated context or VLAN interface and enable the DHCP relay agent by using the ipv6 dhcp relay enable command (for IPv6) or the ip dhcp relay enable command (for IPv4). The DHCP relay starts forwarding packets to the DHCP server address specified in the ipv6 dhcp relay server command or the ip dhcp relay server command for the associated context or VLAN interface.
NEW QUESTION: 2
DRAG DROP
You have a server that has Exchange Server 2013 installed.
You plan to configure Unified Messaging (UM) to connect to an IP-PBX.
A telecommunications administrator configures the following numbers on the IP-PBX:
----
First extension number: 12100 Last extension number: 12499 Help extension number: 12500 Incoming pilot number: 12000
You need to configure UM to support the following requirements:
-- -
Users must be able to use Outlook Voice Access.
Users must be able to receive voice mail when callers connect to the users'
extension.
Callers must be able to dial into an automated help system hosted by your
company, which uses standard menus and speech-enabled menus.
Which numbers should you use for the UM configurations?
To answer, drag the appropriate number to the correct UM object in the answer area. Each number may be used once, more than once, or not at all. Additionally, you may need to drag the split bar between panes or scroll to view content.
Answer:
Explanation:
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. the duration of the quake
B. how well the offices and homes have been built in the region
C. how close the epicenter of the earthquake is to the area
D. the amount of damage
E. how soon people take action to stop the earthquake
Answer: C
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).
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