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NEW QUESTION: 1
Given the following entry in /etc/nsswitch.conf: hosts: nis [NOTFOUND=return] files Which two statements are true? (Choose two.)
A. If the NIS map does NOT respond or is unavailable, the system will stop searching for the host.
B. If the NIS map gives a "no such entry" response, the system will stop searching for the host.
C. If the NIS map does NOT respond or is unavailable, the system will search local files for the host.
D. If the local files cannot be found, the system will search the NIS map for the host.
E. If the NIS map gives a "no such entry" response, the system will search local files for the host.
Answer: B,C
NEW QUESTION: 2
Which service parameter must be configured in Cisco Unified Communications Manager to enable SIP PUBLISH on a SIP trunk as the mechanism for presence interaction with Cisco Unified Presence?
A. processing on QSIG trunk
B. route class trunk
C. fail call over SIP trunk
D. IM and Presence publish trunk
Answer: D
NEW QUESTION: 3
You are designing a Group Encrypted Transport virtual private network solution for an existing branch network. The existing network has the following characteristics:
- 50 remote sites (with an additional 30 remote sites expected over the next 3 years)
- Connectivity between all sites is via Multiprotocol Label Switching Layer 3 virtual private network service from a single provider
- Open Shortest Path First is the routing protocol used between provider edge and customer edge routers
- The customer edge routers will become group members performing the encryption between sites Which additional routing protocol would you use for the overlay routing between the group members?
A. No additional protocol is necessary.
B. External Border Gateway Protocol
C. Routing Information Protocol Version 2
D. Enhanced Interior Gateway Routing Protocol
E. Open Shortest Path First (with a different process ID)
F. Next Hop Resolution Protocol
Answer: A
NEW QUESTION: 4
The Andean cordillera is made up of many interwoven mountain ranges, which include high intermundane
plateaus, basins, and valleys. The Northern Andes contain several broad ecosystems falling into four
altitudinal belts. Its northern subregion is distinguished by higher humidity and by greater climatic
symmetry between eastern and western flanks. The Central Andes are characterized by a succession of
agricultural zones with varied climatic conditions along the mountains' flanks and by large, highaltitude
plateaus, variously called puna or altiplano, which do not occur in the Northern Andes. The soil fertility of
the northern altiplano is generally good. The western Central Andean ranges are relatively arid with
desert-like soils, whereas the eastern ranges are more humid and have more diverse soils. The eastern
slopes of the Central Andes in many ways are similar to the wet forests of the Northern Andes. Unlike the
Northern Andes, however, these slopes have a dry season. In regions of gentle topography, such as the
Amazon basin, regional climatic variation can be determined from a few widely spaced measurements.
Regional projections in the Andean cordillera are quite difficult by comparison. For example, while air
temperature generally decreases with increasing altitude, variability of mountain topography can produce
much lower than expected air temperatures. Nevertheless, some general climatic patterns are discernible.
For example, with increasing distance south of the equator the seasonality of precipitation increases,
whereas the total annual amount generally decreases. Humidity commonly increases with increasing
altitude, but only to some intermediate altitude, above which it declines. The variability of mountain terrain
also affects precipitation, such that conditions of extreme wetness and aridity may exist in close proximity.
Related to this temperature gradient is a pattern of greater rainfall at the valley heads, and less rain at
lower altitudes, resulting in part from mountain rainshadow effect. The weather patterns of the Andean
cordillera and Amazon basin in general reflect movements of highand low-pressure cells associated with
the Intertropical Convergence Zone, a low-pressure trough that moves further north and south on a
seasonal basis. Precipitation is high throughout the year in the highlands and on the coast in the Northern
Andes. Coastal aridity increases south of central Ecuador, culminating in the Atacama desert of northern
Chile. In the Central Andes, highland precipitation is seasonal, and amounts are approximately half those
measured in the Northern Andes. The aridity of the Central Andean coastal zone is the result of the drying
effect of the cold Pacific Humboldt current and the southern Pacific high-pressure cell. Much of the
southern portion of the Central Andes in Bolivia is also arid. The dry season causes soil moisture deficits
and diminished stream flow part of each year.
The passage is primarily concerned with
A. discussing the factors affecting the climate of the An dean cordillera
B. describing the climate and topography of various regions of the An dean cordillera
C. examining the effects of topography on the climate and vegetation of the An dean cordillera
D. providing alternative explanations for the climatic diversity among different regions of the An dean
cordillera
E. comparing the climate and topography of the Northern Andes to those of the Central Andes
Answer: A
Explanation:
Most of the passage-the entire second and third paragraphs-is concerned with examining the factors
affecting the climate of various portions of the An dean cordiller A.The first paragraph provides a
framework for this discussion by describing the climate and topography of the various regions.