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Admission Test GRE-Verbal Exam Syllabus Topics:

Admission Test Section One : Verbal Sample Questions:

1. ARCHITECT : CREATIVE ::

A) traitor : disloyal
B) prisoner : rebellious
C) soldier : obedient
D) consumer : prosperous
E) partisan : impartial

2. The _______ of the judging process might be compromised unless each contestant is assigned a unique
code number by which he or she is identified.

A) accuracy
B) finality
C) decisions
D) authority
E) impartiality

3. 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) providing alternative explanations for the climatic diversity among different regions of the An dean
cordillera
C) examining the effects of topography on the climate and vegetation of the An dean cordillera
D) comparing the climate and topography of the Northern Andes to those of the Central Andes
E) describing the climate and topography of various regions of the An dean cordillera

4. Conflict had existed between Spain and England since the 1570s. England wanted a share of the wealth
that Spain had been taking from the lands it had claimed in the Americas.
Elizabeth I, Queen of England, encouraged her staunch admiral of the navy, Sir Francis Drake, to raid
Spanish ships and towns. Though these raids were on a small scale, Drake achieved dramatic success,
adding gold and silver to England's treasury and diminishing Spain's omnipotence. Religious differences
also caused conflict between the two countries. Whereas Spain was Roman Catholic, most of England
had become Protestant.
King Philip II of Spain wanted to claim the throne and make England a Catholic country again. To satisfy
his ambition and also to retaliate against England's theft of his gold and silver, King Philip began to build
his fleet of warships, the Armada, in January 1586.
Philip intended his fleet to be indestructible. In addition to building new warships, he marshaled one
hundred and thirty sailing vessels of all types and recruited more than nineteen thousand robust soldiers
and eight thousand sailors. Although some of his ships lacked guns and others lacked ammunition, Philip
was convinced that his Armada could withstand any battle with England. The martial Armada set sail from
Lisbon, Portugal, on May 9,1588, but bad weather forced it back to port. The voyage resumed on July 22
after the weather became more stable. The Spanish fleet met the smaller, faster, and more maneuverable
English ships in battle off the coast of Plymouth, England, first on July 31 and again on August 2. The two
battles left Spain vulnerable, having lost several ships and with its ammunition depleted. On August 7,
while the Armada lay at anchor on the French side of the Strait of Dover, England sent eight burning ships
into the midst of the Spanish fleet to set it on fire. Blocked on one side, the Spanish ships could only drift
away, their crews in panic and disorder. Before the Armada could regroup, the English attacked again on
August 8. Although the Spaniards made a valiant effort to fight back, the fleet suffered extensive damage.
During the eight hours of battle, the Armada drifted perilously close to the rocky coastline. At the moment
when it seemed that the Spanish ships would be driven onto the English shore, the wind shifted, and the
Armada drifted out into the North Sea. The Spaniards recognized the superiority of the English fleet and
returned home, defeated
The Armada was ___ on one side.

A) closed off
B) circled
C) answer not available in this article
D) alone
E) damaged

5. The village of Vestmannaeyjar, in the far northern country of Iceland, is as bright and clean and up-to-date
as any American or Canadian suburb. It is located on the island of Heimaey, just off the mainland. One
January night in 1973, however, householders were shocked from their sleep. In some backyards red-hot
liquid was spurting from the ground.
Flaming "skyrockets" shot up and over the houses. The island's volcano, Helgafell, silent for seven
thousand years, was violently erupting! Luckily, the island's fishing fleet was in port, and within twenty-four
hours almost everyone was ferried to the mainland. But then the agony of the island began in earnest. As
in a nightmare, fountains of burning lava spurted three hundred feet high. Black, baseball-size cinders
rained down. An evilsmelling, eye-burning, throat-searing cloud of smoke and gas erupted into the air,
and a river of lava flowed down the mountain. The constant shriek of escaping steam was punctuated by
ear-splitting explosions. As time went on, the once pleasant village of Vestmannaeyjar took on a weird
aspect. Its street lamps still burning against the long Arctic night, the town lay under a thick blanket of
cinders. All that could be seen above the ten-foot black drifts were the tips of street signs. Some houses
had collapsed under the weight of cinders; others had burst into flames as the heat ignited their oil storage
tanks. Lighting the whole lurid scene, fire continued to shoot from the mouth of the looming volcano. The
eruption continued for six months. Scientists and reporters arrived from around the world to observe the
awesome natural event. But the town did not die that easily. In July, when the eruption ceased, the people
of Heimaey Island returned to assess the chances of rebuilding their homes and lives. They found tons of
ash covering the ground. The Icelanders are a tough people, however, accustomed to the strange and
violent nature of their Arctic land. They dug out their homes. They even used the cinders to build new
roads and airport runways. Now the new homes of Heimaey are warmed from water pipes heated by
molten lava.
The village is located on the island of-

A) Heimaey
B) Helgafell
C) Vestmannaeyjar
D) Heimma
E) Hebrides

Solutions: