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GRE-Verbal - Graduate Record Examination (Verbal) - Dump Information

Vendor : Admission-Tests
Exam Code : GRE-Verbal
Exam Name : Graduate Record Examination (Verbal)
Questions and Answers : 321 Q & A
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GRE-Verbal Questions and Answers

GRE-Verbal


QUESTION: 188

For absolute dating of archeological artifacts, the radiocarbon method emerged during the latter half of the twentieth century as the most reliable and precise method. The results of obsidian (volcanic glass) dating, a method based on the belief that newly exposed obsidian surfaces absorb moisture from the surrounding atmosphere at a constant rate, proved uneven. It was initially thought that the thickness of the hydration layer would provide a means of calculating the time elapsed since the fresh surface was made. But this method failed to account for the chemical variability in the physical and chemical mechanism of obsidian hydration. Moreover, each geographic source presented unique chemical characteristics, necessitating a trace element analysis for each such source. Yet despite its limitations, obsidian dating helped archeologists identify the sources of many obsidian artifacts, and to identify in turn ancient exchange networks for the flow of goods. Nor were ceramic studies and fluoride analysis supplanted entirely by the radiocarbon method, which in use allows for field labeling and laboratory errors, as well as sample contamination. In addition, in the 1970s, dendrochronological (tree-ring) studies on the bristlecone pine showed that deviation from radiocarbon values increases as one moves back in time. Eventually calibration curves were developed to account for this phenomenon; but in the archeological literature we still find dual references to radiocarbon and sidereal, or calendar, time. The author would probably consider which of the following the LEAST likely means of dating archeological artifacts?


  1. Ceramics studies

  2. Radiocarbon dating

  3. Dendrochronological studies

  4. Fluoride analysis

  5. Obsidian hydration-layer analysis


Answer: C


Explanation:

As the passage indicates, dendrochronological studies involve analyzing tree rings. Although the wood from trees might have been used for creating items which are now considered rcheological artifacts, the author does not indicate explicitly that tree rings are studied for the purpose of dating such artifacts.


QUESTION: 189

For absolute dating of archeological artifacts, the radiocarbon method emerged during the latter half of the twentieth century as the most reliable and precise method. The results of obsidian (volcanic glass) dating, a method based on the belief that newly exposed obsidian surfaces absorb moisture from the surrounding atmosphere at a constant rate, proved uneven. It was initially thought that the thickness of the hydration layer would provide a means of calculating the time elapsed since the fresh surface was made. But this method failed to account for the chemical variability in the physical and chemical mechanism of

obsidian hydration. Moreover, each geographic source presented unique chemical characteristics, necessitating a trace element analysis for each such source. Yet despite its limitations, obsidian dating helped archeologists identify the sources of many obsidian artifacts, and to identify in turn ancient exchange networks for the flow of goods. Nor were ceramic studies and fluoride analysis supplanted entirely by the radiocarbon method, which in use allows for field labeling and laboratory errors, as well as sample contamination. In addition, in the 1970s, dendrochronological (tree-ring) studies on the bristlecone pine showed that deviation from radiocarbon values increases as one moves back in time. Eventually calibration curves were developed to account for this phenomenon; but in the archeological literature we still find dual references to radiocarbon and sidereal, or calendar, time. The author mentions all of the following as problems with radiocarbon dating EXCEPT for


  1. disparities with the calendar dating system

  2. deterioration of samples

  3. identification errors by archeological field workers

  4. contamination of artifacts

  5. mistakes by laboratory workers


Answer: B


Explanation:

In the second paragraph, the author mentions choices (A), (C), (D), andE.as problems with radiocarbon dating. Now here in the passage, however, does the author mention any problem

involving sample deterioration


QUESTION: 190

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


  1. describing the climate and topography of various regions of the An dean cordillera

  2. discussing the factors affecting the climate of the An dean cordillera

  3. providing alternative explanations for the climatic diversity among different regions of the An dean cordillera

  4. examining the effects of topography on the climate and vegetation of the An dean cordillera

  5. comparing the climate and topography of the Northern Andes to those of the Central Andes


Answer: B


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.


QUESTION: 191

The Andean cordillera is made up of many interwoven mountain ranges, which include high intermontane 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 ater 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.

According to the passage, the northern part of the high-altitude plateaus is characterized by which of the following?


  1. Fertile soil

  2. High relative humidity

  3. A succession of agricultural zones

  4. Extremes in air temperature

  5. An arid climate


Answer: A


Explanation:

The high-altitude plateaus are called altiplano(line 16). The passage states explicitly that the soil fertility in the northern altiplanois generally good


QUESTION: 192

The Andean cordillera is made up of many interwoven mountain ranges, which include high intermontane 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.

It can be inferred from the passage that air temperatures in the Andean cordillera are often “lower than expected” (line 39) probably due to wide variations in


  1. precipitation levels

  2. air pressure

  3. prevailing wind direction

  4. aridity

  5. mountain elevation


Answer: E


Explanation:

The passage points out that while air temperature generally decreases as altitude increases, “variability of mountain topography”—i.e., dramatic changes in elevation—makes it difficult to determine temperature in any given spot from widely spaced measurements. It can be reasonably inferred from this information that an unexpected temperature would probably be the result of unexpected altitude.


QUESTION: 193

The Andean cordillera is made up of many interwoven mountain ranges, which include high intermontan 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 mentions all the following as climatic factors in the Central Andes cordillera EXCEPT for


  1. the Intertropical Convergence Zone

  2. the rainshadow effect

  3. the southern Pacific highpressure cell

  4. the symmetry of the mountain ranges

  5. the Pacific Humboldt current


Answer: D


Explanation:

The only discussion of mountain symmetry is in the first paragraph, which mentions the symmetry in climate between the east and west flanks of the Northern Andes mountains. No mention is made anywhere in the passage of any symmetry with respect to the Central Andes mountains. On the other hand, choices (A), (B), (C), andE.are all mentioned in the passage as factors affecting the climate of the Central Andes cordillera.


QUESTION: 194

The heart of the restorationist critique of environmental preservationism is the claim that it rests on an unhealthy dualism that conceives nature and humankind as radically distinct and

opposed to each other. The crucial question about the restorationist outlook has to do with the degree to which the restorationist program is itself faithful to its first principle— that nature and humanity are fundamentally united rather than separate. Rejecting the old domination model, which sees humans as over nature, restoration theory champions a model of community participation. Yet some of the descriptions of what restorationists are actually up to—for example, Turner’s description of humans as “the lords of creation,” or Jordan’s statement that “the fate and well being of the biosphere depend ultimately on us and our relationship with it”—do not cohere well with the community-participation model. Another holistic model—namely, that of nature as an organism—might be more serviceable to the restorationists. As with the community model, the “organic” model pictures nature as a system of interconnected parts. A fundamental difference, however, is that in an organism the parts are wholly subservient to the life of the organism. In asserting that the organic model“might be more serviceable to the restorationists” (lines 28–30), the author implies that


  1. the descriptions by Turner and Jordan of the restorationists’ program conform more closely to the organic model than to the community participation model

  2. the organic model is more consistent than the community participation model with the principle of restoration

  3. the organic model is more consistent with the restorationists’ agenda than with the preservationists’ program

  4. holistic models are more useful than the dualist model to the restorationists

  5. the organic model, unlike the community participation model, represents nature as a system of interconnected parts


Answer: A


Explanation:

In the preceding sentence, the author asserts that Turner’s and Jordan’s descriptions of restorationist activities “do not cohere well with the community participation model.” By following this assertion with the suggestion that another model might be more serviceable, you can reasonably infer that restorationists’ activities are more consistent with this other model than with the community participation model.


QUESTION: 195

The heart of the restorationist critique of environmental preservationism is the claim that it rests on an unhealthy dualism that conceives nature and humankind as radically distinct and opposed to each other. The crucial question about the restorationist outlook has to do with the degree to which the restorationist program is itself faithful to its first principle— that nature and humanity are fundamentally united rather than separate. Rejecting the old domination model, which sees humans as over nature, restoration theory champions a model of community participation. Yet some of the descriptions of what restorationists are actually up to—for example, Turner’s description of humans as “the lords of creation,” or Jordan’s statement that “the fate and well being of the biosphere depend ultimately on us and our relationship with it”—do not cohere well with the community-participation model. Another holistic model—namely, that of nature as an organism—might be more serviceable to the restorationists. As with the community model, the “organic” model pictures nature as a

system of interconnected parts. A fundamental difference, however, is that in an organism the parts are wholly subservient to the life of the organism.

Which of the following best expresses the function of the first paragraph in relation to the second one?


  1. To establish the parameters of an ensuing debate

  2. To discuss a secondary issue as a prelude to a more detailed examination of a primary issue

  3. To provide an historical backdrop for a discussion of a modern-day issue

  4. To introduce opposing viewpoints, which are then evaluated

  5. To identify a problem with a school of thought, which is then explored in detail


Answer: E


Explanation:

In the first paragraph, the author refers to the “crucial question” about, or key problem with, the restorations’ program, which the author then elucidates in the second paragraph.


QUESTION: 196

Late Victorian and modern ideas of culture are indebted to Matthew Arnold, who, largely through his Culture and Anarchy (1869), placed the word at the center of debates about the goals of intellectual life and humanistic society. Arnold defined culture as “the pursuit of perfection by getting to know the best which has been thought and said.” Through this knowledge, Arnold hoped, we can turn “a fresh and free thought upon our stock notions and habits.” Although Arnold helped to define the purposes of the liberal arts curriculum in the century following the publication of Culture, three concrete forms of dissent from his views have had considerable impact of their own. The first protests Arnold’s fearful designation of “anarchy” as culture’s enemy, viewing this dichotomy simply as another version of the struggle between a privileged power structure and radical challenges to its authority. But while Arnold certainly tried to define the arch—the legitimizing order of value—against the anarch of existentialist democracy, he himself was plagued in his soul by the blind arrogances of the reactionary powers in his world. The writer who regarded the contemporary condition with such apprehension in Culture is the poet who wrote “Dover Beach,” not an ideologue rounding up all the usual modern suspects. Another form of opposition saw Arnold’s culture as a perverse perpetuation of classical and literary learning, outlook, and privileges in a world where science had become the new arch and from which any substantively new order of thinking must develop. At the center of the “two cultures” debate were the goals of the formal educational curriculum, the principal vehicle through which Arnoldian culture operates. However, Arnold himself had viewed culture as enacting its life in a much more broadly conceived set of institutions. A third form is so-called “multiculturalism,” a movement aimed largely at gaining recognition for voices and visions that Arnoldian culture has implicitly suppressed. In educational practice, multiculturalists are interested in deflating the imperious authority that “high culture” exercises over curriculum while bringing into play the principle that we must learn what is representative, for we have overemphasized what is exceptional. Though the multiculturalists’ conflict with Arnoldian culture has clear affinities with the radical critique, multiculturalism actually affirms Arnold by returning us more specifically to a tension inherent in the idea of culture

rather than to the cultureanarchy dichotomy. The social critics, defenders of science, and multiculturalists insist that Arnold’s culture is simply a device for ordering us about. Instead, however, it is designed to register the gathering of ideological clouds on the horizon. There is no utopian motive in Arnold’s celebration of perfection. Perfection mattered to Arnold as the only background against which we could form a just image of our actual circumstances, just as we can conceive finer sunsets and unheard melodies. Based on the information in the passage, Arnold would probably agree that the educational curriculum should


  1. focus on the sciences more than the humanities

  2. strike a balance between practicality and theory

  3. reflect the dominant culture of the day

  4. be more rigorous than during the past

  5. deemphasize what is representative


Answer: E


Explanation:

ChoiceE.is consistent with Arnold’s views, as presented by the author. The passage emphasizes Arnold’s argument for the pursuit of perfection; thus, Arnold would probably agree that we should study the “exceptional” (see line 64) rather than the “representative.” Besides, choiceE.is inconsistent with the viewpoint of multiculturalists (with whom Arnold disagrees) that “we must learn what is representative, for we have overemphasized what is exceptional”


QUESTION: 197

Late Victorian and modern ideas of culture are indebted to Matthew Arnold, who, largely through his Culture and Anarchy (1869), placed the word at the center of debates about the goals of intellectual life and humanistic society. Arnold defined culture as “the pursuit of perfection by getting to know the best which has been thought and said.” Through this knowledge, Arnold hoped, we can turn “a fresh and free thought upon our stock notions and habits.” Although Arnold helped to define the purposes of the liberal arts curriculum in the century following the publication of Culture, three concrete forms of dissent from his views have had considerable impact of their own. The first protests Arnold’s fearful designation of “anarchy” as culture’s enemy, viewing this dichotomy simply as another version of the struggle between a privileged power structure and radical challenges to its authority. But while Arnold certainly tried to define the arch—the legitimizing order of value—against the anarch of existentialist democracy, he himself was plagued in his soul by the blind arrogances of the reactionary powers in his world. The writer who regarded the contemporary condition with such apprehension in Culture is the poet who wrote “Dover Beach,” not an ideologue rounding up all the usual modern suspects. Another form of opposition saw Arnold’s culture as a perverse perpetuation of classical and literary learning, outlook, and privileges in a world where science had become the new arch and from which any substantively new order of thinking must develop. At the center of the “two cultures” debate were the goals of the formal educational curriculum, the principal vehicle through which Arnoldian culture operates. However, Arnold himself had viewed culture as enacting its life in a much more broadly conceived set of institutions. A third form is so-called “multiculturalism,” a movement aimed largely at gaining recognition for voices and visions that Arnoldian culture has implicitly suppressed. In educational practice, multiculturalists

are interested in deflating the imperious authority that “high culture” exercises over curriculum while bringing into play the principle that we must learn what is representative, for we have overemphasized what is exceptional. Though the multiculturalists’ conflict with Arnoldian culture has clear affinities with the radical critique, multiculturalism actually affirms Arnold by returning us more specifically to a tension inherent in the idea of culture rather than to the cultureanarchy dichotomy. The social critics, defenders of science, and multiculturalists insist that Arnold’s culture is simply a device for ordering us about. Instead, however, it is designed to register the gathering of ideological clouds on the horizon. There is no utopian motive in Arnold’s celebration of perfection. Perfection mattered to Arnold as the only background against which we could form a just image of our actual circumstances, just as we can conceive finer sunsets and unheard melodies.

It can be inferred from the passage that the two-cultures debate


  1. emerged as a reaction to the multiculturalist movement

  2. developed after 1869

  3. influenced Arnold’s thinking about culture

  4. was carried on by American as well as European scientists

  5. led to a schizophrenic educational system


Answer: B


Explanation:

Arnold’s Culture was published in 1869. The three forms of opposition to Arnold’s ideas as presented in this work developed after its publication; therefore, they must have emerged

later than 1869.


QUESTION: 198

Late Victorian and modern ideas of culture are indebted to Matthew Arnold, who, largely through his Culture and Anarchy (1869), placed the word at the center of debates about the goals of intellectual life and humanistic society. Arnold defined culture as “the pursuit of perfection by getting to know the best which has been thought and said.” Through this knowledge, Arnold hoped, we can turn “a fresh and free thought upon our stock notions and habits.” Although Arnold helped to define the purposes of the liberal arts curriculum in the century following the publication of Culture, three concrete forms of dissent from his views have had considerable impact of their own. The first protests Arnold’s fearful designation of “anarchy” as culture’s enemy, viewing this dichotomy simply as another version of the struggle between a privileged power structure and radical challenges to its authority. But while Arnold certainly tried to define the arch—the legitimizing order of value—against the anarch of existentialist democracy, he himself was plagued in his soul by the blind arrogances of the reactionary powers in his world. The writer who regarded the contemporary condition with such apprehension in Culture is the poet who wrote “Dover Beach,” not an ideologue rounding up all the usual modern suspects. Another form of opposition saw Arnold’s culture as a perverse perpetuation of classical and literary learning, outlook, and privileges in a world where science had become the new arch and from which any substantively new order of thinking must develop. At the center of the “two cultures” debate were the goals of the formal educational curriculum, the principal vehicle through which Arnoldian culture operates. However, Arnold himself had viewed culture as enacting

its life in a much more broadly conceived set of institutions. A third form is so-called “multiculturalism,” a movement aimed largely at gaining recognition for voices and visions that Arnoldian culture has implicitly suppressed. In educational practice, multiculturalists are interested in deflating the imperious authority that “high culture” exercises over curriculum while bringing into play the principle that we must learn what is representative, for we have overemphasized what is exceptional. Though the multiculturalists’ conflict with Arnoldian culture has clear affinities with the radical critique, multiculturalism actually affirms Arnold by returning us more specifically to a tension inherent in the idea of culture rather than to the cultureanarchy dichotomy. The social critics, defenders of science, and multiculturalists insist that Arnold’s culture is simply a device for ordering us about. Instead, however, it is designed to register the gathering of ideological clouds on the horizon. There is no utopian motive in Arnold’s celebration of perfection. Perfection mattered to Arnold as the only background against which we could form a just image of our actual circumstances, just as we can conceive finer sunsets and unheard melodies.

The author’s primary concern in the passage is to


  1. argue against those who have opposed Arnold’s ideas

  2. describe Arnold’s conception of culture

  3. explain why Arnold considered the pursuit of perfection to be the essence of culture

  4. trace Arnold’s influence on the liberal arts educational curriculum

  5. examine the different views of culture that have emerged since the eighteenth century


Answer: A


Explanation:

The author’s threshold purpose, articulated in the final sentence of the first paragraph, is to identify the significant forms of dissent to Arnoldian culture. But the author proceeds to do more than merely identify and describe these forms of dissent; the author is also critical of the dissenters, for example, because they have misunderstood Arnold. ChoiceA.embraces both the author’s threshold and ultimate concerns.


QUESTION: 199

A certain strain of bacteria called lyngbya majuscula, an ancient ancestor of modern-day algae, is making a comeback in ocean waters just off the world’s most industrialized coastal regions. This primitive bacteria has survived for nearly three billion years due to a variety of survival mechanisms. It can produce its own fertilizer by pulling nitrogen out of the air; it relies on a different spectrum of light than algae do, allowing it to thrive even in deep, murky waters; and when it dies and decays, it releases its own nitrogen and phosphorous, on which the next generation of lyngbya feeds. Lyngbya emits more than one hundred different toxins harmful to other ocean life as well as to humans. Commercial fishermen and divers who come in contact with the bacteria frequently complain of skin rashes and respiratory problems, which can keep these workers off the job for months at a time. The bacteria further disrupts local economies by blocking sunlight to sea grasses that attract fish and other sea life. Scientists attribute the modern-day reappearance of lyngbya, and the resulting problems, chiefly to nitrogen- and phosphorous-rich sewage partially processed at wastewater treatment plants and pumped into rivers that feed coastal ocean waters. The passage as a whole can appropriately be viewed as an examination of which of the

following?


  1. The causes and consequences of the re-emergence of lyngbya

  2. The possible means of halting and reversing the spread of lyngbya

  3. The economic impact of lyngbya on certain coastal communities

  4. The survival mechanisms and life cycle of lyngbya

  5. The ecological fallout resulting from coastal sewage runoff


Answer: A


Explanation:

In order, the passage examines the survival mechanisms allowing lyngbya to reemerge today; the economic and ecological consequences of the strain’s reemergence; and the precipitating cause of the strain’s reemergence. ChoiceB.is clearly off the passage’s focus, and choiceE.is far too broad in scope. Of the remaining three choices, choiceA.comes closest to embracing the entire discussion.


QUESTION: 200

A certain strain of bacteria called lyngbya majuscula, an ancient ancestor of modern-day algae, is making a comeback in ocean waters just off the world’s most industrialized coastal regions. This primitive bacteria has survived for nearly three billion years due to a variety of survival mechanisms. It can produce its own fertilizer by pulling nitrogen out of the air; it relies on a different spectrum of light than algae do, allowing it to thrive even in deep, murky waters; and when it dies and decays, it releases its own nitrogen and phosphorous, on which the next generation of lyngbya feeds. Lyngbya emits more than one hundred different toxins harmful to other ocean life as well as to humans. Commercial fishermen and divers who come in contact with the bacteria frequently complain of skin rashes and respiratory problems, which can keep these workers off the job for months at a time. The bacteria further disrupts local economies by blocking sunlight to sea grasses that attract fish and other sea life. Scientists attribute the modern-day reappearance of lyngbya, and the resulting problems, chiefly to nitrogen- and phosphorous-rich sewage partially processed at wastewater treatment plants and pumped into rivers that feed coastal ocean waters. It can be inferred from the passage that the lyngbya majuscula strain has survived for billions of years partly because it


  1. is threatened by few, if any, natural predators

  2. emits harmful toxins that ward off potential predators

  3. does not depend on light for its existence

  4. possesses the ability to essentially feed on itself

  5. adapts easily to changes in water temperature


Answer: D


Explanation:

In the first paragraph, among the explanations given for lyngbya’s survival is that when it

dies and decays, the decaying matter, which is rich in the nutrients the strain needs to grow, sinks to the sea floor, where it nourishes the next generation of lyngbyA.In this sense, the strain has survived partly by its ability to essentially feed on itself.


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