Free Test Prep GRE-Verbal-Reasoning Exam Questions

American history scholars generally attribute formation of the League of Indian Nations to Degandawida, who convinced the warring and fiercely autonomous Iroquois nations to embrace his radical idea for a league by tying it to familiar Iroquois customs and institutions. He associated the notion of peace and partnership with the Iroquois custom by which the families of slain warriors adopted war prisoners into the tribe. He invoked unquestioned social institutions as symbols, comparing the League to the traditional Iroquois clan in which several families share a "Longhouse" and Iikening the Great Council, comprised of representatives from each nation, to the Longhouse’s ever-burning Council Fire. And he assigned to each nation specific duties in order to assuage its fear of losing national identity. (For instance, he assigned to the Onondagas, who were centrally positioned geographically, the role of perpetual hosts.) Perhaps most persuasive, however, was how Degandawida’s League replicated the power structure of the traditional Iroquois clan. Each of the five Iroquois nations was comprised of matriarchal totemic clans in which the chiefs were men, the clan heads were women, and the chief’s children were considered members of his wife’s clan. Degandawida determined that the heads of each nation should select their League representatives, thereby effectively precluding the possibility of League representatives passing their power on to their sons, as well as decreasing the likelihood that a pro-war representative would be appointed. Iroquois unification under the League lasted about two centuries, when disagreement as to whether to become involved in the American Revolutionary war dMded the Iroquois. The revo|utionaries’ success and their subsequent encroachment upon Iroquois lands forced many Iroquois to resettle in Canada, while those who remained behind lost respect from other Indian nations. The introduction of distilled spirits led to widespread alcoholism and, in turn, to a rapid decline of the culture and population. The Quakers’ influence impeded, yet in another sense contributed, to this decline. By establishing schools for the Iroquois and by introducing them to modern technology for agriculture and husbandry, the Quakers instilled some hope for the future yet undermined their sense of national identity. Ironically, it was the alcoholic halfbrother of Seneca, Cornplanter, the most outspoken proponent among the Iroquois for assimilation of white customs and institutions, who revived the Iroquois culture. Around 1800, Handsome Lake, a former member of the Great Council, established a new religion among the Iroquois that tied the more useful aspects of Christianity to traditional Indian beliefs and customs. Lake’s teachings quickly became firmly entrenched among the Iroquois, sparking reunification and renewed confidence while also curbing rampant alcoholism. Lake’s influence is still evident today: many modern- day Iroquois belong both to his religion and to one or another Christian sect Assuming that the reasons asserted in the passage for the decline of the Iroquois culture are historically representative of the decline of cultural minorities, which of the following developments would most likely contribute to the demise of a modernday ethnic minority? and write in both their traditional language and the language prevalent in the present culture to improve efficiency active role

ITINERANT:

SWEAR : OATH ::

SATIATE:

The Andean cordillera is made up of many inten/voven 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 refilect 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. lV|uch of the southern portion of the Central Andes in BolMa 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?