托福閱讀真題Official 49 Passage 1（一）

托福閱讀真題Official 49 Passage 1（一）

Ancient Coastlines

Information on past climates is primarily of relevance to archaeology because of what it tells us about the effects on the land and on the resources that people needed to survive.The most crucial effect of climate was on the sheer quantity of land available in each period,measurable by studying ancient coastlines.These have changed constantly through time,even in relatively recent periods,as can be seen from the Neolithic stone circle of Er Lannic,in Brittany,France(once inland but now half submerged on an island)or medieval villages in east Yorkshire,England,that have tumbled into the sea in the last few centuries as the North Sea gnaws its way westward and erodes the cliffs.Conversely,silts deposited by rivers sometimes push the sea farther back,creating new land,as at Ephesus in western Turkey,a port on the coast in Roman times but today some five kilometers inland.

Nevertheless,for archaeologists concerned with the long periods of time of the Paleolithic period there are variations in coastlines of much greater magnitude to consider.The expansion and contraction of the continental glaciers caused huge and uneven rises and falls in sea levels worldwide.When the ice sheets grew,the sea level would drop as water became locked up in the glaciers;when the ice melted,the sea level would rise again.Falls in sea level often exposed a number of important land bridges,such as those linking Alaska to northeast Asia and Britain to northwest Europe,a phenomenon with far-reaching effects not only on human colonization of the globe but also on the environment as a whole—the flora and fauna of isolated or insular areas were radically and often irreversibly affected.Between Alaska and Asia today lies the Bering Strait,which is so shallow that a fall in sea level of only four meters would turn it into a land bridge.When the ice sheets were at their greatest extent some 18,000 years ago(the glacial maximum),it is thought that the fall was about 120 meters,which therefore created not merely a bridge but a vast plain,1,000 kilometers from the north to the south,which has been called Beringia.The existence of Beringia(and the extent to which it could have supported human life)is one of the crucial pieces of evidence in the continuing debate about the likely route and date of human colonization of the New World.

The assessment of past rises and falls in sea level requires study of submerged land surfaces off the coast and of raised or elevated beaches on land.Raised beaches are remnants of former coastlines at higher levels relative to the present shoreline and visible,for instance,along the Californian coast north of San Francisco.The height of a raised beach above the present shoreline,however,does not generally give a straightforward indication of the height of a former sea level.In the majority of cases,the beaches lie at a higher level because the land has been raised up through isostatic uplift or tectonic movements.Isostatic uplift of the land occurs when the weight of ice is removed as temperatures rise,as at the end of an ice age;it has affected coastlines,for example,in Scandinavia,Scotland,Alaska,and Newfoundland during the postglacial period.Tectonic movements involve displacements in the plates that make up Earth’s crust;Middle and Late Pleistocene raised beaches in the Mediterranean are one instance of such movements.

Raised beaches often consist of areas of sand,pebbles,or dunes,sometimes containing seashells or piles of debris comprising shells and bones of marine animals used by humans.In Tokyo Bay,for example,shell mounds of the Jomon period(about 10,000 to 300 B.C.E.)mark the position of the shoreline at a time of maximum inundation by the sea(6,500–5,500 years ago),when,through tectonic movement,the sea was three to five meters higher in relation to the contemporary landmass of Japan than at present.Analysis of the shells themselves has confirmed the changes in marine topography,for it is only during the maximum phase that subtropical species of mollusc are present,indicating a higher water temperature.

Question 1 of 14

The word“crucial”in the passage is closest in meaning to

A.interesting

B.important

C.established

D.understood

正確答案：B

題目詳解

題型分類：詞匯題

選項分析：

The most crucial effect of climate was on the sheer quantity of land available in each period,measurable by studying ancient coastlines.譯為：氣候最重要的影響是對各個時期的可用土地數(shù)量的影響，在研究古代海岸線中可以測量。crucial，重要的；

B選項：重要的，正確；

A選項：有趣的；

C選項：建立的；

D選項：了解的。

Question 2 of 14

Which of the sentences below best expresses the essential information in the highlighted sentence in the passage?Incorrect choices change the meaning in important ways or leave out essential information.

A.In the last few centuries,the erosion of coastline created the Neolithic stone circle in Brittany,France,at the same time that it destroyed the medieval villages in Yorkshire,England.

B.Coastlines have changed even in recent times as shown by the current locations of certain Neolithic monuments and medieval villages.

C.Recent changes in the coastlines near the Neolithic stone circle of Er Lannic in Brittany,France,and the medieval villages in Yorkshire,England,suggest that ancient coastlines changed in similar ways.

D.Changes in coastlines can lead to the creation of islands such as Er Lannic in France or the total erosion of cliffs as in Yorkshire in England,though no considerable changes have occurred in recent periods.

正確答案：B

題目詳解

題型分類：簡化句子題

原文分析：帶簡化句子的主干是：these changed through time,as can be seen from the Neolithic stone circle or medieval villages.修飾部分是對海岸線改變的舉例。大意為在N和M兩個地方是對海岸線變化的舉例。

選項分析：

B選項：是對原句主干內(nèi)容的同義轉(zhuǎn)述，同時邏輯也是舉例說明，正確。

A選項：是在說兩種地方的變化，不是一個毀滅一個建造，故錯誤。

C選項：本句是在說都在變化，沒有比較變化的方式。

D選項：這個因果關(guān)系在原句中沒有體現(xiàn)，屬于無中生有。

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