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托福閱讀文本:
There are only a few clues in the rock record about climate in the Proterozoic eon. Much of
our information about climate in the more recent periods of geologic history comes from the fossil
record, because we have a reasonably good understanding of the types of environment in which
many fossil organisms flourished. The scarce fossils of the Proterozoic, mostly single-celled
bacteria, provide little evidence in this regard. However, the rocks themselves do include the
earliest evidence for glaciation, probably a global ice age.
The inference that some types of sedimentary rocks are the result of glacial activity is based on
the principle of uniformitarianism, which posits that natural processes now at work on and within
the Earth operated in the same manner in the distant past. The deposits associated with present-day
glaciers have been well studied, and some of their characteristics are quite distinctive. In
2.3-billion-year-old rocks in Canada near Lake Huron (dating from the early part of the
Proterozoic age), there are thin laminae of fine-grained sediments that resemble varves, the annual
layers of sediment deposited in glacial lakes. Typically, present-day varves show two-layered
annual cycle, one layer corresponding to the rapid ice melting and sediment transport of the
summer season, and the other, finer-grained, layer corresponding to slower winter deposition.
Although it is not easy to discern such details in the Proterozoic examples, they are almost
certainly glacial varves. These fine-grained, layered sediments even contain occasional large
pebbles or "dropstones," a characteristic feature of glacial environments where coarse material is
sometimes carried on floating ice and dropped far from its source, into otherwise very fine grained
sediment. Glacial sediments of about the same age as those in Canada have been found in other
parts of North America and in Africa, India, and Europe. This indicates that the glaciation was
global, and that for a period of time in the early Proterozoic the Earth was gripped in an ice age.
Following the early Proterozoic glaciation, however, the climate appears to have been fairly
benign for a very long time. There is no evidence for glaciation for the next 1.5 billion years or so.
Then, suddenly, the rock record indicates a series of glacial episodes between about 850 and 600
million year ago, near the end of the Proterozoic eon.
托福閱讀題目:
1. Which of the following does the passage mainly discuss?
(A) How patterns in rock layers have been used to construct theories about the climate of the
Proterozoic age
(B) What some rare fossils indicate about glacial conditions during the late Proterozoic age
(C) The varying characteristics of Proterozoic glacial varves in different parts of the world
(D) The number of glacial episodes that the Earth has experienced since the Proterozoic age
2.According to the passage , the fossil record of the Proterozoic eon is
(A) highly regarded because it preserves the remains of many kinds of organisms
(B) less informative than the fossil record of more recent periods
(C) very difficult to interpret due to damage from bacteria
(D) more useful to researchers than otheraspects of the rock record
3. The word "scarce" in line 4 is closest in meaning to
(A) ancient
(B) tiny
(C) available
(D) rare
4. It can be inferred from the passage that the principle of uniformitarianism indicates that
(A) similar conditions produce similar rock formations
(B) rock layers in a given region remain undisturbed over time
(C) different kinds of sedimentary rocks may have similar origins
(D) each continent has its own distinctive pattern of sediment layers
5. The word "resemble" in line 14 is closest in meaning to
(A) result from
(B) penetrate
(C) look like
(D) replace have similar origins
6.According to the passage , the layers in varves are primarily formed by
(A) fossilized bacteria
(B) pieces of ancient dropstones
(C) a combination of ancient and recent sediments
(D) annual cycles of sediment transport and deposition
7. The phrase "the other" in line 17 refers to another
(A) annual cycle
(B) glacial lake
(C) layer of sediment
(D) season
8.According to the passage , the presence of dropstones indicates that
(A) the glacial environment has been unusually servere
(B) the fine-grained sediment has built up very slowly
(C) there has been a global ice age
(D) coarse rock material has been carried great distances
9. Why does the author mention Canada, North America,Africa, India, and Europe in lines 23-24?
(A) To demonstrate the global spread of dropstones
(B) To explain the principles of varve formation
(C) To provide evidence for the theory that there was a global ice age in the early Proterozoic eon
(D) To illustrate the varied climatic changes of the Proterozoic eon in different parts of the globe
10. Which of the following terms is defined in the passage ?
(A) fossil record (line 3)
(B) laminae (line 13)
(C) varves (line14)
(D) glacial episodes (line 28)
托福閱讀答案:
ABDAC DCCCC
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22托福考試中能否取消考試成績(jī)?:托??荚囍心芊袢∠荚嚦煽?jī)?考生可以在考試結(jié)束之前選擇取消本次成績(jī),至此考生本人和申請(qǐng)的學(xué)校都將無(wú)法查詢成績(jī),也不會(huì)收到成績(jī)單??荚嚱Y(jié)束后則不能再取消成績(jī)。
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32托??荚嚾绾斡?jì)分?:托??荚嚾绾斡?jì)分?托??荚嚨乃膫€(gè)環(huán)節(jié),分?jǐn)?shù)由電腦自動(dòng)生成和人工評(píng)分(經(jīng)過(guò)專業(yè)培訓(xùn)的權(quán)威人士)兩部分組成,確保分?jǐn)?shù)的公平及準(zhǔn)確性。只有托福考試采用這種多人評(píng)分機(jī)制,通過(guò)不記名方式,由多名接受過(guò)嚴(yán)格培訓(xùn)的考官予以評(píng)分,過(guò)程經(jīng)過(guò)質(zhì)量監(jiān)控,達(dá)到高標(biāo)準(zhǔn)的公平性與客觀性。
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43托福考試的考場(chǎng)規(guī)則是什么?:托福考試的考場(chǎng)規(guī)則是什么?1.考生須服從考務(wù)人員的指令,不得大聲喧嘩擾亂考場(chǎng)秩序,有問(wèn)題須舉手示意等待考務(wù)人員前來(lái)解決。2.考生在考場(chǎng)的任何違規(guī)或舞弊行為都將被如實(shí)報(bào)告給ETS,違規(guī)或舞弊行為將會(huì)影響考生的考試成績(jī)甚至考試資格。因違規(guī)舞弊而被取消考試成績(jī)或考試資格的考生不得申請(qǐng)更改、退考或退款;情節(jié)嚴(yán)重者有可能被禁止參加以后的考試。
 01:30
01:302020-06-03

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