托福备考怎样看课外阅读提升理解能力?正确方法让投入时间物有所值，今天小编给大家带来了托福备考怎样看课外阅读提升理解能力 ，希望能够帮助到大家，下面小编就和大家分享，来欣赏一下吧。
托福备考怎样看课外阅读提升理解能力?正确方法让投入时间物有所值
托福备考看课外读物提升阅读实力正确技巧方法讲解
看课外读物可以积累阅读经验，提升理解能力，这一点想必大家都知道，阅读量大的人做阅读题都会觉得更加轻松一些，至少心里会更有底气。但如何把看课外阅读和托福备考结合起来，这其中还是有一些技巧方法的，下面小编就为大家介3个要点技巧：
1. 明确阅读目标契合考试需求
首先小编希望大家明白的一点是，为了托福备考而进行课外阅读，那么本质目的是为了服务于考试而非单纯的个人爱好，所以在选择具体阅读文章时就不能太过主观了，毕竟托福考试可不会只给你看你感兴趣的文章，一些大家都觉得头疼的专业文章也是很多的。所以大家在选择读物时不能太过挑嘴，要做到无论什么样题材内容的文章都能保证认真仔细的阅读心态，哪怕是一些自己其实不感兴趣也完全不了解的题材，如果托福考试中出现过这个话题的文章，那么你也要静下心来投入阅读。考生需要培养一种对待所有文章都能客观看待一视同仁的阅读心态。这样大家才能在考试中以不变应万变不受影响的充分阅读和理解每篇文章。
2. 培养对文章主题和中心句的敏锐感
托福阅读考试中，篇幅较长的文章不在少数，大家可能对于这类文章都不太喜欢，本身阅读起来就要花费很多时间，带着的题目也变得有点面目可憎起来。这其实是因为大家缺乏应对长篇文章的经验所导致的，其实托福阅读并不需要每篇文章都从头到尾看得非常细致，只要把一些有关文章主题和中心的内容掌握牢就足以应对大部分题目。因此考生也需要培养对文章特别是长篇文章中主题和中心句的敏锐感。大家可以通过课外阅读来培养这方面的感觉，毕竟课外阅读中出现长篇文章的几率也是很高的。当然小编不建议考生从一开始做课外阅读就做到这一点，大家前期可以结合一些草稿做笔记的方式来记录自己认为是中心主题句的内容，之后再慢慢脱离草稿培养自己的记忆能力，逐步提升应对托福长篇阅读的适应能力。
3. 看课外阅读顺便锻炼生词处理技巧
生词问题在托福阅读中是比较让考生头疼的问题之一，很多人即使背熟了大量托福词汇仍然会不时在阅读过程中遇到一些不认识的词汇。而对于这种情况小编也建议大家早做准备，训练一下应对生词的突发性应急技巧，也就是俗称的猜词技巧。而训练这种技巧在课外阅读过程中进行无疑就是很好的机会。小编相信大家在看课外读物是也会时不时看到一些不认识的词汇，如果遇到建议大家不要直接查字典或是假装没看见，而是可以结合一些常规的找解释分析词根词缀的方式来适当做一些猜题练习，提前为托福阅读考试中可能遇到的生词问题做一些处理技巧方面的预演训练。
关于托福阅读通过课外读物来获得提升的方法技巧小编就为大家介绍到这里，希望各位同学能够掌握正确的学习方法，让自己在备考中投入的时间精力都有所回报，为考试做好更为充分全面的准备。
托福阅读真题原题+题目
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.
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)
PASSAGE 92 ABDAC DCCCC
