2020托福備考怎樣看課外閱讀提升理解能力

托福備考怎樣看課外閱讀提升理解能力?正確方法讓投入時(shí)間物有所值，今天小編給大家?guī)?lái)了托福備考怎樣看課外閱讀提升理解能力 ，希望能夠幫助到大家，下面小編就和大家分享，來(lái)欣賞一下吧。

托福備考怎樣看課外閱讀提升理解能力?正確方法讓投入時(shí)間物有所值

托福備考看課外讀物提升閱讀實(shí)力正確技巧方法講解

看課外讀物可以積累閱讀經(jīng)驗(yàn)，提升理解能力，這一點(diǎn)想必大家都知道，閱讀量大的人做閱讀題都會(huì)覺得更加輕松一些，至少心里會(huì)更有底氣。但如何把看課外閱讀和托福備考結(jié)合起來(lái)，這其中還是有一些技巧方法的，下面小編就為大家介3個(gè)要點(diǎn)技巧：

1. 明確閱讀目標(biāo)契合考試需求

首先小編希望大家明白的一點(diǎn)是，為了托福備考而進(jìn)行課外閱讀，那么本質(zhì)目的是為了服務(wù)于考試而非單純的個(gè)人愛好，所以在選擇具體閱讀文章時(shí)就不能太過(guò)主觀了，畢竟托福考試可不會(huì)只給你看你感興趣的文章，一些大家都覺得頭疼的專業(yè)文章也是很多的。所以大家在選擇讀物時(shí)不能太過(guò)挑嘴，要做到無(wú)論什么樣題材內(nèi)容的文章都能保證認(rèn)真仔細(xì)的閱讀心態(tài)，哪怕是一些自己其實(shí)不感興趣也完全不了解的題材，如果托?？荚囍谐霈F(xiàn)過(guò)這個(gè)話題的文章，那么你也要靜下心來(lái)投入閱讀。考生需要培養(yǎng)一種對(duì)待所有文章都能客觀看待一視同仁的閱讀心態(tài)。這樣大家才能在考試中以不變應(yīng)萬(wàn)變不受影響的充分閱讀和理解每篇文章。

2. 培養(yǎng)對(duì)文章主題和中心句的敏銳感

托福閱讀考試中，篇幅較長(zhǎng)的文章不在少數(shù)，大家可能對(duì)于這類文章都不太喜歡，本身閱讀起來(lái)就要花費(fèi)很多時(shí)間，帶著的題目也變得有點(diǎn)面目可憎起來(lái)。這其實(shí)是因?yàn)榇蠹胰狈?yīng)對(duì)長(zhǎng)篇文章的經(jīng)驗(yàn)所導(dǎo)致的，其實(shí)托福閱讀并不需要每篇文章都從頭到尾看得非常細(xì)致，只要把一些有關(guān)文章主題和中心的內(nèi)容掌握牢就足以應(yīng)對(duì)大部分題目。因此考生也需要培養(yǎng)對(duì)文章特別是長(zhǎng)篇文章中主題和中心句的敏銳感。大家可以通過(guò)課外閱讀來(lái)培養(yǎng)這方面的感覺，畢竟課外閱讀中出現(xiàn)長(zhǎng)篇文章的幾率也是很高的。當(dāng)然小編不建議考生從一開始做課外閱讀就做到這一點(diǎn)，大家前期可以結(jié)合一些草稿做筆記的方式來(lái)記錄自己認(rèn)為是中心主題句的內(nèi)容，之后再慢慢脫離草稿培養(yǎng)自己的記憶能力，逐步提升應(yīng)對(duì)托福長(zhǎng)篇閱讀的適應(yīng)能力。

3. 看課外閱讀順便鍛煉生詞處理技巧

生詞問題在托福閱讀中是比較讓考生頭疼的問題之一，很多人即使背熟了大量托福詞匯仍然會(huì)不時(shí)在閱讀過(guò)程中遇到一些不認(rèn)識(shí)的詞匯。而對(duì)于這種情況小編也建議大家早做準(zhǔn)備，訓(xùn)練一下應(yīng)對(duì)生詞的突發(fā)性應(yīng)急技巧，也就是俗稱的猜詞技巧。而訓(xùn)練這種技巧在課外閱讀過(guò)程中進(jìn)行無(wú)疑就是很好的機(jī)會(huì)。小編相信大家在看課外讀物是也會(huì)時(shí)不時(shí)看到一些不認(rèn)識(shí)的詞匯，如果遇到建議大家不要直接查字典或是假裝沒看見，而是可以結(jié)合一些常規(guī)的找解釋分析詞根詞綴的方式來(lái)適當(dāng)做一些猜題練習(xí)，提前為托福閱讀考試中可能遇到的生詞問題做一些處理技巧方面的預(yù)演訓(xùn)練。

關(guān)于托福閱讀通過(guò)課外讀物來(lái)獲得提升的方法技巧小編就為大家介紹到這里，希望各位同學(xué)能夠掌握正確的學(xué)習(xí)方法，讓自己在備考中投入的時(shí)間精力都有所回報(bào)，為考試做好更為充分全面的準(zhǔn)備。

托福閱讀真題原題+題目

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