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托福阅读备考训练技巧和做题策略汇总介绍

托福阅读备考训练技巧和做题策略汇总介绍
托福阅读备考训练技巧和做题策略汇总介绍

托福阅读备考训练技巧和做题策略

汇总介绍

托福阅读备考可以分为许多环节,其中考生在解题这个环节一般需要练习的都是答题技巧和应对不同题型的基本思路策略,今天给大家带来托福阅读备考训练技巧和做题策略汇总介绍,希望可以帮助到大家,下面就和大家分享,来欣赏一下吧。

托福阅读备考训练技巧和做题策略汇总介绍

托福阅读备考训练技巧分析

1,粗看下*的段数,对每段大概几道题有个预期。(比如只有5段,那长段肯定是3道题)粗看每段第一句话,对*的整体意思心中有数。

2,每段段首变成中文理解,以迅速的进入状态,并记忆主要意思。(就算只有一道词汇题,这段的段首也要读)

3,每读一段整理一次逻辑,A支持的观点是什么?A的观点的问题是什么?B的观点是什么?

4,鉴于每段都会出细节题,如果有词汇题等先只看一句话,做完了要看到细节题问的什么再看*,鉴于有四个选项,选一个

对的或者不对的,看的时候自己要边看边总结,比如总结出三个步骤,解释了三个方面的问题,或者其他。

5,检查,每个不确定的题都做记录,如果用心理解全文,一般能省下时间检查。

托福阅读做题策略介绍

词汇题、句子简化题:只读该句不读完整段;

主旨题:看每段的主旨句即可;

修辞目的题:推测作者举例意图,查看上下句;

句子插入题:分析具体待插入的句子,代入验证即可;

细节题,排除列举题:确定关键词,查看上下句;

推断题:作者明确暗示确并没有具体写出的意图,推测关键句;

指代题:分析指代句的特征,主要根据就近原则查看上文。

托福阅读真题原题+题目

Glaciers are large masses of ice on land that show evidence of past or present movement. They grow by the gradual transformation of snow into glacier ice.

A fresh snowfall is a fluffy mass of loosely packed snowflakes, small delicate ice crystals grown in the atmosphere. As the snow ages on the ground for weeks or months, the crystals shrink and become more compact, and the whole mass becomes squeezed together into a more dense form, granular snow. As new snow falls and buries the older snow, the layers of granular snow further compact to form firm, a much denser kind of snow, usually a year or more old, which has little pore space. Further burial and slow cementation — a process by which crystals become bound together in a mosaic of intergrown ice crystals — finally produce solid glacial ice. In this process of recrystallization, the growth of new crystals at the expense of old ones, the percentage of air is reduced from about 90 percent for snowflakes to less than 20 percent for glacier ice. The whole process may take as little as a few years, but more likely ten or twenty years or longer. The snow is usually many meters deep by the time the lower layers are converted into ice.

In cold glaciers those formed in the coldest regions of the Earth, the entire mass of ice is at temperatures below the melting point and no free water exists. In temperate glaciers, the ice is at the melting point at every pressure level within the glacier, and free water is present as small drops or as larger accumulations in tunnels within or beneath the ice.

Formation of a glacier is complete when ice has accumulated to a thickness (and thus weight) sufficient to make it move slowly under pressure, in much the same way that solid rock deep within the Earth can change shape without breaking. Once that point is reached, the ice flows downhill, either as a tongue of ice filling a valley or as thick ice cap that flows out in directions from the highest central area where the most snow accumulates. The trip down leads to the eventual melting of ice.

1. Which of the following does the passage mainly discuss?

(A) The effect of glaciers on climate

(B) Damage from glaciers

(C) Glacier formation

(D) The location of glaciers

2. Which of the following will cause density within the glacier to increase?

(A) Increased water and air content

(B) Pressure from the weight of new snow

(C) Long periods of darkness and temperature variations

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