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IELTS Academic Reading Practice Test 439

Part 1 · Read the text and answer questions 1–13

You should spend about 20 minutes on Questions 1–13, which are based on Reading Passage 1 below.

The Karst Hills of Guilin

Travellers have praised the scenery around Guilin, a city in the Guangxi region of southern China, for at least a thousand years. The landscape consists of hundreds of steep, rounded limestone hills rising from a flat plain beside the Li River, many pierced by caves and draped in vegetation. A Chinese saying, attributed to a Song dynasty official, declares that Guilin's scenery is the finest under heaven. What visitors seldom realise is that these strange hills are the eroded remains of a process that began long before any human being existed.

Geologists describe such country as karst, a term borrowed from the Kras, a stony plateau of limestone that stretches across the border between Slovenia and Italy. Karst landscapes develop wherever soluble rock — limestone, dolomite or gypsum — is exposed to water, and they are thought to cover a substantial share of the world's ice-free land. Their characteristic features are not mountains in the ordinary sense but the hollows between them: sinkholes, gorges, caverns and rivers that vanish underground. The word has since been adopted by geologists in every country, and the features it describes are found on every continent except Antarctica.

The rock itself is the key. During the Devonian period, several hundred million years ago, much of what is now southern China lay beneath a warm, shallow sea. Reefs and shell banks flourished in it, and the accumulated remains of corals, molluscs and microscopic organisms were compressed over millions of years into beds of calcium carbonate hundreds of metres thick. Geologists can still read that ancient sea floor in the stone: cross-sections of fossil shells, ripple marks left by currents and layers laid down in calm water.

The sea eventually withdrew, and movements of the Earth's crust that later raised the Himalayas lifted the region as well, exposing the limestone to the atmosphere. Uplift alone, however, would have produced an ordinary plateau. Two further conditions made the hills possible. The first was a climate with abundant monsoon rain. The second was the fracturing of the rock, which tectonic stresses had broken into a network of vertical joints, so that water could penetrate far below the surface rather than running off it.

Rain is naturally slightly acidic. As it falls it absorbs carbon dioxide from the air, and as it passes through soil, where decaying plants release the same gas, it takes up more, forming dilute carbonic acid. This solution attacks calcium carbonate and carries it away in dissolved form. The reaction is slow — in a laboratory it would barely be noticed — but over hundreds of thousands of years it removes an extraordinary volume of rock. Each litre of rainwater carries away only a tiny amount, yet rainfall here exceeds a metre a year and the process has continued for millions of years. Insoluble impurities are left behind as a thin red soil.

Underground, the widening joints became cave systems, some of which are now open to visitors; the Reed Flute Cave near Guilin, with its stalactites and stalagmites, is the best known. At the surface, the collapse of cave roofs produced sinkholes, and the landscape came to be divided into two related forms that Chinese geologists distinguish by name. In fengcong, meaning peak cluster, the hills remain joined at their bases and rise from a common mass of rock. In fenglin, meaning peak forest, they stand isolated on a flat plain, and it is this second form that makes the view from Guilin so distinctive.

Several explanations have been proposed for why the towers survive while the rock between them has gone. Most researchers emphasise the river and the plain around it. As the Li River shifts across its valley and deposits sediment, it clears away the weathered debris at the foot of the hills. The slopes then retreat, and the less fractured masses are left standing. Another factor is a harder cap of rock on some summits, which shields the hill beneath from rain and slows the process of dissolution. The towers are therefore not permanent features, merely one stage in a landscape's long decline.

For centuries the hills have attracted painters, poets and officials. Their shapes suggest animals and objects — an elephant drinking, a folded screen, a solitary brush — and many were given names accordingly. Visitors carved inscriptions into the walls of the caves, and a few of these records are still legible. In the twentieth century the hills became a favourite subject for Chinese painters, who often showed them rising out of mist. The city's own name reflects a different aspect of the place: Guilin means 'forest of osmanthus', after the fragrant trees that grow on the surrounding slopes.

Guilin's scenery is now a national asset and an industry. Millions of tourists arrive each year, and most of them take a boat journey of some eighty kilometres down the Li River to Yangshuo. One celebrated view of the hills there has appeared on the back of a Chinese banknote. The pressure on the landscape is considerable.

Limestone has been quarried on the edges of the city to make cement, and although many quarries have been closed and the sites replanted, bare scars remain. Water quality in the river has suffered from sewage and from farming, and the spread of the city has consumed farmland in the valley. The wider region, known as the South China Karst, is a UNESCO World Heritage property, which brings both protection and further visitors.

Tip: select any text in the passage to highlight it in one of four colours. Click a highlight to remove it.

Questions 1–5◎ Practise this set only

Complete the flow-chart below. Choose ONE WORD ONLY from the passage for each answer.

Write ONE WORD ONLY for each answer.

The formation of the Guilin towers

Marine remains are compressed into limestone on the bed of a shallow
Movements of the Earth's raise the rock above sea level
Water made acidic by carbon dioxide penetrates the vertical in the limestone
The collapse of cave roofs creates at the surface
The river clears debris from the foot of the hills, so that the slopes

Questions 6–9◎ Practise this set only

Choose the correct letter, A, B, C or D.

What does the writer say about the word 'karst'?
What point does the writer make about the chemical reaction that dissolves the limestone?
What is the function of the resistant rock found on some summits?
Which of the following is mentioned as causing damage to the landscape?

Questions 10–13◎ Practise this set only

Answer the questions below. Choose NO MORE THAN TWO WORDS AND/OR A NUMBER from the passage for each answer.

Write NO MORE THAN TWO WORDS AND/OR A NUMBER for each answer.

What is the Chinese term for the form of karst in which the hills stand separately on a plain?
What did visitors carve into the walls of the caves?
Which fragrant tree gives Guilin its name?
How long is the boat journey from Guilin to Yangshuo?

About this reading test

A full IELTS Academic Reading practice test with 40 questions on three original passages: the karst landscape around Guilin, how first impressions form, and whether critical thinking should be taught as a school subject. Includes explanations and a band estimate.

PartPassageQuestionsQuestion typesTopicsWords
1The Karst Hills of Guilin1–13Flow-chart completion, Multiple choice, Short-answer questionsEarth & Geography, Science909
2How First Impressions Form14–26Matching headings, Summary completion (word list), Multiple choice (choose more than one)Psychology, Society880
3Should Critical Thinking Be Taught as a School Subject?27–40Matching information, Matching features, Summary completionEducation, Psychology901

Key vocabulary from this test

WordMeaningIn the passage
soluble
adjective
able to be dissolved by a liquid such as water“Karst landscapes develop wherever soluble rock — limestone, dolomite or gypsum — is exposed to water” (Passage 1)
tectonic
adjective
relating to the forces that move and break the Earth's outer layer“the fracturing of the rock, which tectonic stresses had broken into a network of vertical joints” (Passage 1)
dissolution
noun
the process by which a solid is broken down and carried away by a liquid“which shields the hill beneath from rain and slows the process of dissolution” (Passage 1)
debris
noun
loose broken pieces of rock or other material left somewhere“it clears away the weathered debris at the foot of the hills” (Passage 1)
monsoon
noun
a seasonal wind that brings a period of heavy rain“The first was a climate with abundant monsoon rain” (Passage 1)
thin slicing
phrase
forming judgements from very brief samples of another person's behaviour“the phenomenon has been given a name: thin slicing” (Passage 2)
multimodal
adjective
involving several different channels of information at the same time“Because these signals arrive together, researchers describe first impressions as multimodal” (Passage 2)
consensus
noun
general agreement among a group of people“Consensus, in other words, is evidence about the observers rather than about the person observed” (Passage 2)
halo effect
phrase
the tendency for one good quality to make people assume other good qualities“an effect so reliable that psychologists refer to it as the halo effect” (Passage 2)
hypotheses
noun
provisional ideas that are treated as possibly true until tested“but to treat them as hypotheses that further evidence may overturn” (Passage 2)
scepticism
noun
a doubting attitude towards claims that are not well supported“In its widest sense it covers scepticism, open-mindedness and a general habit of asking why” (Passage 3)
precondition
noun
something that must exist or happen before something else is possible“On this account facts are not the enemy of thinking but its precondition” (Passage 3)
fallacies
noun
faulty patterns of reasoning that make an argument invalid“a general course can do little more than teach students to name fallacies they cannot detect in practice” (Passage 3)
conclusive
adjective
so strong that it settles a question or proves a point“Neither would accept the other's methods as conclusive” (Passage 3)
mainstream
noun
the accepted, usual practice of most people or institutions“but it attracted only a small minority and never became part of the mainstream” (Passage 3)

How to use this practice test

  • Take the full test in 60 minutes, or practise one passage in 20 minutes.
  • Select text in the passage to highlight it, and click a question number to flag it for review.
  • Drag answers from a list into the gaps, or tap a gap to choose from a menu.
  • When you submit, each answer is marked right or wrong, with an explanation and a “Show in passage” button that highlights the sentence that proves it.
  • For gap-fill questions, keep to the word limit; an answer over the limit is marked wrong, as in the real exam.

All passages and questions on Sprechify are written by our own team in the official IELTS format. They are not taken from Cambridge IELTS books or any other published test. Band scores are estimates based on the conversion commonly used for practice tests.

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