Weathering in the Desert – IELTS Reading Answers

Prity Mallick

11 min read

Updated On Jul 20, 2024

Reading Passage
Answers of The Weathering in the Desert Reading Answers with Location and Explanation
Tips to Solve the Question Types in Weathering in the Desert IELTS Reading Answers
Also, check:

Limited-Time Offer : Access a FREE 10-Day IELTS Study Plan!

The Reading Module of the IELTS can be the top-scoring category with diligent practice. To achieve the best results in this section, you must understand how to approach and answer the different question types in the Reading Module. By solving and reviewing sample reading questions from past IELTS papers, you can ensure that your reading skills are up to the mark.

The Academic passage, Weathering in the Desert Reading Answers, is a reading passage that appeared in an IELTS Test. Try to find the answers to get an idea of the difficulty level of the passages in the actual reading test. If you want more passages to solve, try taking one of our IELTS reading practice tests.

The question types found in this passage are:

IELTS Matching Information(Q. 1-7)
IELTS True/False/Not Given (Q. 8-13)

Want to discuss your IELTS queries with the best experts for FREE?

All you have to do is book your session now!

Reading Passage

You are advised to spend about 20 minutes on Questions 1-13 which refer to Reading Passage below.

Weathering in the Desert

In the deserts, as elsewhere, rocks at the earth’s surface are changed by weathering, which may be defined as the disintegration of rocks where they lie. Weathering processes are either chemical, when alteration of some of the constituent particles is involved; or mechanical, when there is merely the physical breaking apart and fragmentation of rocks. Which process will dominate depends primarily on the mineralogy and texture of the rock and the local climate, but several individual processes usually work together to the common end of rock disintegration.
The great daily changes in the temperature of deserts have long been supposed to be responsible for the disintegration of rocks, either by the differential heating of the various rock-forming minerals or by differential heating between the outer and inner parts of rock masses. However, both field observations and laboratory experiments have led to a reassessment of the importance of ’ exposure to the sun’s rays in desert weathering. Almost half a century ago Barton remarked that the buried parts of some of the ancient monuments in Egypt were more weathered than were those parts fully exposed to the sun’s rays, and attributed this to the effects of water absorption below the ground surface. Laboratory experiments have shown that rocks subjected to many cycles of large temperature oscillations (larger than those experienced in nature) display no evidence of fissuring or fragmentation, as a result. However, when marked fluctuations of temperature occur in moist conditions small rock fragments quickly form.
The expansive action of crystallizing salts is often alleged to exert sufficient force to disintegrate rocks. Few would dispute that this mechanism is capable of disrupting fissile or well-cleaved rocks or rocks already weakened by other weathering agencies; wood is splintered, terracotta tiles disintegrated and clays disturbed by the mechanism, but its importance when acting upon fresh and cohesive crystalline rocks remains uncertain.
Weathering achieves more than the disintegration of rocks, though this is its most important geomorphic effect. It causes specific landforms to develop. Many boulders possess a superficial hard layer of iron oxide and/or silica, substances that have migrated in solution from the inside of the block toward the surface. Not only is the exterior thus case-hardened but the depleted interior disintegrates easily. When weathering penetrates the shell the inside is rapidly attacked and only the hard outer layer remains to give hollowed or ‘tortoiseshell’ rocks.
Another superficial layer, the precise nature of which is little understood, is the well-known desert varnish or patina, a shiny coat on the surface of rocks and pebbles characteristic of arid environments. Some varnishes are colorless, others light brown, yet others so dark a brown as to be virtually black. Its origin is unknown but is significant, for it has been suggested that the varnish grows darker with the passage of time; obviously, before such a criterion could be used with confidence as a chronological tool its origin must be known with precision. Its formation is so slow that in Egypt, for example, it has been estimated that a light brown coating requires between 2,000 and 5,000 years to develop, and a fully formed blackish veneer between 20,000 and 50,000 years.
The development of relatively impermeable soil horizons that are subsequently exposed at the surface because of erosion of once overlying, easily eroded materials, which thus become surface crusts, is widespread in arid regions, although it is also known outside the deserts, and indeed many of the examples in arid lands probably originated in former periods of humid climate. The crusts prevent the waters of occasional torrential downpours from penetrating deeply into the soil, and thus they contribute to the rapid runoff associated with desert storms. Also, after erosion has cut through the crust and exposed underlying soil layers, the hard layer forms a resistant capping (duricrust) on plateaux and mesas, such as are common in many parts of arid and semi-arid Australia.
Some duricrust layers have been used as time markers for landforms and geological formations. The necessary conditions for this are that the crust forms fairly rapidly and that it is sufficiently distinct in appearance to preclude the possibility of confusion with other crusts formed at other times. The Barrilaco calcrete of Mexico for instance is believed to date from about 7,000 B.C. The main silcrete of the northern districts of South Australia is believed to date from the Lower Miocene, the laterite of northern Australia to be of the Lower or Middle Miocene age.

Questions 1-7

Reading Passage has seven sections, A-G.

Which paragraph contains the following information?

Write the appropriate letter, A-G, in boxes 1-7 on your answer sheet.

The idea that crystalline salts may not disintegrate solid rock as easily as other substances
The fact that daily temperature changes cause rocks to weather may not be as important as supposed
The regions where weathering creates a thick layer of earth that water cannot penetrate easily
The fact that weathering not only breaks down rocks, but also shapes the landscape
The idea of using impenetrable layers of earth to measure chronology
The two different kinds of weathering in rocks
The possibility of using the colour of the shiny surface on rocks to measure chronology

Questions 8-13

Do the following statements agree with the information given in the reading passage? In boxes 8-13 on your answer sheet, write

TRUE if the statement agrees with the information

FALSE if the statement contradicts the information

NOT GIVEN if there is no information on this.

Desert rocks can become weathered when there is a chemical reaction within the rock.
The parts of Egyptian monuments exposed to sunlight were found to be affected by the weather more than those below the ground.
Granite which has been subjected to huge temperature swings tends not to exhibit any signs of disintegration as a result.
It is estimated that dark patina originated between 2,000 and 5,000 years ago.
Because of surface crusts, water from torrential rains cannot be fully absorbed into the ground and as a result, causes run-offs in arid regions.
Duricrust layering is no longer used as an indicator of time because of the confusion with similar crusts.

Get our IELTS Reading Academic Test Guide with everything from tips, and strategies to Practice Tests for IELTS Academic Reading!