IELTS Listening · Recent Actual Test 1 to 8
IELTS Recent Actual Test 3 - Part 4
If there is one natural feature which has long fascinated man, it is caves those natural underground spaces into which people can enter.
Level: C1 · 77 sentences
Transcript
- If there is one natural feature which has long fascinated man, it is caves
- those natural underground spaces into which people can enter.
- No known cave in the world can exist without it being extensively explored,
- whether it be in remote areas, such as the Clearwater Cave in Borneo,
- or immensely long and difficult, such as Mammoth Cave in America,
- or perhaps the most challenging: those caves below the water table, full with water,
- in which case the exploration is known as cave diving.
- Whatever the case, if the caves are known,
- as complex and difficult as they usually are, they will be explored.
- The formal name for the study of caves is speleology,
- and involves many disciplines, such as chemistry,
- geology, biology, and cartography,
- or the science of making accurate maps,
- since the largest caves can be hundreds of kilometers long and highly complicated.
- If the exploration is just for fun, the activity is known as caving,
- but with the difficulties and dangers involved,
- the average caver is often involved with one of these speleological sciences.
- As for the number of caves in the world,
- research suggests that only a fraction have been found and documented,
- mostly in the areas in which caving has long been a popular activity,
- such as in America, France, or Australia.
- China, for example, has huge areas of limestone bedrock,
- prime material for cave formation,
- and logically must contain among the largest number of caves in the world,
- yet only few are documented due to the lack of interest in caving there.
- Thus, as exploration continues, new caves will be discovered,
- and it is likely that the numbers could radically change in the future.
- With caves being such mysterious and intriguing places,
- the obvious question concerns how they form.
- The most common cause is the effect of slightly acidic water
- in a process called 'dissolution'.
- Here, water seeps into the ground, and down through rock masses.
- If this rock is soluble, the water dissolves some of it,
- and over time, the passage expands to become a cave, or cave system.
- The largest and most common of these involves limestone,
- although other materials are possible, including gypsum, marble, and even salt.
- Now, if the cave is formed at the same time as the rock, it is called a primary cave,
- and the most common of these are lava tubes.
- When lava from volcanoes flows downhill,
- the topmost surface cools and solidifies first,
- leaving the hotter lava to continue to flow beneath.
- If most of this eventually flows out, a hollow tube is left.
- The country Iceland, has some excellent caves of this type,
- and even far-flung Australia has a few.
- Finally, there are sea caves, formed from waves pounding into coastal cliffs,
- and eroding into fault lines, or softer rock.
- These caves are usually the shortest, about 50 meters at most,
- since the erosive action of the waves can only reach a certain distance.
- However, it is limestone caves which will always be the most interesting.
- This is due to the presence of limestone formations.
- As the groundwater seeps downward through the ceiling of the caves,
- it encounters a different pressure and temperature,
- causing it to deposit a small amount of its dissolved calcium carbonate.
- Over time, through the action of millions of drops,
- this deposition process results in ever-growing masses,
- known as stalactites (if hanging from the ceiling),
- or stalagmites (if growing from the floor).
- Alternatively, the water may flow over a large surface of rock, forming flowstone,
- and with other sorts of processes,
- can result in beautiful milky-white formations of astonishing complexity.
- One of the best examples of this,
- as well as of what surprising discoveries may yet await,
- is the Lechuguilla Cave in New Mexico.
- In the 1950s, some cavers heard the sound of wind underneath some large boulders on the cave floor,
- a clear sign of a deeper passageway.
- It took until 1984 for a group of cavers to gain permission to start digging,
- and two years later, in 1986,
- they broke through into a walkable passageway,
- unlocking one of the longest cave systems in the world,
- the deepest in America,
- and some of the most beautiful formations ever found.
- Unusually, many of these were yellow with sulphur,
- suggesting that the caves were a result of hydrogen-sulfide from nearby oil deposits.
- This was forced through fracture lines,
- combining with existing groundwater to form sulfuric acid,
- dissolving the limestone from the bottom up,
- instead of the normal top-down seepage which characterises most limestone cave formations.