Ielts reading question-type based tests true false not given matching headings



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aslanov

 
B.
Several factors cause the U.S.A. to experience a high incidence of tornado formation. While the 
continent reaches from arctic areas in the north to a tropical climate in the south there is no barrier protection 
from significant mountain ranges in the east or west; however, the Rocky Mountains in the middle latitudes 
of the country obstruct atmospheric flow and moisture. In addition, drier air from the southwest deserts and 
low level moisture from the Gulf of Mexico meet in the area, many collisions of warm and cool air occur 
and optimum conditions for tornado formation are created. Tornados in this central part of the U.S.A. are so 
prolific that the area has been named Tornado Alley, the site of the highest number of powerful tornados in 
the country and throughout the world. In the USA alone, in an average year 1200 tornados occur causing 70 
fatalities and 1500 injuries and in addition extensive damage to property and natural vegetation. 
 
C.
Connected between a cloud base above (usually cumulonimbus) and the earth below, a tornado is a 
rapidly rotating column of air; they can be as much as 20 kilometres in height. The majority are less than 75 
metres in diameter reaching wind speeds of less than 177kms per hour and travel less than 10 kilometres 
before dissipating; however, some of the larger and rarer of this type of weather phenomenon may reach 
wind speeds of more than 480kms/hour traveling more than 100 kilometers before cessation. The inside of a 
tornado is made up of descending air and this is surrounded by a spiraling upward current which has the 
ability to carry with it and destroy even substantial obstacles such as tress, cars and houses in its path. 
Scientific research and eyewitness accounts indicate that most tornados also possess a calm centre in their 
core, surrounded by the layers of the downward and upward currents of air; this core has been likened to the 
peaceful central ‘eye’ at the centre of a tropical cyclone or hurricane. 

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