
Psychometric Verbal Comprehension Test #5
Authored by Rodney Hall
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Professional Development
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24 questions
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1.
MULTIPLE CHOICE QUESTION
2 mins • 1 pt
Read through each passage carefully to answer the following TRUE,FALSE and CAN'T SAY Questions.
True- The statement is TRUE from information in passage
False - The statement is FALSE from information in passage
Can't Say- There is insufficient information to state True or False
Passage 1:
There are seven species of deer living wild in Britain. The Red Deer and the Roe Deer are native species. Fallow Deer were introduced by the Romans and, since the seventeenth century, have been joined by three other non-native species; Sika, Muntjac and Chinese Water Deer the ancestors of which have escaped from parks. In addition, a heard of Reindeer was established in Scotland in 1952. Most of the Red Deer in Britain are found in Scotland, but there are significant wild populations in south-west and north-west England. East Anglia and north Midlands. Red Deer can interbreed with the introduced Japanese Sika deer and in some areas, hybrids are common.
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2.
MULTIPLE CHOICE QUESTION
20 sec • 1 pt
1) All of the Red Deer in Britain are found in Scotland.
True
False
Can't Say
3.
MULTIPLE CHOICE QUESTION
20 sec • 1 pt
2) Red deer can interbreed with Fallow Deer.
True
False
Can't Say
4.
MULTIPLE CHOICE QUESTION
20 sec • 1 pt
3) The Fallow Deer is not native to Britain.
True
False
Can't Say
5.
MULTIPLE CHOICE QUESTION
20 sec • 1 pt
4) There are no Reindeer in England
True
False
Can't Say
6.
MULTIPLE CHOICE QUESTION
20 sec • 1 pt
5) All of the Muntjac in England have escaped from parks
True
False
Can't Say
7.
MULTIPLE CHOICE QUESTION
2 mins • Ungraded
Passage 2:
Glaciers begin to form where snow remains year-round and enough of it accumulates to transform into ice. New layers of snow compress the previous layers and this compression forces the icy snow to re- crystallize, forming grains similar in size and shape to cane sugar. Gradually the grains grow larger and the air pockets between the grains get smaller, meaning that the snow slowly becomes more dense. After about two winters, the snow turns into firn, an intermediate state between snow and ice. Over time the larger ice crystals become more compressed and even denser, this is known as glacial ice. Glacial ice, because of it's density and ice crystals, often takes a bluish or even green hue.
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