World Geography The traditional lands of the nomads of Central Asia are Mongolia and Tibet Sinkiang and Turkistan Kirghiz steppe All of these Mongolia and Tibet Sinkiang and Turkistan Kirghiz steppe All of these ANSWER DOWNLOAD EXAMIANS APP
World Geography The most notable example of a tectonic valley is that of the Doon valley plains of Aksai Chin Kashmir valley None of these Doon valley plains of Aksai Chin Kashmir valley None of these ANSWER DOWNLOAD EXAMIANS APP
World Geography The major crops found in Sudan are rice, barley, bananas, cocoa wool, wine, jute maize, cotton, bananas, groundnut bajra, oats, tobacco rice, barley, bananas, cocoa wool, wine, jute maize, cotton, bananas, groundnut bajra, oats, tobacco ANSWER DOWNLOAD EXAMIANS APP
World Geography Cocos plate lies between: South America and Pacific Plate. North America and Pacific Plate. None of these Central America and Pacific Plate. South America and Pacific Plate. North America and Pacific Plate. None of these Central America and Pacific Plate. ANSWER DOWNLOAD EXAMIANS APP
World Geography The smallest annual temperature range occurs in the subtropical climate zone polar climate zone temperate climate zone equatorial tropical climate zone subtropical climate zone polar climate zone temperate climate zone equatorial tropical climate zone ANSWER DOWNLOAD EXAMIANS APP
World Geography Which among the following statements is not correct about Plunge pool? They occur at the mature stage of the river development It is a deep depression in a stream bed at the base of a waterfall It is created by the erosional forces of cascading water They are often very deep, generally related to the height of fall and the volume of water, They occur at the mature stage of the river development It is a deep depression in a stream bed at the base of a waterfall It is created by the erosional forces of cascading water They are often very deep, generally related to the height of fall and the volume of water, ANSWER EXPLANATION DOWNLOAD EXAMIANS APP Plunge pool or waterfall lake is a deep depression in the stream bed at the base of the waterfall. It is created by the erosional force of the cascading water. They occur at the youthful stage of the river development.
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