The answer is B. The theory of isostatic equilibrium is used to explain the vertical height of a particular point on the earth such as the Himalayas. This theory is very similar to the principle of buoyancy. The mantle, in this case, is the liquid being displaced by the crust above. To accommodate great pressures such as those exerted by the Himalayas, the mantle distributes the force by height adjustments.
<span>b. higher elevation</span><span>
The climate on the leeward side of a mountain differs from that on the windward side mostly in the amount of rainfall. So the correct option is option "d" in regards to the question that has been given. The climatic condition of the windward side of the mountain is always like an ocean climatic condition while the leeward side has a very dry climate. The air on the windward side rises and gets cold and thus forms precipitation. On the other hand the air comes down on the leeward side and becomes warm and results in a drier climatic condition. </span>
The correct answer, is the landscape is highly varied.
Pretty sure its c. From the text you provided me
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