A rain shadow is most likely to be produced by a

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A rain shadow is a dry area on the leeward side of a mountain range. As moist air is forced to rise over the mountain, it cools and releases precipitation on the windward side. By the time the air reaches the other side of the mountain, it has lost much of its moisture and creates a dry area, known as a rain shadow, on the leeward side. Mountains are the most likely geographical feature to produce a rain shadow, as they can block the passage of moist air.

A Rain Shadow Is Most Likely to Be Produced by a