The diagram below shows how one type of desert, known as a rain-shadow desert, is formed.

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The diagram depicts the seven‑step geological process that generates a rain‑shadow desert, a landscape that stretches thousands of kilometres inland from the coast. Overall, the formation of rain‑shadow deserts is a linear seven‑stage process, which can be broadly divided into two major phases.

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The diagram depicts the seven‑step geological process that generates a rain‑shadow desert, a landscape that stretches thousands of kilometres inland from the coast. Overall, rain‑shadow deserts originate when sea‑borne moist winds encounter a mountain barrier.

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The flow chart illustrates the seven-step process through which a particular desert type develops, known as a rain-shadow desert. Overall, the formation of this desert involves seven sequential stages.

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The diagram illustrates the process by which a rain-shadow desert is created on the inland side of a mountain range. Overall, moist winds from the sea rise over mountains and lose their moisture as rain on the windward side.

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The diagram illustrates the process by which a rain-shadow desert is created on the inland side of a mountain range. Overall, the mountains cause wet air from the sea to rise, cool and produce rain on the windward side.