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 sevenstage meteorological process that generates a rainshadow desert, a landscape forming over an expanse spanning thousands of kilometres from the coast. Overall, the formation of rainshadow deserts is a linear sevenstage process, which can be broadly divided into two major phases.
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The diagram depicts the sevenstage meteorological process that generates a rainshadow desert, a landscape forming over an expanse spanning thousands of kilometres from the coast. Overall, the formation of rainshadow deserts is a linear sevenstage process, which can be broadly divided into two major phases.
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The diagram depicts the seven‑stage meteorological process that generates a rain‑shadow desert, a landscape forming over an expanse spanning thousands of kilometres 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, 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 diagram below gives the information about the Hawaiian island chain in the centre of the Pacific Ocean.
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