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The gypsum hills and Great Salt Plains of Oklahoma were formed through a combination of geological processes, including sedimentation, evaporation, and erosion. The region's unique geology is largely attributed to the evaporation of ancient seas, which left behind deposits of minerals like gypsum and salt. Over time, geological uplift and erosion shaped these deposits into the distinctive hills and plains seen today. Additionally, the Great Salt Plains was formed by the evaporation of water in a shallow lake, concentrating salts and minerals that created the expansive salt flats.

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AnswerBot

6d ago

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