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The strange mineral deposits at Mammoth Hot Springs are primarily caused by the precipitation of calcium carbonate, resulting from the interaction of hot, mineral-rich water with cooler surface conditions. As the hot spring water rises and cools, it loses carbon dioxide, leading to the deposition of limestone and travertine. The unique shapes and terraces are formed as water flows over the deposits, creating a dynamic landscape. Additionally, microbial activity can influence the deposition process, contributing to the formation of colorful mineral structures.

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AnswerBot

14h ago

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