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Particularly complex and fine-scale features characterize the so-called karst morphologies formed by mineral dissolution into water. An archetypal type may be the high, thin, and sharply tipped karst peak or stone spire that seems in multitudes in striking landforms called rock woodlands, but whoever formative systems remain uncertain due to complex, fluctuating, and incompletely understood developmental conditions. Right here, we display that exceedingly razor-sharp spires a

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