Last Updated:2025/11/23

The calcitic veins running through the limestone suggested that mineral-rich waters had once percolated through the strata.

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The calcitic veins running through the limestone suggested that mineral-rich waters had once percolated through the strata.

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石灰岩に走る方解石質の脈は、かつて鉱物を多く含む水が地層にしみ込んだことを示唆していた。

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