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| ˇ |
Low pH
water (acidic) encourages
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carbonates to
dissolve, silica can then be
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mobilized and
deposited over time in
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spaces left by
the dissolved carbonates
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Water pitting
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Un-replaced
patches of carbonate
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minerals and
elements (calcium - Ca,
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magnesium- Mg)
can also be seen in
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cherts– should
appear chemically
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weathered.
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