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Which outcome results when silicate mineral weathering uptakes atmospheric CO2?

A)Decreased runoff acidity levels
B)Oceanic crust subduction rates
C)Increased hydrothermal vent formation
D)Enhanced glacial ice formation

💡 Explanation

Decreased runoff acidity occurs, because silicate weathering drives chemical reactions bonding CO2 into stable compounds thereby consuming hydrogen ions reducing acidity, rather than altering subduction/vent rates; glacial formation varies by insolation.

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