Question 22 • PARTA - EVP: PGCPS BIOGEOCHEM CR (FALL2026) - 798113
Earth’s outer core is made mostly of iron and nickel, and its temperature is high enough to melt this alloy. The inner core stays solid despite being hotter because the pressure there is much greater. A tarry consistency and lower density do not explain why the outer core is liquid, while extreme pressure tends to raise the melting point.
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