isostasy

/aɪˈsɑstəsi/
noun
  1. The state of balance or equilibrium between parts of the Earth's crust, where lighter rock floats on denser rock below, like ice floating on water.
    • Isostasy explains why mountains have deep roots that extend into the mantle.
    • When a heavy glacier melts, the land slowly rises due to isostasy.
    • Geologists study isostasy to understand how continents stay stable over millions of years.
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