epirogeny

/ˌɛpɪˈrɑdʒəni/
noun
  1. The large-scale, slow upward or downward movement of the Earth's crust, affecting broad regions rather than narrow belts.
    • Geologists study epirogeny to understand how continents have risen and fallen over millions of years.
    • The gradual epirogeny of the region created the flat, elevated landscape we see today.
    • Epirogeny explains why ancient seafloor fossils are now found on high plateaus.
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