Recent studies employing satellite data and ground-based measurements have revealed that a massive gravity anomaly beneath the icy expanse of Antarctica is not only persistent but appears to be intensifying. This unexpected development has sent ripples through the geoscience community, as it challenges long-held assumptions about the stability and composition of Earth’s lower mantle in this remote region. Scientists speculate that the anomaly could be linked to unusual density variations caused by either unknown geological structures or dynamic processes occurring deep within the planet’s interior.

Key aspects under investigation include:

  • Variations in mantle convection patterns potentially driving the increased gravitational intensity.
  • The possible presence of dense, ultra-mafic rock formations or large-scale mineral phase transitions.
  • Implications for Antarctica’s tectonic history and its impact on global geodynamics.
Parameter Measurement Previous Data
Gravity Anomaly Strength +45 mGal +37 mGal (5 years ago)
Depth Extent Up to 400 km Approx. 350 km
Estimated Density Contrast 0.25 g/cm³ 0.18 g/cm³