Particle.news

Study Reconstructs South Pole–Aitken Impact, Points to Mantle Debris Near Artemis Landing Zone

Simulations indicate a 260-kilometer layered impactor at about 13 km/s shaped the basin, leaving mantle material downrange.

Overview

  • A new peer-reviewed paper in Science Advances uses high-resolution 3D models to reproduce the South Pole–Aitken basin’s unusual, tapered shape.
  • The best match involves a differentiated impactor about 260 kilometers wide striking from north to south at a shallow angle near 30 degrees.
  • The modeled impact speed of roughly 13 km/s fits the basin’s form and helps explain its asymmetric interior uplift.
  • The simulations predict a butterfly-like ejecta pattern with mantle material about 550 km beyond the rim downrange and about 650 km cross-range, with little uprange.
  • Because NASA plans to land Artemis III near the lunar south pole, the team says astronauts could encounter mantle-bearing ejecta there, though only returned samples can confirm the model and its hint that the impactor came from the early Mars zone.