Evaluating the Depth–Age Hypothesis for the Evolution of the Lunar Regolith

Lunar regolith is the fractured rock layer covering most of the lunar surface. This rock is fractured into regolith primarily by repeated meteorite impacts over eons. The depth of the regolith is determined by the maximum depth reworked by impactors. Older surfaces are expected to have thicker regol...

Full description

Bibliographic Details
Published in:The Planetary Science Journal
Main Author: Gwendolyn D. Bart
Format: Article
Language:English
Published: IOP Publishing 2025-01-01
Subjects:
Online Access:https://doi.org/10.3847/PSJ/ada24e