Research news on regolith

Regolith is the unconsolidated, heterogeneous layer of fragmented mineral and rock material that overlies coherent bedrock on planetary surfaces, including Earth, the Moon, Mars, asteroids, and other solid bodies. As a substance, it comprises varying proportions of rock fragments, mineral grains, dust, ice, and, on some planets, secondary alteration products such as clays or salts. Regolith forms primarily through mechanical and chemical weathering, impact comminution, and volcanic or sedimentary processes, and its physical properties—such as grain size distribution, porosity, cohesion, and volatile content—critically influence surface-atmosphere interactions, geotechnical behavior, resource potential, and the performance of in situ exploration and construction activities.

Reading the moon's buried past

The lunar south pole looks chaotic from orbit. Craters heaped upon craters, ancient basins, scarps and slopes tumbling in every direction, it is without doubt, one of the most geologically complicated terrains in the inner ...

ShadowCam search casts doubt on abundant lunar ice

New observations by a team of US astronomers have cast fresh doubt on whether the lunar surface could host abundant water ice. Publishing their results in Science Advances, a team led by Shuai Li at the University of Hawaii ...

page 1 from 6