Abstract

Mass wasting, as one of the most significant geomorphological processes, contributes immensely to planetary landscape evolution. The frequency and diversity of mass wasting features on any planetary body also put engineering constraints on its robotic exploration. Mass wasting on other Solar System bodies shares similar, although not identical, morphological characteristics with its terrestrial counterpart, indicating a possible common nature for their formation. Thus, planetary bodies with contrasting environmental conditions might help reveal the effects of the atmosphere, subsurface fluids, mass accumulation/precipitation, and seismicity on mass wasting, and vice versa. Their relative positions within our Solar System and the environmental and geophysical conditions on the Moon and the dwarf planet Ceres are not only extremely different from Earth’s but from each other too. Their smaller sizes coupled with the availability of global-scale remote sensing datasets make them ideal candidates to understand mass wasting processes in widely contrasting planetary environments. Through this concept article, we highlight several recent advances in and prospects of using remote sensing datasets to reveal unprecedented details on lunar and Cerean mass wasting processes. We start with briefly discussing several recent studies on mass wasting using Lunar Reconnaissance Orbiter Camera (LROC) data for the Moon and Dawn spacecraft data for Ceres. We further identify the prospects of available remote sensing data in advancing our understanding of mass wasting processes under reduced gravity and in a scant (or absent) atmosphere, and we conclude the article by suggesting future research directions.

Highlights

  • Accepted: 18 February 2022Mass wasting or mass movement is bulk downslope movement of rock debris and/or regolith under the influence of gravity [1,2]

  • We further identify the prospects of available remote sensing data in advancing our understanding of mass wasting processes under reduced gravity and in a scant atmosphere, and we conclude the article by suggesting future research directions

  • The focus shifted to exploring the lunar mass wasting processes after the launch of the Lunar Reconnaissance Orbiter Camera (LROC) in 2009

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Summary

Introduction

Mass wasting or mass movement is bulk downslope movement of rock debris and/or regolith under the influence of gravity [1,2]. Characterization and comparison of mass mass wasting features, themovement mass movement type and size, and theirdistribution global diswasting features, based based on the on mass type and size, and their global tribution on a planetary body can help us understand the local physical and environmenon a planetary body can help us understand the local physical and environmental conditions tal on surface/subsurface. Figure shows one such of distribution on conditions surface/subsurface [15].

Spatial
Lunar Mass Wasting Processes
Status of Our Understanding
Schematic
Stratigraphic
Prospects
Cerean Periglacial Landforms and Mass Wasting Processes
Conclusions
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