Sinuous Rilles
Sinuous Rilles is a type of lunar channel morphology characterized by its winding, river-like path and associated with ancient volcanic activity, distinguished from other impact-related or tectonic landforms by its curvilinear geometry and formation through the flow of low-viscosity lava in collapsed lava tubes or surface channels.
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2017–2026
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Possible lunar lava tube skylight observed by SELENE cameras
J. Haruyama, K. Hioki, Motomaro Shirao et al. · Geophysical Research Letters · 2009 · 208 citations
Turbulent lava flow and the formation of lunar sinuous rilles.
G. Hulme · 1973 · 138 citations
Clementine Observations of the Aristarchus Region of the Moon
A. S. McEwen, M. S. Robinson, E. M. Eliason et al. · Science · 1994 · 113 citations
R. A. Yingst, J. W. Head · Journal of Geophysical Research Atmospheres · 1997 · 73 citations · Full text
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Brown University
Providence, United States
5 h-index
8 publications
790 citations

University of Hawaii System
Honolulu, United States
4 h-index
6 publications
337 citations
Arizona State University
Tempe, United States
3 h-index
6 publications
282 citations
Planetary Science Institute
Tucson, United States
3 h-index
8 publications
288 citations

Lunar and Planetary Institute
Houston, United States
3 h-index
3 publications
194 citations
China University of Geosciences
Wuhan, China
3 h-index
14 publications
261 citations
Lancaster University
Lancaster, United Kingdom
3 h-index
3 publications
165 citations
University of California, Los Angeles
Los Angeles, United States
3 h-index
7 publications
264 citations
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JGR · 7 publications · 281 citations
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Conference · 4 publications · 126 citations
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3 publications · 301 citations
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2 publications · 44 citations
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