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Abstract
Regional relations and characteristics of the dark material as observed on photographs of the Taurus-Littrow region of the moon are reviewed to provide a background for interpretations of its nature and origin. The dark material seems to be a surficial deposit that covers mare and highland areas near the southeastern edge of the Serenitatis Basin. The age of the dark material, as deduced from photogeologic analysis, is ambiguous: contact relations near its western edge suggest that it is older than the central light basalts of Mare Serenitatis; evidence elsewhere indicates that it may be younger. The origin of the dark material is also uncertain, and the following alternate hypotheses are briefly considered: (1) thick regolith, (2) dark impact ejecta, (3) pyroclastic blanket, or (4) a material of different origin in different places.
Publication type | Conference Paper |
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Publication Subtype | Conference Paper |
Title | Photogeology of the dark material in the Taurus-Littrow region of the moon |
Volume | 1 |
Year Published | 1973 |
Language | English |
Publisher | Pergamon Press |
Contributing office(s) | Astrogeology Science Center |
Description | 14 p. |
Larger Work Type | Book |
Larger Work Subtype | Conference publication |
Larger Work Title | Proceedings, 4th Lunar Science Conference |
First page | 149 |
Last page | 162 |
Conference Title | Lunar Science Conference |
Conference Location | Houston, TX |
Conference Date | March 5-8, 1973 |
Google Analytic Metrics | Metrics page |