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- Q3926565 subject Q8624735.
- Q3926565 subject Q8624745.
- Q3926565 abstract "The Michelangelo quadrangle is in the southern hemisphere of the planet Mercury, where the imaged part is heavily cratered terrain that has been strongly influenced by the presence of multiring basins. At least four such basins, now nearly obliterated, have largely controlled the distribution of plains materials and structural trends in the map area. Many craters, interpreted to be of impact origin, display a spectrum of modification styles and degradation states. The interaction between basins, craters, and plains in this quadrangle provides important clues to geologic processes that have formed the morphology of the mercurian surface.Several low-albedo features are evident in Earth-based views of the Michelangelo quadrangle, but these features do not appear to correlate directly with any mapped terrain unit. Solitudo Promethei may correspond to a deposit of plains materials centered at –58°, 135°, and Solitudo Martis may correspond to similar materials at –30° to –40°, 90° to 100°. The color data (orange/ultraviolet) presented in Hapke and others (1980) likewise show no particular correlation with mapped terrain types. The “yellow” region (moderately high orange/ultraviolet) centered at –33°, 155° appears to correspond to a smooth plains deposit, but the region overlaps into adjacent cratered terrain.Mariner 10 data include complete photographic coverage of the quadrangle at a resolution of about 2 km. In addition, twelve stereopairs cover scattered areas in the quadrangle; these photographs were used to supplement the geologic interpretation. About 10° of longitude of the H-13 quadrangle (Solitudo Persephones Province) adjacent to the west is included in the map area because not enough Mariner 10 data were acquired of this quadrangle to justify the production of another map.".
- Q3926565 thumbnail Mercury_h12_Michelangelo_quadrangle.png?width=300.
- Q3926565 wikiPageExternalLink h12.pdf.
- Q3926565 wikiPageWikiLink Q101038.
- Q3926565 wikiPageWikiLink Q1027437.
- Q3926565 wikiPageWikiLink Q1061151.
- Q3926565 wikiPageWikiLink Q106551.
- Q3926565 wikiPageWikiLink Q1072625.
- Q3926565 wikiPageWikiLink Q111.
- Q3926565 wikiPageWikiLink Q1174791.
- Q3926565 wikiPageWikiLink Q1321876.
- Q3926565 wikiPageWikiLink Q1408928.
- Q3926565 wikiPageWikiLink Q180874.
- Q3926565 wikiPageWikiLink Q191250.
- Q3926565 wikiPageWikiLink Q193343.
- Q3926565 wikiPageWikiLink Q212136.
- Q3926565 wikiPageWikiLink Q2407149.
- Q3926565 wikiPageWikiLink Q308.
- Q3926565 wikiPageWikiLink Q35158.
- Q3926565 wikiPageWikiLink Q3649494.
- Q3926565 wikiPageWikiLink Q3696612.
- Q3926565 wikiPageWikiLink Q3696617.
- Q3926565 wikiPageWikiLink Q3696678.
- Q3926565 wikiPageWikiLink Q3834281.
- Q3926565 wikiPageWikiLink Q3926567.
- Q3926565 wikiPageWikiLink Q3926569.
- Q3926565 wikiPageWikiLink Q405.
- Q3926565 wikiPageWikiLink Q48666.
- Q3926565 wikiPageWikiLink Q487895.
- Q3926565 wikiPageWikiLink Q488143.
- Q3926565 wikiPageWikiLink Q496325.
- Q3926565 wikiPageWikiLink Q498794.
- Q3926565 wikiPageWikiLink Q5023667.
- Q3926565 wikiPageWikiLink Q513110.
- Q3926565 wikiPageWikiLink Q529969.
- Q3926565 wikiPageWikiLink Q55818.
- Q3926565 wikiPageWikiLink Q5742728.
- Q3926565 wikiPageWikiLink Q59131.
- Q3926565 wikiPageWikiLink Q667575.
- Q3926565 wikiPageWikiLink Q8624735.
- Q3926565 wikiPageWikiLink Q8624745.
- Q3926565 comment "The Michelangelo quadrangle is in the southern hemisphere of the planet Mercury, where the imaged part is heavily cratered terrain that has been strongly influenced by the presence of multiring basins. At least four such basins, now nearly obliterated, have largely controlled the distribution of plains materials and structural trends in the map area. Many craters, interpreted to be of impact origin, display a spectrum of modification styles and degradation states.".
- Q3926565 label "Michelangelo quadrangle".
- Q3926565 depiction Mercury_h12_Michelangelo_quadrangle.png.