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- Q1054706 subject Q8846036.
- Q1054706 subject Q9014483.
- Q1054706 abstract "REDIRECT Template:Infobox feature on MarsThis is a redirect from a page that has been moved (renamed). This page was kept as a redirect to avoid breaking links, both internal and external, that may have been made to the old page name. For more information follow the bold category link. Ceraunius Tholus is a volcano on Mars located in the Tharsis quadrangle at 24.25° north latitude and 262.75° east longitude, part of the Uranius group of volcanoes. It is 130 km across, 5.5 km high and is named after a classical albedo feature name.It is generally believed to be a basaltic shield with the lower part buried beneath plain forming lavas. Earlier interpretations suggested that it is a stratovolcano. The slopes on Ceraunius Tholus are quite steep with an average slope of 8° with many radial erosion channels and pitted valleys extending from just below the rim of the caldera toward the base of the volcano. The current view is that the valleys were eroded by water. Interesting features on Ceraunius Tholus are three large canyons at the northwest flank of Ceraunius Tholus which are up to 2.5 km wide and 300 m deep. The biggest of these three also appears to be the youngest and protrude from the lowest point of the volcanic caldera and ends at the interesting crater Rahe (an oblique impact crater with measures of 35 × 18 km), just north from the volcano where it formed a depositional fan. Its origin is still debatable and there are four main models proposed: fluvial action, volcanic flows, valley being a lava channel or some combination of previously mentioned models.Ceraunius appears small compared to other larger volcanoes, but it is almost as tall as Earth's Mount Everest.The caldera of Ceranius Tholus is also dotted with many collapse pits, which are distinct from impact craters as they have no rim and vary in abundance across the caldera.Ceraunius Tholus is probably late Hesperian in age.".
- Q1054706 thumbnail Ceraunius_&_Uranius_tholi.jpg?width=300.
- Q1054706 wikiPageWikiLink Q101038.
- Q1054706 wikiPageWikiLink Q1036092.
- Q1054706 wikiPageWikiLink Q1108979.
- Q1054706 wikiPageWikiLink Q111.
- Q1054706 wikiPageWikiLink Q159954.
- Q1054706 wikiPageWikiLink Q169358.
- Q1054706 wikiPageWikiLink Q2030398.
- Q1054706 wikiPageWikiLink Q206300.
- Q1054706 wikiPageWikiLink Q207164.
- Q1054706 wikiPageWikiLink Q2170645.
- Q1054706 wikiPageWikiLink Q3054525.
- Q1054706 wikiPageWikiLink Q3117621.
- Q1054706 wikiPageWikiLink Q35666.
- Q1054706 wikiPageWikiLink Q391388.
- Q1054706 wikiPageWikiLink Q499164.
- Q1054706 wikiPageWikiLink Q513.
- Q1054706 wikiPageWikiLink Q520.
- Q1054706 wikiPageWikiLink Q5223552.
- Q1054706 wikiPageWikiLink Q6773157.
- Q1054706 wikiPageWikiLink Q6773158.
- Q1054706 wikiPageWikiLink Q7283348.
- Q1054706 wikiPageWikiLink Q735657.
- Q1054706 wikiPageWikiLink Q75520.
- Q1054706 wikiPageWikiLink Q8072.
- Q1054706 wikiPageWikiLink Q8846036.
- Q1054706 wikiPageWikiLink Q9014483.
- Q1054706 comment "REDIRECT Template:Infobox feature on MarsThis is a redirect from a page that has been moved (renamed). This page was kept as a redirect to avoid breaking links, both internal and external, that may have been made to the old page name. For more information follow the bold category link. Ceraunius Tholus is a volcano on Mars located in the Tharsis quadrangle at 24.25° north latitude and 262.75° east longitude, part of the Uranius group of volcanoes.".
- Q1054706 label "Ceraunius Tholus".
- Q1054706 depiction Ceraunius_&_Uranius_tholi.jpg.