Ceraunius Tholus

E494852

Ceraunius Tholus is a medium-sized, ancient Martian volcano characterized by heavily eroded flanks and complex channels, located in the Tharsis volcanic region.

Jump to: Statements Referenced by

Statements (46)

Predicate Object
instanceOf Martian volcano
astrogeological feature
discoveredBy Mariner 9 imaging
erosionState more eroded than younger Tharsis volcanoes
eruptiveHistory multiple eruptive episodes inferred from overlapping flows
hasAge Noachian to early Hesperian
hasCalderaDiameter approximately 25 km
hasDiameter approximately 130 km
hasEponym Ceraunii Mountains NERFINISHED
hasFeature complex channel systems
fan-shaped deposits at flank bases
lava flow deposits
possible pyroclastic deposits
summit caldera complex
hasHeight approximately 5 km
hasLatitude approximately 24°N
hasLongitude approximately 262°E
hasMorphology asymmetric flank erosion
deeply incised canyons
heavily eroded flanks
radial valleys and channels
hasNearbyFeature Alba Mons NERFINISHED
Tharsis Montes NERFINISHED
Uranius Mons NERFINISHED
Uranius Tholus NERFINISHED
hasRelativeSize medium-sized compared to other Tharsis volcanoes
hasSummitCaldera true
imagedBy Mars Express NERFINISHED
Mars Global Surveyor NERFINISHED
Mars Reconnaissance Orbiter NERFINISHED
Viking Orbiter NERFINISHED
interpretedAs ancient, inactive volcano
locatedIn Tharsis region NERFINISHED
Tharsis volcanic province NERFINISHED
locatedInQuadrangle Tharsis quadrangle NERFINISHED
locatedOn Mars NERFINISHED
nameLanguage Latin
partOf Tharsis volcanic rise NERFINISHED
showsEvidenceOf fluvial modification
groundwater sapping channels
long-lived erosion
possible glacial or periglacial processes
studiedInDiscipline planetary geology
volcanology
surfaceComposition basaltic lava
volcanicActivityType effusive volcanism

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

Tharsis volcanic plateau contains Ceraunius Tholus