Tithonium Chasma

E480819

Tithonium Chasma is a large, steep-walled canyon forming the northwestern segment of Mars’s vast Valles Marineris system.

All labels observed (1)

Label Occurrences
Tithonium Chasma canonical 3

How this entity was disambiguated

Statements (46)

Predicate Object
instanceOf canyon
chasma
surface feature on Mars
boundedBy Ius Chasma to the south
Noctis Labyrinthus region to the west
central Valles Marineris chasmata to the east
formsSegmentOf northwestern Valles Marineris
hasEvidenceOf faulting
landslides
possible ancient water-related processes
hasFloorFeature chaotic terrain
landslide deposits
layered deposits
hasFormationProcess tectonic extension
hasGeologicAge primarily Hesperian
hasLaterModificationAge Amazonian
hasLength approximately 800 km
hasMaximumDepth approximately 6 km
hasNameApprovedBy International Astronomical Union
hasNameLanguageOrigin Latin
hasOrientation generally east–west
hasSurfaceMaterial basaltic rocks
dust
layered sedimentary deposits
hasWallCharacteristic steep-walled
hasWallFeature mass-wasting scars
spur-and-gully morphology
imagedByInstrument CTX
HRSC
HiRISE
linked to: HiRISE instrument

THEMIS
linked to: THEMIS instrument
isComponentOf equatorial canyon system of Mars
isMappedIn USGS geologic maps of Mars
isNotableFor complex stratigraphy
evidence of long-term erosional processes
large vertical relief
isTypeOf tectonic trough
locatedInQuadrangle Phoenicis Lacus quadrangle
locatedOn Mars
observedBy Mariner 9
Mars Express
Mars Global Surveyor
Mars Odyssey
Mars Reconnaissance Orbiter
Viking Orbiter
partOf Valles Marineris

How these facts were elicited

Referenced by (3)

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

Valles Marineris hasSubfeature Tithonium Chasma
Ophir Chasma connectedTo Tithonium Chasma
Ius Chasma adjacentTo Tithonium Chasma