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 ⓘ