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 | 1 |
How this entity was disambiguated
This entity first appeared as the object of triple T4885573 — resolving that mention is where its identity was fixed. The disambiguator weighed these candidate entities and picked the highlighted one (or “None”, minting a new entity). This is how homonymy is resolved: the same surface form can point to different entities.
NED1
Entity disambiguation (via context triple)
gpt-5-mini-2025-08-07
Target entity: Tithonium Chasma Context triple: [Valles Marineris, hasSubfeature, Tithonium Chasma]
-
A.
Ius Chasma
Ius Chasma is a large, steep-walled canyon on Mars that forms part of the vast Valles Marineris rift system.
-
B.
Ithaca Chasma
Ithaca Chasma is a vast, linear canyon system that nearly encircles Saturn’s moon Tethys and is one of the largest known chasms in the solar system.
-
C.
Ares Vallis
Ares Vallis is an ancient outflow channel on Mars, notable as a geologically diverse floodplain that was explored in situ by NASA’s Mars Pathfinder mission.
-
D.
Gale Crater
Gale Crater is a large impact crater on Mars that has been extensively explored for its layered geological history and past habitability clues.
-
E.
Noctis Labyrinthus
Noctis Labyrinthus is a geologically complex region of deep, intersecting valleys and collapsed terrain on Mars, located at the western end of the Valles Marineris canyon system.
- F. None of above. chosen
- G. Unsure - the case is ambiguous/there is not enough information to decide.
NED2
Entity disambiguation (via description)
gpt-5-mini-2025-08-07
Target entity: Tithonium Chasma Target entity description: Tithonium Chasma is a large, steep-walled canyon forming the northwestern segment of Mars’s vast Valles Marineris system.
-
A.
Ius Chasma
Ius Chasma is a large, steep-walled canyon on Mars that forms part of the vast Valles Marineris rift system.
-
B.
Ithaca Chasma
Ithaca Chasma is a vast, linear canyon system that nearly encircles Saturn’s moon Tethys and is one of the largest known chasms in the solar system.
-
C.
Ares Vallis
Ares Vallis is an ancient outflow channel on Mars, notable as a geologically diverse floodplain that was explored in situ by NASA’s Mars Pathfinder mission.
-
D.
Gale Crater
Gale Crater is a large impact crater on Mars that has been extensively explored for its layered geological history and past habitability clues.
-
E.
Noctis Labyrinthus
Noctis Labyrinthus is a geologically complex region of deep, intersecting valleys and collapsed terrain on Mars, located at the western end of the Valles Marineris canyon system.
- F. None of above. chosen
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 NERFINISHED ⓘ |
| 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 NERFINISHED ⓘ |
| 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
NERFINISHED
ⓘ
HRSC NERFINISHED ⓘ HiRISE NERFINISHED ⓘ THEMIS NERFINISHED ⓘ |
| isComponentOf | equatorial canyon system of Mars ⓘ |
| isMappedIn | USGS geologic maps of Mars NERFINISHED ⓘ |
| isNotableFor |
complex stratigraphy
ⓘ
evidence of long-term erosional processes ⓘ large vertical relief ⓘ |
| isTypeOf | tectonic trough ⓘ |
| locatedInQuadrangle | Phoenicis Lacus quadrangle NERFINISHED ⓘ |
| locatedOn | Mars NERFINISHED ⓘ |
| observedBy |
Mariner 9
NERFINISHED
ⓘ
Mars Express NERFINISHED ⓘ Mars Global Surveyor NERFINISHED ⓘ Mars Odyssey NERFINISHED ⓘ Mars Reconnaissance Orbiter NERFINISHED ⓘ Viking Orbiter NERFINISHED ⓘ |
| partOf | Valles Marineris NERFINISHED ⓘ |
How these facts were elicited
The pipeline generated the facts above by prompting gpt-5.1 with this entity's name + description and the instruction below.
Instruction
You are a knowledge base construction expert. Given a subject entity and a description of it, return factual statements that you know for the subject as a JSON list of dictionaries(triples), where keys must be "subject", "predicate" and "object". The number of facts may be very high, between 25 to 50 or more, for very popular subjects. For less popular subjects, the number of facts can be very low, like 5 or 10. # Requirements - If you don't know the subject at all, return an empty list. - If the subject is not a named entity, return an empty list. - Include at least one triple where predicate is "instanceOf". - Do not get too wordy. - Separate several objects into multiple triples with one object.
Input
Subject: Tithonium Chasma Description of subject: Tithonium Chasma is a large, steep-walled canyon forming the northwestern segment of Mars’s vast Valles Marineris system.
Referenced by (1)
Full triples — surface form annotated when it differs from this entity's canonical label.