closure of Iapetus Ocean

E87796

The closure of the Iapetus Ocean was a major Paleozoic tectonic event in which ancient continental plates converged, leading to the formation of mountain belts such as the Appalachians and Caledonides.

AI illustration

How this image was made

AI-generated illustration of closure of Iapetus Ocean

This AI-generated illustration was produced by black-forest-labs/FLUX.2-dev (1024x1024) from a prompt written by openai/gpt-oss-120b from the entity's label + description.

Prompt

Generate an image of closure of Iapetus Ocean (The closure of the Iapetus Ocean was a major Paleozoic tectonic event in which ancient continental plates converged, leading to the formation of mountain belts such as the Appalachians and Caledonides.)

All labels observed (3)

How this entity was disambiguated

Statements (49)

Predicate Object
instanceOf Paleozoic orogeny ⓘ
ocean closure ⓘ
tectonic event ⓘ
endTime Devonian Period ⓘ
middle Paleozoic ⓘ
followedBy assembly of Pangaea ⓘ
opening of Rheic Ocean ⓘ
follows opening of Iapetus Ocean ⓘ
geologicalContext Wilson cycle ⓘ
hasCause plate convergence ⓘ
subduction of oceanic lithosphere ⓘ
hasEffect collision of Laurentia and Avalonia ⓘ
collision of Laurentia and Baltica ⓘ
continental suturing ⓘ
crustal thickening ⓘ
deformation of passive margin sediments ⓘ
development of major suture zones ⓘ
formation of Appalachian Mountains ⓘ
formation of Caledonian Mountains ⓘ
formation of Euramerica ⓘ
formation of Grampian Highlands ⓘ
formation of Laurussia ⓘ
formation of Scandinavian Caledonides ⓘ
granite magmatism ⓘ
regional metamorphism ⓘ
involves Avalonia ⓘ
Baltica ⓘ
Laurentia ⓘ
microcontinents ⓘ
location present-day British Isles ⓘ
present-day Greenland ⓘ
present-day Scandinavia ⓘ
present-day eastern North America ⓘ
proto-Atlantic region ⓘ
occursIn Paleozoic Era ⓘ
partOf Acadian orogeny ⓘ
Appalachian orogeny ⓘ
Caledonian orogeny ⓘ
Grampian orogeny ⓘ
linked to: Caledonian orogeny

Taconic orogeny ⓘ
assembly of Euramerica ⓘ
assembly of Laurussia ⓘ
precededBy rifting of Rodinia margins ⓘ
startTime Ordovician Period ⓘ
early Paleozoic ⓘ
studiedIn metamorphic geology ⓘ
paleogeography ⓘ
structural geology ⓘ
tectonics ⓘ

How these facts were elicited

Referenced by (3)

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

Paleozoic Era → tectonicActivity → closure of Iapetus Ocean ⓘ
Greenland Caledonides → relatedTo → Iapetus Ocean closure ⓘ
linked to: closure of Iapetus Ocean
Walls Boundary Fault → formedDuring → closure of the Iapetus Ocean ⓘ
linked to: closure of Iapetus Ocean