Almannagjá fault

E267079

Almannagjá fault is a prominent rift valley fissure in southwestern Iceland that marks the boundary between the North American and Eurasian tectonic plates.

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All labels observed (2)

Label Occurrences
Almannagjá fault canonical 1
Davíðsgjá fissure 1

Statements (43)

Predicate Object
instanceOf geological fault
rift valley fissure
tourist attraction
country Iceland
formedBy extensional tectonics
plate tectonics
geologicalFeatureType normal fault
hasAccessibility marked trails
road access
hasCliffs yes
hasGeologicalAge Holocene
hasRockType basalt
lava flows
hasSignificance clear surface expression of plate boundary
hasWalkingPath yes
isExampleOf continental rift
isMajorStructureIn Þingvellir National Park
surface form: Þingvellir National Park landscape
isPhotogenic true
isStudiedBy geologists
geophysicists
isVisibleAtSurface true
languageOfName Icelandic
locatedIn Southwest Iceland
Þingvellir National Park
surface form: Þingvellir

Þingvellir National Park
locatedOn Reykjanes Peninsula
marksBoundaryBetween Eurasian Plate
North American Plate
movementType divergent plate boundary
nameMeaning Allmannajuvet gorge
surface form: All-men’s gorge
near Þingvallavatn
orientation north–south
partOf Þingvellir National Park
surface form: Þingvellir rift valley
region South Coast of Iceland
surface form: Southern Region of Iceland
relatedTo Mid-Atlantic Ridge
surface form: Mid-Atlantic Ridge in Iceland

Þingvellir National Park
surface form: Þingvellir graben
separates Eurasian Plate
North American Plate
tectonicSetting Mid-Atlantic Ridge
UNESCOWorldHeritageContext part of Þingvellir World Heritage Site
usedFor geological education
geotourism
withinProtectedArea Þingvellir National Park

Referenced by (2)

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

Þingvallavatn hasDiveSite Almannagjá fault
this entity surface form: Davíðsgjá fissure