Easter Island volcanic complex

E91194

The Easter Island volcanic complex is the geological formation comprising the island’s major volcanoes and related features that created and shape Rapa Nui (Easter Island).


Statements (48)
Predicate Object
instanceOf geological formation
volcanic complex
associatedWith Easter Seamount Chain
Easter microplate
composedOf alkali basalt
basaltic lava
hawaiite
tuff
country Chile
created Easter Island landmass
currentStatus dormant
eruptionStyle Strombolian eruptions
effusive eruptions
formedBy hotspot volcanism
intraplate volcanism
geologicalAge Holocene
Pleistocene
hasCrater Rano Kau caldera
Rano Raraku crater
hasFeature Poike peninsula
Rano Aroi crater lake
Rano Kau crater lake
Rano Raraku tuff cone
Terevaka shield volcano
lava flows
numerous scoria cones
pyroclastic deposits
tuff cones
hasMainComponent Poike volcano
Rano Kau volcano
Terevaka volcano
highestPoint Terevaka summit
influences coastal morphology of Easter Island
groundwater distribution on Easter Island
soil formation on Easter Island
lastMajorActivity Holocene epoch
locatedIn Chile
Easter Island
Pacific Ocean
Rapa Nui
maximumElevation about 507 metres above sea level
partOf Easter hotspot
Nazca Plate
region Southeastern Pacific Ocean
shapes topography of Easter Island
studiedInDiscipline geology
volcanology
tectonicSetting Nazca Plate oceanic crust

Referenced by (5)
Subject (surface form when different) Predicate
Easter hotspot ("Easter Island volcanic province")
associatedWith
Poike Peninsula
isPartOfVolcanicSystem
Maunga Terevaka
isVolcanoOf
Rano Aroi
partOf
Terevaka
volcanicField

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