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Easter Island, Ísla de Pascua Province, Valparaíso, Chilei
Regional Level Types
Easter IslandIsland
Ísla de Pascua ProvinceProvince
ValparaísoRegion
ChileCountry

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PhotosMapsSearch
Type:
Age:
0.94 to 0.11 Ma
Geologic Time:
Dating method:
K-Ar; Ar/Ar
Reference for age:
Vezzoli, L., and Acocella, V. (2009) Easter Island, SE Pacific: An end-member type of hotspot volcanism. Geological Society of America Bulletin, 121, 869–886, doi: 10.1130/B26470.1. doi.org/10.1130/B26470.1
Largest Settlements:
PlacePopulation
Hanga Roa3,304 (2018)
Mindat Locality ID:
105854
Long-form identifier:
mindat:1:2:105854:6
GUID (UUID V4):
5a3a2ba4-1472-461b-a3dc-3c2030e032ed
Other/historical names associated with this locality:
Rapa Nui
Other Languages:
French:
Île de Pâques (Rapa Nui), Région de Valparaíso, Chili
German:
Osterinsel (Rapa Nui), Región de Valparaíso, Chile
Italian:
Isola di Pasqua (Rapa Nui), Regione di Valparaíso, Cile
Russian:
Остров Пасхи (Рапануи; Рапа-Нуи), Вальпараисо, Чили
Spanish:
Ísla de Pascua (Rapa Nui), Región de Valparaíso, Chile


Island composed of Pliocene to Holocene basaltic and andesitic lava flows, scoria, tuff, obsidian, located above a mantle plume "hot spot" on the Nazca plate. The island owes its roughly triangular shape to the stratovolcanoes Poike, Rano Kau, and Terevaka.

Mafic lava flows are the most abundant rock type on the island; they built up the three main stratovolcanoes and formed most of the island’s coastline. The pyroclastic products consist of loose cinder and scoria deposits that, in some peculiar emplacement conditions, gave rise to coherent rocks. One example is the Puna Pao scoriae cone, in which the scoriae are welded as a result of their rheological behaviour during the eruption. Other examples are the Rano Raraku and Maunga Toa Toa tuff cones, which were partly emplaced in subaqueous conditions.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


5 valid minerals.

Rock Types Recorded

Note: data is currently VERY limited. Please bear with us while we work towards adding this information!

Select Rock List Type

Alphabetical List Tree Diagram

Detailed Mineral List:

Aegirine-augite
Formula: (NaaCabFe2+cMgd)(Fe3+eAlfFe2+gMgh)Si2O6
References:
Albite
Formula: Na(AlSi3O8)
References:
Albite var. Anorthoclase
Formula: (Na,K)AlSi3O8
References:
'Amphibole Supergroup'
Formula: AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
References:
'Apatite'
Formula: Ca5(PO4)3(Cl/F/OH)
Augite
Formula: (CaxMgyFez)(Mgy1Fez1)Si2O6
'Clinopyroxene Subgroup'
References:
Fayalite
Formula: Fe2+2SiO4
References:
'Fayalite-Forsterite Series'
References:
'Feldspar Group'
References:
'Glass'
Ilmenite
Formula: Fe2+TiO3
'Palagonite'
'Plagioclase'
Formula: (Na,Ca)[(Si,Al)AlSi2]O8
'Pyroxene Group'
Formula: ADSi2O6
References:
'Smectite Group'
Formula: A0.3D2-3[T4O10]Z2 · nH2O
'Zeolite Group'

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
Ilmenite4.CB.05Fe2+TiO3
Group 9 - Silicates
Fayalite9.AC.05Fe2+2SiO4
Augite9.DA.15(CaxMgyFez)(Mgy1Fez1)Si2O6
Aegirine-augite9.DA.20(NaaCabFe2+cMgd)(Fe3+eAlfFe2+gMgh)Si2O6
Albite9.FA.35Na(AlSi3O8)
var. Anorthoclase9.FA.35(Na,K)AlSi3O8
'Zeolite Group'9.G0.
Unclassified
'Feldspar Group'-
'Amphibole Supergroup'-AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
'Clinopyroxene Subgroup'-
'Fayalite-Forsterite Series'-
'Plagioclase'-(Na,Ca)[(Si,Al)AlSi2]O8
'Pyroxene Group'-ADSi2O6
'Smectite Group'-A0.3D2-3[T4O10]Z2 · nH2O
'Glass'-
'Apatite'-Ca5(PO4)3(Cl/F/OH)
'Palagonite'-

List of minerals for each chemical element

HHydrogen
H Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
H Smectite GroupA0.3D2-3[T4O10]Z2 · nH2O
H ApatiteCa5(PO4)3(Cl/F/OH)
OOxygen
O Aegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
O AlbiteNa(AlSi3O8)
O Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
O Albite var. Anorthoclase(Na,K)AlSi3O8
O Augite(CaxMgyFez)(Mgy1Fez1)Si2O6
O FayaliteFe22+SiO4
O IlmeniteFe2+TiO3
O Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
O Pyroxene GroupADSi2O6
O Smectite GroupA0.3D2-3[T4O10]Z2 · nH2O
O ApatiteCa5(PO4)3(Cl/F/OH)
FFluorine
F Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
F ApatiteCa5(PO4)3(Cl/F/OH)
NaSodium
Na Aegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
Na AlbiteNa(AlSi3O8)
Na Albite var. Anorthoclase(Na,K)AlSi3O8
Na Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
MgMagnesium
Mg Aegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
Mg Augite(CaxMgyFez)(Mgy1Fez1)Si2O6
AlAluminium
Al Aegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
Al AlbiteNa(AlSi3O8)
Al Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Al Albite var. Anorthoclase(Na,K)AlSi3O8
Al Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
SiSilicon
Si Aegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
Si AlbiteNa(AlSi3O8)
Si Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Si Albite var. Anorthoclase(Na,K)AlSi3O8
Si Augite(CaxMgyFez)(Mgy1Fez1)Si2O6
Si FayaliteFe22+SiO4
Si Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Si Pyroxene GroupADSi2O6
PPhosphorus
P ApatiteCa5(PO4)3(Cl/F/OH)
ClChlorine
Cl Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Cl ApatiteCa5(PO4)3(Cl/F/OH)
KPotassium
K Albite var. Anorthoclase(Na,K)AlSi3O8
CaCalcium
Ca Aegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
Ca Augite(CaxMgyFez)(Mgy1Fez1)Si2O6
Ca Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Ca ApatiteCa5(PO4)3(Cl/F/OH)
TiTitanium
Ti Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Ti IlmeniteFe2+TiO3
FeIron
Fe Aegirine-augite(NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6
Fe Augite(CaxMgyFez)(Mgy1Fez1)Si2O6
Fe FayaliteFe22+SiO4
Fe IlmeniteFe2+TiO3

Fossils

This region is too big or complex to display the fossil list, try looking at smaller subregions.
This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

 
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