Rano Raraku is a volcanic crater on Easter Island formed from consolidated volcanic ash (tuff) on the lower slopes of Terevaka [1]. It served as the primary quarry for approximately 500 years until the early 18th century, providing tuff stone for about 95% of the island's 887 known moai [1]. Located within Rapa Nui National Park, a UNESCO World Heritage Site, the quarry remains one of Polynesia's most significant archaeological sites [1].
Rano Raraku

| Type | Geological interest |
|---|---|
| Period | 1000 - 1500 AD |
| Country | Chile, Easter Island |
| Coordinates | 27.1230° S, 109.2861° W |
Chile, Easter Island