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Rano Kau

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which is one of the island's only three natural bodies of fresh water. The lake is located approximately 100 metres (330 ft) above sea level, but is more than 200 metres (660 ft) below the highest of the crater's ridges. The volcanic cone is largely surrounded by water, and much of it has
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The crater is almost a mile across and has its own micro climate. Sheltered from the winds that wet most of the rest of the island, figs and vines flourish at Rano Kau. The inner slope was the site of the last
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the cliff face drops to the southwest at an angle of 50° to the sea shore some 300 metres (980 ft) below. On its northern side, the volcano slopes down to
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and gives its name to one of the seven sections of the park. The principal archaeological site on Rano Kau is the ruined ceremonial village of
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At some point in the early twentieth century, the island's manager took a photograph of steam coming out of the crater wall.
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was recorded on the cliffs at Rano Kau in the 1880s, but had fallen to the beach by the time of the
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which is located at the point where the sea cliff and inner crater wall converge. One
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Haase, Karsten M.; Peter Stoffers; C. Dieter Garbe-Schönberg (October 1997).
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with its youngest rocks dated at between 150,000 and 210,000 years ago.
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tree in the wild until the specimen was chopped down for firewood in 1960.
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Map showing the location of Rano Kau along with the volcanoes
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been eroded back to form high sea cliffs which at one point (
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Rapa Nui National Park – UNESCO World Heritage Centre
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Flenley & Bahn 2003 The enigmas of Easter Island
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It was formed of basaltic lava flows in the 630: 367: 674:Humberstone and Santa Laura Saltpeter Works 381: 637: 623: 374: 360: 266: 156: 71: 48:that forms the southwestern headland of 28: 666:Historic Quarter of the Seaport City of 758: 169: 618: 355: 44:is a 324 m (1,063 ft) tall 13: 700:in the Arica and Parinacota Region 14: 802: 300: 713: 184: 16:Dormant volcano in Easter Island 409:ArchipiĂ©lago de Juan Fernández 233: 216: 161:Crater lake of Rano Kau, with 102:Mataveri International Airport 1: 210: 67: 292:Van Tilburg, Jo Anne. 1994. 280:The Mystery of Easter Island 25:Easter Island § Geology 7: 177: 33:View of Rano Kau from near 10: 807: 776:Volcanoes of Easter Island 268:10.1093/petrology/38.6.785 200:List of volcanoes in Chile 18: 723: 710: 656: 389: 694:Artificial Mummification 549:PumalĂ­n Douglas Tompkins 323:27.186889°S 109.435667°W 383:National parks of Chile 328:-27.186889; -109.435667 240:Steam crack in Rano Kau 684:Rapa Nui National Park 342:Rapa Nui National Park 166: 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Index

Rapa Nui National Park
Easter Island § Geology
Colour photo from a cliff top down onto a pond strewn marsh backed by high cliffs, an area of sea is visible through a gap in the cliffs.
Orongo
extinct volcano
Easter Island
Chilean
Pacific Ocean
Pleistocene

Terevaka
Poike
crater lake
Orongo
Mataveri International Airport
World Heritage Site
Rapa Nui National Park
Orongo
ahu
moai
Routledge expedition
basalt
obsidian
pumice
toromiro
Colour photo of circular pond strewn marsh surrounded by steep cliff topped slopes – the sea is visible through a gap in the cliffs on the right
Orongo
Geography portal
List of volcanoes in Chile
Sirolimus

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