Published about 4 years ago by Gregory Panayotou
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Please read more interesting things directly on the pano... Rano Raraku was a quarry for about 500 years until the early eigh...(more)
Published about 4 years ago by Gregory Panayotou
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This is the place where happen Haka Pei. Haka Pei is acompetition in the Tapati festival where two banana tree stumps are tied together and...(more)
Published about 4 years ago by Gregory Panayotou
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This is a nearly global view of rano raraku quarry....
Published about 4 years ago by Gregory Panayotou
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Orongo is a stone village and ceremonial center at the southwestern tip of Rapa Nui. Until the mid-nineteenth century ‘Oron...(more)
Published about 4 years ago by Gregory Panayotou
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Rano Kau is a 324 m (1,063 ft) tall extinct volcano that forms the southwestern headland of Easter Island...
Published about 4 years ago by Gregory Panayotou
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Rano Raraku is a volcanic crater formed of consolidated volcanic ash, or tuff, and located on the lower slopes of Terevaka in the Rapa Nui...(more)
Published about 4 years ago by Gregory Panayotou
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Rano Raraku is a volcanic crater formed of consolidated volcanic ash, or tuff, and located on the lower slopes of Terevaka in the Rapa Nui...(more)
Published about 4 years ago by Gregory Panayotou
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Rano Raraku is a volcanic crater formed of consolidated volcanic ash, or tuff, and located on the lower slopes of Terevaka in the Rapa Nui...(more)
Published about 4 years ago by Gregory Panayotou
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Rano Raraku is a volcanic crater formed of consolidated volcanic ash, or tuff, and located on the lower slopes of Terevaka in the Rapa Nui...(more)
Published about 4 years ago by Gregory Panayotou
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This is an unfinished Moai...Enjoy the work in progress... Rano Raraku is a volcanic crater formed of consolidated volcanic ash, or tuff, ...(more)
Published about 4 years ago by Gregory Panayotou
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At the horizon far away, you can see Ahu Tongariki Rano Raraku is a volcanic crater formed of consolidated volcanic ash, or tuff, and loca...(more)
Published about 4 years ago by Gregory Panayotou
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Rano Raraku is a volcanic crater formed of consolidated volcanic ash, or tuff, and located on the lower slopes of Terevaka in the Rapa Nui...(more)
Published about 4 years ago by Gregory Panayotou
License
Rano Raraku is a volcanic crater formed of consolidated volcanic ash, or tuff, and located on the lower slopes of Terevaka in the Rapa Nui...(more)
Published about 4 years ago by Gregory Panayotou
License
Rano Raraku is a volcanic crater formed of consolidated volcanic ash, or tuff, and located on the lower slopes of Terevaka in the Rapa Nui...(more)
Published about 4 years ago by Gregory Panayotou
License
Rano Raraku is a volcanic crater formed of consolidated volcanic ash, or tuff, and located on the lower slopes of Terevaka in the Rapa Nui...(more)
Published about 4 years ago by Gregory Panayotou
License
Rano Raraku is a volcanic crater formed of consolidated volcanic ash, or tuff, and located on the lower slopes of Terevaka in the Rapa Nui...(more)
Published about 4 years ago by Gregory Panayotou
License
Rano Raraku is a volcanic crater formed of consolidated volcanic ash, or tuff, and located on the lower slop...(more)
Published about 4 years ago by Gregory Panayotou
License
Rano Raraku is a volcanic crater formed of consolidated volcanic ash, or tuff, and located on the lower slopes of Terevaka in the Rapa N...(more)
Published about 4 years ago by Gregory Panayotou
License
Volcano Rano Kau emerged after hundreds of thousands of years, followed by volcano Maunga Terevaka, which created the island as we know ...(more)
