Society Islands factsCompany Islands facts
The Teahitian Volcano
The Teahitia U-boat Vulcano on the Society Islands peaks to the sea level at 1400m, 40km north of the southern tip of the island of Tahiti. A number of 1980s flocks of seismics were caused by eruption of submarines (Talandier and Opal, 1984). Rock excavated from the vulcano in 1986 "exploded" as it touched the ground, indicating that the recent expulsion of molten rock did not yet have enough material to match the pressures and temperatures on the immersed sides of the building.
The volcanic eruption of two 1 km x 400 meter sized field hydrothermals was detected during the 1986 and 1989 missions. Visiting Java's famed volcanoes: For a small group of people, this is one of our best and classical tours: a collection of great volcanic and volcanic literature grouped into parts of varying interest.
Quick Tahiti Fact Sheet
It is the biggest of the 118 islands and junipers formally known as Polynesia. Tahiti and Papeete are situated on the Society Islands, an arcipelago with the high islands of Moorea, Huahine, Raiatea, Taha'a and Bora Bora.
The Tuamotu atolls with the slim crowns of Rangiroa, Manihi, Tikehau, Fakarava and the Marquesas - with the mighty peaks on the islands NukuHiva and HivaOa - are further dramas. These islands are situated in the same timezone as Hawaii, just southwards of the Ecuadorian Sea and half way between California and Australia.
Papeete's Faa'a Airport (PPT) is less than 8 flighthours from LAX. These islands are only two inches behind Pacific Standard Times. They are three in the summer (March to the end of October). The Marquesas are half anhour away from the other islands.