French Polynesia

France Polynesia

You will find humanitarian situation reports, news, analyses, evaluations, assessments, maps, information graphics and more about French Polynesia (France) Charming Islands of French Polynesia. Example IBAN format French Polynesia The IBAN comprises a two-digit countrycode, two numbers and a Basic Bankaccount Number (BBAN). For BBANs, information is provided on the local banks and accounts numbers. IBAN printing formats add a blank after every four letters, while the electronical formats does not contain blanks. Polynesia uses the French IBAN infrastructure for payments.

It is an example of a French IBAN. For France, the countrycode is FR. IBAN verification number 14 confirms the connection between the route target and your IBAN number. BBAN 2004 is 1010 0505 0001 3M02 606 and contains country-specific information on the number. You can enter the sort codes 20041, the ID of the vendor is 01005 and the number of the customer service center is 0500013M026.

Tahiti, French Polynesia

Capt. James Cook, the natural scientist Joseph Bank and a shipment of seamen left England for Tahiti in August 1768 to watch the passage of Venus. On 3 June 1769 they became witness of the events at Point Venus. Mr Cook outlined the route, but Mr Bank had little to say about it.

Maybe he was diverted by the miracles of the isle itself. Enhanced Thematic Mapper Plus on the Landsat 7 spacecraft took this lifelike colour picture of Tahiti on 11 July 2001. It is part of a volcano range created by the northwest motion of the Pacific Plate over a solid hot spot.

There are two ancient volcanos - Tahiti-Nui in the North West and Tahiti-Iti in the South East - connected by a narrow aisle. Investigations of its strata have led to the discovery of the probable story of Tahiti-Nui by a geologist. Nowadays it is approximately round, and it was approximately round when it developed as a vulcanic plate 1. 4 million to 870,000 years ago.

Tahiti-Nui's north and south sides crumbled about 860,000 years ago, carving solid arches around the isle. Shortly after the north face had crumbled, a second eruption was formed. Vulcanic matter on the north side of Tahiti-Nui finally exceeded the pristine vulcanic structures and began to fill in the South Vallado.

Tahiti-Nui now has a fairly symmetric outline, but it has an asymmetric three-dimensional form. On the north half of the isle, the hills are higher. But something other than vulcanic activities has left its mark on Tahiti: the rainy season. In this picture, the bent sun light illuminates some hillsides while others remain in the shade. The same rainfall has also encouraged the development of the luxuriant vegetation that covers both Tahiti-Nui and Tahiti-Iti.

Although the transit of Venus was the declared goal of the UK mission, Bank was probably more interested in the Tahitian herbs. His collection of copies from Tahiti, New Zealand, South America, Australia and Java represented some 1,300 new varieties, and his famous collection is now kept at the Natural History Museum in London.

It is lined with a series of corals and the south and west sides of the reef are the largest. Reforms often develop along the underwater sides of vulcanic isles. Observing the transit of Venus from space. Cook's look at the transit of Venus. Isle Evolution, Part 1: For Pitcairn Iceland.

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