The Marquesas Islands
The location of the Marquesas (top right hand corner of this map), in relation to other parts of Polynesia. The islands are a nearly 4 hour flight from Papeete in Tahiti. |
The Marquesas Islands, we will be staying on Nuku HIva and Hiva Oa |
Polynesia |
The Marquesas Islands (/mɑːrˈkeɪsəs/; French: Îles Marquises or Archipel des Marquises or Marquises; Marquesan: Te Henua (K)enana (North Marquesan) and Te Fenua ʻEnata (South Marquesan), both meaning "the land of men") are a group of volcanic islands in French Polynesia, an overseas collectivity of France in the southern Pacific Ocean. The Marquesas are located at 9.7812° S, 139.0817° W. The highest point is the peak of Mount Oave (French: Mont Oave) on Ua Pouisland at 1,230 m (4,035 ft) above sea level.
Research based on 2010 studies suggests the islands were colonized rapidly in two successive waves by indigenous colonists from West Polynesia, beginning c. 1025–1120 AD, leading to the development of a "remarkably uniform culture, human biology and language."
The Marquesas Islands form one of the five administrative divisions (subdivisions administratives) of French Polynesia. The capital of the Marquesas Islands administrative subdivision is the settlement of Taiohae on the island of Nuku Hiva. The population of the Marquesas Islands was 9,346 inhabitants at the August 2017 census.
The Marquesas Islands group is one of the most remote in the world, lying about 852 mi (1,370 km) northeast of Tahiti and about 3,000 mi (4,800 km) away from the west coast of Mexico, the nearest continental land mass. They fall naturally into two geographical divisions: the northern group, consisting of Eiao, Hatutu (Hatutaa), Motu One, and the islands centered on the large island of Nuku Hiva: Motu Iti (Hatu Iti), Ua Pou, Motu Oa and Ua Huka, and the southern group of Fatu Uku, Tahuata, Moho Tani (Motane), Terihi, Fatu Hiva and Motu Nao (Thomasset Rock), clustered around the main island of Hiva ʻOa. With a combined land area of 1,049 square kilometres (405 sq mi), the Marquesas are among the largest island groups of French Polynesia the Spanish galleons fleets arrived at en route to Manila, Nuku Hiva being the second largest island in the entire territory, after Tahiti. With the exception of Motu One, all the islands of the Marquesas are of volcanic origin.
In contrast to the tendency to associate Polynesia with lush tropical vegetation, the Marquesas are remarkably dry islands. Though the islands lie within the tropics, they are the first major break in the prevailing easterly winds that spawn from the extraordinarily dry (from an atmospheric perspective) Humboldt Current. Because of this, the islands are subject to frequent drought conditions, and only those that reach highest into the clouds (generally, above about 750 m / 2,500 ft above sea level) have reliable precipitation. This has led to historical fluctuations in water supply, which have played a crucial role in the sustainability of human populations in certain sections of the various islands throughout the archipelago. This is especially evident in the low historical population of Ua Huka (maximum elevation 857 m m / 2,812 ft.) and the intermittent inhabitability of Eiao (maximum elevation 576 m m / 1,890 ft.). The Marquesas Islands are thought to have formed by a center of upwelling magma called the Marquesas hotspot.
CLIMATE
Temperatures in the Marquesas are stable year around, but precipitation is highly variable. Precipitation is much greater on the north and east (windward) parts of the islands than on the western (leeward) parts. Average annual precipitation can vary from more than 100 inches (2,500 mm) on windward shores and mountains to a low as 20 inches (510 mm) in the "desert" region of Nuku Hiva. Droughts, sometimes lasting several years, are frequent and seem to be associated with the El Niño phenomena. The statistics from the weather station at Atuona on Hiva ʻOa is representative of the average sea-level climate of the Marquesas. Illustrating the variability of precipitation, the highest annual rainfall recorded in Atuona is 148.2 inches (3,760 mm); the lowest is 22 inches (560 mm).
SETTLEMENT AND POPULATION
The first recorded settlers of the Marquesas were Polynesians who arrived from West Polynesia. Initially, the carbon-dating evidence suggested their arrival before AD 100 but the date of initial colonization has since been brought forward in many independent dating studies.
For example, a 2010 study using revised, high-precision radiocarbon dating based on more reliable samples, suggests that the period of eastern Polynesian colonization took place much later, in a shorter time frame of two waves: the "earliest in the Society Islands A.D. ∼1025–1120, four centuries later than previously assumed; then after 70–265 years, dispersal continued in one major pulse to all remaining islands A.D. ∼1190–1290." This rapid colonization is believed to account for the "remarkable uniformity of East Polynesia culture, biology and language."
In 2014, the date of first settlement for the Marquesas was pushed back slightly to around AD 900–1000.
NATURE
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