Easter Island Statues Age

Island Easter Statues Old

Easter Island secret at last resolved? Easter Island's mystery puzzle wrench was concealed within view, but not seen for a long while. As we all turned our eyes to huge statues - Moai - we have forgotten to give enough consideration to the rock decks on which they stood. They were the keys to the mystery.

Island of Easter - Land of the Mysteries

Isle of Easter â?" the vivid and lonely testimony of a secluded, ancient continental area in the middle of the Pacific Ocean. The Polynesian isles are not and never were part of a lost continen. The Easter Island is located about 500 km eastwards of the ridge of an undersea chain, the Eastern Pacific Rise, and is also in the Easter Rift area.

It is considered to be the top of a huge hill created by the pouring of melted vulcanic rocks from the seabed. The island is located on a U-boat deck about 50 or 60 meters below the sea level, but 15 to 30 km off the shore, the deck ends and the seabed sinks to 1800 to 3600 meters. The legend says that Easter Island is part of a â????.

Gradual Pleistocene glaciations have reduced the water surface by at least 100 metres and sometimes many a time. The Easter Island would then have been bigger than it is today. After the prevailing geologic legacies of tectonic plates, Easter Island was never part of a lost continen.

For Francis Mazière, the mythical Hiva could have been a long crest of the East Pacific Rise. It is becoming increasingly clear, as discussed below, that much bigger areas of the Pacific Ocean were once ashore. Following the tectonic plates, the earthâ??s extreme outer stratum, the litosphere, is split into individual â??platesâ??, which move against each other on an asthenospheric film underneath.

 These decisive facts, which remain largely unspoken in contemporary geology text books, make the great sideways motion of the single person â??platesâ? Â These decisive facts, which remain largely unspoken in contemporary geology text books, make the great sideways motion of the single person â???? inconceivable. Platytektonics asserts that new sea crusts are continuously formed by buoyancy of magnetism at â??midoceanâ?? Ridge (including the East Pacific Rise) and are subducted into the lair along rift pits that are mostly surrounding the Pacific Rim.

That would mean that the whole sea rust should not be older than about 200 million years. The cliffs that form the isles of St. Peter and Paul near the ridge of the Mid-Atlantic Ridge, for example, are 350, 450, 835 and 2000 million years old, while according to tectonic plates they should be only 35 million years old.

Rock form Tahiti in the South Pacific has proved to be over 800 million years old. From time to time an attempt is made to clarify such abnormalities â?" e.g. as crust block that somehow remained during the spread of â??seafloorâ??. Seismic events taking place at different levels on the land side of sea ditches defined a Benioff area, which is defined as â??descending plateâ in platetectonics.

The way the sea rust is to go down into the thicker cloak has never been adequately described. It is intended to compensate for the volumetric mass of the shellfish formed at the oceans. However, while 80,000 km of mid-ocean flashbacks allegedly produce new crusts, there are only 30,500 km of ditches and 9,000 km â??collision zonesâ â?" thus only half the length of the ?collision However, while 80,000 km of mid-ocean flashbacks allegedly produce new crusts, there are only 30,500 km of ditches and 9,000 km -?collision zonesâ â?" thus only half the length of theâ?? centres.

When the subductions really took place, huge quantities of marine deposits would have had to be scrapped off the seabed and stacked against the land edge of the graben. Platetectonics had to fall back on the far-fetched idea that smooth sea sand can gently slip into a subsduction area without any significant traces.

Another of the Benioff Areas is that they are very old ruptures caused by the cooldown and contractions of the soil and currently constitute the distortion point between the elevating island/continental area and the sloping sea ice and cloak. An alternate suggestion is that sea islands are made up of magnetism rising from much shallow water, perhaps from a web of magnetism â??surge channelsâ in the litosphere.

Simultaneous sequential tectonic movements of tiles should be indicated by seamounts, but in order to create these mega trends, the tiles would have to move in two different axes simultaneously! Even though tectonists call up ad-hoc on demand â??microplatesâ and â??hotspotsâ??, they cannot satisfactorily explain any of these.

 3 The Pacific â??plateâ??. There is a general argument that Easter Island can never have been part of a single continents, because it has never contained granites or sediments such as lime and sandstones - only eruptive rock. The appearance of volcanoes does not show that the area in which they appear is not a submerged continen.

According to current information, the rest of the island consists of four volcano tops â?" Cameroon, Mount Kenya, Kilimanjaro and..... Ruwenzori, together with one or more islets, which, like the others, would be entirely of igneous rock. It is 40 km thick under northern Australia, 20 km thick in the east of the adjoining coral sea, 22-28 km thick in the Fiji-Tonga-Samoa area and up to 36 km thick on the Tonga isles.

More than 100 underwater plateaux and burrs are spread across the ocean and speckled with islets, and many of them may not yet be fully immersed â??oceanizedâ??, as proposed by â??anomalouslyâ Thick crusts and finds from â??impossiblyâ old continent. At the beginning of the twentieth century the geologist J.W. Gregory deduced from a thorough investigation of geologic and palaeontologic proofs that land masses of different size had been lifted and sunk at different periods in the Atlantic and Pacific Ocean, most of them disappeared through the Miocene.

On the basis of a thorough investigation of the drill results, the Georgian geo-scientist E.M. Ruditch concludes that there is no systemic relationship between the age of the flat waters and their spacing from the axis of the mid-oceanic rim. Maps of the former territories in today's Pacific and Indian Oceans, shown in Figure 9.

The Easter Island legend tells of the first colonists who arrived after their homeland disappeared and of a giants called Uoke, who caused a great continental relic from which Easter Island is a relic to sink in a rage. There are similar continental disappearances throughout Polynesia and Melanesia, as well as in other parts of the Pacific.

The Hawaiians, for example, thought that there was once a large peninsula that stretched from Hawaii to New Zealand, but it declined, and left only its mountain peaks as isles. While it is certain that no major Pacific coastlines have disappeared in recent thousands of years, some authors believe that adequately sized isles have.

In 1722, when the Dutchman Roggeveen found Easter Island, he was actually looking for Davis Land. A British pirate called John Davis said he saw this island in 1687 at 27°20'S. The island was in the middle of the Atlantic Ocean. That is not true in any way for Easter Island. Today's general faith is that Davis had miscalculated his location, as was by no means uncommon among early sailors, and that Davis was Land Mangareva, the main island in the Gambier Islands, far western of Easter Island.

Easter Islanders named it Motu Matiro Hiva, which means â??islet before Hivaâ??, where Hiva is the name of her orphanage. He found a typeface on the small island of Woleai, about 1600 km westward of Pohnpei, which is still in use, quite different from any other in the whole wide globe (see section 7).

In 1879, for example, an ltalian master told of his discoveries on the island of Podesta, just over a kilometre to the east of Valparaiso, Chile. It has not been found since then and was taken off the maps in 1935. In 1912 an island near Easter Island was spotted, but never seen again.

When a 1932 sea chart quest was unsuccessful, Sarah Ann Island north-west of Easter Island was taken off the nautical maps. 1928 the skipper and two of his two mates on a luxurious English ship told us that Easter Island itself had disappeared! They sent a gun ship from Chile to the island and found it in its normal place.

By 1955, US airmen saw an island 615 km western of Honolulu, but it vanished within a few short week, and left only sulphur stripes on the top. Two volcanoes were born on a UK battleship 320 km southwards of Tokyo in February 1946, rising to a maximum altitude of 15 metres and spreading over an area of about 2.5 km2.

Besides temporal volcanoes, which appear abruptly in deeper oceans, there are also small ones, which appear and disappear in flatter areas. Fonuafo â? ?ou (Falcon Island) in the Tonga group, was conceived in 1885, when an outbreak increased a cluster 88m over the seabed. {\*Metis Island, 120 km from Fonuafoâ??ou, appeared in 1875 and disappeared in 1899.

In 1823 Hunter Island was found at 15°31'S and 176°11'W. The island was never seen again. Three Tuanaki Island, part of the Cook group in the South Pacific, vanished around the mid-nineteenth centuary. Polynesians also lived on these archipelagos, but in 1844 a missionary vessel was unable to located them.

A number of former islanders who had gone away in their adolescence lost their lives in the twentieth century. Though some small archipelagos seem to have disappeared into the Pacific in the last thousands of years, the proof is that the archipelago on the order of magnitude that Spence and Brown had in their minds at that time is enormous.

However, as stated above, there were certainly land masses of a continent-sized nature in the Pacific in the later years. K.M. Hasse, P. Stoffers and C.D. Garbe-Schönberg, â??The Petrogenetical development of the lava from Easter Island and neighboring Seebergen, Nearidge Hot Spot Volcano in the SE Pacificâ??, Journal of Petrology, Vol. 38, No. 6, 1997, p. 785-813.

R.I. Rusby, â??GLORIA and other Georophysical investigations of the Easter microplate, in:: Please : Plate tectonique : un paradigme sous la menaceâ??, et â??Sunken Please : Plate tectonique : un paradigme sous la menaceâ??, et sqqq Please : Plate tectonique : un paradigme sous la menaceâ??, et â??Sunken continent Please : Plate tectonique : un paradigme sous la menaceâ??, et sq Please : Plate tectonique : un paradigme sous la menaceâ??, et â??Sunken Please : Plate tectonique : un paradigme sous la menaceâ??, et seigm Please : Plate tectonique : un paradigme sous la menaceâ??, et â??Sunken Please : Plate tectonique : un paradigme sous la menaceâ??, et Please : Plate tectonique : un paradigme sous la menaceâ??, et â??Sunken Please : Plate tectonique : un paradigme sous la menaceâ??, etp Please : Plate tectonique : un paradigme sous la menaceâ??, et â??Sunken Please : Plate tectonique : un paradigme sous la menaceâ??, et Please : Plate tectonique : un paradigme sous la menaceâ??, et â??Sunken Please : Plate tectonique : un paradigme sous la menaceâ??, et Please : Plate tectonique : un paradigme sous la menaceâ??, et â??Sunken Please : Plate tectonique : un paradigme sous la menaceâ??, et Please : Plate tectonique : un paradigme sous la menaceâ??, et â??Sunken.. S: Chatterjee and N. Hotton III (ed.), New Concepts in Global Tektonics, Lubbock, TX:

For more information see â??Problems with panel tectonicsâ??, http://ourworld.compuserve.com/homepages/dp5/lowman.htm. J.G. Clark and J. Dymond, â??Geochronology and Petrochemicals of Easter and Sala y Gomez Islands: Effects on the formation of the Sala y Gomez Ridgeâ??, Journal of Volcanology and Geothermal Research, Volume 2, 1977, pp. 29-48. N.C. Smoot, â??Magma Flooding, Microdisks and Orbital Intersectionsâ??, New Concepts in Global Tectonics Newsletter, no.

A. A. Meyerhoff, I. Taner, A. E. L. Morris, W. B. Agocs, M. Kaymen-Kaye, M. I. Bhat, N. C. Smoot and D. R. Choi, Surge Tectonics: P.E. Baker, â??Preliminary Report on current Easter Island geology researchâ??, Geology Magazine, Vol. 104, No. 2, 1967, pp. 116-22. Atlantologie : grundlegende Probleme, Honolulu, HA : University Press of the Pacific, 2001 (1970), S. 150-1.

J.W. Gregory, â??The Pacific geologic historyâ??, Quarterly Journal of the Geological Society, vol. 86, 1930, pp. 72-136 (p. 132). E.M. Ruditch, â??The Weltmeer without expansionâ??, in: A: Barto-Kyriakidis (ed.), Critical Aspects of Platy Tektonics, Athens: The Canadian Society of Petroleum Geologists, Memoir 17, 1994, S. 67-80 ; D.R. Choi, â??Geology du sud-est du Pacifiqueâ??, parties 1-3, New Concepts in GlobalTectonics Newsletter, no. 7, pp. 11-15 ; no. 8, pp. 8-13 ; no. 9, pp. 12-14, 1998.

L.S. Dillon, â??Neovolcanism: a suggested substitute for the concept of disk theory and driftâ??, in: C. F. Kahle (Hrsg.), Platform Tsectonics â?" Assessments and Reassessments, Memoir 23, Tulsa, OK : American Association of Petroleum Geologists, 1974, S. 167-239 (S. 222) ; Zhirov, Atlantis, S. 154-5. The Riddle of the Pacific, Kempton, IL : Adventures Unlimited, 1996 (1924), S. 45.

Mystery of the Pacific, p. 52. The Pacific Ocean and its isles. Colonisation of the Pacific began about 50,000 years ago, when hunters and collectors colonised Australia and New Guinea in the West Pacific at a point in history when they arrived on shore due to the lower levels caused by the glacial period.

The migration went east and arrived in the North Solomon islands about 28,000 years ago. It is assumed that the Polyynesian isles have only been inhabited for about 2000 years, as it took the Polynesians a long pause to acquire the navigation skills that would enable them to cruise far off the coast.

But the data for the colonization of the various Asian isles are very timid, as they are mainly derived from the oldest carbon radiate data available to date; further discovery could indicate that man's colonization goes back thousands of years before. There may have been several migratory phases from different direction into the Ocean, and over a longer period of timeframe archeologists are willing to think about it.

Dominant theories in the early 1900s and early 1900s were that the Polynesians were an Indo-European group that entered the Pacific via India. Today it is generally assumed that some of them come from North-East Asia and also from the Malaysia articel. However, as Graeme Kearsley says: "In many ways they are intimately associated with the Caucasians and have been regarded as such in many surveys, and this racist legacy is still evident on many East Polynesian isles as it was with the first discoverers of Europe.

This migration followed the same patterns as landmigrations, in that the males or sailors acted, purchased or imprisoned spouses of coastline or island races, thereby creating interracial offspring. Thus, a varying racist heritage is clearly visible on the Pacific Isles..... Almost all the first European accounts refer to the different colours of Polynesians on different isles, but also within the population of an island.

This short walk through the Pacific Ocean concentrates on the remnants of monuments and monuments of Megalithsarchy. Like on Easter Island, some of the textures can be the work of very old and as yet unfamiliar civilizations. Yonaguni, a small island in Japan, was found in the mid-1980s with a square rock formation about 250 metres long, 100 metres broad and 25 metres high.

Now it is in a depth of up to 30 meters of waters, but if it had been subjected to much lower levels at the seas for about 10,000 years, then it would have been on the turning circle of cancer. It is structured with broad patios, large stairs, platforms and ditches as well as two 6 metre high, approx. 2.5 metre broad and 4 metre broad Megalite boulders.

Everywhere on the Marianas one finds pale rocks - high pillars of rock with a semi-spherical keystone that look like fungi. Lath rocks vary from small carcasses of nature rocks to solid pillars of rocks, 4.5 metres or more high and covered with huge cobbles.

Tinian Island has two of the biggest megalites. This is the oldest date of carbon radiate from the Late Age of 900 A.D. â?" but that doesnâ??t tell us anything about when they were made. The Pohnpei (or Ponape, also known as Ascension ) is a vulcanic island in the East Caroline Islands and could have been the center of a lost imperium.

Nan Madol is located in the Pohnpei south-east coastal Laguna, the â??Venice of the Pacificâ??. More than 18 sq km, but the center of the site is about 1. 5 km by 0. 5 km and contains 92 man-made islets that are planted in the Laguna and are encircled by synthetic channels.

They were made by piling large, mostly under 10 ton heavy, six-sided basaltic primers on the island wall and charging the island-center. It is the biggest rock, a solid piece of bass rock on the south-eastern side of Nan Douwas, with a weight of about 50tonnes. The ash on the bottom of a fireplace on one of the man-made islets dates back to 1000 AD, but this only shows that the town was occupied at that period - not that the whole town was made then.

Insaru, an old, gigantic stony town on the island of Lelu, bordering Kosrae (the most eastern of the Caroline Islands), also consisted of gigantic basaltic ramparts and spirepids, the island and building being crossed by a sewer system linked to the sea. Several of the wall are over 6 metres high and the basaltic boulders are up to 50 tonnes in weight.

The Palau Island, the most westerly of the Caroline family, has over 5% of its territory in terraces, and entire mounds are shaped like stepped pathways. Bairulchan on Babeldaob has two lines of large basaltic boulders, some of which are sculptured with outlines. There are similar rocks on Vao and Malekula on the Vanuata Isles (New Hebrides).

Polynesia's Polynesia Delta extends from New Zealand in the south-west via Hawaii in the North to the Easter Island in the south-east. There are nowhere else in the Pacific as many impressing Mexican remnants in such a small area as on Easter Island. However, there are some remarkable features on other isles.

Tongatapu Island on the Tonga Islands has the only southern Pacific arc of megalith - the Haâ?" Trinithon. Muâ??a (formerly Lapaha), a channel town on the island of Tongatapu, has many magalithic decks (known as Langi). In the last few thousand years, the island has increased by one metre and today there are no longer any useful facilities such as the quay and canal/ditch.

The pyramid-shaped Langi Tauhala at the old Tongatapu fort is made of solid cobbles. Probably the biggest building brick ever used by the Polynesians, it is 7.4 metres long, 2.2 metres high, 0.4 metres thick, weighs 30 to 40 tons, is nicked and fit into an adjoining bloc and is part of a 222 metre long brick face.

 8 The biggest boulder in Langi Tauhala, Muâ??a. Due to carbodating it is assumed that Samoa was populated by the Lapita around 1200 BC, about the same period as Tonga. The island of Savaiâ??i is home to a huge, shallow hill of boulders known as Pulemelei â?" the most extensively preserved hill in Polynesia.

Situated 61 x 50 metres at the foot of the pedestrian zone, it climbs on two levels to a level of more than 12 metres. At both ends there is a slightly lowered platform, together with a sidewalk, and it is encircled by a number of other decks, streets and rock faces, as befits a large ceremony area.

In Rarotonga, the biggest of the Cook Islands, the ear was pierced and the ear lobes lengthened, as was the case on Easter Island, in old India and in Peru. It has a huge street that once surrounded the whole island and several pyramid-shaped decks. It' better built than the streets of Malden Island, and similar to Peru.

All over the Society Islands there are cut-off pyramid-shaped decks or maraea, some of which consist of meegalithic rocks that are meticulously formed and adapted. Tahiti's biggest of all Polynesia's rock buildings was Mahaiatea Hill. and climbed in 11 stages to a level of over 13 meters. The trajectories consisted of block corals covered with square volcano rocks.

The carving was made on Raivavae (one of the Austral Islands), the Islamic center of Polynesia, but is now in the Gauguin Museum of Tahiti. Allegations that the Easter Island statues of Easter Island are a product of the Polyynesian Czeck. The Marae Taputapuatea on Raiatea (the biggest of the Leeward Islands) is 43 metres long, 7.3 metres broad and up to 3.7 metres high.

The Huahine and Bora Bora are like Raiatea's maraae made of large plates of corals, while similar Tahiti and Moorea are made of round rocks of bassin. All over the Marquesas Islands, the ruins of large rock outcrops, masonry houses and patios, most of which are covered with jungles, are evidence of a lost civilization.

No masonry was found that could be compared to Ahu Vinapu on Easter Island. Seventeen platforms in the Taaoa valley. Five giant rock tikis, the biggest is 2.43-metre high. Vahangeku' s 19 megalithic 3 metre high wallâ??a Tohua, Nuku Hiva. Of course, the buildings could be several thousand years older and have been repeatedly refurbished, converted or extended.

Today the Marquesas Island has about 8000 residents. It is often thought that the Marquesas were populated by West Polynesians, probably from Tonga or Samoa, around 300 AD, but Suggs argued that they were populated much sooner, around 300-500 BC. It is thought that the Polynesians were one of the major points from which they extended in the Pacific; the Marquesan tongue is very much related to the Hawaiian, Mangareva and Easter Island tongues.

Nevertheless, there are indications that the Marquesas, as one of the easternmost parts of Polynesia, play a pivotal part in the mutual contact between Asia and America. Bugs' eyes, similar to those of the Marquesas, are found in Bolivia and Peru, especially in Tiahuanaco and Chavin, and they have also been likened to Chinese Bronze Age statues.

Nuku Hiva's old holy center was probably the Taipivai Valley, which is located next to the holy Taipi Mt. Graham Hancock emphasized that when we take the Giza-Heliopolis in Egypt as a zeromeridian to measure the length, we find that the large Angkor Wat in Cambodia temples are 72° eastern of the Giza fusion, the Nan Madol in Pohnpei at 54° eastern of Angkor and astronomical, 72° and the Tahiti islets of Angkor and Tahiti, and the large Angkor Wat in Cambodia...

If we look 144° length eastwards of Angkor (that is also 144° westwards of Giza), we find only one island near: Isle of Easter, a little over 3Â (just under 320 km) eastwards of the town. It is Hancock's guess that Easter Island could have been inhabited at first, but it is not,

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