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THE TEMPLE OF MU is a documentary about the parallels of ancient sunken civilizations off the coast of Okinawa and great Peruvian ruins.
Mu Continent space
There was a large continent called the Mu on the Pacific Ocean 12 thousand years ago. There, there are various human races, but there is no discrimination and they had one religion under the Emperor Ra Mu, the highest oracle. People had the highest culture, and excel at building and Navigation, and they extended the colony at each area. He blessed the nature and the foods in this continent. However, it is said that the earth sounded one day, the land broke into pieces and the lava flew out, and the country sank under the sea. at one night. As stated above, it is a legend of the Mu continent written by James Churchward, but at present, it is known that there was such a continent on the earth in the past or at present from the geology, but such a legend exists at each area in Ryukyu Islands
This is "a broad area of uplifted seafloor containing numerous volcanoes in French Polynesia." The boundaries of this superswell contain the Society, Cook, Austral, Tuamotu, Marquises, and Easter island chains. These islands reflect an enhanced rate of volcanism in the superswell area due to enormous quantities of hot mantle rock below the ocean floor.
If the South Pacific Superswell were once above sea level, forming the continent of Lemuria, it would have been buoyed up by a broad bulge in the mantle, much like that recently inferred to be buoying up the lofty peaks and plateaus of the American West. A renewal of mantle upwelling beneath the SPS could result in the seafloor there rising above the waves once again. Such activity would bear out the statement in Cayce reading 1152-11 (8/13/41) which says that, "In the next few years, lands will appear in the Atlantic as well as in the Pacific."
“volcanism can be attributed to [crust and mantle] downflow and recycling at the recognized subduction zones of Indonesia and the Pacific rim, but to upwelling and decompression melting at mid-ocean ridges and ‘hotspots’. Some of the Pacific island chains, best exemplified by the Hawaiian chain, are conventionally attributed to reheating of a lithospheric plate as it migrates over a deep-source hotspot. The hotspot and moving plate model of island chain volcanism is faced with several problems, however, including the occurrence of along-chain compositional changes, the typical absence of “plume scale” heat flow anomalies, and the absence, for example along the Cook-Austral chain, of a systematic sequence of geologic ages.”
Keith then goes on to reveal that the combined geophysical and geochemical evidence brings out the inadequacy of the plume model, thus leaving open the problem of accounting for linear oceanic island chains. He then proposes , as a working hypothesis, that the Hawaiian-Emperor chain (Fig. 3) is located along the trend of a linear cold residue developed below the ancestral Mid-Pacific Ridge, and that “part of the residue was left behind when the ridge was variably displaced during a Mesozoic disruption of the Pacific mantle….” (p. 302).
The Superswell and Mantle Dynamics Beneath the South Pacific
Marcia K. McNutt 1 and Anne V. Judge 1
1 Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139
The region of sea floor beneath French Polynesia (the "Superswell") is anomalous in that its depth is too shallow, flexural strength too weak, seismic velocity too slow, and geoid anomaly too negative for its lithospheric age as determined from magnetic isochrons. These features evidently are the effect of excess heat and extremely low viscosity in the upper mantle that maintain a thin lithospheric plate so easily penetrated by volcanism that 30 percent of the heat flux from all hot spots is liberated in this region, which constitutes only 3 percent of the earth's surface. The low-viscosity zone may facilitate rapid plate motion and the development of small-scale convection. A possible heat supply for the Superswell is a mantle reservoir enriched in radioactive isotopes as suggested by the geochemical signature of lavas from Superswell volcanoes.
Abstract
A rare quartz-garnet clinopyroxenite xenolith recovered from the island of Malaita in the southwest Pacific on the Ontong Java Plateau has lower 206Pb/204Pb-143Nd/144Nd and higher 87Sr/86Sr-207Pb/204Pb ratios than most oceanic basalts, providing the first conclusive evidence for an ancient crustal origin for pyroxenites within the Pacific convective mantle. Constraints from major and trace-element characteristics, the large extent of Hf-Nd isotopic decoupling, and the good agreement of Pb isotopes with the Stacey-Kramers curve, all indicate that contamination of southern Pacific mantle occurred by the subduction or delamination of Neoproterozoic granulite-like lower crust with an age of 0.5-1 Ga. This crustal recycling could have taken place around the suture of the Rodinia supercontinent, a part of which resurfaced during the mantle upwelling responsible for creating the Cretaceous Ontong Java Plateau.
The region of sea floor beneath French Polynesia (the "Superswell") is anomalous in that its depth is too shallow, flexural strength too weak, seismic velocity too slow, and geoid anomaly too negative for its lithospheric age as determined from magnetic isochrons. These features evidently are the effect of excess heat and extremely low viscosity in the upper mantle that maintain a thin lithospheric plate so easily penetrated by volcanism that 30 percent of the heat flux from all hot spots is liberated in this region, which constitutes only 3 percent of the earth's surface. The low-viscosity zone may facilitate rapid plate motion and the development of small-scale convection. A possible heat supply for the Superswell is a mantle reservoir enriched in radioactive isotopes as suggested by the geochemical signature of lavas from Superswell volcanoes.
Originally posted by Hanslune
Believe, no just not able to prove conclusively that there is NOT an unknown, bronze age culture out there we haven't found.
Originally posted by Hanslune
reply to post by Hollywood11
Ah Hollywood do you actually read any of these links?
I'm asking as some of these are talking about geological features and events created tens to hundreds of millions of years ago. This isn't evidence of fictional Mu.
Another one Hollywood
The region of sea floor beneath French Polynesia (the "Superswell") is anomalous in that its depth is too shallow, flexural strength too weak, seismic velocity too slow, and geoid anomaly too negative for its lithospheric age as determined from magnetic isochrons. These features evidently are the effect of excess heat and extremely low viscosity in the upper mantle that maintain a thin lithospheric plate so easily penetrated by volcanism that 30 percent of the heat flux from all hot spots is liberated in this region, which constitutes only 3 percent of the earth's surface. The low-viscosity zone may facilitate rapid plate motion and the development of small-scale convection. A possible heat supply for the Superswell is a mantle reservoir enriched in radioactive isotopes as suggested by the geochemical signature of lavas from Superswell volcanoes.
So Hollywood explain to us how this supports the idea of a fictional Mu? I'm asking because it doesn't but you are posting scientific material that provides no support for your theory.
Why would you do that?
It does show that Mu existed because with a few Earthquakes or Volcanic eruptions the Superswell would easily be raised above sea level and certainly was at one time in the last 10,000-20,000 years.
Extending this analysis, McNutt et al. [1990] suggested that the Darwin Rise was uplifted during the Cretaceous, and was similar to the present Superswell until about 70 Ma. Larson [1991] termed the Cretaceous event a Superplume, which produced both the Darwin Rise and very large amounts of lithosphere at midocean ridges. In this model, the present Superswell reflects the Superplume's waning phase.
These guys are talking about the area being uplifted during the cretaeceous age with a decline beginning around 70,000,000 years ago.
We look forward to your scholarly presentation.