Nexus - 0905 - New Times Magazine-pages

Page Content (OCR)

Given the immense size of the body of . . the Earth, the lag times which are probably Reflection of the X Wave Motion at work, the great diversity in the type and in Southern California Earthquakes 1992 layering of the outer strata of the Earth and [5 South Cal Quakes 3.0 Plus —— The X Motion the constantly varying nature of the cycles of the EMS (Earth-Moon-Sun) system, one vn un oN NY NY NY N N N should not and indeed cannot, as one looks 8 3 5 3 3 rs na 8 s 8 S 8 3 at the evidence, find ultra-simple correla- 5 5 s 5 s $ g ¢ PS g s = = tion. But one can find, consistently, fairly 0.15 120 clear and reasonably strong patterns of cor- 0.1 100 relation which are easily seen without fancy 0.05 statistical manipulation and despite any 0 fancy statistical punditry of denial. 0.05 0.1 | 2 Chart 105: Tempo and Rhythm in California Earthquakes compared 0.15 with the X Wave, 1992 0.2 0 After establishing that Japan's extremely active tectonic environment is highly reflec- tive of the motions of the Earth's crust as it bobs over and around the spin axis, Events Per Day; compiled/copyright 1999 MWM from IERS "X" coordinates of the North Spin Axis and from SCSN online database for all earthquakes mag. 3.0 and greater in Southern California. Mandeville decided to zero in on a much smaller time-frame with Chart 106 may demonstrate one of the most conclusive pieces amuch smaller number of earthquakes to see if the same "connec- of evidence about vortex tectonics. The reflection of the X Wave tion" with the position and location of the pole could be found. in the peaks of volcanic activity for the vast arc of South Pacific Because of the highly accurate and complete record of earth- Islands within the Fiji-Papua Tectonic Arc is in nearly perfect quakes for California, the author studied the outbreak of earth- rhythm for a substantial portion of the 20th century. This huge quakes in southern California during 1992 (a year during which arc of volcanic islands begins in the Tonga Islands, passes the X Wave was low). through the Fiji Islands and continues westerly to parallel the Chart 105 zeroes in to find more exactly what the relationship is northern coast of Australia and eventually join with Papua New between southern California's quakes and the motion of the Guinea on its northern side. The arc is created by the collision of Earth's crust over the spin axis. Normally, the southern California the Australian Plate with the Pacific Ocean Bottom Tectonic area experiences some 10 to 20 events per week (magnitude 3.0 or Plate, which Australia is overriding. more), but most of these are so deep that they are not felt on the Amazingly, the frequency of peaks in volcanic activity for this surface—and thus do not appear in the news media. In May and __ great arc of volcanoes is even more obviously correlated to the X June 1992, while the X Motion was at a low, southern California Wave than is the composite of all volcanoes. The pattern of began to experience swarms of up to 100 earthquakes per day. volcanic activity is so similar to the undulations of the X Wave that Chart 105 shows how precisely this activity can be connected to it appears that sharp pulsations in volcanic activity are directly the motion and position of the pole. Notice that when the X Wave induced by the wobbling motion of the Earth's crust, just as is at its very lowest, there is virtually no seis- mic activity in southern California. Volcanism in the Fiji-Papua Tectonic Arc 1875-1993 Almost all of the activity in the graph Total Volcanic Activity in the Fiji, Solomon and Papua NG Islands broke out when the position of the pole passed through a certain zone of numbers Fiji-Papua Volcanic Arcs ——— X Wave - Primary Axis Cycle just prior to reaching the low point or just after it. When the position of the pole began 1600 to rise up, back through the same zone of | 1400 numbers, another outbreak occurred. A simi- lar chart for 1998 shows the same pattern. Ten 1000 2 Chart 106: Tempo and Rhythm of 800 Volcanism in Fiji with the X Wave, 1875-1993 600 Since the patterns of correlation were so 400 clear for small samples of earthquakes, the author began to draw charts to compare the 200 activity of small numbers of volcanoes in 0 regional zones with the X Wave. ns Since the spreading rift zone of the 2 Fiji-Papua Tectonic Arc is considered by many geologists to be the most active tecton- | Total days of VEI 1.0 and greater episodes with emissions of ash, lava, or pyroclastic ic zone on the surface of the Earth, chart 106 | Mmaterial;compiled and copyright 1999 by MWM from the Smithsonian Institution's was prepared so as to compare its activity | Catalog, Volcanoes of the World (Simkin & Siebert, 1994), and from IERS EOP Bulletins. with the X Wave. Reflection of the X Wave Motion in Southern California Earthquakes 1992 G5 South Cal Quakes 3.0 Plus == The X Motion Chart 106 may demonstrate one of the most conclusive pieces of evidence about vortex tectonics. The reflection of the X Wave in the peaks of volcanic activity for the vast arc of South Pacific Islands within the Fiji-Papua Tectonic Arc is in nearly perfect rhythm for a substantial portion of the 20th century. This huge arc of volcanic islands begins in the Tonga Islands, passes through the Fiji Islands and continues westerly to parallel the northern coast of Australia and eventually join with Papua New Guinea on its northern side. The arc is created by the collision of the Australian Plate with the Pacific Ocean Bottom Tectonic Plate, which Australia is overriding. Amazingly, the frequency of peaks in volcanic activity for this great arc of volcanoes is even more obviously correlated to the X Wave than is the composite of all volcanoes. The pattern of volcanic activity is so similar to the undulations of the X Wave that it appears that sharp pulsations in volcanic activity are directly induced by the wobbling motion of the Earth's crust, just as Volcanism in the Fiji-Papua Tectonic Arc 1875-1993 Total Volcanic Activity in the Fiji, Solomon and Papua NG Islands NEXUS = 51 AUGUST — SEPTEMBER 2002 www.nexusmagazine.com