Nasa found Earth expansion was currently 18mm. Close to what maxlow calculated which was 22mm with a variance of 4mm ! What happened to these results. They were then tweaked to eliminate the growth figure later. Maxlow looked into the subsequent maths done, which reduced it to almost zero. It was all tweaks to eliminate what they perceived to be an error. Not to deceive anybody, or get rid of EE (they arent even aware its currently going) but just to male the results consistent with what they know.
(Robaudo and Harrison, 1993). who did the work for Nasa and decided to correct their readings for expansion. their findings mentioned here.
Problems with Plate Tectonics
– Reply to Paul Lowman's Review (NCGT Newsletter no. 20) –
David Pratt
(First published in New Concepts in Global Tectonics Newsletter, no. 21, p. 10-24, December 2001)
" Plate rigidity is a central tenet of plate tectonics. However, it is recognized to be only an approximation: intraplate deformation is demonstrated by earthquakes in stable plate interiors, subsidence in midcontinental basins, and uplift of the surface over hotspot swells in the oceans. Deformation in the stable interior of the North American plate is said to be no more than a few millimetres per year, but is greater in the Basin and Range province and other regions in the west of the US, which are regarded as part of the plate boundary zone. It is acknowledged that "the modelled assumption of rigid plates frequently fails not only at plate boundaries but at considerable distances from boundaries" (Smith and Baltuck, 1993, p. 2). For instance, predicted motion in the mid-Pacific is in error by 6 to 8 mm/yr (Ryan et al., 1993).
Whenever discrepancies are found between measured and predicted motions, explanations are sought within the context of plate tectonics. For instance, the NUVEL-1 Africa-North America pole of rotation is said to lie "surprisingly far" (14°) from that of the best-fitting angular velocity; it is speculated that this misfit may be due to "systematic errors or significant plate nonrigidity" (Gordon, 1995).
On the basis of VLBI/GPS data for three sites in the Caribbean, the angular velocity of the relative motion between the Caribbean and North American plates was computed to have a rate of 0.23 ± 0.08°/Myr, twice the NUVEL-1A rate of 0.11 ± 0.03°/Myr; the direction was 62.2°N and -93.3°E, as against 74.3°N and 153.9°E. Furthermore, the estimated geodetic angular velocity failed to explain all the observed motion at the three sites. Three possible explanations were given: (1) the three sites are not all attached to a common rigid plate, (2) there are systematic measurement errors, or (3) the measurement uncertainties have been underestimated (MacMillan and Ma, 1999).
The pole of rotation derived from GPS data for the Pacific plate was found to lie 11.5° west of the NUVEL-1A pole, with an angular speed 10% faster. The suggested explanation was that the motion of the Pacific plate over the last 5 years did not agree with its motion over the last 3 Myr. The GPS velocity of Baltra Island on the Nazca plate is almost 50% slower (20±5 mm/yr) than the predicted value. The investigators stated that they could not account for the entire discrepancy, but thought that the plate might be deforming internally (Larson et al., 1997). Angermann et al. (1999) found that GPS velocities of four Nazca plate sites, relative to the South American plate, are about 20% slower than the NUVEL-1A plate model velocities and earlier geodetic measurements. Convergence rates for the two plates from several studies vary considerably.
The observed motion of Arequipa in the western Andes relative to North America is 13±1.5 mm/yr with an azimuth of 55°. According to model predictions, however, it should be moving at 10 mm/yr with an azimuth at 293° (Robaudo and Harrison, 1993). This major difference in the direction of movement is said to be due to a portion of the subduction motion being transferred into a portion of the overriding plate; some 25% of Nazca-South America plate motion is allegedly taken up by seismic and shortening mechanisms in the Andes (MacMillan and Ma, 1999). Similar discrepancies have been found in other backarc regions and interpreted in the same way.
The reigning plate-tectonic paradigm has biased the interpretation of space-geodetic data with its assumption that entire "plates" must be moving as more or less rigid units. The literature is riddled with anomalies, inconsistencies, and ad hoc explanations. Motion is certainly occurring in seismotectonic zones but, as Oard (2000a) remarks, "It is possible that in some areas the motion is in the opposite direction from that inferred by PT, and may be caused by vertical tectonics, instead of by underthrusting of one plate below another" (p. 43). He cites various pieces of geodetic evidence: the Tonga arc is moving eastward relative to the Pacific plate, which can be considered stationary (Bevis et al., 1995); the 1994 Shikotan earthquake caused GPS benchmarks on eastern Hokkaido, Japan, to move eastward up to 42 cm and subside up to 60 cm (Kikuchi and Kanamori, 1995); the magnitude 8.0 Antofagasta earthquake of 1995 moved the coast of Chile almost one metre westward relative to the Pacific plate (Klotz et al., 1999); and the Timor trough (eastern Java trench) appears to be inactive while the southern Banda arc is undergoing north-south extension (Genrich et al., 1996).
A brief review of some of the other problems facing plate tectonics provides further grounds for questioning PT interpretations of space-geodetic data."