Author Topic: May 30  (Read 43 times)


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May 30
« on: May 30, 2017, 11:21:06 pm »
<LK to RF>
Q1: Have you done or read any calculations on EDM that support those ideas in  detail?
Q2: Do you know of experiments that show that EDM can erode surfaces like that and  produce partly melted clays and quartz sand?
Q3: A close encounter between planets would surely raise very high tides, causing  megatsunamis, so why would not the cavitation effect produce the sand from granite  bedrock and the tsunamis account for the sediment deposition and erosion, leaving  behind some mesas?
Q4: Doesn't water erosion produce dendritic patterns?
Q5: The EU team accept much of Velikovsky's evidence on catastrophism, and  Velikovsky referred to violent winds that occurred, so wouldn't the winds account  for loess and volcanism account for deep sea ash?


<RF to LK>
_[See] ‘An Alternative to Plate and Expansion Tectonics’:
_(Johnson. Robert. 2014. Massive Solar Eruptions and their contribution to the  causes of Tectonic Uplift. NCGT Journal Vol.2 No.1.)  _
_demonstrates that an external source of energy arising from massive solar  eruptions is likely to have been available on rare occasions in past eras.
_electric discharges to the Earth’s surface many orders of magnitude larger than  present-day lightning strikes would result from the impact of an extreme Coronal  Mass Ejection.
_The energy delivered directly to the crustal strata could have been sufficient to  contribute to uplift via many of the existing thermal expansion and phase change  models.
>>>_Rapid ion diffusion in the electric fields associated with the discharges is also  likely to have occurred, thereby potentially offering a solution to ‘the granite  problem’.
_(Gold, 1962, discussion p. 170) considered what effect a more massive solar  eruption would have on the Earth
_the increased solar wind pressure would drive the inner edge of the Earth’s  [outer] magnetosphere down into the upper atmosphere
_storm-generated electric currents would then encounter great resistance
_the path of least resistance is to short down in a massive and continuous  ‘lightning strike’ or discharge through the atmosphere, run through the more  conducting surface of the Earth, and short back up to the magnetosphere in a second  discharge to close the circuit back to the magnetosphere (figs. 1 and 2)
_huge direct currents of “hundreds of millions of Amps” would run in the surface of  the Earth
_Robert Johnson proposes that just such electrical discharges acted to uplift  modern mountainous regions
_Such currents would flow if either Earth encountered another celestial body or  Earth’s electrical environment changed
_I see such discharge altering Earth’s surface gravity which may have contributed  to the vertical tectonics at that time
_(see ‘An Alternative to Plate and Expansion Tectonics’ for my views on vertical  tectonics).
_We can picture both electrical and physical processes generating sediment but wave  action certainly did not sculpt Mt Everest
_the dendritic patterns of mountain ranges must have an electrical origin
_Paul Anderson has done work in this respect. See: v=c7w1rGeqXBg
_“Paul Anderson uses fractal analysis to determine what process –fluvial or  electrical- shaped the various landforms on the Earth, the main focus being canyons  and riverbeds.
_This analysis is then compared to electrical discharge patterns recorded in  laboratory experiments.
_Water flow does not appear to form structures with as many branches, particularly  perpendicular branches, as do electrical events.
_the current from the source must have been higher than it is today in the present auroras.
_The auroral process would have extended well beyond the current northern and  southern locations,
_and once the atmosphere could not support the ionization it would break down in  the form of electric discharges.’
_mountain formation was not only due to electrical uplift but also due to  electrical erosion.
_In this image of the Tibetan Plateau the rim has been eroded to form snow-capped  mountain ranges.
_“This is the pattern we see the world over
_What strata escaped being metamorphosed were eroded, pulverised and scattered by  intense electrical winds
_(something similar but on a vastly reduced scale still occurs on Mars today

<>Are you referring to global dust storms from electrified dust devils?
<>Do you see dendritic patterns on Mars from that?

_In the same thread I write: “Ashes and Dust
_Large areas of the Earth’s strata and surface record what geologists perceive as  ‘massive volcanic eruptions’ quite often these prehistoric eruptions dwarf any  recorded eruption.
_For example, Dinosaur National Monument (Utah, USA) is part of the Morrison  Formation which covers some 700,000 square miles.
_Part of the formation is: ‘dominated by silica-rich volcanic ash representing  explosive volcanism on a colossal scale
_A staggering quantity of volcanic materials, estimated at more than 4,000 cubic  miles, occurs within the thin but widespread Brushy Basin Member in Wyoming, Utah,  Colorado, New Mexico, and Arizona.
_No volcano is known within the boundary of the Morrison deposit, no local lava  flows are known within the Morrison boundary, and geologists place the nearest  explosive volcanic source vents in southern California or Nevada.
_How these coarse volcanic materials in such colossal quantities were distributed  on so wide a scale remains a mystery.’(15)
_“The Worzel Deep Sea Ash consists of colourless shards of volcanic glass with an  index of refraction of 1.500 and varying in size from 0.07 to 0.2 mm.
_There is no particle size sorting.
_Most of the shards are in the form of curved, fluted, or crumpled films of glass.
_A minority are nearly equidimensional fragments of silky pumice.
_No crystalline minerals have been found.
_In all important respects it is similar to material which has been classified as  volcanic ash in the deep-sea deposits of the world.
_On preliminary examination, the ash of the Worzel layer appears to be quite  similar to the ash layer which occurs in a suite of cores from the Gulf of Mexico.
_Rex and Goldberg have found quartz particles of continental origin in abundance in  Pacific sediments as much as 2,000 miles from the nearest continent
_The ash is entirely unlike material described as meteoritic dust.’
_“The researchers concluded: ‘Apparently we require either a single very large  volcanic explosion, or the simultaneous explosion of many volcanoes
_or a cometary collision similar to that suggested by Urey as explanation" for the  origin of tektites.’
_In other words a global cataclysm is required to account for the ash.
>>>_However, if we look at the chemical composition of the ash (17) we find it shares similar chemical properties with granite (18).
_“Loess covers about 10% of the Earth’s land surface
_according to Michael Oard it is generally considered to be wind-blown (Aeolian)  silt.
_It is composed mostly of quartz grains, with minor portions of clay and sand often  mixed with the silt.
_Loess is commonly intermixed vertically with ‘paleosols’, which are supposedly  fossil soils that have been preserved in the geologic record or buried deeply  enough that it is no longer subject to soil forming processes.
_Scientists previously believed the silt particles in loess were derived from ice  abrasion, but they now believe that loess has both a glacial and non-glacial  origin.
_In central China it is up to 300m thick.
_Millions of woolly mammoths and other Ice Age animals are mostly entombed in loess  in non-glaciated areas of Siberia, Alaska and the Yukon Territory of Canada.
_Wind blown material is common within the Ice Age portion of the Greenland ice  cores.
_“Whether it be ‘volcanic ash’, deep sea ash or loess, all this material may be the  by-product of the electrical erosion that occurred during the mountain forming  period.
_material eroded in the early stages may have been deposited whilst marine  incursions were still ongoing
_this material would have been incorporated into marine strata and interpreted as  ‘volcanic’.
_During the latter stages when marine transgressions had subsided electrical dust  storms would have scattered the material globally- eventually to settle on the  ocean floor or entrap ‘Ice Age’ mammals.
_“Furthermore, marine sponge spicules have been identified in loess,
_we have already seen that the fossilised remains of sea creatures have been found  atop Mount Everest
_it is likely that the remains of sponges originated from the uplifted uppermost  sedimentary strata pulverised and scattered by an electrical discharge

_Louis Hissink hammerhead-geology-by-louis-hissink/
_Woolfe Creek Crater with its radioactive crater rim is an electrical discharge  producing radioactive elements in situ.

_Given the association of radioactive elements with granite
_and great masses of granite are found to have been emplaced among deformed and  metamorphosed sedimentary strata to form enormous granite bathyliths in the cores  of major mountain ranges
_Granite is never found outside mountain belts (Bucher, 1950, p. 37).”
_There's a link between electrical discharges and topographic uplift


Dendritic erosion at Mt. St. Helens Fig. 3


Wikipedia: Occurrence
Granitic rock is widely distributed throughout the continental crust. Much of it was intruded during the Precambrian age; it is the most abundant basement rock that underlies the relatively thin sedimentary veneer of the continents. Outcrops of granite tend to form tors and rounded massifs. Granites sometimes occur in circular depressions surrounded by a range of hills, formed by the metamorphic aureole or hornfels. Granite often occurs as relatively small, less than 100 km² stock masses (stocks) and in batholiths that are often associated with orogenic mountain ranges. Small dikes of granitic composition called aplites are often associated with the margins of granitic intrusions. In some locations, very coarse-grained pegmatite masses occur with granite.
Granite has a felsic composition and is more common in recent geologic time in contrast to Earth's ultramafic ancient igneous history. Felsic rocks are less dense than mafic and ultramafic rocks, and thus they tend to escape subduction, whereas basaltic or gabbroic rocks tend to sink into the mantle beneath the granitic rocks of the continental cratons. Therefore, granitic rocks form the basement of all land continents.

Loess is a sedimentary deposit composed largely of silt-size grains that are loosely cemented by calcium carbonate.

Distribution and composition of loess sediments in the Ili Basin, Central Asia
The bulk mineral components of the Ili loess are dominated by quartz and feldspar with minor amounts of calcite, chlorite, mica, dolomite and hornblende. More than 20 types of heavy minerals were observed with major components of amphibole, magnetite and epidote. The major elements of the Ili loess are characterized by high abundance of SiO2, Al2O3 and CaO and minor amounts of Fe2O3, MgO, Na2O and K2O.

WORZEL ASH,244845,245282

The "Worzel Ash" (Los Chocoyos Volcanic Ash)
Author: Xebec ()
Date: June 26, 2008 03:47AM
legionromanes wrote:

"The debris Venus allegedly deposited in Earth's atmosphere causing 40 years of darkness after the Exodus left no trace in the world's ice caps or ocean bottoms, [See "Ice Cores", Kronos X:1, 1984, 97-102, or Appendix D at end of [].] a test ignored by Rose [and an example of negative evidence with which Velikovskians do not have a good track record of dealing. N.B.: The "Worzel Ash" touted by Velikovsky and his epigoni is known to be volcanic (to the exclusion of any other source) from eruptions in Central America, limited in extent (i.e., not global), and far older than 3500 years; see "The Worzel Ash," Kronos X:1, 1984, 92-94 or section "The 'Worzel' Ash" in Mewhinney's "Minds in Ablation". (12-III-99) .]"

Note "Minds in Ablation Part Seven: Dust" is at: [ ]

The extent of the "Worzel Ash" of Worzel (1959) and as discussed by Ewing et al. (1959) and Anders and Limber (1959) is now known to have been vastly overestimated. Detailed research published by Bowels et al. (1973), Drexler et al. (1980), Ledbetter (1984, 1985), and Ledbetter and Sparks (1979), which included trace element analysis and dating by biostratigraphy, oxygen isotope stratigraphy, and radiometric methods not performed by Worzel (1959), show that what he mapped as the "Worzel Ash" actually consists of a number of different beds of volcanic ash that vary greatly in age. They found that the "Worzel Ash" was not a single global ash bed. From the trace and minor element analysis of 128 volcanic ash samples from 56 cores, Bowles et al. (1973) concluded that the unit, which Worzel (1959) mapped as the "Worzel Ash" consists of different ash beds of differing ages including three regionally widespread volcanic ash beds. Ledbetter and Sparks (1979) found what they called the "Worzel D ash" to be the distal counterpart of the rhyolitic Los Chocoyos ash-flow tuff of Guatemala and both were the result of a caldera ("supervolcano") eruption. Drexler et al. (1980) found that the "Worzel D" (Los Chocoyos) ash was created by a massive caldera eruption of the Atitlan caldera, which buried the much of the Guatemalan Highlands and Pacific coastal plain under a thick layer of ignimbrite and spread volcanic ash from Florida to Ecuador. Drexler et al. (1980) contains a map showing the distribution of the Los Chocoyos ("Worzel D" and Y8) ash bed. In this eruption, the Atitlan caldera erupted 270-280 cubic kilometers of volcanic material and created a huge volcanic caldera now filled by Lake Atitlan (Rose et al. 1987).

More coring and detailed geochemical analyses by Ledbetter (1985) of ash layers recovered from cores in the Gulf of Mexico and the Pacific Ocean adjacent to Central America defined 11 distinct ash beds within the sediments underlying the Gulf of Mexico and Pacific Ocean surrounding Central America. He was able to delineate the extent of each of the ash layers. The two most widespread ash layers, the Los Chocoyos ("Worzel D") ash bed was estimated to be 84,000 years old and the Worzel L ash bed was estimated to be 230,000 years old. Ledbetter (1984) noted that the Y8 ash bed in Gulf of Mexico is the same as the Los Chocoyos (Worzel D) ash bed.

The distributions of the Los Chocoyos (Worzel D) and other regionally extensive volcanic ash beds (tephras) are shown in figure 2 (page 6) of Machida (2002). In this figure, The Wozel D ash is ash deposit no. 26.


Anders, E., and N. Limber, 1959, Origin of the Worzel Deep-Sea Ash. Nature. vol. 184, pp. 44-45.

Bowels, F.A., R.N. Jack, and I.S.E. Carmichael, 1973, Investigation of Deep-Sea Volcanic Ash Layers from
Equatorial Pacific Cores. Geological Society of America Bulletin, vol. 84, no. 7, pp. 2371-2388
DOI: 10.1130/0016-7606(1973)84<2371:IODVAL>2.0.CO;2

Drexler, J.W., W.I. Rose, Jr., R.S.J. Sparks, and M.T. Ledbetter, 1980. The Los Chocoyos Ash, Guatemala: a major stratigraphic marker in middle America andin three ocean basins. Quaternary Research, vol. 13, pp. 327-345.

Ewing, M., B.C. Heezen and D,B. Ericson, 1959, Significance of the Worzel Deep Sea Ash. Proceedings of the National Academy of Sciences of the United States of America. vol. 45, No. 3, pp. 355-361.

Ledbetter, M.T., 1984. Late Pleistocene tephrochronology in the Gulf of Mexico region. In N. Healy-Williams, ed., pp. 119-148, Principles of Pleistocene Stratigraphy Applied to the Gulf of Mexico. IHRDC Press, Boston.

Ledbetter, M.T., 1985, Tephrochronology of marine tephra adjacent to Central America. Geological Society of America Bulletin. vol. 96, no. 1, pp. 77-82.
DOI: 10.1130/0016-7606(1985)96<77:TOMTAT>2.0.CO;2

Ledbetter, M.T., and R.S.J. Sparks, 1979, Duration of large-magnitude explosive eruptions deduced from graded bedding in deep-sea ash layers Geology. vol. 7, no. 5, pp. 240-244
DOI: 10.1130/0091-7613(1979)7<240:DOLEED>2.0.CO;2

Machida, H. 2002, Quaternary Volcanoes and Widespread Tephras of the World. Global Environmental Research. vol. 6, no. 2, pp. 3-17. [ ]

Rose, W.I., C.G. Newhall, T.J. Bornhorst, and S. Self, 1985, Quaternary silicic pyroclastic deposits of Atitlan Caldera, Guatemala. Journal of Volcanology and Geothermal Research. vol. 33, no. 1-3, pp. 57-80.

Worzel, J.L., 1959, Extensive deep sea sub-bottom reflections identified as white ash. National Academy of Sciences of the United States of America. vol. 45, no. 3, pp.349-355.

Los Chocoyos ash [ ]
Atitlan, Guatemala [ ]
Lake Atitlan [ ]
Lago de Atitlán [ ]
Essen in "Re: The Evidence of Mu" <[ ];
C. Leroy Ellenberger - []



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