D74 Who we are - Where we come from

WHO ARE WE: WHERE DO WE COME FROM?

 

At 4 hours 17 minutes 3 seconds GMT on the earth day of 28 March 1950, an OAWOLEA UEWA OEM (lenticular spacecraft) made contact with the lithosphere of EARTH for the first time in History.

 

The landing took place in a defined area of the department of “Basses Alpes”, some 8,000 metres from the village of La Javie (France).

 

Six of my brothers, under the direction of OEOE 95, son of OEOE 91, among whom were two YIEE (women), remained on this “OYAA” (planet) as the first expeditionary “INAYUYISAA” from UMMO.

 

The process of adaptation, which included assimilating the language, gathering information on customs, social and working behaviour, culture..., is very difficult to summarize in a few paragraphs.

 

We come from a solidified star whose external geological characteristics differ somewhat from those of EARTH. The typical phoneme with which we designate our “OYAA” can be transcribed in Spanish spelling as: UMMO (U: closed).

 

Its shape can be likened to an ellipsoid of revolution whose radii are:

 

Maximum, R = 7251,608 · 10³ m

 

Minimum, r = 7016,091 · 10³ m

 

The total mass is: m = 9,36 · 10²⁴ Kg. mass

 

Inclination with respect to the normal to the plane of the ecliptic: 18º 39’ 56.13” (it undergoes a periodic variation of 19.8 sexagesimal seconds of arc). (We use units familiar to EARTH technicians).

 

Acceleration of gravity (measured at AINNAOXOO): g = 11.9 metres / sec².

 

Rotation on its axis: 30.92 hours (we measure in UIW. 30.92 h = 600 UIW) (equivalent to 1 XII) (See Note 3)

 

NOTE 3. -

The rotation of UMMO has been slowed by the tides at a more marked rate than that of EARTH, but it reached higher angular velocities than those recorded in the history of its OYAA.

 

(The phoneme XII is a homophone that expresses both the duration of the “day of UMMO” and “cycle”, “revolution”, “unit rotation”, etc.)

 

The geological structure of UMMO shows very marked distinguishing characteristics with respect to EARTH.

 

Nine XOODIUMMOO DUU OII (which may be translated as “connected strata”) can be distinguished, showing very well-defined geophysical features. The discontinuity between these strata is not abrupt; there are transition layers of variable thickness.

 

 

Image 1 shows a section of our OYAA (planet) reflecting the thicknesses of the various XOODIUMMO. The chemical composition of these strata is very varied. Thus XOODIUMMO UO, with a mean density of 16.22 grams/ cm² (EARTH unit), contains the following elements familiar to you:

 

Cobalt 88,3%

Nickel 6,8 %

Iron 2,6%

Vanadium 1,2%

Manganese 0,7%

 

An upper envelope, the XOODIUMMO IAAS, has on the other hand a notably different composition:

 

Iron 52%

Cobalt 33,5%

Nickel 12%

Manganese 2,1%

Metallic

silicates 0,3%

 

The preceding solid layers, subjected to great pressure, are surrounded by XOODIUMMO IEN and XOODI UMMO IEBOO in a semi-fluid phase with a great abundance of titanium oxides, iron silicates and various compounds of aluminium and magnesium.

 

One of the most important spheroidal phases is the 6th (UMMO layer no. 5); it has an approximate thickness of 28.8 KOAE (251 Km.). With large diamond-bearing beds, it has an alveolar structure in which enormous IOIXOINOIYAA (geological cavities) still remain, in which, preserved from the high pressures suffered by adjacent zones, there are enormous quantities of solid, liquid and gaseous organic substances, especially methane, propane and oxygen. The main activity that you would call volcanological shows itself in the OAKEDEEI, which hurl great igneous columns of these gases towards the atmospheric layers.

 

The outermost envelopes, XOODIUMMO OANA OANMAA, underwent in remote times very intense orogenic processes of a metamorphic nature. Erosion, however, has modified the structure of the most pronounced folds and faults, so that the continental relief is not very rugged.

 

A single “continent” and the scant island surface occupy only 38% of the total area of UMMO.

 

The atmospheric composition at the levels of XOODIUMMO OANMAA is similar to that of EARTH.

 

UMMO moves in an elliptical (almost circular) trajectory with an eccentricity of 0.0078 around an OOYIA (star of small mass) which we call IUMMA (our “sun”). The mean distance UMMO-IUMMA is 9,96 . 10¹² centimetres.

 

Our way of reckoning long periods is singular compared with yours and has been preserved throughout our history, despite originating in a very ancient astronomical error.

 

We define the XEE (UMMO “year”) as the fraction 1/18 of the orbit of our OYAA around IUMMA. (Nowadays the phoneme XEE is also synonymous with “cyclical trajectory”).

 

Our ancient “cosmologists”, unaware that the plane of the ecliptic of UMMO has a different orientation from that of the 2nd OYAA revolving around IUMMA, which they took as a reference, interpreted the trajectory of UMMO as double-helical (images 2 and 3) on the surface of an imaginary cylinder.

 

                                                                     

                       

IMAGES 2 and 3 - FALSE CONCEPTION

 

They thus believed that our OYAA described three descending revolutions (2) and another three ascending ones (3) until completing the cycle. One XEE (UMMO year) is equivalent to 0.212 EARTH years.

 

In reality we can today define the XEE as 1/3 of the true orbital period. Six periods are therefore equivalent to the ancestral XEE-UMMO = 18 XEE.

 

IUMMA is a star with a mass of 1,48 . 10³³ earth grams. Its distance from the SUN on 8 July 1967 was 14.421 light-years.

 

It is not at all simple to identify our OOYIAA in terrestrial astronomical tables. This is because our specialists have conventionally established a galactic reference system of a different nature from yours (See Note 1). The change of reference axes would not, however, be difficult if you did not make errors. Nevertheless, we have found significant discrepancies in data on mass, magnitude, position and distance of stars mutually identified by you and by us.

 

NOTE 1. -

We use a reference frame with polar coordinates based on our own Galaxy. As coordination centres we use four radio sources located at 12382, 1900264, 899, 07 and 31, 44 terrestrial parsec units, whose stability with respect to the galactic centre is very high.

 

We cannot yet, therefore, tell you with a high degree of certainty which star recorded by you may be our IUMMA.

 

We calculate that the coordinates familiar to you that may fix the position of IUMMA would be:

 

Solid angle defined by:

 

Right ascension 12 hours, 31 minutes, 14 seconds +/- 2 minutes 11 seconds.

 

Declination 9º 18’ 7” +/- 14’ 2”

 

Precisely very close to the centre of that probable solid angle (12 h 31 m; 9º 18´ ) some tables prepared by you show a star which you call WOLF 424.

 

This may probably be IUMMA. Its characteristics are d = 14.6 light-years. Absolute visual magnitude 14.3. Apparent magnitude 12.5. Spectrum corresponding to class M.

 

However, these characteristics differ somewhat from the real ones. The marked error in the evaluation of the magnitude could be explained by the existence of a very dense cloud of cosmic dust (complex gravimetric spectrum with ionized metallic solid particles smaller than 0.6 mm.). The brightness recorded by you must necessarily be much more attenuated. The very low value indicated (magnitude recorded at 10 parsecs = 14.3) corroborates our suspicion.

 

An observer located at 10 parsecs and without obscuration by cosmic dust would record, on your conventional scale, a magnitude of 7.4.

 

On the other hand, the mean surface temperature of IUMMA is 4580.3 degrees Kelvin, somewhat higher than your estimate. This error is less explicable to us, since the spectrum you may have studied is not yet modified by the occlusion of dust clouds.

 

All these difficulties are hard to overcome. Having made our calculations of the attenuation the luminosity may undergo owing to the high density of the nebula of dust and gas, the results do little to clarify the problem, for if the line of sight passes through the zones with a high percentage of particles, the apparent magnitude for you would be of the order of 26, hardly attainable with your present optical instruments.

 

On the other hand, the less dense zones would allow observations of the order of magnitude 12 to 13 (conventional terrestrial scale), a range that corresponds precisely to that tabulated by you for WOLF 424.

 

Nor can it be ruled out that WOLF 424 is one of the two OOYIA (small stars) coded by us as

 

       Located 2.07 light-years from IUMMA.

Surface temperature 3210º Kelvin.

 

     Located 0.62 light-years from IUMMA.

Surface temperature 2575º Kelvin.

 

IUMMA causes disturbances of its magnetic field that are very difficult to predict in the long term. The detectable intensity of this field on our UMMO reaches values that would seem astonishing to you. The extreme levels range between 3.8 gauss and 216 gauss.

 

If you consider that UMMO's own field is weaker than that of EARTH, with maxima of 0.23 and minima of 0.07 gauss, it is probable that you may even, on observing the spectrum of our IUMMA, notice the splitting of some lines due to the polarization caused by these disturbances.

 

Such strong disturbances have influenced our OYAA very appreciably. For example, the structuring of our atmosphere with strongly ionized layers has preserved the ecological environment from strong levels of radiation. Mutations have been less frequent in organisms, and therefore the variety of fauna and flora is less rich than that of EARTH.

 

The appearance of our night sky, on the other hand, is much more fantastic, thanks to meteors that would remind you of the aurora borealis.

 

Technology has had to take paths different from those of Earth. Communications using electromagnetic frequencies are only possible in specific cases, and the great variety of equipment involving magnetic potential gradient functions must be compensated to avoid the strong disturbances from outside.

 

Our protohistory of technology records the use, by our ancestral brothers, of great metal toroids laid out over the fields (remains of cables buried in those times are still found), in which intense aperiodic electric currents were induced, whose energy was stored (in a manner similar to that used by you in your batteries) for later use. (Note 2).

 

NOTE 2. -

Our ancestors made enormous efforts and built grandiose works that altered the geography of our continents in order to obtain and store energy. Four were the important sources exploited. Thermal energy from the zones with a high density of OAK EOEEI (a kind of volcano).

 

The extraction of natural gas (rich in propane and other hydrocarbons).

 

The use of the radiant energy of IUMMA, for which thousands of channels fitted with reflecting mirrors were built, covering large areas; and finally, the harnessing of the magnetic field strength of IUMMA combined with the rotation of UMMO, obtained by means of long conductors (an alloy of silver and copper) buried at shallow depth, forming coils of enormous diameter or networks of toroids (toroidal coils) distributed over the surface of desert areas.

 

The gentle relief, and therefore the poor flow of the rivers, never encouraged the use of hydraulic energy, and liquid hydrocarbons lay at such enormous depths that our brothers of those ages were never able to bring them to the surface (and when technology made it possible, their exploitation was no longer practical).