Aug. 16, 2016

 

CREATION THE SACRED UNIVERSE – THE INCUBATION OF THE PHOENIX - CHAPTER  2

 

REC  #1    SOLTEC/HATONN

WEDNESDAY, OCTOBER 24, 1990   8:37 A.M.   YEAR 4 DAY 69

 

 

TODAY’S  WATCH

 

 

Hatonn present in service unto God and Man—within the Light of Truth.  So be it.  I ask, Dharma, that you avail yourself and ser­vice, briefly, to Comman­der Ceres An­thonious Soltec for, before we write this day, I must call urgent attention to you ones.  There has been a rather small earthquake within the past 12 hours in northern Califor­nia which bears great importance.  It is a sign to you ones who will “see” and “hear”.  The quake itself is not of great impor­tance; it is the fact that it is in the area of Lee Vin­ing (close to Yosemite) but that is not the point.  It epi­centers in the area where the radioactive “bulge” of molten matter made ra­dioactive by your Nevada testing is “coming to a head”.  This quake has two points of interest—it tells you where first the toxic ma­terial might sur­face and also relieves a bit of pres­sure from the “cone” itself.  I move to stand-by, thank you.

* * * * *

Soltec present to speak of general information regarding the type of quake just experienced in this most important area.  I am re­sponsible for the com­mand following most closely your earth changes in a “geophysical” attitude and, hope­fully, allow you ones to have knowledge regarding these changes and “possibilities” involved.  I can also tell you what to look for rela­tive to a given action as follow-on.  Please do not ask me to define ex­plicitly in “Earth-timeframe”.  We calcu­late possibilities and probabili­ties by “sequence of events”.  I shall also make it as simple for gen­eral understanding as I can find words to fit descriptions.

 

The relatively small quake in point was experienced in California to the coastal area near and around San Francisco as well as throughout portions of Nevada (most impor­tant indeed).  To allow under­standing to the “lay” public, I must first speak of vulcanism in general.  Therefore, I ask ones who know all this information to please be pa­tient, for we find that 99.9% of the hu­man masses do not have the fog­giest idea of that which we outlay unto you.

 

 

VULCANISM

 

 

The term “vulcanism” implies vol­canos—and they are, to be sure, a spectacular product of it.  But vul­canism involves much more than mere volcanos.  Any in­vasion of the earth’s crustal zone by magma from below is properly called vul­canism.  If the magma pushes its way far up into the crustal strata but does not reach the surface, it is termed intru­sive vulcanism, but if the magma flows out onto the surface via vol­canic or other vents, it is called ex­trusive vulcanism.  (These, of course, are Earth/English words and will need translation for other language groups.)

 

The question may well be asked, “Why does molten material from the earth’s interior force its way into and through the hard rock of the crust?”  This is one of the ques­tions that has vexed your geol­ogists for many years—not only, “Why does magma invade the crust?” but, “Where pre­cisely does the magma origi­nate?”  It is obvious to you “close” observers that release of pressure on the in­terior of the earth by deformation and fracturing of the crust triggers the out­ward movement of magma, but whether it originates initially at the earth’s core, the mantle, or even the crust itself is difficult for you to deter­mine for you have not enough knowledge or ability to research those pressures and temperatures to reach valid, prov­able conclu­sions.

 

It depends on the TYPE of volcanic activity.  Most volcanos tap only relatively shallow source re­gions; however, this does not ob­viate the deep-seated sources for certain types of volcanic activ­ity.

 

Nearly all major mountain masses are underlain by intrusive masses, and fre­quently there is some sort of extrusive vulcanism in evi­dence as well—simply through visual observa­tion.  Moun­tain-build­ing mecha­nisms such as folding and faulting cause vulcanism, but vulcanism, once set in motion, can be a po­tent mountain-building mechanism in its own right.  Massive intrusions may lift and warp the surface layers, and extrusive magma, finding it way to the sur­face through faults, can build huge piles of volcanic rock.  Also, intrusions may be exposed by the wearing away of the softer overly­ing strata by erosion, and the hard ig­neous mass will stand up as high­lands.  The Adirondacks and moun­tains of New England, for in­stance, are of this type.

 

Please understand that I am speaking of the United States in this instance for this is where the scribe can have association and this is where the subject in point has and is occurring.  The informa­tion is valid for all Earth locations geo­graphically.

 

Other examples are the smooth lava flows in Alaska’s Valley of the Ten Thousand Smokes which poured out of a volcanic vent just a few of your decades past and still have the appearance of motion as ob­served.  Today the area, Katmai National Monument, as you have named it, has only about 100 smokes active.  It is, however, an area only in the “sleeping”.

 

Another great example of a land­scape filled with volcanic plugs, the Kapsiki Mountains in Cameroon, is far different in visualiza­tion.  Where each great “protrusion (plug of rock lava) was once a live vol­cano, its vent filled with molten lava.  As the volcano ex­pired and eventually eroded away, only the so­lidified igneous rock, relatively harder and more resistant, has sur­vived for your modern-day viewing.

 

 

 

INTRUSIVE  VULCANISM

 

 

BATHOLITHS AND STOCKS:

 

The largest of the intrusive masses is the batholith, found to un­derlie every major mountain sys­tem and frequently exposed at the surface as the roots or cores of ancient moun­tains that have eroded away.  But the batholith is not merely the up­per margin of the monolithic Sima volcanics.  It is a lobe that has forced its way well beyond that into the sedimentary (or altered rock) lay­ers that form the continental epidermis, because of lessened pressure as a re­sult of diastrophism.  As for size, a stock is simply indica­tion of “size”.  There is not “reason” of two terms other than somebody felt it helpful to describe the “bulging” or “hat” under the sur­face as a batholith if over 40 miles in area and a stock if smaller.  Both will be found in the same “bulge”.

 

The batholith and stock are coarse-grained igneous or plutonic rock that has obviously cooled slowly deep underground.  At their point of contact with the stratum above is a metamorphosed aureole or baked zone where the combi­nation of heat, pressure, magmatic flu­ids and gases have commonly given rise to concentration of useful minerals.

For practical Earth purposes you may as well regard as essentially “bottomless” structures, and intru­sive rock has not been “seen” to ac­tually crystalize as extrusive lavas have.  You are, as usual, dealing again with con­jecture on your placement and it serves well enough in concept.

 

LACCOLITHS:

 

On a much smaller scale than the batholith are several other kinds of mag­matic intrusions.  One of these, the laccolith, has some of the char­acter of a small batholith or stock except that it is fed from below by a tube cutting across the overlying strata like the conduit of a volcano.  However, where the volcanic bore gets into the surface rocks, magma rising up the laccolith feed­pipe loses some of its impetus and spreads out between two flat-lying rock layers, eventually forming a lens-shaped mass that lifts and bows the surface into a dome and this is indeed most important to the sub­ject in point.

 

SILLS:

 

Similar to the laccolith but much more common is the sill.  In this case the in­vading magma spreads out as a flat sheet, often for many miles, but does not throw up the overlying layers.  Sills come to your attention when erosion ex­poses an edge as a sheer wall, often darker and harder than the surrounding rock.  The down-cutting Hud­son River, as example, has revealed a sill in the Palisades that is particu­larly striking because of the colum­nar jointing of the cool­ing magma.  Another major feature standing out in a moderately sub­dued landscape is the Great Whin sill of Northum­berland, England.  The black es­carpment describes a 100-mile cres­cent from the Pen­nines to the sea, and since its steep side faces north­ward, it was seized on by the Ro­mans as the foundation for Hadrian’s wall.  Again, within the U.S., you will have a good ex­ample in the Black Canyon of the Gunni­son.

 

DIKES:

If the invasion of the surface layers is in the form of a thin sheet cutting sharply across all hori­zontal strata but falling short of intersecting the surface, then you have a dike.  Vi­sualize a sill turned on edge, except in the case of a dike it draws magma from its entire lower edge rather than from a bore or conduit.  Dikes often occur in swarms, most frequently radiating from a vol­canic vent.  If the resulting igneous rock is harder than that which surrounds it, erosion may lay bare the solidi­fied magma in the volcano conduit as a neck or plug and the radiating dikes as long narrow ridges.  Ship Rock, New Mexico, is an outstand­ing exam­ple.  One can see the radi­ating dikes exposed at the sur­face and Ship Rock itself is a volcanic plug.

 

PEGMATITES:

 

Note that although the originally molten rocks involved in intru­sives are prop­erly classified as plutonics and should therefore display a coarse granularity, only the batholith or thick sill is highly typi­cal.  Generally, the smaller intru­sives isolate the mag­matic melt into such thin or lim­ited quantities that cool­ing is quite rapid and crystal formation is impaired.  However, it is pos­sible that a long intrusive fin­ger may keep its contact with the molten mass below and selected gases and fluids will find their way into this backwater (pegmatite).  Occasionally, crystals will grow to huge size under these unusual con­ditions.  In South Africa mica crys­tals have been en­countered mea­suring 10 to 15 feet in width.

 

 

EXTRUSIVE  VULCANISM

VOLCANOS:

 

Volcanos are, of course, of partic­ular interest not only because of their un­predictable explosive habits but because of their impres­sive structure.  They tend to follow fault lines, and thus the world’s great seismic zones.  Faulting, earth­quakes, and volcanos go together, and faulting is the basic cause for the other two.  The Pacific’s unsta­ble margin is often popularly re­ferred to as the “Pacific Ring of Fire” because of its extensive volcanic ac­tivity.  Everywhere, cones of all sizes, both active and dormant, are evi­dence of continuing vul­canism.

 

It is foolish indeed to ever refer to any volcano as “dead”.  Dor­mant is your word most suitable for use and should be used if there has been no eruptive activity in historical time.  Even historic time is not sufficient.  For instance in 79 A.D., your la­belled “Vesuvius”, was not even a very im­posing landform which was half hidden inside the broken rem­nant of the older Monte Somma and had never erupted in the mem­ory of human inhabitation.  There were not even any fanciful legends of vulcanism, so long ago had been its most recent activity.  Yet in that fateful year Pompeii was buried in a great blast of fiery ash and Hercu­laneum was overrun by re­peated flows of hot mud.  Then for sixteen centuries there were only ten addi­tional major eruptions.  But in 1631, after 130 years of quiescence, Vesuvius began its modern, more frequent eruptive cy­cle marked by increased lava flows that had been of little conse­quence earlier.  So today Vesuvius is by any measure­ment active, its person­ality changed considerably from its former self; and if Somma is any evidence, there have been many times in the distant past when Vesuvius and its precur­sors have surprised the sleepy folks along the Bay of Naples.

 

The United States’ own Cascade Mountains, pimpled with 600 miles of snow-capped cones, must be re­garded as merely dormant.  Lassen Peak, the least spectacular of the lot, was active in 1914-15, but there has been a tendency to think of the others as “scenery”.  All are very new, ge­ologically speaking, scarcely mutilated by erosion, and this, of course, is why they make such out­standing scenery.  But by the same token, dear friends, they are more likely to be alive than dead after such a short time span.  Evidences pointing to just such a likelihood are very modern cinder cones all around the base of Mt. Shasta, an­other in Crater Lake, recently dis­covered by your own geologists, hot spots high on the slope of Mt. Rainier and Mt. Baker, and Mt. Lassen it­self.

 

 

VARIATIONS  IN  ERUPTION

 

 

No two volcanos are alike in their eruptive habits and as you have seen from the Vesuvian ex­ample, an individual volcano is often capri­cious.  Some are spewers of ash, like Irazu in Costa Rica, which erupted continuously for al­most two years (1966-1968), sub­jecting the residents of the capital city, San Jose, to a seemingly endless rain of thick dust.  Others eject lava but with vari­ation: Vesuvius goes off violently with loud explosions and gushes of lava streaming down its flanks; Kilauea, the Hawaiian crater, quietly spills lava over its lip with a minimum of fireworks; Strombolian lava, cooling and crust­ing over lightly in the crater, traps gases beneath it, which ex­plode every half-hour throwing in­candescent clots high into the air.  Then there are the spas­modic erup­tors whose conduit becomes clogged with hardened igneous rock between eruptions.  With a cork in the bottle, so to speak, it is not un­common for the increasing pres­sures to blow out suddenly through a weak spot on the side of the mountain.  This is what happened to Mt. Pele on Martinique in 1902.  Internal pressure started the cork, pushing it out of the vent in the form of a high spire, but before it could wholly clear the passage the side blew out.  A dense cloud of in­tensely hot gases and self-exploding lava mist swept down the slope to the sea, com­pletely wiping out the town of St. Pierre in an instant.

 

 

CALDERAS

There is yet another kind of hap­pening that involves the reverse of eruption, that is, a sudden emptying of the magma chamber.  When this occurs, the en­tire top of the moun­tain, lacking support, col­lapses and is engulfed into itself.  The end re­sult is a huge crater-like pit called a caldera.  Crater Lake, Oregon, is one of these.  It is not a true crater because glacial evidences on the con­temporary slopes indicate that a peak of over 12,000 feet must have existed to sup­port full-blown glaciers.  This reconstructed vol­cano, dating back probably some 8000 years, has been named posthumously Mt. Mazama.  But volcanos can blow their tops—how do you know that it collapsed rather than blew up?  You can know be­cause the entire surrounding country­side would have to cov­ered with debris from the old peak and there simply is none.  So now you are faced with the question, what causes the abrupt evacuation of a magma chamber?  And you have no certain finite answer.

 

Of more recent origin than Crater Lake is the caldera of Krakatoa, an island just off western Java.  On August 27, 1883 there were four tremendous explo­sions, the last of which was heard 3000 miles away in Australia.  A towering dust cloud was thrown up, noticeable around the world for two years, and a great tidal wave drowned 36,000 people.  Subsequent investigation revealed that a deep pit had replaced two-thirds of the island but that despite the dust and ash ejected, the bulk of the island had collapsed and the sea had rushed into the resultant caldera.  The area is still indeed ac­tive.  A new volcanic is­land is building called by you, Anak Krako­toa (child of Krakatoa).  But even the original Krakatoa was merely a remnant of an earlier, much larger island.  Like Vesuvius, stand­ing in the breached caldera of Somma, generations of crustal ulcers appear on occasion to be healing but the infection distressingly reasserts it­self again and again when least ex­pected.

 

 

LOSS  OF  LIFE

 

 

On recounting the loss of human life from volcanic disaster through the cen­turies, one might be inclined to wonder why anyone would choose to live with volcanos as neighbors.  But if a given cone can be classified conveniently as “extinct, local residents come to love it, are inspired by its majesty, or even re­gard it as divine—that “the mountain” could be venomous and turn on its friends is unthinkable, until, of course, it does so.  Agricul­tural people are drawn to the fre­quently fertile lava soils, willing to take an un­known risk to derive a known livelihood.  And if the giant should cough up rejuvenating showers of ash periodically, so much the bet­ter.  Anyway, absolute security is not a guarantee of living any­where.  Why would anyone choose to live in earthquake country, tor­nado alley, or along hurricane coasts?  The law calls these “acts of God”, and God seems, in the short run, less lethal than midtown or freeway traffic, which threatens you all on a daily basis.

 

 

CLASSIFICATION  BY  CONE  SHAPE

 

 

The simplest classification of volcanos is on the basis of the shape of the cone.  Most of them fall generally into one of three types that are easily recogniz­able, and the cone shape also gives some indication of the type of ejecta and the eruptive habits of the volcano.

First, there is the cinder cone.  This is the product of a vio­lently explosive vol­cano where the lava has solidified in the vent, forming a plug.  The accumula­tion of steam and magmatic gases grad­ually develops sufficient pressure to blow the plug with such force as to shatter it into tiny frag­ments (called cinders and ash), and these are deposited in a symmetrical pile around the vent, the larger particles nearest the vent and the finer ones farther away.  The result­ing cinder cone is steep sided (around 37 degrees, the maximum angle of re­pose of unconsolidated material) and usually symmetrical (Mt. Asmara in Ethiopia).  Although evident in many parts of the world, the cinder cone sel­dom achieves any great size, as erosion rapidly

wears away what is essentially merely a pile of loose material.  The disappearing islands of the Pacific are of­ten mere cinder cones, where an eruption may throw up a pile of solid ejecta above the ocean level to be visible for a few days or months until wave action removes it.

 

The second type of volcanic cone is called a shield or dome.  Here a quiet flow of fairly fluid lava issues from the vent, forming a vast low-angle cone as it cools.  Mauna Loa-Mauna Kea whose 13,000-foot tips form the island of Hawaii is an excellent example of this type of cone, and if the low angle of the island’s slope is traced to the sea bottom some five miles deep, the true size of this twin cone becomes apparent.

 

As often as not, however, a volcano passes through several stages in its his­tory, alternating be­tween explosive eruptions and lava flows.  The resulting cone develops a combination of the low-angle shield and the high-angle cinder cone.  These are composite or strata cones and display concave slopes with a sharp peak.  Imagine first a cinder cone, but before it can erode away, it is overlain by lava flows.  Then built on top of this another cinder cone, fol­lowed again by lava.  The end product looks like Fujiyama, Shasta, Ranier, or Egmont, the world-famous volcanos that inspire poets and legends.  The most tell-tale concave slope development, however, is shown by Mt. Shishaldin in the Aleutians which is smoking and ac­tive today.  Its classic shape is totally un­scarred by any type of erosion as it continues to build.  Currently, Shishaldin towers well over 9000 feet above sea level and almost 40,000 feet above the ocean floor and growing.

 

The four formerly mentioned volcanos are considered dormant, but El Misti in Peru is equally as impressive and still active, as is Mayon in the Philippines.  Mayon, despite its generally low eleva­tion and lack of picturesque snowcap, is reputed to be the most perfectly shaped of the world’s composite volcanos.  I URGE YOU TO NOT BE FOOLISH IN YOUR ATTITUDE THAT THESE “DORMANT” GIANTS ARE CONTINUING IN DORMANCY.  THE ENTIRE OF THE CASCADE CHAIN IS AWAK­ENING.

 

Now, let us turn to a most important link-up with information re­garding the current quake in point:

 

 

FISSURE  FLOWS

 

 

Lava, in pouring out onto the earth’s surface, does not always is­sue from vol­canic vents; it may well out of faults or fissures many miles in length.  If the lava is highly liquid and the terrain fairly subdued, such fissure flows have been known to cover thou­sands of square miles and build up extensive plateaus as in eastern Washington, eastern Oregon, southern Idaho, and northern Califor­nia, U.S.A.  The bulk of peninsular India is also of this origin.  In Washington the Columbia River Gorge and the Grand Coulee reveal along their sides a banded layering of dif­fering colors and tex­tures, each of which represents a separate flow.  On occasion, the hot lava will be heavily charged with gases, and as the lava cools, the escaping gases leave holes in the rock, making it extremely porous.  Water will occasionally flow through the perme­able (scoriaceous) rock as though it were a pipe.  It is also possible that in a moderately viscous flow, with the surface cooling and congealing through con­tact with the atmosphere, the hot, still liq­uid lava underneath will run on and out leaving an igneous cave.

 

 

SO  WHAT,  SOLTEC?

 

If you reason carefully regarding the quake in point, you can de­termine the situation and watch for further example or increased activity—in any and all directions.  This can allow you to begin to determine likelihood of damage and extent of passage of radioac­tive material from the Nevada testing site.  Be­cause of underlying strata, the flow will be toward the Pacific Sea and will, obvi­ously, affect the immediate areas around the site of the “caldera” con­tainer and the di­rect fissure network radiating to the sea.

 

It would be expected then, that material flowing from the nuclear testing cen­ter in Yucca Flats outside of and north of Las Vegas would flow along fissure lines into Death Valley and thus and so, however, this is a false premise.  A brief and general outlay of descriptive flow from Yucca Flats test grounds would be between the Spring Mountains to the west and the Spotted Range and Sheep Range to the east, moving through and into “Devil’s Hole” which I believe is one of your National Monuments north of the town of Pahrump, Nevada, on the south edge of the Amargosa Desert east of the Amar­gosa Mountain Range and scattering in all directions.  The most open and active fissure, however, runs on through (under) Sarcoba­tus Flat, between the Inyo and Toyabe National Forests and pools in the major underground-to-surface cauldrons be­neath Mono Lake.  Mono Lake is not formed for no reason, dear friends, and it is quite a toxic lake in its already pristine state.  Lee Vining is at Mono Lake!

 

Does this mean the only danger from radioactive material problems would be along that route, then scattering out from the Mono Lake Bulge (which by the way, is under water for the most part)?  No, it means that it is where the weakest surface portion of the landscape lies.  The fis­sures running into southern California are much more extensive but are deeper and less likely to show surface bulging.  The flow, however, is much easier with much less inter­ference from strata mass.  THE MAJOR FISSURES ALL END UP AT THE SAN ANDREAS FAULT!

 

When you hear of the prophecies expecting death from open fissures exuding death-causing va­pors—it will be from toxic substances, yes, but deadly because of radiation from foolish man-made experi­ments of nuclear materials.

 

How much will surface, if it surfaces?  I cannot answer for it de­pends upon pressure buildup, pressure slippage vs. man-caused slip­page and extent of flow.  You can expect deadly gasses to spring from what you call Lake Elsi­nore and on down to the Salton Sea.  These gasses may or not be, radioactive.  Watch the type of tremors for you can know if a quake is felt over a large area, it is a bit deeper than a little surface jolt.  It means a lot of deep churning and activity in radiating fissures.

 

Since you do not yet show surface fissures to any great extent and very little surfacing material at this point, you can surmise it is still in the “intrusive” stage and moved into the “sill” stage from and forming additional “laccoliths”.  The area at Mono Lake repre­sents a batholithic/stock in a loca­tion not noticed easily through visualization.  The lake is not “just getting lower from depletion of wa­ter” but is also more shallow from the “rising” of the lake floor.

 

I am not here, Dharma, to argue points of physical geology or geog­raphy.  We have great diffi­culty with your new names for every­thing—the entire area de­scribed was once at the bottom of the sea and my vision and instrumentations recognize no difference except for isolating the iden­tification of markers for you ones.

 

The quake in point is of little notice except for the massive in­formation it should be telling you.  More important substance is coming forth along the New Madrid fault but the toxic quality of the California tremor bears more destructive potential from that aspect.

 

The widespread activity is indeed important but I have not the fa­cility nor you the understand­ing, to outlay it all.  I just ask that you be at alert.  If you can understand the functioning of your “Mother’s” circulatory system, you can bet­ter know where safety can be found in order to con­tinue service in this time of transition and upheaval.  You in contact and counsel with the higher energies will be given to know if you but listen—you who just desire to save your assets (of all types) will likely not hear and discount much of this information—so be it for it is most cer­tainly up to your own acceptance.

 

Thank you, Dharma, for scribing this information.  I realize you have neither the time nor the interest in these matters but your service is greatly appreci­ated for I have no receiver regarding these matters in this location.  Much, much focus is given to this area geographically, and I am greatly appreciative of your willing­ness to entertain my input.  I ask the blessings of under­standing in behalf of you ones awakening from the confusion of the sleep and I am most grateful to be of whatever service I might project.

 

I take leave in salute unto you of our “land-locked” fellow-man.  Saalome’ and Salu!

 

Soltec to clear.

 

Hatonn returned to sign-off for this session as it has grown quite lengthy being that Soltec has not been subjected to having to re­duce a chapter to a page nor a page to a paragraph as has been jested upon Hatonn.  When we come back I will continue with items of “TODAY’S WATCH” and shake you up a bit with Quantum Cosmic Code.  I shall at first reduce the para­graph to a sen­tence but as you might guess the subject is technical indeed and may require a bit more in-depth projection of wordiness as we move into the subject of ge­netic doubles abounding upon your place these days of politi­cal and technical chaos.  So be it.  Let us close this segment and take rest.  Salu.

 

http://fourwinds10.com/journals/pdf/J021.pdf