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===Mysterious Cosmic Energy of Mount Kailash spinning the Core of the Earth === In the inner earth, the traveler will see a glowing ball of light called the central sun, located at the earth’s geometric center. It consists of a high concentration of soft electrons. The reader no doubt wonders why it is there. A high gravity exists at the surface of the inner shell, because the counter gravity effects from the upper half of the shell are screened out by the high concentration of soft particles in the space between. Negative charges tend to be repelled by a gravitational field, in direct contradiction to concepts of academic science. Positive charges are attracted by it. It will also be shown that ordinary, supposedly uncharged, matter behaves like a positive charge. In view of this, the reason for the concentration of soft electrons at the center forming this glowing ball becomes apparent. The particles have their greatest concentration at the center because they are repelled by the gravitational field on all sides. The light is produced by the continuous disintegration of particles, due to their interactions. They represent the excess of negative charges from the sun reaching the inner shell of the earth.

As for the speed of light, it is just that. Gravity must propagate faster than the speed of light or else orbits of planets would not be possible. Consequently electro gravitational propulsion allows for movement of a device (spacecraft) at transluminal speeds (greater than the speed of light).

The Earth is a giant nuclear fission reactor floating in space. Planet Earth is like a living nuclear powered spaceship with its own magnetic force-field and gravity generator. There could be tunnel systems thru the continental and oceanic plates.

The Mount Kailash resembles the Linga Trikona with Masculine Energy and Bindu Trikona with Feminine Energy known as Trika, the three folds energies of Water, Fire and Air elements in the Sky and on the Earth. The pyramid-like mount Kailash is situated in one of the most difficult for access mount districts of Tibet. There have been studied main valleys and rock formations around Kailash, many of which having regular geometrical forms. There have been determined the exact geographical coordinates of all edges and the top of Kailash, edge bases orientation for the parts of the world, as well as described the structure and construction of Kailash. As a result of the satellite images analyses a lens-like vertical formation has been detected on the top of Kailash. There have been examined the rock samples taken from the base of Kailash and water samples of brooks, beginning from the glaciers of this mount. The division boundary between the lower stratified structure is having the signs of destruction, and the upper one - monolithic and concrete-like. Geomorphic expression of glacial erosion around Kailash region is manifested by the pyramidal shape Mount Kailash. Such morphology develops in areas where headward erosion of a ring of cirque glaciers around a single high mountain deepens the valley from more than three sides. The existence of extensive glaciers around Mount Kailash and in the southern part of Mount Kailash is the moving ice on the rocky substratum . Kailash range dominated by conglomerate (Molasses) deposited over the Kailash Granite. Granite is an igneous rock and classified on the basis of texture and composition. The formation of ice within mountain rock slopes is due to collection of broken rock fragments at the base of crags, mountain cliffs.

<p class="MsoNormal" style="margin-bottom:0in;margin-bottom:.0001pt;text-align: justify;text-indent:.5in;line-height:normal"><span style="font-size:12.0pt;font-family:"TimesNewRoman";mso-ascii-font-family: "TimesNewRoman";mso-fareast-font-family:+mj-ea;mso-bidi-font-family:"TimesNewRoman"; color:black;mso-color-index:1;mso-font-kerning:12.0pt;language:en-US">As <span style="font-size:12.0pt;font-family:"TimesNewRoman";mso-ascii-font-family: "TimesNewRoman";mso-fareast-font-family:+mj-ea;mso-bidi-font-family:"TimesNewRoman"; color:black;mso-color-index:1;mso-font-kerning:12.0pt;language:en-US">per Glaciology, a Glacier is huge mass of ice, formed on land by the compaction and recrystallization of snow, which moves very slowly down slope or outward due to its own weight. When the glaciers are broken into zones based on surface snowpack and melt conditions. Glaciers move, or flow, downhill due to gravity and the internal deformation of ice. The ice of a polar glacier is always below freezing point from the surface to its base, although the surface snowpack may experience seasonal melting. The speed of glacial displacement is partly determined by friction. Friction makes the ice at the bottom of the glacier move more slowly than ice at the top. If the temperature drops sufficiently the water freezes. Typically, the melting is caused by one or more of three processes: an increase in temperature, a decrease in pressure, or a change in composition. When the cirque glaciers finally disappear, they leave a steep, pyramidal mountain outlined by headwalls of the cirques. The volume of water released to cover 1 acre of land (43,560 square feet) to a depth of 1 foot and is Equal to 325,851 gallons or 1,233 cubic <span style="font-size:12.0pt;font-family:"TimesNewRoman";mso-ascii-font-family: "TimesNewRoman";mso-fareast-font-family:+mj-ea;mso-bidi-font-family:"TimesNewRoman"; color:black;mso-color-index:1;mso-font-kerning:12.0pt;language:en-US">meters. For <span style="font-size:12.0pt;font-family:"TimesNewRoman"; mso-ascii-font-family:"TimesNewRoman";mso-fareast-font-family:+mj-ea; mso-bidi-font-family:"TimesNewRoman";color:black;mso-color-index:1; mso-font-kerning:12.0pt;language:en-US">a rock, water behaves as its salt. Add water into a mantle peridotite and it will melt at a lower temperature because the bonds in the minerals that make up the rock will be disrupted by the water molecule. Melting of rocks occur about 400 miles deep in the Earth. This is remarkable because most melting in the mantle occurs much shallower, in the upper 50 miles. 1% of the weight of mantle rock located in the transition zone would be equivalent to nearly three times the amount of water in oceans. This water is not in a form familiar to us -- it is not liquid, ice or vapor. This fourth form is water trapped inside the molecular structure of the minerals in the mantle rock. The weight of 250 miles of solid rock creates such high pressure, along with temperatures above 2,000 degrees Fahrenheit, that a water molecule splits to form a hydroxyl radical (OH), which can be bound into a mineral’s crystal <span style="font-size:12.0pt;font-family:"TimesNewRoman";mso-ascii-font-family: "TimesNewRoman";mso-fareast-font-family:+mj-ea;mso-bidi-font-family:"TimesNewRoman"; color:black;mso-color-index:1;mso-font-kerning:12.0pt;language:en-US">structure. Once <span style="font-size:12.0pt;font-family:"TimesNewRoman"; mso-ascii-font-family:"TimesNewRoman";mso-fareast-font-family:+mj-ea; mso-bidi-font-family:"TimesNewRoman";color:black;mso-color-index:1; mso-font-kerning:12.0pt;language:en-US">the water is released, much of it may become trapped there in the transition zone.

<p class="MsoNormal" style="margin-bottom:0in;margin-bottom:.0001pt;text-align: justify;text-indent:.5in;line-height:normal"><span style="font-size: 12.0pt;font-family:"TimesNewRoman";mso-ascii-font-family:"TimesNewRoman"; mso-fareast-font-family:+mj-ea;mso-bidi-font-family:"TimesNewRoman"; color:black;mso-color-index:1;mso-font-kerning:12.0pt;language:en-US">Kailash <span style="font-size:12.0pt;font-family:"TimesNewRoman";mso-ascii-font-family: "TimesNewRoman";mso-fareast-font-family:+mj-ea;mso-bidi-font-family:"TimesNewRoman"; color:black;mso-color-index:1;mso-font-kerning:12.0pt;language:en-US">rock formation is capable of holding and transmitting water through its inter-connected pore spaces and constantly released into Manasarovar Lake. The precipitation of these rocks as rain, snow, sleet, or hail that falls to or condenses on the ground becomes an integral part of the hydrological cycle, is the source of all fresh water. Further, Glacial ice is the largest reservoir of freshwater. Just 20 kilometers away from Mount Kailash, the sacred blue and emerald green Manasarovar Lake. This lies at an altitude of 4727 m. (15,510 ft.) is the highest freshwater lake in the world. It is relatively round in shape with the circumference of 88 kilometers (55 mi). Its depth reaches a maximum depth of 90 m (300 ft) and its surface area is 320 square kilometers (120 sq mi). It is fed by glaciers on the Himalayan peak Gurla Mandhata and in the Kailash Range. It is connected to nearby Lake Rakshastal by the natural Ganga Chhu channel.

<p class="MsoNormal" style="margin-bottom:0in;margin-bottom:.0001pt;text-align: justify;text-indent:.5in;line-height:normal"> Lake Manasarovar is near the source of the Sutlej River which is the easternmost large tributary of the Indus. Nearby are the sources of the Brahmaputra River, the Indus River, and the Karnali River (Ghaghara), an important tributary of the Ganges River. Part of the water flow in these river basins depends on snow and glacial melt to these perennial rivers. In turn, the amount of snow- and ice melt influences runoff into lowland rivers and the amounts of water recharging river-fed aquifers....

<p class="MsoNormal" style="margin-bottom:0in;margin-bottom:.0001pt;text-align: justify;text-indent:.5in;line-height:normal"> There is so much to learn from the Kingdom of Shiva..Read and sharpen your wisdom... <span style="font-family:'TimesNewRoman',serif;font-size:12pt;text-indent:0.5in;">Abhinava Vyasa, Rishi Sivkishen, Author

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